PB86-173598
THE LUBBOCK LAND TREATMENT SYSTEM RESEARCH AND
DEMONSTRATION JROJECT:  VOLUME I.  DEMONSTRATION/
HYDROGEOLOGIC STUDY
Lubbock Christian College
Lubbock, TX
Feb 86
                  U.S. DEPARTMENT OF COMMERCE
               National Technical Information Service

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c/EPA
           United States
           Environmental Protection
           Agency
           Robert S. Kerr Environmental
           Research Laboratory
           Ada OK 74820
EPA/600/2-86/027a
February 1986
           Research and Development
The Lubbock Land
Treatment System
Research and
Demonstration
Project:
           Volume
           Demonstration/
           Hydrogeologic Study

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                                   TECHNICAL REPORT DATA
                            (Please read Instructions on the reverse before completing}
1. REPORT NO.
  EPA/600/2-86/027a
                             2.
                                                           3. RECIPIENT'S ACCESSION-NO.
                                                1 7
4. TITLE AND SUBTITLE
  THE LUBBOCK LAND TREATMENT SYSTEM RESEARCH AND
  DEMONSTRATION PROJECT:  Volume I. Demonstration/
  Hydrogeologic Study
                                                           5. REPORT DATE
                                       February 1986
                                     6. PERFORMING ORGANIZATION CODE
7. AUTHOR(S)
  D.B. George, D.B.  Leftwich, N.A. Klein
                                                           8. PERFORMING ORGANIZATION REPORT NO.
9. PERFORMING ORGANIZATION NAME AND ADDRESS
  Lubbock Christian  College
  Institute of Water Research
  Lubbock TX  79409
                                     10. PROGRAM ELEMENT NO.
                                        CAZB1B
                                     11. CONTRACT/GRANT NO.

                                        CS-806204
12. SPONSORING AGENCY NAME AND ADDRESS
  U.S. Environmental  Protection Agency
  Robert S. Kerr  Environmental Research Laboratory
  P.O. Box 1198
  Ada, OK  74820
                                     13. TYPE OF REPORT AND PERIOD COVERED
                                        Final  (11/27/78  -  12/31/85)
                                     14. SPONSORING AGENCY CODE
                                        EPA-600/15
15. SUPPLEMENTARY NOTES
  Project Officers:
  Curtis C. Harlin
Lowell E. Leach, Jack  Witherow,  H. George Keeler, and
16. ABSTRACT
       The Lubbock  Land Treatment System Research  and  Demonstration Project, funded  by
  Congress in  1978  (H.R.  9375)., was designed to  address  the various issues concerning
  the use of slow rate land application of municipal wastewater.  The project  involved
  the 1) physical expansion of an overloaded 40-year old Lubbock slow rate land  treat-
  ment system;  2) characterization of the chemical, biological  and physical conditions
  of the ground water, soils and crops prior to  and during irrigation with secondary
  treated municipal  wastewater; 3) evaluation of the health effects associated with
  the slow rate land application of secondary effluent and 4) assessment of the
  effects of hydraulic, nutrient and salt mass loadings  on crops, soil and percolate.
  Information  provided in this volume details the  system operations, ground water
  effects of reduced hydraulic loading on the Gray farm  and ground water hydraulic
  and quality  changes at  the Hancock farm resulting from wastewater irrigation
  practices.
17.
                                KEY WORDS AND DOCUMENT ANALYSIS
                  DESCRIPTORS
                                              b.IDENTIFIERS/OPEN ENDED TERMS
                                                     COSATI Field/Group
13. DISTRIBUTION STATEMENT

  RELEASE TO PUBLIC
                        19. SECURITY CLASS (This Report)
                          UNCLASSIFIED
21. NO. OF PAGES
    640
                                              20. SECURITY CLASS (Tills page)
                                                UNCLASSIFIED
                                                                         22. PRICE
EPA Form 2220-1 (9-73)


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                                           EPA/600/2-86/027a
                                           February  1986
          THE LUBBOCK LAND TREATMENT SYSTEM
         RESEARCH AND DEMONSTRATION PROJECT
                      VOLUME I
          Demonstration/Hydrogeologic Study
                         by
      D. B. George, D. B. Leftwich, N. A. Klein
Lubbock Christian College Institute of Water Research
                Lubbock, Texas 79407

             B. J. Claborn, R. M. Sweazy
                Texas Tech University
                Lubbock, Texas 79409
        EPA COOPERATIVE AGREEMENT CS806204
                  Project Officers

                   Lowell E. Leach
                  Jack L. Witherow
                  H. George Keeler
                  Curtis C. Harlin
            Wastewater Management Branch
    R. S. Kerr Environmental Research Laboratory
                 Ada, Oklahoma 74820
  ROBERT S. KERR ENVIRONMENTAL'RESEARCH LABORATORY
         OFFICE OF RESEARCH AND DEVELOPMENT
        U. S. ENVIRONMENTAL PROTECTION AGENCY
                 ADA, OKLAHOMA 74820
                           •JO

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                          DISCLAIMER
     The information in this  document has  been funded in part
by the  United  States  Environmental  Protection Agency  under
assistance agreement No.  CS806204 to  the Lubbock  Christian
College Institute of Water Research.   It  has  been  subjected
to the Agency's peer and  administrative  review and  has  been
approved for publication  as   an  EPA document.   Mention  of
trade names  or  commercial products  does  not  constitute  en-
dorsement or recommendation for  use.

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                                FOREWORD
     The U.S.  Environmental  Protection Agency was established  to  coordinate
the administration  of major Federal programs designed to  protect  the. qual-
ity of our environment.

     An important part of  the  Agency's  effort involves  the searc-h  for
information about  environmental  problems, management techniques, and new
technologies  through  which optimum  use  of the Nation's land  and water
resources can  be assured and the threat pollution poses to  the welfare of
the American people  can be minimized.

     The  U.S.  Environmental  Protection  Agency's Office  of Research  and
Development conducts this search through a nationwide network of research
facilities.  As  one of these facilities,  the Robert S.  Kerr  Environmental
Research Laboratory  is  responsible  for the management of programs  including
the development and  demonstration of soil and other  natural  systems  for  the
treatment and  management of  municipal wastewaters.

     The slow rate land treatment process of municipal wastewaters uses  the
unsaturated soil profile and agricultural • crops  managed  as the  treatment
media.   The Lubbock Land Treatment System Research and  Demonstration Pro-
gram, funded by Congress in  1978 (H.R. 9375)  was designed  to address the
various issues limiting the use of slow rate land application of  municipal
wastewater.  The project involved expansion of the Lubbock  Land  Treatment
System  to 2,967 hectares; characterization of the chemical, biological  and
physical condition of the ground water, soils and crops prior  to  and during
irrigation with  secondary  treated municipal wastewater;  and  evaluation of
the U.S. Environmental  Protection Agency's design criteria for  slow rate
land  application.   Results demonstrate that, where such systems are cor-
rectly designed and  operated,  they can be cost effective  alternatives  for
municipal sewage treatment  at sites where conditions are  favorable  for  low
hydraulic loading combined with  cropping practices.

     This  report contributes to  the knowledge which is  essential  for  the
U.S. Environmental Protection  Agency to meet requirements of environmental
laws  and  enforce pollution control  standards which are reasonable, cost
effective and  provide adequate protection for the American public.
                                                Clinton W.  Hall,  Director
                                             Robert S. Kerr Environmental
                                             Research Laboratory
                                    111

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                                ABSTRACT

     The Lubbock Land  Treatment System consists of  two  privately  owned
farms.   The  Gray  farm comprises  1,489 ha  and  has been  reusing treated
wastewater  for  crop irrigation for  more  than  40 years.   In 1981  the  land
application system was enlarged to  include the  Hancock farm which had 1,153
ha under cultivation.  The primary  irrigation mode employed by both  farms
was spray  irrigation using  center  pivot irrigation machines.  The Demon-
stration/hydrogeologic Study which  was a portion of the Lubbock Land Treat-
ment System Research and Demonstration Project  involved the physical expan-
sion of the the Lubbock Land Treatment System and characterization of chem-
ical,  biological  and physical  conditions of  the ground water, soils, and
crops prior to  and during irrigation with'  secondary  treatment municipal
wastewater-  The study was designed  to determine the short term effects of
1) reducing the quantity  of wastewater  irrigation  at  the Gray  farm on
crops,  soils and ground water; arid 2) slow rate land application of secon-
dary effluent on crops, soils and ground water  at the Hancock farm.
     During the  period when a portion  of the  treated  wastewater  was
diverted to the Hancock farm, a decrease in the ground-water level beneath
the Gray farm  was measured.  In  conjunction with the  lowering of  the
ground-water  table, there was an increase in  water quality beneath most of
the farm (primarily the ground water  underlying the spray irrigated areas).
The cultivation of alfalfa in the spray  irrigated areas  was probably  the
primary factor  affecting the quantity and quality of percolate.
     Chemical and nutrient constituents  in the  treated wastewater applied
to the  Hancock farm were removed  by the soil-crop matrix.  An increase in
ground water beneath the Hancock farm resulted from deep percolation of
surface  runoff collected in moats surround  the reservoirs and excavations
constructed to  reduce flooding of crop land.  Deep percolation of surface
runoff  leached existing nitrate and salt deposits within the soil profile
to the ground water; thereby, causing increased ground-water nitrate  and
total  dissolved solids concentrations.
     The Demonstration/hydrogeologic Study was conducted by Lubbock Chris-
tian College  Institute of Water Research (LCCIWR) and Texas Tech University
                                IV

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 (TTU).  This report  was  submitted  in  fulfillment of CR80620401  by LCCIWR
under primary sponsorship of  the U.S.  Environmental Protection Agency.  This
report covers a summary of research  activities performed  from May  1,  1980
through December 31,  1983.  This work  was completed on June 30, 1985.

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                                 CONTENTS

Foreword	iii
Abstract	iv
Figures	-jx
Tables	x-jj-j
Acknowledgement  	 XVI
   1 .   Introduction	   1
   2.   Summary and Conclusions 	  4
          Summary	4
          Conclusions  	  6
             Land Application System Design and Effluent 	  6
                Hancock Farm	7
                Gray Farm	10
   3.   Recommendations	16
   4.   Lubbock Slow Rate Land Application System Description 	  18
          Facilities Description 	  18
          Facilities Completion	35
          System Evaluation	35
   5.   Monitoring Approach 	  56
          Hydrogeology 	  57
          Soils	84
          Crops	93
          Irrigation Records 	 100
          Economics	101
          Statistical Analysis 	 102
   6.   Results and Discussion	104
          Wastewater Effluent	104
          Farming Operations 	 119
          Hydrogeologic Investigation  	 128
          Soils	201
          Crops	250
          Economics	259
        Preceding page  blank
VI 1

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References	273
Appendicies
     A.  Sample Preservation and Analytical Methods  	  279
     B.  Hancock Farm Records Forms	292
     C.  Water Quality Data and Figures	299
     D.  Hydrologic Data and Figures	514
     E.  Soil Characterization Data and Figures	539
     F.  Crop Characterization Data and Figures	593
     G.  Land Application System Operation Data and System Expansion
         Cost Data	602
                                   vn

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                                  FIGURES

Number-	Name	Page

    1      Regional Setting for the Lubbock Land Treatment  Research
          and Demonstration Program  	   19
    2     Gray and Hancock Land Treatment Site Locations	22
    3     Southeast Water Reclamation Plant Flow Diagram   	   23
    4     Gray Farm Land Treatment Site	28
    5     Soil Types on the Gray Farm	29
    6     Location of New Pump Station to Existing Plant   	  .   30
    7     Hancock Farm Land Distribution System 	   32
    8     Soil Types on the Hancock  Farm	34
    9     Overview of Sand Trap and  Fittings  for End  Gun	39
   10     Breakdown of Booster Pump  and  End Gun Assembly,  as
          Originally Installed	40
   11     Modifications Made to Some Center Pivot Irrigation Machines   41
   12     Relation of Screen to Flow Meter as Designed  and Installed    43
   13     Position of Flow Meter to  Achieve Proper Operation   ....   44
   14     Concrete Pivot Pads	45
   15     Modifications Made to Stabilize Pads	47
   16     How Pad Could have been Poured to Avoid Stability Problem  .   48
   17     Nelson Spray Nozzles as They were Designed  to be Installed.   49
   18     Actual Inverted Installation	50
   19     Types of Splash-pans Available	51
   20     Improper Installation Diagram  from  "As-built  Drawings".  .  .   53
   21     Proper Installation of Flow Transmitter as  Described  in  the
          Manufacturer's Manual 	   55 '
   22     Gray Farm Ground Water Monitoring Locations 	   59
   23     Hancock Farm Ground Water  Monitoring Locations	60
   24     Hancock Farm Drinking Water Sampling Locations	61
   25     Two-Step Construction Sequence used for Multiple Depth Wells 64
   26     Typical Rotary Drilled Well used to Obtain  Water Levels  and
          Water Quality Samples	65
                                   IX

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27     Cemented Reservoir Monitoring Well .............   68
28     Sampling Grid for Reservoir #1 .............  .•  •   75
29     Location of Neutron Access Tubes, LCCIWR and TTU Research
       Areas, Hancock Site ....................   "'
30     Grid for Random Selection-of Soil and Crop Sampling Loca-
       tions, Gray Farm  .....................   86
31     Grid for Random Selection of Soil and Crop Sampling Loca-
       tions, Hancock Farm ....................   87
32     Soil Sample Locations, Hancock Farm ............   88
33     Soil Sample Locations, Gray Farm  .............   89
34     Crop Sample Locations, Hancock Farm ............   94
35     Crop Sample Locations, Gray Farm  .............   95
36     With These Categories Pulled Together, More of the Farming
       Operations can be Compared from Tenant to Tenant ......  103
37     Hydraulic Flow to Consumers in 1982 ............  105
38     Hydraulic Flow to Consurner-s in 1983 ............  106
39     Nitrogen Cycle in Waste Stabilization Ponds ........  113
40     Precipitation During Project Period ............  120
41     1983 Design Hydraulic Loading to Pivot #15 by Crop .....  125
42     Winter 1982 Crop and Grazing Areas at Gray Farm ......  126
43     Water Level Contours in Feet, December 1981, Gray Farm.  .  .  133
44     Water Level Contours, December 1981, Hancock Site ..... .136
45     Water Content (Percent by Volume) During Flooding Tests,
       August 1983, LCCIWR #4  ..................  139
46     Water Content as Indicated by Neutron Probe, LCCIWR #4   .  .  140
47     Variation of Average Water Content as Indicated by the
       Neutron Probe .......................  142
48-49  Lead Concentration in Well Water over Time, Hancock Farm.  .  157
50     Molybdenum Concentration in Well Water over Time, Hancock
       Farm  ...........................  159
51     Selenium Concentration in Well Water over Time, Hancock
             ...........................  160
52     Copper Concentration in Well Water over Time, Hancock Farm.  161
53     Cadmium Concentration in Well Water over Time, Hancock Farm  163
54     Atrazine Concentration in Well Water over Time, Hancock
       Farm  ...........................  164

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55     Propazine Concentration in Well Water over Time, Hancock
       Farm	166
56     Nitrate Concentration (mg/1) in Well Water under Gray Farm
       Baseline Period, 1981-1982  	 172
57     Average Nitrate Concentration (mg/1) in Well Water under
       Gray Farm, Past Baseline, 1983	174
58     Total Kjeldahl Nitrogen Concentration in Well Water over
       Time, Gray Farm	175
59     Total Kjeldahl Concentration in Well Water over Time, Gray
       Farm	176
60     Ammonia Concentration in Well Water over Time, Gray Farm.  . 178
61     Ammonia Concentration in Well Water over Time, Gray Farm.  . 179
62     Total Phosphorus Concentration in Well Water over Time,
       Gray Farm	180
63     Total Phosphorus Concentration Is Well Water over time,
       Gray Farm	181
64     Chemical Oxygen Demand Concentration in Well Water over
       Time, Gray Farm	183
65     Total Organic Carbon Concentration  in Well Water over Time,
       Gray Farm	184
66     Chemical Oxygen Demand Concentration in Well Water over
       Time, Gray Farm	185
67     Total Dissolved Solids Concentration in Well Water over
       Time, Gray Farm	187
68     Gray Wells which Contain Water wLth SARadj Greater Than 9  . 190
69     Iron Concentration in Well Water over Time, Gray Farm . .  . 191
70     Chloride Concentration in Well Water over Time, Gray Farm  . 194
71     Lead Concentration in Well Water over Time, Gray Farm . .  .195
72     Cadmium Concentration in Well Water over Time, Gray Farm.  . 197
73     Silver Concentration in Well Water  over Time, Gray Farm .  . 199
74     Propazine Concentration in Well Water over Time, Gray Farm. 202
75     Illustration of Nitrite plus Nitrate Lenses in Hancock Soil,
       1981  	206
76     Inorganic Nitrogen in 183 cm Profile at the Hancock Farm.  . 211
77     Inorganic Nitrogen in Hancock Soils  	 213
78     Inorganic Nitrogen in Hancock Soils Receiving 68.9 cm
       Hydraulic Loading 	 214
79     Soil Phosphorus Fixation by the Formation of Less Soluble
       Phosphates of Iron, Aluminum (for Clays) and Calcium   .  .  .215

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80     Total Phosphorus in Hancock Soils  	  216
81     Total Phosphorus in Hancock Soils  Receiving  68.9  cm
       Hydraulic Loading 	  217
82     Total Dissolved Solids in Hancock  Soils Receiving 68.9  cm
       Hydraulic Loading 	  220
83     Total Dissolved Solids in Hancock  Soils 	  221
84     Sodium in Hancock Soils	223
85     Sodium in Hancock Soils Receiving  68.9 cm Hydraulic  Loading  224
86     Chlorides in Hancock Soils Receiving 68.9 cm Hydraulic
       Loading	227
87     Nitrite plus Nitrate in Gray Soils	231
88     Organic Nitrogen in Gray Soils	233
89     Inorganic Nitrogen in 183 cm Profile Cotton/Alfalfa, Gray
       Farm	  .  235
90     Inorganic Nitrogen in 183 cm Profile Wheat Area,  Gray Farm.  237
91     Total Dissolved Solids in Gray Soils. ,	240
92     Sodium in Gray Soils	241
93     Chlorides in Gray Soils	244
94     Sulfates in Gray Soils	245
                               xn

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                                  TABLES
Number	Name	Page

   1      Ground-water Quality Beneath the Gray Farm June 1980 to 1982 . 20
   2     Industrial Contribution to the City of Lubbock Sewage System . 24
   3     Trickling Filter System Effluent Characteristics, Southeast
         Water Reclamation Plant, Lubbock, Texas   	 27
   4     Basic Design Information for Lubbock Land Treatment System Ex-
         pansion (Hancock Farm)  	 33
   5     Types of Underground Water Sampling Points by Site  	 58
   6     Completion Data for Well Used During the  Project Period   ... 62
   7     Sampling Intervals for Multi-depth Well (6893), Gray Site  . . 63
   8     Reservoir Monitoring Well Completion Data  	 69
   9     Nitrite Plus Nitrate (N0.2/N03) Concentration at 1 m and 4 m for
         Locations 2, 7, and 10  as Shown in Figure 11	76
  10     Variation of Dissolved Oxygen, Temperature and Specific Con-
         ductance with Depth in  Reservoir 1	77
  11     Reservoir #1 Survey of Specific Conductance, Ammonia and  Total
         Organic Carbon, September 1982 	 79
  12     Water Quality Analysis  	 83
  13     Soil Quality Analysis	92
  14     Crop Analysis	98
  15     Crop Analysis Protocol	99
  16     Design Efficiencies and Effluent Qualities of Conventional and
         Advanced Waste  Treatment Processes 	  108
  17     Characterization of Effluent Produced by  Southeast Water
         Reclamation Plant from June 1980 through  January 1982   ...   110
  18     Percentage of Free Ammonia (as Nh^) in Fresh Water at Varying
         pH and Temperature	114
  19     Concentration of Trace Elements in Treated Wastewater.  .  . .  116
  20     Water Salinity  Scale (U.S. Geological Survey)	116
  21      Total Water Applied to Hancock Farm in 1982	122
  22     Total Water Applied to Hancock Farm in 1983	124
  23     Gray Farm Hydraulic Loadings/Crops	127
  24     January Water Levels in State Wells  	  130
                                    xn

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25     Statistics of Depth to Water in Observation Wells  at  Gray
       Site During Project	
26     Statistics of Depth to Water in Observation Well at Hancock
       Site During Project	
27     Correlation Matrix for Water Content in Texas Tech University
       Plot Observation Sites, Hancock Farm 	
28     Percent of Hancock Farm Well Water Samples which Exceed  or
       Equal Drinking Water Standards for the Following Parameters.   144
29     Sodium Adsorption Ratio for Hancock Farm Well Water   ....   153
30     Relative Tolerance of Selected Crops to Foliar  Injury  from
       Saline Water Applied by Sprinklers 	   155
31     Percent of Gray Farm Well Water Samples which Exceed  or.  Equal
       Drinking Water Standards for the Following Parameters  ...   169
32     Sodium Adsorption Ratio for Ground Water Beneath Gray  Farm  .   189
33     Input Parameters and Coefficients for Hancock Soils -  N  Mass
       Balance Model  	   210
34     Phosphorus Mass Balance, Hancock Farm	218
35     Mass Total Dissolved Solids Measured in Hancock Soils  .  .  .   222
36     Sodium Mass Balance on Hancock Soils 	   222
37     Potassium Mass Balance, Hancock	225
38     Metals Mass Balance for Hancock Farm	228
39     Input Parameters and Coefficients for N Mass Balance  Model  .   234
40     Total Phosphorus Mass Balance on Gray Soils	238
41     Mass Balance on TDS in Soils Profile on Gray Farm	238
42     Sodium and Potassium Mass Balance on Gray Soils	242
43     Chloride and Sulfate Mass Balance on Gray Soils	   246
44     Trace Metals Mass Balance on Soils Collected from Flood  Irri-
       gation Area	246
45     Mass of Priority Organics Applied to Gray Farm	249
46     Cotton Yields, Hancock Farm  	   252
47     Ranges of Specific Elements Presented in the Crop Tissue
       Obtained from Hancock Farm	253
48     Elemental Shifts in Cotton Tissues Obtained from Hancock Farm
       1981 vs. 1983	254
49     Concentration Ranges of Specific Elements in Grain Sorghum
       Tissue Collected from Hancock Farm 	   256
50     Crop Yields Obtained from Gray Farm in 1982 and 1983  (kg/ha)   257
51     0 & M Costs of Land Treatment Sites (EPA, 1982)	262
                                  xiv

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52     Hancock Farm Revenues	266
53     Summary of Gross Income of Tenants 	  267
54     Lubbock County, Texas Gross Cotton Revenue vs. Hancock Farm.  267
55     Balance Sheet, Total Hancock System vs. Hancock Farm ....  269
56     Comparisons of Shift in Farmers; Income Pre-effluent to
       Post-effluent  	  270
57     City's Net Cost in Variations in Funding Hancock Extension
       of Lubbock Land Treatment System	272
                                  xv

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                       ACKNOWLEDGEMENTS

      Special  recognition is to be given to  Congressman  George
Mahon who,  along with representatives of Lubbock Christian Col-
lege,  sought  financing of the project  through  USEPA.  A note  of
appreciation  is due the City of Lubbock, Lubbock Christian Col-
lege Investment  Corporation, and J.E. (Gene)  Hancock for  their
cooperation  and financial  aid  in  completion  of the project's
objectives.
     A special  thanks is due to the  City of Wilson, residents of
Wilson and  neighbors of  the Hancock farm for  their patience,
understanding and cooperation of the Lubbock Land Treatment Re-
search and  Demonstration Project.  A deep appreciation goes  to
the farmers  of the Hancock  farm for their efforts in the con-
struction,  operation, and maintenance  of the Lubbock Land  Treat-
ment  System,  Hancock Farm Extension.  Additional recognition is
due Frank Gray for his cooperation in  the the research and  moni-
toring programs  at the Lubbock Land Treatment System — Gray Farm
Extension.
     The authors acknowledge the invaluable assistance and guid-
ance of  the laboratory staff and project officers from  USEPA
(RSKERL),  especially George  Keeler  who assisted in the project
from beginning to end.
     Finally, the  authors acknowledge the vital contribution of
the many laboratory technicians,  field personnel, and clerical
staff who  assisted in this  study.   Without their concerted in-
volvement,  dedication and prudent regard for the results of their
work,  the objectives of this project  would not have been met.
                             xvi

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                               SECTION 1

                              INTRODUCTION

     The hydrologic  cycle  is a hydrologic system which  consists  of various
processes such  as  precipitation, evaporation,  transpiration,  infiltration,
detention,  retention, surface runoff,  subsurface runoff,  and  ground water
flow. These  hydrologic processes are combined through circulation,  distri-
bution and hydraulic  continuity to form the cycle (Chow,  1970). Disparities
in global distribution of water in conjunction  with  increasing  water  de-
mands  by agriculture,  industry, and  municipalities  have created severe
water shortages in numerous  regions of the world.  Factors  compounding  the
water supply problem  are (Williams, 1982):
     1.  Shortages resulting  from inadequate distribution systems
     2.  Ground-water overdrafts
     3.  Surface water and  ground-water quality degradation
     4.  Institutional constraints
     5.  Competition  between  uses
With   existing or potential water  crises facing  many water consumers,
reclaiming or reuse of wastewater streams has become  an  attractive option.
     In  the  United States  the  major user  of freshwater  is   agriculture.
Agriculture  plus steam electric plants  use over 75 percent of all  fresh-
water withdrawn in the United States (Williams, 1982).   Irrigation consumes
approximately 99 percent of  the water used in  the agricultural  industry.
The  amount  of  freshwater withdrawal  for irrigation  can be  reduced by
application  of municipal wastewater to agricultural land.  Development of
municipal wastewater and application systems  within the United  States has
been limited by 1) overly conservative and, consequently, costly  design of
slow-rate (water reuse and  nutrient recycle)  systems;  and 2)  requirements
of a substantially higher and more costly level of pre-appl ication  treat-
ment  than is  needed to protect health and  ensure  design  performance
(Thomas, 1982).  Slow rate  wastewater application, usually  in  the  form of
spray irrigation,  is  the most widely used form of land  application.
     Advantages of slow rate  systems include the maximization  of  crop pro-
duction, high treatment efficiencies, the elimination of surface  water  dis-
                                  1

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charges,   potential  economic   return through  crop production,  and ground-
water recharge.  Although  some  seasonal variations occur, very high  removal
efficiencies for biochemical oxygen demand and suspended solids are common.
Nutrient  removal due to adsorption and crop utilization is also very  high.
Disadvantages  of  slow  rate systems  include  relatively low application
rates (1  cm/wk to 10 cm/wk), possible increases in soil salt concentrations
because of evapotranspiratLon,  potential leaching of salts into the ground
water causing reuse  limitations,  and the formation  of pathogenic aerosols
(Bausum,  Schaub,  and Kenyon,  1978; Torpy et al. , 1975; Webber and Leyshan,
1975; 3ohnson et al., 1978)..
     The Lubbock Land Treatment System Research and Demonstration Program,
funded by Congress in 1978  (H.R. 9375), was designed to address the various
issues limiting  the use of slow rate land application of municipal waste-
water-  The project  involved the 1) expansion of the Lubbock Land Treatment
System; 2)  characterization of the chemical, biological and physical condi-
tion of the ground water, soils and crops prior  to and during irrigation
with  secondary treated  municipal wastewater; 3) evaluation of health ef-
fects associated with the   slow rate land application of  secondary efflu-
ent;  and 4) assessment of  the effects of hydraulic, nutrient and salt mass
loadings  on crops, soil and percolate.    Results from the   Lubbock  Land
Treatment Research and Demonstration Project are published in four volumes:
     1.  Volume  I:   Demonstration/hydrogeologic study
     2.  Volume  II:   Percolate Investigation in the Root Zone (Ramsey  1985)
     3.  Volume  III:  Agricultural Research Study (George et al 1985)
     4.  Volume  IV:   Lubbock Infection Surveillance Study (Camann  et al
                     1985).
     During the  1930s the City of Lubbock entered into a contractual agree-
ment with Dr. Fred Standefer to pump all the sewage effluent to his  farm.
Mr. Frank Gray was hired  as  manager of the  farm and subsequently became a
partner and finally  owner of the farm.  As Lubbock grew, the Gray farm was
able  to  expand  to encompass 1489 ha.  Nonetheless, the Gray farm could not
adequately  manage  the hydraulic flow pumped from the City of Lubbock.   Con-
sequently,   the  farm  was  overirrigated  and ground-water  accumulation oc-
curred beneath the farm with associated water quality problems.
     In November  1980 construction commenced to expand the Lubbock Land

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Treatment  System to include  the Hancock  farm located 25 km southeast  of
Lubbock.   The  expansion was designed to reduce  the hydraulic  and nutrient
overloaded  condition of  the  Gray farm.   The  combined area of the  Lubbock
Land Treatment system was 2967 ha.
     The Demonstration/hydrogeologic study was designed to  determine the
short term  effects of 1) reducing the quantity  of wastewater irrigation  at
the  Gray  farm on crops,  soils, and ground water; and 2) slow rate  land
application  of secondary effluent on crops,  soils, and ground  water  at the
Hancock  farm.  The transient response of the ground-water  elevation and
guality to  irrigation practices and climatological  factors were measured
for  a  three year period.  Variations in quality and quantity  of crops  pro-
duced on both  farms  were monitored.  In addition, chemical,  physical and
biological  analyses of the  soil profile  were conducted to  ascertain the
effects of the reuse of secondary effluent  on the second largest slow rate
land application  system in the United States.

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                                SECTION  2
                         SUMMARY AND  CONCLUSIONS
SUMMARY
     The Lubbock Land  Treatment System consists  of  two privately owned
farms.   In  the past years, the Gray  farm  has  suffered from inadequate stor-
age and  distribution piping network  to  properly manage effluent produced by
Lubbock's Southeast Water  Reclamation Plant (SeWRP).   Consequently,  an
increase in ground-water elevation  and degradation of ground-water quality
occurred beneath the farm.  The system  was  expanded in 1981 to include  the
1478 ha Hancock  farm which  is  located  25 km southeast of Lubbock, Texas.
The expanded slow rate land application system encompassed  approximately
2967 ha.   From  June 1980 to  October 1983,  both farms were monitored to
assess  the  impacts to ground  water, soils and  crops of  1)  reducing  the
hydraulic, chemical, and biological mass loading  for the Gray farm; and 2)
spray irrigation of effluent to the  Hancock farm which was primarily  a  dry
land farm  during  the previous  ten years  prior to 1982.   The findings of
the project indicated that the major recharge  of ground  water beneath  the
Gray farm  was from flood irrigated  wheat areas.   Deep percolation of irri-
gation  water and precipitation continued  in 1982 and  1983  in the  flood
irrigated  areas.   Physical limits  of  irrigation  equipment,  hydraulic dis-
tribution system, water storage,  and crop cultivation eliminated the  capa-
bilities for proper water, management.   With adequate winter storage and the
hydraulic capability to distribute more water on the alfalfa in 1982  and
1983, minimal  deep  percolation would  have occurred through the  soil
throughout  the farm.  Comparison of  1981  and  1983 ground-water elevation
data  indicated  that the  ground-water levels  beneath the  Gray  farm de-
creased.
     During the period  from  February  1982 to October 1983,  an increase in
the ground-water quality also  occurred  beneath most of the Gray farm.  Mass
balances conducted on nutrient and minerals indicated continued leaching of
constituents through a soil depth of 183 cm  beneath the  flood irrigated
area; whereas, most of the chemical  constituents applied by sprinkler irri-
gation  were retained and/or removed  through crop uptake  beneath the  spray

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irrigated  areas. Statistically significant decreases  in nitrite  plus
nitrate  nitrogen (NQ.2 + NQ.3-N) levels occurred.  A comparison of baseline
data (June  1980  to February 1982) and data collected  after February  1982
indicated  a decrease in the frequency of ground-water N0£ + NQ.3-N concent-
rations equaling or  exceeding drinking water  standards in nine of  27 wells
monitored.
     Wastewater treated by  SeWRP  was  primarily derived  from domestic
sources  with less  than 30  percent  contributed by  industrial sources.
Consequently, trace metals posed no potential toxicity problems to humans
or plants.
     Total  irrigation  at the  Hancock farm varied from 16 cm to 20 cm in
1982 and 36 to 49 cm in 1983.  An overall increase in  ground-water  eleva-
tion  occurred beneath the  Hancock farm.  A maximum rise of three to five
meters was  experiences in ground-water wells  in close proximity to surface
runoff collection  areas.  Increases in ground-water elevation beneath the
Hancock farm were primarily due to percolation of surface  runoff through
coarse material contained in moats surrounding  the reservoirs and excava-
tions constructed to reduce flooding of cropland  and migration of percolate
through  material surrounding poorly  sealed  well  casings.  Increases in
ground-water elevation commenced approximately  two months after heavy  pre-
cipitation  events.
     Chemical  constituents contained in the treated wastewater applied to
the Hancock farm were removed by the soil-crop  matrix  from percolate water.
Increases  in ground-water  chemical parameters  appeared  to be associated
with deep percolation of surface runoff contained in moats  and excavation
pits  constructed to "contain  surface  runoff.   Existing salt and nitrate
deposits within  the  soil profile were leached with percolate to the  ground
water; thereby causing increase in nitrate and  total dissolved solid levels
in several  wells.
     In general, no  significant changes in trace  metals or priority organic
pollutants  occurred in  the  ground  water during the monitoring  period.
Based  on values cited in literature, trace elements posed no public health
problems.
     Salt accumulation  occurred in the upper 183 cm of the soil profile.

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As expected,  salt  accumulations were directly proportional to mass loadings
from irrigation.   Insufficient water was applied (less  than 21 cm  in 1982
and less than 50 cm  in  1983) to leach salts below the root zone.  Exchange-
able sodium percentage  increased  from two to six percent  in the top  30 cm
of soil during the period  from February 1982 to October 1983.
     Cotton and grain sorghum (milo) were the  primary  crops grown  on the
Hancock farm in  1980,  1981 and  1983.  Due to severe weather in 1982, sun-
flowers, soybeans  and grain sorghum were planted  as alternative crops to
cotton.  While milo yields  were low due to late planting and trifluralin
damage, sunflower  and soybean yields were average for the High Plains area
of Texas.  An improvement  in cotton crop production occurred in 1983.  With
effluent irrigation, the cotton yields for the farm were 48 percent greater
than  the Lubbock County  average.   Cotton yields  in 1983  may  have been
limited by possible  nutrient shortages, boll  worm infestation, and cool
weather during the late  growing season.  Cotton production in 1983 ranged
from 353 to 740 kg/ha.   Based on  the information gathered during the Demon-
stration/Hydrogeologic  Study the  following specific conclusions were made.
CONCLUSIONS
Land Application System  Design and Effluent
1.  The doubled loop distribution pipe network at the Hancock farm afforded
    the farmers better  reuse of water and nutrients.  Irrigation water could
    be derived directly  from the  distribution pipe network as the flow was
    was pumped from  Lubbock and/or indirectly through the reservoirs to the
    center pivot machines.
2.  The Hancock hydraulic  distribution system was not designed to transport
    particulates.  Major problems associated  with the design of the system
    were caused by lack  of  in-depth considerations  of the impact particu-
    lates would have on  automation and clogging of pressure regulators.
3.  Based on  the hydraulic distribution within the SeWRP, insufficient flow
    was available  at the new pump station  to pump the design flow rate of
    2.8  x  104 m3/d.   An  annual flow  of 4,128,219 m3 and  4,135,244 m3
    was pumped to  the Hancock farm in 1982 and 1983,  respectively.
4.  A minimum  of  four months  hydraulic residence  time which  existed in

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    reservoirs   constructed  on   the  Hancock  farm   provided  ample  time  for
    storage  of  wastewater during crop  planting  and harvesting.   Estimated
    hydraulic  detention within  storage ponds  on the  Gray  farm was 10 days.
5.  Major operational problems  at the  Gray  farm   resulted from  inadequate
    hydraulic capacity in the storage ponds  and  distribution network.
6.  Wastewater  treated  by SeWRP  was   primarily   derived  from   domestic
    sources.   Trace metals posed no  potential   toxicity problems to humans
    or plants.
7.   The  adjusted sodium- adsorption ratio  (SAR)  of the effluent  stream  was
    approximately 22. Sodium  concentrations  in  the effluent  stream,  there-
    fore,  may create sodic conditions  in  the  soil.  In fact, a  general  in-
    crease in the exchangeable sodium percentage was  measured in  the 30 cm
    of soil throughout the Hancock farm.
Hancock Farm
1 .   Odor problems  created by  irrigation with  effluent   directly from  the
    SEWRP  were remedied  by  transporting  all  effluent through  the  reser-
    voirs  prior to  land application.   Irrigation only from reservoirs  re-
    duced the particulate mass load to  center  pivots,  thereby,  decreasing
    labor requirements  for cleaning  in-line  screens  and  nozzle  orifices.
    Nitrogen concentration in the irrigation  water,  however,  was reduced
    by 71 percent from 42 to  12  mg-N/1.
2.  Algal activity in the reservoirs  changed  the alkalinity  balance  in the
    reservoirs  and the effluent  increased  from an average  value of 7.8 to
    8.3.
3.   Total  phosphorus  concentrations  (primarily  orthophosphate  phosphate)
    were decreased by 47 percent in the reservoirs.
4.   Annual irrigation  at the Hancock  farm  varied  from 16  cm   to 20 cm in
    1982 and 36  to 49 cm in 1983.
5.  An overall increase in ground-water elevation  of 30 cm in approximately
    18 months occurred beneath the Hancock  farm.   A maximum rise of three
    three to five meters  was experienced  in   ground-water  wells in close
    proximity to surface runoff  collection areas.
6.  Increases  in ground-water elevation beneath the  Hancock farm were  pri-

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     marily due  to  deep percolation  of surface runoff through coarse mater-
     ial contained   in moats  surrounding the  reservoirs;  excavations con-
     structed to reduce   flooding of crop land; and hydraulic short circuit-
     ing along casing of  poorly constructed wells.
 7.  Rises in ground-water depth  commenced  approximately  two months after
     heavy precipitation  events.
 8.  Existing salt  and nitrate deposits within the soil profile appeared to
     have been leached with percolate to the ground water; thereby, causing
     increases  in  N03-N and total dissolved solids (IDS) levels in several
     wells.  Increases in water quality parameters appeared to be associated
     with  deep   percolation of  surface  runoff  contained in  moats  and
     excavation  pits constructed to contain surface runoff.
 9.  Trace metals (i.e.,  Cr, Cd", Pb,  As, Ag, Tl,  Co, and Cu)  posed no public
     health hazard  or phytotoxic ity  problems.   No  significant changes  in
     trace metals occurred in the ground water during the monitoring period.
10.  Priority organic pollutants in the ground water did  not  pose a public
     health  problem.   Dibutylphthalate and diethylphthalate were the only
     organic compounds exhibiting significant (a  = .05)  increases in four of
     28 monitoring  wells.
11.  During  the baseline monitoring period  (June 1980 to February  1982)
     ground water beneath the Hancock farm contained coliform bacteria  and
     fecal  streptococcus.  Prior to transporting the effluent stream to  the
     Hancock  farm,  Salmonella was  also isolated  in nine of 28 monitoring
     wells.
12.  Neutron  probe  measurements failed to  detect moisture fronts migrating
     through the soil profile after irrigation events.
13.  Salt accumulation  occurred  in  the  upper 183  cm of the  soil profile.
     Salt accumulations were directly  proportional  to  mass  loadings from
     irrigation.   Insufficient water was  applied  (less than 21  cm in 1982
     and less than 50 cm in 1983)  to  leach salts  below the root zone.
14.  Exchangeable sodium percentage increased  from  two to six percent  in  the
     top 30 cm of soil during the  period from February 1982 to October  1983.
15.  Due to minimal water available  in the  crop  root zone, increased sodium
     concentrations  in the soil  solution resulted in higher sodium uptake by

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     crops on  the  Hancock  farm than measured in similar crops collected  from
     the Gray  farm.
16.   The major mechanism for nitrogen removal from the soil  profile  was  crop
     uptake.   Nitrogen  removed by crops always exceeded the  N mass input by
     irrigation.   In  general, nitrogen did not appear to be  leached  past the
     183 cm depth.
17.   Naturally occurring  nitrate lenses in the soil profile were  diminished
     in 183 cm soil cores  extracted in 1981 and  1983 by crop  utilization,
     denitrification, and  leaching to a deeper depth within  the root  zone.
18.   Grain sorghum harvested in  1982 consumed  more phosphorus than  was
     applied  by  irrigation.  In 1983, however, phosphorus removal by cotton
     was less  than the  mass applied.  In the alkaline soils, availability of
     phosphorus to crops was inhibited by calcite-phosphorus reactions.
19.   Crops utilized more potassium than provided by the irrigation water.
20.   Chloride and 50^ anions  accumulated  in the upper 122 cm of  the  soil
     profile.
21.   The  changes  in  the mass of metals detected within the  183 cm soil  pro-
     file from 1981 to  1983 was affected more  by  spacial variability  than
     the  mass of  trace metals applied to the soil by irrigation from Febru-
     ary 1982  to October 1983.
22.   Certain priority organics, such as atrazine, dichloroaniline, dichloro-
     benzene,  chloroform,  benzene, tetrachloroethylene and carbontetrachlor-
     ide,  which  were  associated with herbicides, were found at significant
     concentrations in  the Hancock soils.  A mass balance of priority organ-
     ic  pollutants applied to  the farm through irrigation showed  that the
     applied effluent was  probably not the source.  The solvents  seemed to
     penetrate to greater soil  depths than  the herbicides and herbicide
     derivatives.
23.   Irrigation  with  effluent  apparently  increased  the  concentration of
     total coliforms, fecal coliforms, fecal streptococcus,  and  actinomy-
     cetes  in the  upper 91 cm of soil.  Fecal streptococcus seems to have  a
     slower die-off rate than fecal coliform bacteria.  Increase in   actino-
     mycetes concentrations may have reflected a general increase  in biolog-
     ical activity  within  the soil profile.

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24.  Cotton and  grain sorghum  (milo)  were  the  primary  crops  grown on  the
     Hancock  farm in 1980, 1981 and 1983.   Due to  severe  weather  in 1982,
     sunflowers,  soybeans, and  grain  sorghum were  planted  as alternative
     crops to  cotton.  While milo yields were  low  due  to late planting  and
     trifluralin damage, sunflower and soybean yields  were average  for  the
     High Plains  area of  Texas.  An improvement  in crop  production  occurred
     in 1983.  Cotton yields for the farm  were 48 percent greater than  the
     Lubbock  County average.  1983 cotton  yields  produced at  the  Hancock
     farm may have  been limited  by  possible nutrient  shortages, boll worm
     infestation,  and cool weather during  late growing season.   Hancock farm
     cotton production in 1983 ranged  from  353 to  740  kg/ha.
25.  Calcium,  potassium,  sodium, iron, barium, chromium  and lead concentra-
     ted more in the  cotton stalk than seed.  Arsenic  was below detectable
     limits in all cotton samples.  As copper  became depleted in the soil,
     any available copper was transported  to the seed.   The concentration of
     elements  in  crops was partially dependent on  the  concentration of those
     macro and micro nutrients in_ the  irrigation water and soil  solution.  A
     majority  of  the elements which remained constant  were in  the seed  tis-
     sue with corresponding stalk parts  showing  decreases in concentration
     levels from  1981 to  1983.
26.  Phosphorus  levels   in cotton  stalks decreased 51  percent  from 1981  to
     1983,  which  may have limited production.  Consequently,  the mass  of
     phosphorus  removed  from the soil profile in  1983 was less  than antici-
     pated .
27.  Arsenic   and cadmium were concentrated  more in  the  milo stalk than seed
     and 1983  levels were less than concentrations measured in 1982.   No
     accumulations  of trace metals in  crops  appeared to have resulted from
     land treatment.
28.  The overall  decrease of nitrogen and phosphorus  in plant  tissue from
     1981  to 1983 was partially due to the failure  of  the effluent hydraulic
     loading and  nutrient content  and  meet crop nutrient requirements.
Gray Farm
 1.  Prior to 1982,  the  annual  hydraulic flow to  the Gray farm  was  approxi-
                                   10

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    mately  20,805,000 m3 (5.50 x 109 gal).   In  1982 and 1983, the Gray farm
    received 12,522,394 m3  and  11,406,297 m3, respectively, from SeWRP.
    Before  1982,  the hydraulic loadings to  cotton was  about 65 cm/yr  and
    wheat  received about 465 cm/yr.   Once effluent was pumped from SeWRP to
    the Hancock  farm, alfalfa received  55  cm/yr and  wheat was irrigated
    with 207  to  230 cm of effluent per year.
2.  Comparison of 1981 and 1983 ground-water  elevation data  indicated  that
    the ground-water level beneath the Gray  farm decreased an average of 30
    cm.
3.  Major  recharge  of ground  water beneath  the Gray farm was from flood
    irrigated, wheat areas.  Deep percolation of  irrigation  water and  pre-
    cipitation continued in 1982 and 1983 in  the  flood irrigated areas.
4.  Physical  limits of the irrigation equipment, hydraulic distribution
    system,  and water storage eliminated the capabilities for proper water
    management.   With adequate winter storage and the hydraulic capability
    to  distribute more water on the alfalfa  in 1982 and 1983, no deep per-
    colation  would have occurred through the  soil throughout the farm.
5.  Statistically  significant  decreases  in NO^-N levels were measured in
    five of 27 monitoring wells  from February 1982 to  October 1983.   In
    general, 17 of  27 wells  experienced  a  decrease in ground-water N03-N
    levels.
6.  A comparison of baseline and data collected after February 1982 indi-
    cated  a  decrease in the  frequency of ground-water N03~N concentrations
    equaling  or  exceeding drinking water standards in nine of 27 wells mon-
    itored.
7.  Average  total phosphorus levels in the  ground water decreased in 18 of
    27 wells.
8.  The information gathered during this study  supports the  conclusion that
    with adequate water  storage,  increased hydraulic  distribution and
    applied  capacity,  and production of alfalfa  as the  major crop, the
    hydraulic and nutrient mass  loadings  discharged  by  SeWRP could have
    been effectively  removed  by the existing  land application site con-
    trolled by Frank Gray.
9.  Precipitation events appeared to have  affected the chemical character-

                                    11

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     istic of the  ground water.
10.  Ground  water total dissolved solids  concentration remained relatively
     constant throughout the project monitoring period. A change in the com-
     position  of  salts present in the ground water (i.e., higher concentra-
     tion of Ca and  Mg and lower levels of Na)  resulted  in  a decrease  in
     adjusted sodium adsorption ratio.
11.  The majority of  trace metals measured in the ground water beneath the
     Gray farm were  at low levels.   During the  project monitoring period
     trace metals posed no public  health  hazard or  toxicity problems  to
     plant or animals.
12.  Bacterial indicator organisms were present in the ground  water through-
     out the monitoring period.  The frequency of isolation  of Salmonella
     decreased  from five during the baseline period to only one from Febru-
     ary 1982 to October 1983.
13.  The soil  matrix  was efficient in removing and biologically degrading
     priority organic compounds applied to the soil.  Consequently, organic
     compounds in  the municipal effluent or applied in herbicides and insec-
     ticides presented no hazards to public health.
14.  The Gray  soils had a higher  percentage of coarse material throughout
     the upper 122 cm of the soil profile than the Hancock  farm and a  sim-
     ilar indurated  caliche material at depths from 40 to 183  cm.
15.  Mass balance  conducted on nutrient and minerals indicated continued
     leaching  of  constituents  through a soil  depth of 183  cm beneath the
     flood irrigated areas; whereas, most of the  chemical constituents ap-
     plied by sprinkler irrigation were retained  and/or removed through crop
     uptake beneath  the spray irrigated areas.
16.  Beneath the center pivot  irrigation machines,   soil nitrates decreased
     -during the  project period primarily due  to the changing of the cropping
     pattern from  cotton to alfalfa.   Ammonia,  found primarily in the  upper
     30 cm,  remained relatively constant.   Organic nitrogen,   which was the
     major nitrogen  form in the soil, decreased with depth and time through-
     out the  project.
17.  Nitrogen mass balances indicated that  the major mechanisms for nitrogen
     loss was crop uptake and denitrification  for  the sprinkler irrigated

                                    12

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     areas and  deep  percolation of nitrates for the flood and  row irrigated
     areas.
18.  Only 33  percent  of  the total phosphorus (TP) applied through  irrigation
     was consumed  by  crops.   TP concentrations  decreased with  depth.  An
     important  mechanism  in phosphorus removal was phosphate-calcite  reac-
     tions.
19.  Total dissolved solids  (TDS) decreased  with depth beneath sprinkler
     irrigation  areas; whereas, frequent leaching of salts in the  flood and
     row irrigating  areas  produced  a more uniform TDS concentration through-
     out the  soil  profile.
20.  Sodium  did not appear  to  be associated  with the  increases in  TDS.
     Sodium  levels  were maintained sufficiently low  by leaching  to prevent
     sodic conditions for  both the sprinkler and the flood or  row irrigated
     areas.
21.  The potassium (K) concentration in the wastewater   (K/N  =  1.21) did not
     did not  inhibit   crop  utilization of nitrogen in the wastewater.   The K
     concentration decreased with depth and time under the  sprinkler  irri-
     gated areas,  but was  relatively uniform throughout the soil  profile in
     the  flood  and row irrigated areas.   Sprinkler  irrigated  cotton and
     flood or row irrigated wheat consumed  less  K than applied.   Alfalfa,
     due to  its  higher nitrogen requirement, utilized more nitrogen than was
     applied.
22.  Chlorides and sulfates were the major  anion associated with  the applied
     salts,  and  similarly  were leached in the flood or  row irrigated  areas
     and were concentrated  in the sprinkler irrigated areas.
23.  The input  of trace metals  through irrigations  to the  soils  was  low,
     however, arsenic,   chromium  (VI), barium, copper, and  nickel appeared
     to be transported by  percolate beyond  the 91 cm soil  depth.   Possible
     accumulation of cadmium, cobalt and  lead was observed  in the upper 91
     cm of soil  in the flood  irrigated areas.
24.  The majority of soil samples contained  levels  of priority organics
     below their respected  detection limits.  Basically,  the  same organic
     compounds  which were prevalent within the soil profile at  the Hancock
     farm dominated  the  Gray  farm soils.  Similar to soil data obtained from

                                   13

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     the Hancock farm,  solvents  were  found at deeper depth than other types
     of  trace organics.   The  priority  organic mass balance  showed that  al-
     though the Gray farm  had higher mass loadings than the Hancock farm,
     the major source of priority organics was  herbicides  and pesticides
     used  in farming operations.  The  flood  irrigated  areas,  having  had
     higher  hydraulic and consequently higher priority organic mass  load-
     ings,  appeared to  have  priority organics detected at higher  concentra-
     tions  and frequencies than the sprinkler irrigated areas.  There  was
     evidence that  greater  soil moisture in the flood irrigated areas  may
     have enhanced biological degradation of certain priority organics.
25.   Total  coliforms (TC), fecal  coliforms (FC)  and fecal  streptococcus (PS)
     were primarily retained  in the upper 30 cm  of soil;  however, certain
     cores  from flood irrigated areas had TC and PS too numerous to count at
     a depth of 183 cm.   PS  was detected at greater concentrations  in  the
     spray  irrigated areas  in 1983 than in 1981.  Pecal streptococcus  ap-
     peared  to survive for longer periods of time.  Pungi  and actinomycetes
     concentrations  within  the soil profile  were  relatively constant
     throughout the soil profile  and monitoring  period regardless  of hydrau-
     lic load or cropping patterns.
26.   Cotton yields  prior to 1982 equaled or  exceeded those for irrigated
     cotton  farms in Lubbock  County.  Only three  to four  alfalfa cuttings
     were  obtained  in  1983  compared to the five to. seven cuttings obtained
     for Lubbock County.  In  1980 and 1981 over  1,000 head  of  cattle were
     grazed on the Gray farm and in the winter  of 1982 and  1983,  3,000 head
     of  cattle grazed the wheat and alfalfa areas.
27.   In  1981 cotton  plant  tissue accumulated  more K, Na,  Ca and Ba in  the
     stalk  tissue than in the seed and N, P and  Cd were at  higher concen-
     trations in the seed.   Cr, As and Pb  were below detection limits in
     1981 cotton samples.  Copper was found to accumulate  more in  the cotton
     seed than in the stalk.   Possibly due to  the higher moisture  content of
     Gray soils, cotton  from  the  Gray  farm had  a lesser  concentration  of
     sodium than cotton  from the Hancock farm.  In 1983,  alfalfa contained
     higher  levels of Na than normal cited values.  Wheat  and milo samples
     had higher concentrations of calcium than cited in literature.

                                   14

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28.  Potential  toxic trace metals did not appear in significant  concentra-
     tions in the  crop  tissue.
 Economics
 1.  Amortized system construction cost over a 20 year period  at  ten  percent
     annual  interest rate would be $167/1000 m3 per year  ($0.63/1000 gal).
     With 85 percent  federal cost sharing amortized construction  cost would
     have been  reduced  to $25/1000 m3/yr  ($0.10/1000 gal).   Inclusion of
     land cost would  have increased annual capital cost by  24  percent.
 2.  Total  operation and maintenance (0 & M) costs associated  with the Lub-
     bock Land  Treatment System Expansion were $156/1000 m3($0 .59/1000 gal)
     in  1982 and  $139/1000 m3  ($0.53/1000 gal).  The City of Lubbock bore
     $71/1000 m3  of the  total  0  & M cost in 1982 and $58/1000 m3 in 1983.
     The  farmer's portion of the 0 & M was $85/1000 m3 ($0.32/1000 gal) and
     $81/100 m3 ($0.31/1000 m3) in 1982 and 1983., respectively.
 3.  Gross revenues received for crops harvested from the Hancock farm in-
     creased from  1980  to 1983.  Government subsidies accounted for approxi-
     mately 26 to-40  percent of the farmer's  total revenue in 1980, 1981,
     and  1982.   Crop  revenues  increased  from  $199,505.40 in 1982  to
     $543,781.44 in 1983 and government support decreased from $102,709.56
     (1982)  to $49,239.65 (1983).
 4.  The  economic balance of  cost expended and revenues  received showed  a
     net negative  balance each year during the project period  (1980  through
     1983)  ranging  from  $701,661.81 (1981)  to $1,103,687.57 (1982).  Net
     cost were  $267.35/1000 m3 ($1.00/1000 gal) in 1982 and $161.28/1000 m3
     ($0.61/1000 gal  in  1983.  Crop revenues offset costs by 18 percent and
     47 percent of total costs in 1982 and 1983, respectively.
 5.  The economic  analysis of the Hancock farm  operation indicated a net
     loss in  investment in 1980 and 1982 and a return of $48,603.64  in 1981
     and $28,535.24 in  1983.  The landowner was unable to make land payments
     with revenues received in 1980, 1981 and 1982, but received a profit of
     $84,171 in 1983.  The average net revenues  to each farmer after sub-
     tracting  farming  cost was approximately $7,857 over  four years.  This
     return  on the farmer's investment had to pay  for his living expenses.

                                    15

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                               SECTION 3
                            RECOMMENDATIONS
    Based upon  the  results of this  study,  the  following  recommendations
are presented:
1.   The major problem  associated with the operation  of  the  Gray  farm  was
     the  inability to manage water effectively.   Crop  and water  management
     operation  manuals and procedures for slow rate land application sys-
     tems need to be developed for use by municipalities  and  farmers.
2.    With the rapid  rise in ground water beneath  the Hancock  farm, it  is
     important to define the effects of indurated  zones, macropores and
     micropores on  the hydraulic conductivity and transport of chemicals
     such as  nutrients and trace organics through the  vadose  zone.
3.    Research should be conducted to  better  define what  mechanisms govern
     the  leaching of organics, trace metals and other  chemical  constitu-
     ents during precipitation events.
4.    Studies  should be conducted to determine the potential  transport  of
     chemical constituents contained  in surface  runoff collected  in playa
     lake areas  to the ground-water table.
5.    Since the  surface runoff collection moats were a  source  of ground-
     water recharge and pollution, more stringent design  specifications  on
     surface  runoff collection areas need to  be developed.
6.    In order to reduce the frequency of engineering design  errors  which
     have resulted  in  the operations problems,  a  documentation of design
     errors constructed in existing land application systems  and associa-
     ted  remedial action taken to alleviate  the  problems needs  to be pre-
     pared.   This document will  be  invaluable  to regulatory  agencies,
     municipalities and engineering consultants.   Furthermore,  this docu-
     ment should include a general evaluation of operation  problems and
     appropriate remedial actions.
7-    Modifications should be made on the Gray farm  to  increase  the storage
     capacity and hydraulic distribution capacity throughout  the  farm.
     Furthermore, a high water and nutrient consuming  crop (such as alfal-
     fa)  needs to be  planted in  the  flood   irrigated areas of the Gray
     farm.

                                 16

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An optimization procedure  needs to  be developed to allow engineers
and decision makers to design and approve systems  which most  effec-
tively reuse vital nutrients and water resources.
Existing  nitrate  and salt lenses in the  soil  profile were leached
during precipitation events at the Hancock  farm.  A research effort
should be conducted to ascertain the chemical  composition of  these
deposits  and what processes govern their deposition and dissolution.
                             17

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                               SECTION 4

           LUBBOCK  SLOW RATE LAND APPLICATION SYSTEM DESCRIPTION

FACILITIES DESCRIPTION
     Lubbock  is  located in the Southern High Plains region of northwestern
Texas (Figure  1).   A semiarid climate dominates the Southern  High Plains.
Average  annual temperature is 15.6°C (60°F)  with the recorded temperatures
ranging  from -26.7°C (-16°F) to 41.7°C (107°F).  The normal daily maximum
temperature recorded "in July is 33°C (91°F).   The normal daily minimum tem-
perature in January is -3.9°C (25°F).  The growing season is approximately
210 days.  The region averages 168 clear days, 106 partly cloudy,  and 91
cloudy days per .year (Lubbock Christian College Institute of Water Research
1979).
     Annual precipitation for the region is  45.7 cm (18 in).  Approximately
70 percent of  the total annual rainfall occurs  during  the  growing season
between  April  and September.
     The economic  base for the region is irrigated agriculture.  Principal
crops grown are cotton, grain sorghum, wheat, and soybeans.  Primary  source
of irrigation  water is the Ogallala aquifer which underlies the area.   Dur-
ing the  past three  decades, the withdrawal of ground water from the aquifer
has exceeded  the  natural  recharge (Bell and Morrison 1978). If the  over-
draft continues,  the saturated thickness of the aquifer will be depleted to
a  level  where it  may not  be economically  feasible to withdraw water for
irrigation. Existing  and  projected limited  ground-water  resources  and
increasing energy costs to mine  ground water have caused farmers to seek
more economical  and available water resources.    Since  1938  the effluent
produced by Lubbock's Southeast Water Reclamation Plant (SeWRP) has been
reused for irrigation  of crops grown on the Gray farm.   As the wastewater
discharge increased due to population growth, the Gray farm was expanded to
treat the increased hydraulic and nutrient mass loading. Eventually,  insuf-
ficient land was  available to adequately assimilate the hydraulic flow from
the SeWRP.  The  ground-water  elevation  which was normally greater than 30 m
from  the surface  rose  to  a depth  from 3 m to 22 m.  Associated with the
rise  in ground-water  elevation was a degradation of water quality (Table 1)
                                  18

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     Gray  site             [>-•^TT-.^-CUBSOC,.
     Existing irrigated  area  	'LUe*E*pMg?ti  COOMTY
Hancock site               '   -" ^'^~
     proposed  for irrigation
               EXPLANATION

               HH  OGALLALA ACQUIFER

               [~j  SOUTHERN.HIGH PLAINS

                     REGION

  Figure 1.   Regional Setting  for the Lubbock Land Treatment Research and
             Demonstration  Program
                                       19

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TABLE 1.   GROUND-WATER  QUALITY BENEATH GRAY FARM JUNE 1980 TO 1982

            Parameter                                Range
 Inorganics  (mg/1)
      Alkalinity                                   224-402
      Conductivity (umhos)                         1244-2882
      Total  Dissolved Solids (IDS)                 1010-2271
      pH                                           7.10-7.72
      Chloride  (Cl)                                208-680
      Sulfate (S04)                                149-795

 Nutrients (mg/1)
      Total  Kjeldahl Nitrogen (TKN)                0.28-6.97
      Nitrite plus Nitrate (N02/N03)               5.05-35.89
      Ammonia (NH3)                                0.02-2.05
      Total  Phosphorus (TP)                        0.10-3.49
      Ortho  Phosphorus (PO^                       0.01-0.84
      Organic Phosphorus (Or-g. P)                  0.08-2.31
 Organics (mg/1)
      Chemical  Oxygen Demand (COD)                 27.2-125.4
      Total  Organic Carbon (TOC)                   12.2-38.6
 Bacteria (per  100 ml)
      Total  Coliforms                                0-5669
      Fecal  Coliforms                                0-3002
      Fecal  Streptococci                             0-3601
 Dissolved Metals (mg/1)
      Aluminum  (Al)                              0.116-1.806
      Arsenic (As)                              <0.005-0.009
      Barium (Ba)                                 0.058-0.226
      Boron  (B)                                   0.653-3.671
      Cadmium (Cd)                              <0.001-0.004
      Cobalt (Co)                                <0.005-0.006
      Chromium  (Cr)                             <0.005-0.025
      Copper (Cu)                                <0.005-0.106
      Iron (Fe)                                   0.021-0.467
      Lead (Pb)                                  
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beneath  the farm.   In  November 1980,  construction began on  a  pump  storage
and distribution   system  to divert 50 percent of the total  flow  pumped to
the Gray farm to  the Hancock farm.  The Lubbock Land Treatment,  therefore,
consisted of two privately owned  farms.
     The total  land application  system encompasses 2967  ha.  The  Gray  farm,
located east of  the City of Lubbock (Figure  2)  has a total land  area of
1489 ha.   Approximately  1210 ha of the total area is cultivated. About 25
km southeast of  Lubbock is the  Hancock farm  (Figure 2).  The  land  area of
the Hancock farm is 1478  ha of which 1351 have been cultivated.  During the
five year period from 1977 to 1982, the Hancock farm    was  primarily  a dry
land farm with little ground-water  irrigation.
     The land application  system  receives secondary treated  wastewater  from
the City of Lubbock's   SeWRP.  The  SeWRP  consists  of two trickling filter
systems and an activated sludge system (Figure 3).
     Due to the predominately  agricultural economic base  for the  Lubbock
area, domestic  sewage  comprises the bulk of  the wastewater treated by
SeWRP.   Lubbock1 s  industrial sewage flow represented an estimated  30  per-
cent of the total sewerage flow.   In recent years, industrial wastewater
flow has been reduced  due to an  uncertain economy which  has  caused  several
industrial contributors to curtail  their operations or close  their plants.
     Monthly records on surcharge  contract industrial customers  were  main-
tained by Lubbock.  Data  did not exist on non-contract industrial  cus-
tomers.   Table  2 presents types  of industrial contributors  and correspond-
ing specific wastewater characteristics monitored by the  City  of Lubbock.
Average  high levels of chromium  (42 ppm) and nickel (17.2  ppm)  discharged
by an electroplating plant contributed the highest mass  loading of heavy
metals during the project  period.
     Industries on a surcharge contract with the city contributed approxi-
mately  22  percent of  the total  five day biochemical oxygen demand (6005)
mass loading and 15 percent of the  total suspended solids (TSS) mass load-
ing to  the waste water  treatment  plant.
      Trickling  Filter  Plant No.  1 (Figure  3)  has a hydraulic capacity
of approximately  2.3  x  10^  m-Vd  (6 mgd) .  The trickling filters  in  Plant
No.1  contain 2.1 m of plastic media.  Plant No. 2 was designed to treat  a
maximum  flow of 7.6 x 1Cn m-vd  (20 mgd).  Normal flow through Plant  No.  2
                                   21

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                                                         GRAY LAND
                                                     TREATMENT  SITE
          HANCOCK LAND
        TREATMENT SITE
            S«WRP

       •^™ FORCE MAIN

       + + + + DISPOSAL SITE
\
Figure 2.   Gray and Hancock"Land Treatment Site Locations
                                     22

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K5
                              Aeration
                     Lime p  Treatment
                                       Supernatant
                                           Return Sludae
                    	Grit
                    Screens Chamber
                        Primary
                        Clarifiers
Trickling   Secondary
 Filters    Clarifiers
                                          , Anaerobic Digesters
                                                                 	^"Digested Sludge
                                              ;  w   ^^  v^x I
                                 Primary
                                Clarifiers
                                        Trickling
                                        Filters
                                                                                                            Hancock
                                                                                                            Lagoons
                                                           Secondary
                                                           Clarifiers
                   Screens  Grit
                          Chamber
                                      Return Sludge
                                                        Plant Generator
                                                      Return Sludae
                                                    Aeration
                                                    Basins
                                                                  Secondary
                                                                  Clarifiers
Screens Chamber
         ol-*
                                                                                           Chlorine
                                                                                           Contact Chamber
                 	T	SJujlg^Thjckejw^^A^^^pigested Sludge	
                                                                 Hancock
                                                                  Farm
       Figure  3.   Southeast Water Reclamation  Plant  Flow  Diagram

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TABLE 2,   INDUSTRIAL  CONTRIBUTION  TO  THE CITY  OE  LUBBOCK SEWAGE SYSTEM
                          (Provided by City of Lubbock)

INDUSTRY CATEGORY
DAIRY INDUSTRIES
1*
2*
Total Flow
LAUNDRY INDUSTRIES
1*
2
3»
4
5
LARGE BAKERY INDUS.
1
2
Total Flow
BOTTLING INDUSTRY
1
M 2
•f> Total Flow
ELECTRONIC COMPONENT
1*
2
Total Flow
FIRE SPRINKLER
EQUIP. MANUFACTURER
FOOD INDUSTRIES
1*
2
3*
Total Flow
RESTAURANTS
1*
2*
3*
4*
Total Flow
COTTON MILLS
1*
2*
Total Flow
ELECTROPLATING
1
2
3
Total Flow
BOD
mg/1

1710
1950


2340
540
1170
160
210

180
240


320
330


100


50


1560

2160


1500
1110
1020
1800


600
367





COD
mg/1

2016
2256


3088
1424
2584
880










112


100


1840

2196


1864
2176
1132
1640


1152
330





GrtLASE
mg/1

125
313


525
450
400











250


50


50

0


475
500
200
575


0
79





PH

9.24
9.24


8.71
10.65
10.62
11.70
8.43

9.32
8.94


11.07
10.14


7.35


9.18


9.56

4.63


8.76
6.86
7.00
7.13


8.44
9.54

8.20
7.71
7.81

TSS
mg/1

421
1617


1531
744
842
299
113

237
191


215
33


26


84


759

363


297
444
447
393


187
80





Ho. Amt. Heavy Metal3 Cm9/1) Total Toxic
of Flow (m1) Fl Cr Ag Mi Cd Cu Zn Pb Fe Cn Organics

2952
2498
5450

3406
4542
4164

13,248

1325
1211
2536

6056
2157
8213

45,420
757
46,177 2.2 .0573 .039 .0008 .0397 .111 .0362 .40 .088 ppm
1892 .1486 .045 .0660 4.595 .424 .3520 1.40 0.0
,

10,018
1126
3026
24,981

2271

1514
1136
4920+

5678
34,065
39,742
946 42. 0§ 17.25 .44 .16 .06 1.9
189 .1188 .702 .0007 .25 1.48 .10 4.9
76 .204 .388 .022 .0845 .359 .138 1.02
1211 Continued

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         Table  2,  continued
BODs COD GREASE
INDUSTRY CATEGORY mg/1 mg/1 mg/1
PHOTO DEVELOPERS
1
2
Total Flow
LIVESTOCK FEED
INDUSTRY 2350 175
TSS
pH mg/1

8.57 1.0



7.49 938
Mo. Amt.
of Flow (m1'

151
189
341

37,850+
Metals (mg/1) Total Toxic
,F1- Cr Ag Ni Cd Cu Zn Pb Fe Cn _0rganics

.005
.0011



         * Designates industry is currently on contract with the City of Lubbock

           These concentrations are averages.  These concentrations have
           are well below City ordinance limits.

           Industry has digesters and pond —Not much flow to sewers now.
§ These concentrations are averages.   These concentrations have  been consistently  reducing during the past  six nonths (Fall,  1983)  and  all  levels
  are well below City ordinance limits.
VJ1

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ranged  from 3.0 x 104 to 4.9 x 104 m3/d (8 to 13 mgd) .   The depth of rock
media in the trickling filters was 1.8 m.  The majority of water pumped  to
the  Hancock farm  was treated by Plant No. 2.  Plant No.  1  provided most of
the water for the  Gray farm.
     Effluent  quality from the trickling filter system has been equivalent
to the composition of a  typical medium to strong untreated domestic  waste
water  (Table 3).  Effluent chemical oxygen demand  (COD)  has averaged 298
mg/1 and total Kjeldahl  nitrogen   (TKN) has  ranged  from  20 to 70  mg/1 .
Ammonia-nitrogen was the primary nitrogen form in the effluent stream.
     Treatment Plant No. 3 was an activated sludge system.   The activated
sludge  system had a maximum design hydraulic capacity of 7.6 x lO'V/d (20
mgd).  Effluent from Plant No. 3 was disinfected with chlorine.  South-
western Public Service  (SPS,  a power utility)  utilized the major portion
of the flow discharged by Plant No. 3.  A portion of the activated sludge
effluent was transported to the Gray farm.  The average  daily contribution
from the activated sludge system for irrigation was less  than five percent.
A total  wastewater discharge (approximately 5.5  x 10^m-Vd, 15 mgd) not
utilized by SPS was to be  divided equally  between the  Gray and Hancock
land application sites.
     The Gray  farm (Figure 4) occupies 1489 ha (3680 acres) of which 1210
ha (2990 acres) are irrigated.  There are four pipelines  which convey  water
from SeWRP to the  Gray farm.  Approximately, 1.48 x 10^m3 (1200 acre-ft)  of
wastewater storage capacity exists at the farm.  An estimated 50 percent  of
the  irrigated land employs center pivot irrigation machines; the remaining
agricultural land  is irrigated by flood or row irrigation.  The soil  types
dominating the Gray farm are primarily Acuff and Estacado loams (Figure 5).
These loamy soils  were found in calcareous, loamy eolian  deposits.
     The Hancock  farm was included in the Lubbock Land Treatment System to
reduce the hydraulic and nutrient overloading experienced at the Gray  farm.
Effluent from SeWRP is conveyed from a three-pump, pumping station through
25 km of 0.69 m force main.  The pumping station is located adjacent to the
existing effluent pumping  station at  the Lubbock SeWRP (Figure 6).  The
pumping station and the force main were designed to accommodate a flow  of
2.8  x  10V (7.4  mgd) utilizing two pumps.  The third pump was provided as
a backup unit.
                                    26

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TABLE 3.  TRICKLING FILTER SYSTEM EFFLUENT CHARACTERISTICS
     SOUTHEAST WATER RECLAMATION PLANT,  LUBBOCK,  TEXAS

Parameter
Alkalinity (mg CaC03/l)
Conductivity (pmhos/cm)
TDS (mg/1)
PH
Cl (mg/1)
504 (mg/1)
TKN (mg-N/1)
N0~ + NO (mg/N/1)
NH3 (mg-N/1)
TP (mg-P/1)
P04 (mg-P/1)
Org P (mg/1)
COD (mg/1)
TOC (mg-C/1)
Mean
335
2199
1671
7.56
450
309
42.42
0.28
25.75
14.13
8.25
4.86
298
114
Standard
Deviation
34
295
538
0.23
164
50
40.57
0.30
6.62
4.42
2.07
4.24
134
47
                           27

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ho
CO
                                                                                          Pipeline
                                                                                          Water
                                                                                          = 0.27 km
      Figure 4.  Gray Farm Land  Treatment  Site

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                                                                                                                                     Reproduced from
                                                                                                                                     best available copy.
                                                                                                                       LEGEND
                                                                                                                                              Oncrlptton

                                                                                                                               01 ten clay !«•. 0-11 ur4

          Acuff IOM. 1-Jl dopes.  Dec*, gently sloping leu* end
            city loin; nodtriuly to wderately slowly peraeiblt
            subsoils: slight to noderite Kind ut*r end fertility holding capacities

          Hansker loam. 1-31 slopes.
          Posey fine sandy loan. 0-11 slopes.  Level In f""» sloping
            loans and fine sandy loans;  Moderately pemelble sutrsolls:
            soft caliche «llhln 20 Inches: noderate  »lnd erosion hiiard,
            noderate water erosion haiard on slopes
                   Figure   5.     Soil  Types  on  the  Gray  Farm

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                 J
 PLANT 1
 SECONDARY
 CLARIFIERS
   EXISTING
   SUMP
\

1


1
^
/
M:I
'•'•'•
•cjij

PLANT 1
IISCHARGE
<




•^ *•• M*^^«B ^
•^•^


|

1C*1
^
1
1
1
1
1
1
;

_ /
-'
                                        PLANT 2
                                        DISCHARGE
    HANCOCK
    PUMP STATION
                           EXISTING
                           PUMPS
69cm FORCE MAIN-
Figure 6.  Location of New  Pump Station to Existing Plant
                       30

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     At the northern boundary of the Hancock farm, the effluent is routed
through three  0.38  m  plastic  pipelines to three separate reservoirs (Figure
7).   The  reservoirs  were constructed on natural playa lakes.   Reservoir  1
(eastern  reservoir)  had 1.53 x 10^m-^ of storage.  The storage capacity of
Reservoir .2 (central  reservoir) and Reservoir 3 (western reservoir)  was 6.9
x 10^m^  and 7.36 x  10^m^,  respectively.   Irrigation pump stations were
provided at each reservoir.
     The  irrigation system  was designed  to irrigate 1153 ha with 991 ha
irrigated by center pivot irrigation machines.  Two loops were  used to dis-
tribute  the water to  each pivot.  The two .southernmost piplines,  however,
required two high head booster pumps with one  located  at  Reservoir 1 and
one  at Reservoir 3.   Each center pivot had a centrifugal booster pump. The
booster  pumps increased  the  line pressures from 1.8 x 10° pascals  (26 psi)
to  an operating level of 3.1 x 10° pascals (45 psi). Each center pivot was
designed to irrigate  up to 15 cm in 20 days after allowing  for 20 percent
loss due to evaporation.   Without the use of the reservoirs, five to six
center pivots could be operated at the same time, utilizing the flow pumped
directly from Lubbock's wastewater treatment plant.
      The Hancock land application system was designed to operate at design
capacity immediately upon  completion of construction and system  startup.
Basic design information  for  the primary lift station, distribution piping,
shortage reservoirs,  and  irrigation system is provided in Table 4.
      The City of Lubbock's wastewater discharge  permit  required a 46  m
buffer zone along the northern boundary of the farm.  In addition,  a 400  m
buffer zone was established immediately north  of the city  of  Wilson.  No
spray irrigation was  permitted within these buffer zones.  Plastic  tubing  3
m x  1.3 cm (9 ft x 1/2 in) was attached to the nozzles  on  pivots affected
by the buffer zone in order to furrow irrigate these areas.
     Prior to 1982,   the  Hancock farm was primarily a dryland,  cotton farm.
The  soils on the  farm are  of the Amarillo series (Figure 8)  which were
formed in calcareous, loamy eolian deposits. In dry climates where evapora-
tion  exceeds precipitation  resulting in long periods of dry  soil, ground
water slowly migrates to  the  surface by capillary attraction  and  evapor-
ates. Dissolved calcium salts contained in the ground water precipitate and
form calcium deposits near the surface of the  soil.   These deposits are
                                  31                                  I

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                             fFurrow Irrigation





                            (^Distribution Can




                              Pipeline
Figure  7.   Hancock Farm Land Distribution
System
                                        32

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       TABLE 4.  BASIC DESIGN INFORMATION FOR LUBBOCK LAND TREATMENT
                     SYSTEM EXPANSION (HANCOCK FARM)
Primary lift station

     Design flow is 2.8 x loV/d (7.4 mgd)
     3-Vertical turbine pumps 1 1.4 x 10%i3 (3.7 mgd) each

Distribution piping
     25 km (15.5 mi) of 0.69 m (27 in) force main
     26 km (16 mi) of 0.38 m (15 in) plastic irrigation pipe

Storage reservoirs
     Cell #1 - 1.5 x 106m3 (1243 ac ft) with irrigation pumps:
          11.4, 13.6, and 7.6 m3/min (3000, 3600, and 2000 gpm)
     Cell #2 - 6.9 x 105m3 (560 ac ft) with 1 irrigation pump:
          12.2 mVmin (3500 gpm)
     Cell #3 - 7.4 x lO^m3 (597 ac ft) with 2 irrigation pumps:
          7.6, 7.9 mVmin (2000 gpm)

     Total storage is 2.96 x 1O6 x 106m3 (2400 ac ft)

Residence time is 3 1/2 months

Total Storage _    2.96 x 106m3
                  1 .8 x 104m3/day
Irrigation Site

     Land area irrigated is 1153 ha (2850 ac)
     1082 ha (2673 ac) are irrigated by center pivot
     72 ha (177 ac) are irrigated by furrow technique
     Primary crop is cotton

Irrigation Equipment

     Center Pivot

          305-469 m (100-1540 ft) radius
          4 m3/ha . hr (7.1 gpm/ac) application rate
          Maximum intensity § end of pivot is 6.1 cm/hr (2.4 in/hr)
          80-85 percent efficiency

Furrow Technique

     Risers set at locations requested by owner
     Low head gated pipe with gates on 1 m (40 in) centers
     Gate delivery rate is 5.6 to 9.1 m3/hr (25-49 gpm)
                                  33

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                     Ao Aifwrill
                     Ab Arrarill
                     Ac Amor, 11
                     Ad Axorlll
                     C. Church
                     P« P*rf«l«
                     Pk P.rl«l«
                     PC P*rt«l«
                     H P..t«l«
                     >. l.it^U
                     Za Zf'« fl»«	T •
                     Ic III. l*mm 0-1 S
f in« tondy !•« n 0 1 % «lop«
fin* — dy l««™ 1-}%ll**«
(••fit 0*1 ^ fll«p*
 «m l-3\ •!•*.
fin* i.nWr iMm O'l % >!•••
fl»« I«R^T !••»> 1-3 % •!•*.
l«-o 0-1 * •!••.
IMOT 1-3 % •!.*.
Figure 8.   Soil Types on the  Hancock  Farm
(Environmental Assessment, Lubbock Land
Treatment  Research  and  Demonstration  Project,
Scheaffer  and  Roland, Inc.)

                                            34

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referred to   as  caliche   and are present  within the  upper 1  m of the soil
profile on both  the  Gray  and Hancock  farms.

FACILITIES COMPLETION
     Facilities to  convey, irrigate,  and store wastewater from SeWRP were
completed as designed  by  July  1981.   On December 21, 1981, the City of Lub-
bock  was issued  the  final  wastewater  discharge  permit.  The permit re-
quired the installation of  an  additional 30  cm  of clay in the bottoms  of
each  reservoir.  Furthermore, construction of all facilities were  to  be
approved by the  Texas  Department of Water Resources (TDWR)  prior to  their
use.  Since the  system  could be operated without reservoirs, the TDWR ap-
proved the irrigation  directly from the distribution line.  Once the  addi-
tional 30 cm of  clay material  was installed  in a reservoir, TDWR  inspected
and approved the reservoir.  After having obtained State approval, the res-
ervoirs were placed  on-line. Reservoir 1  was completed  and  place on-line
April 13, 1982.   Reservoirs 2  and 3 were put into service  in September and
October, 1982, respectively.

SYSTEM EVALUATION
     During the  1982 irrigation season for the  Lubbock Land Treatment Sys-
tem Expansion, a critical evaluation  of the  system's performance was  con-
ducted.   The following  discussion  is presented to create an awareness  of
good engineering design  and certain aspects  of  the system which hindered
the successful operation  of this particular  treatment system as designed.
Primary Lift Station and  Force Main
     A 69 cm  diameter force  main, 25 km long, was the most cost effective
means to transport water  to the Hancock farm.  The effluent pump station  at
the  Lubbock  SeWRP  had  three 30 cm  vertical  turbine  pumps  with electric
drives.   Each  pump had  a capacity  of  1 .4 x 10^m-Vd (3.7 mgd) at 36.6 m
total dynamic head.   The  pumps were alternated in use to maximize the  com-
bined service life.  The  pump   station was   interconnected to   the existing
107 cm discharge line  from  trickling  filter  plant 2 (Figure 3). The exist-
ing effluent line  entered an existing  sump which collected water from
trickling filter  plants  1  and 2.  An assumption was made in the  design
                                  35

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 that the new  sump   would  have  first priority for  effluent  water  produced
 by   plant 2 and therefore,   would  maintain a  sufficient  water  level to
 continuously   operate  a minimum   of  two pumps.   This  would  insure  the
 transport of an average flow rate of 2.8 x 10V/d (7.4  mgd)  to the  Hancock
 farm.    Review of historical hydrographs data  for  each month,  however,
 indicated during the  month of  July insufficient effluent  was available to
 pump 2.8 x 104mVd  (7.4 mgd) to the Hancock farm.   Furthermore, the daily
 variation  of flow through  each  plant due to the  management of  water  be-
 tween the trickling  filter  plants 1, 2,  and the  activated  sludge system to
 accommodate Southwestern Public Service (SPS)  water needs reduced flow
 through  the  trickling filters from 2:00 a.m.  to  10:00 a.m.  each day to
 only 315 m3/hr (2.0  mgd).   The  pump capacity and sump were not designed to
 absorb the variations in flow from the trickling  filter  plant.  Consequent-
 ly,  the dynamic nature of the effluent  hydrograph  made  it impossible to
 operate  two pumps for more than  16 hours  each day. Therefore, the resultant
 average daily  quantity of effluent transported to the  Hancock  farm was
 approximately 1.7 x 10^m .
      The pump motors  were controlled by  float  switches.  The design of the
 sump  created vortexing  at  the float  switches,  which peridically  caused
 tangling of float lines.   The entanglement  of lines caused the control
 mechanism to switch off the  electrical drives.
 Irrigation Distribution and Application System.
      Irrigation at the Hancock farm  was  accomplished  primarily by electric
 drive center pivot irrigation machines.   A major  advantage of the  center
 pivot is lower labor  requirements than  other  methods.  In addition to the
 22 center pivots, 33  risers  were installed to  furrow  irrigate area  not
 irrigated by the pivots.
     Each center pivot machine was  isolated  from the distribution network
by a 20 cm  electric butterfly valve.   This  valve  was  located  on the suction
side  of  each  booster  pump.   A control system's  electric actuator, located
above ground, automatically opened  and closed the valve upon receiving a
signal from  the  center pivot.  The  valve  closed automatically when the cen-
ter  pivot shut down.   The pivot  could be  shut down manually or due  to  low
temperatures  (less  than 3°C),  low  pressures, and/or towers not  in proper
                                  36

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alignment.
     In-line  strainers  were placed between the centrifugal booster pumps
and the center pivots to  reduce  clogging  of  the spray nozzles.  The strain-
ers were  0.91 m long with  4.8 mm  diameter perforations.  A totalizing flow
meter  was located between the in-line strainers and the bottom elbow on the
center pivot riser pipe.
     The spray nozzles on each irrigation machine were on drops located 3.2
m apart.  The size of the nozzles  varied  from 2.4 mm  (3/32 in) to  7.1  mm
(9/32  in).   Nozzles were positioned a  distance of 1.2 m to 1.8 m above the
ground which allowed easy "maintenance of  the nozzles.
     In addition, end guns  were  provided  on  each pivot to irrigate the cor-
ners.   Calculated high operating pressure  requirements  for the end  guns
necessitated the installation of a small  booster pump.
Automation—
     Automation was employed in end gun  operation, drain valves, and pivot
operation to minimize  labor  requirements  and system   damage.  Automatic
drain  valves  were  located  on  the booster  pump housing,  between the flow
meter  and bottom elbow on the center pivot  riser pipe, and near the  bottom
elbow  (underground) between the butterfly valve and pump inlet on the suc-
tion line.  These valves  were designed  to open when pivot operation ceased;
and thereby, automatically draining the pump and lines.  This would prevent
pump and pipe damage during  freezing temperatures.  Conceptually, automa-
tion has definite advantages in  the protection and ease of operation of the
distribution  and application system.   The majority of automation incorpor-
ated into the system, however,   was not designed to function properly while
while transporting water  containing particulates.
     The drain valve on the booster pump  was actuated by a solenoid. During
system operation, suspended solids in the wastewater  stream were concen-
trated in the valve opening, and consequently, caused the valve to malfunc-
tion.   The valves would either remain open or closed.  Due to the undepend-
able operation  of  the solenoid actuated drain valves, the valves were re-
moved  and replaced with  manual  ball valves.  This manual operation in-
creased labor requirements; however, it was  more dependable.
     End guns  were located on  each pivot  to  irrigate  a portion  of the
corners  of  each quarter  section of land.   The calculated pressure require-
                                  37

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 ment of the  end  gun dictated  the installation  of booster pumps.  The
 gun  operation and booster pump were controlled  from a pivot collec
 located near the top elbow of the pivot  riser pipe.  Changing the plastic
 cams under  the collector ring would alter  the operating location of the end
 gun.  This automation was included to  prevent water from being applied to
 roads and  field boundaries.
      Sand  traps were located prior  to each end gun booster pump. Sand traps
 removed  sand and gravel which would damage the pump.  Figure  9  shows  the
 position  of the sand traps  on  the cantilevered  portion extending past the
 last tower.  The boo-ster pumps were  attached  directly  to  the top  of  the
 sand traps  (Figure 10).
      During system operation,  particulates transported through the booster
 pumps impinged on a conical screen  which was approximately  25 mm long  and
 had  a 9.5 mm opening.  The screen  was part of  the valve assembly (Figure
 10).  The  mesh size of the screen   was about  150 or 200 openings/inch (106
 to 75 urn) A solenoid opened   a valve   which  controlled  water  passage
 through  the screen to a diaphragm.   Water  pressure  depressed  the dia-
 phragm which forced open the  main  valve to the  end  guns.   Particulates
 impinged on the screen and  plugged  the pores; thereby,  increasing the head-
 loss across the screen.   When the solenoid valve was actuated, insufficient
 pressure was transmitted  to  the  diaphragm. Consequently, the valve remained
 closed and failed to allow  passage of water to the end  guns.   Furthermore,
 particulates lodged in the valve to the end guns or the solenoid valve pre-
 vented proper  closure of  valves; therefore, allowing some end  guns to water
 roads. This problem was  eliminated by removing the solenoid  and diaphragm
 valve assembly and  installing  a manually operated ball valve (Figure 11).
 A  pipe extension was  attached to operate the  valve  from  the ground.   In
 addition,  adequate pressure was  maintained  without  the booster  pumps to
 satisfy  proper end gun   operation  requirements.   Therefore,   all  booster
 pumps were  removed.
     Automatic drain valves located on the  bottom elbows  on the center
 pivot riser pipe,  also, failed to open or close due to solids jamming  the
valves.  These  valves were removed  and  the hole plugged.   Manual gate
valves were installed  to  drain the riser pipe.  A hose  was attached to  the
valve  and  the  water was  piped to  the  field during  draining  to  prevent
                                   38

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MD
                                                                    T
      DETAIL "A"
                                 SAND  TRAP —
         Figure 9.    Overview of Sand Trap and Fittings for End Gun

-------
                                                        BOOSTER
                                                      /PUMP
                                 ASSEMBLY
                                  VALVE
                                    SAND TRAP	!
Figure 10.  Breakdown of  Booster  Pump and End Gun Assembly,
            as Originally Installed
                         40

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                    BALL VALVE
Modifications Made to Some Center Pivot Irrigation Machines




                       41

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 accumulation of water around  the  pivot pad.
     Automation of the 20 cm  electric butterfly valve controlling  the flow
 of  water to the entire pivot  is essential.  Flow from the distribution line
 to  the pivot must be stopped  whenever the  center  pivot  shuts down. With
 proper electrical adjustments, this control mechanism has operated success-
 fully.

 Screens—
     In-line  screens were installed between the booster pumps and the cen-
 ter pivots to remove particulates  which would clog the spray nozzles.  The
 screens  consist  of 1  m long conically  shaped steel with 2.4 mm diameter
 perforations.  The perforations correspond  to the smallest  sprinkler head
 orifice.  Prior  to designing the  in-line screens and specifying their
 appropriate location, the consulting engineer requested the City of Lubbock
 to  install screens at the primary lift station.  The City engineers, how-
 ever, failed to see the need  for  screens at the  pump station.  In  retro-
 spect, operational problems   might have been  minimized if screens had been
 placed at the pump station.
     Figure  12 shows  the location of the screens.  The mild stock metal
 used to construct each screen corroded within six months.  Several screens
 broke  free from their  retaining rings and damaged  flow meters. The screens
 should be constructed of stainless steel or a non-corrosive material.  Fur-
 thermore,  the metal  ring employed to retain  the screens in position needs
 to be continuously welded  to  the screen and not spot welded.
     The impact  the proximity of the screen to flow meters would have on
 flow measurements was  not  evaluated.  Hydraulic turbulence  created  by  the
 screens reduced the  flow reading from 15 to 75 percent of estimated values.
 Proper installation  of  flow meters specifies the device should have  been
 placed five  pipe diameters before and 10 diameters after  any device which
 can alter the  hydraulic  flow regime.  Figure 13 shows the present  location
 of the flow meters to comply with  installation specifications.
 Concrete  Support  Pads—
     The  center pivot booster pump was supported by a concrete slab with no
thrust  blocking.   A  concrete pad with footings supported the pivot  (Figure
 14).

                                  42

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                                                              SCREEN
Figure 12.  Relation of Screen to  Flow  Meter  as Designed and  Installed

-------
Figure 13.   Position  of Flow Meter to Achieve  Proper  Operation
                               44

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Figure 14.  Concrete Pivot Pads

-------
      Thrust created during pump startup  and back pressure created from in-
 creasing  head  losses through the in-line  screens and  nozzles caused  the
 pump support  pad to settle and move  away from the pivot.  The movement of
 the pad  was  enhanced by supersaturated soil conditions surrounding the  pad
 resulting  from  the draining of the pump and irrigation machine.  This mo-
 tion of  the  pad caused improper  alignment of the coupler between motor  and
 pump and  the discharge side of pump and pipe leading to the pivot.  To rem-
 edy the  problem, thrust blocking was  placed on  the side  of  the pump  pad
 (Figure  15).   In addition,  concrete was poured between the  pivot  pad and
 the pump  pad.  The bridging slab helped prevent  settling  of  the pump  pad
 and provided  firm footing  for  access and maintenance of in-line screens.
 Construction of a unified foundation to support both pivot  and pump  (Fig-
 ure 16)  would have avoided  the problem.
 Spray Nozzles—
      Spray nozzles were attached  to drops and were positioned  approximately
 1 .8 m from the ground surface.   The position of the nozzle  was predicated
 on ease  of maintenance,  spray intensity and spray pattern.   Nelson® nozzles
 were installed.  Figure 17  illustrates normal installation of  Nelson® noz-
 zles.  In this position,  the nozzle provides a 360°,  downward spray pat-
 tern.  The nozzles, however,-  were  inverted and  attached  to  the drops as
 shown in Figure  18.   The  energy dissipating,  deflector incorporated into
 the nozzle assembly was  a concave plastic plate  (Figure 19,  Type 1).  The
 water discharged  through  the orifice was deflected  upward once it  struck
 the deflector.  The design enhanced the creation of aerosols.  Upward  move?-
 ment of  water  increased drift and evaporation of water;  thereby, reducing
 the  amount of water actually  applied to the land.   The U.S. Dept.  of Agri-
 culture,  Soil  Conservation Service, evaluated  Type  1  and Type 2 deflectors
 to  determine the application  patterns  and water  applied  to  the soil.  A
 convex deflector   (Type 2, Figure 19)  directed  the  water downward, reduced
 drift, and produced  a 25 percent  increase in total  water  applied  to  the
 soil.  Convex deflectors have been installed  on  most nozzles.
     Pressure regulators were  installed before  nozzles  (Figure  18) on
 pivots which had  sufficient variation in the  terrain  to  cause changes in
operating  pressures.  The small clearance between the  energy dissipator in
the  pressure regulator  and  the regulator's outlet orifice caused a  rapid
                                  46

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Figure 15.  Modifications Made to Stabilize Pads

-------
CO

                                         ,
                  •«'*»' •  '.0  '.
                   V.'»
                  2» .• "-
                      . •f
                 •' .  o-
                                                                         *  e
              Figure 16.   How Pad Could Have  Been Poured to Avoid Stability Problem

-------
     PRESSURE
     REGULATOR
                                                 -NELSON SPAY NOZZLE
                                                   — PIPE
Figure 17.   Nelson  Spray Nozzles as They Were Designed to  be  Installed

-------
        PIPE —
            PRESSURE
            REGULATOR
                                                         -DROP
                                                          WITHOUT
                                                         'RESSURE
                                                          EGULATOR
                                                          SED AT
                                                         IANCOCK
                                                          FARM)
                               -NELSON SPRAY
                                  NOZZLE
Figure  18.  Actual Inverted  Installation


                              50

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                  Type 1
Type 2
Figure 19.  Types of Splash-pans Available
                             51

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 entrapment of  solids.   No effective  means of cleaning  the  regulators  in
 place  was available.  Consequently,  these  regulators were  removed.   No
 appreciable difference  was observed in spray coverage after removal  of the
 pressure regulators.
 Reservoirs.
     The  reservoirs were  designed not only  to  provide  emergency storage
 during rainfall events,  but also  to prevent the  necessity of  irrigating
 during periods of   cultivation,  seeding,  and harvesting  of  crops.   An
 equivalent of one  month's   storage was calculated  to be sufficient for
 emergency storage.   An additional three  month's storage was designed  to
 contain water during crop planting  and harvesting.
     Reservoir dike walls  were  constructed  from onsite soil  materials.
 Slope  stabilization  consisted of decreasing  the slope from 3:1  (original
 design) to 4:1  and seeding  with bermuda  grass.   These  methods  were selected
 primarily due to lack of funds.  Severe  wave actions  within the reservoirs,
 however,  eroded the existing slopes.  A properly  designed riprap is  recom-
 mended for adequate  slope stabililty.
     The pump station located at Reservoir 1  (eastern  reservoir)  had  a var-
 iable speed (lead) pump  and  a constant speed (lag) pump to maintain con-
 stant  pressures throughout  the system.   Both pumps were controlled by sys-
 tem pressure and discharge  flow rate.  The flow transmitter shut down the
 lag  pump  when  the lead pump  demand decreased by 7.6 m-Vmin.  The flow
 controller was  designed  to stop the lead pump when the demand  was less than
 0.76 mVmin.   Figure 20   shows  the  placement   of  the flow transmitter
 depicted  in  the as built drawings.   The  location  of the transmitter  failed
 to comply  with  installation  procedures  as  described  in the manufacturer's
 manual  (i.e.,   10 pipe  diameters of  straight   pipe should precede the
 meter  and  five  pipe diameters  of  straight pipe  after  the meter). Less than
 one meter  of straight pipe existed prior  to  the  sensor.  According to manu-
 facturer   specifications,  approximately  five  meters  of  straight pipe was
 required   before  the sensor.  Consequently, erroneous readings were ob-
tained.  Once the transmitter was  correctly  located, it was determined that
small debris and hair would  hinder or prevent  the impeller   from moving.
Flow  transmitters (utilizing sonic  or venturi sensors) capable of operating
                                 52

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Ul
                            PUMP  STATION
                            RESERVOIR  1
              Figure 20.  Improper Installation Diagram from "As Built Drawings"

-------
in water streams  containing suspended debris should have been used.  Figure
21 shows the  proper  installation of the flow transmitter  as described in
the manufacturer's manual.
                               54

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                        To Distribution Can 1
                                     Pump Station
                                     Rvservolr 1
Figure  21.   Proper Installation of  Flow Transmitter  as Described
             in the Manufacturer's Manual
                                55

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                               SECTION 5
                           MONITORING APPROACH

     "The  Lubbock Land  Treatment Research  and Demonstration  Project"
involved the comprehensive  characterization of  the  chemical, physical and
biological conditions of water,  soil and  crops two  years prior to  irriga-
tion (baseline period) and two years during irrigation of the Hancock  site.
A sampling scheme was designed  to  adequately represent the entire land
application  site  while maintaining a manageable analytical load.   Water
samples consisted of applied  effluent and  ground water.  Soil and crop
samples were obtained from each pivot or field.  • Locations of the  soil and
crop  samples were initially randomly  determined  within a field or  plot.
The same locations were sampled each year.
     Water,  soil  and  crop samples were each  analyzed for approximately 80
chemical, physical and biological  parameters.  A parameter was included  in
the monitoring program if it was related to:
     1.   Federal  and State of Texas drinking  water  standards;
     2.   Toxicity to plants;
     3.   Potential accumulation in soils;
     4.   Potential human health risk; and
     5.   Nutrient mass balance.
     The objective of  the monitoring scheme was to establish a data base
characterizing conditions at the Gray  and Hancock farms  that would allow
the detection of  any changes  which might occur  in the ground water, soils,
and crops due to reduction of  sewage effluent  loading at the Gray  farm and
use of sewage effluent at the Hancock farm.   The specific objective of the
monitoring program was  to  characterize  the  chemical,  biological and
physical  conditions of water, soil and crop  samples collected from  the
Gray and Hancock farms.
     The project  monitoring  period  was divided  into  two phases.   The
baseline monitoring period extended from June  1980 to February 1982 prior
to transport  of effluent  to the  Hancock farm.  Once water was diverted from
the Gray farm to the Hancock  farm  in February  1982,  the irrigation monitor-
ing period  began  and samples  were  obtained until the fall and early winter
of 1983.
                                  56

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HYDROGEOLQGY
     The objective  of  the hydrogeologic investigation was to   determine the
effects on the quality and  quantity of ground water caused by using  treated
sewage  effluent  for  irrigation.  Data consisting of water levels  and  water
quality parameters  were obtained  from June, 1980 through October,  1982.
Monitoring Wells
     Underground water at  the  Gray and  Hancock farms was  monitored each
year at after spring  pre-irrigation (April), the end of  summer  irrigation
(August), and winter  (December).  Underground water samples were taken from.
monitoring wells  constructed  by  the project, pre-existing irrigation wells,
seeps  and springs at the  Gray  farm, and drinking water wells of  residents
on  or  near  the  Hancock farm.   Table  5  gives  the number  and  types  of
ground-water monitoring  .wells  at  each site.   Sampling locations  were
selected using hydrogeologic  data in order to best monitor the movement and
quality of water on  the farms.  Figures 22, 23 and 24 show the ground-water
monitoring location for each  site.  Table 6 lists the wells and  completion
data for most of  the  wells  monitored during the project.
Non-Contaminated  Well—
     One  well was  constructed at each site (Gray Farm - Well 6894;  Hancock
Farm - Well 10542)   in a manner  to minimize priority organic  pollutant con-
tamination of the aquifer during the construction phase.  The wells were
dug to the bottom of  the ground-water table with a cable  tool  using  dis-
tilled  water (VOP  1966).   Stainless steel pipe, 20.3 cm (8 in)  in diameter
was used for casing.   Three meters (10 ft) of stainless  steel well  screen
were attached to  the bottom of the  casing.  No special precautions were
taken with the driller's tool beyond rinsing with distilled water. The zone
between  the  well  casing   and wall  of the well hole  was left  void.  In
retrospect the void space between the well casing and the  borehole  should
have been filled with cement from the top of the ground-water table to the
ground  surface.   A  1.2 m x  1.2 m   (4 ft x 4  ft) concrete pad  was  poured
around  the casing. The casing  was cut off approximately  20.3  cm (8 in)
above ground and  covered with a  locking metal box.

                                   57

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 TABLE 3.   TYPES OF UNDERGROUND WATER SAMPLING POINTS BY SITE
 No.  of
 Wells                   Type  of Soil

                         Hancock Farm
  1        Organic Non-contaminated Well  20 cm  (8  in)
  5        Continuous Water Level  Recording Wells   20  cm (8  in)
  3        Non-continuous  Recording Observation  Wells   10 cm  (4 in)
 15        Pre-existing Irrigation Wells (currently  in  use)
 14        Home Drinking Water Wells

                          Gray Farm
  1       Organic Non-contaminated Well  20 cm (8 in)
  5       Continuous Water Level Recording  Wells  20 cm  (8 in)
11       Non-nontinuous  Recording Observation Wells  10 cm (4 in)
10       Pre-existing  Irrigation Wells  (currently in use)
 1       Multiple Depth  Well [includes four,  12.5  cm (5 in)  wells]
11       Seeps,  Springs  and  Retention Pond Overflows
                           58

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MD
                                                                                  '	' = O,27 km
                                                                                  —••• Boundary
                                                                                      Road
                                                             NON-CONTAMINATED

                                                                 WELL
        Figure 22.   Gray Farm  Groundwater Monitoring Locations

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                      GROUND WATER
          20243
10212
T -

             30312
                  Reservoir
              ------ Playa Lake
               •  Well
              — Boundary
              	Road
                    = 0.27 km
                                                         NON-
                                                       CONTAMINATED
                                                     _J  WELL
 Figure 23.  Hancock Farm Ground Water Monitoring Locations

                                 60

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                                DRINKING WATi
                    Sampling
                    Location
/ Road
Hancock
Farm
.  0.62 km
   Scale
Figure 24.  Hancock  Farm  Drinking Water Sampling Location

                                   61

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Well
Nimber

6880
6881
6882
6883
6884
6885
6886
6887
6888
6889
6890
6891
6892
6893
6894
6895A
6895B
6895C
68950
6896
7000
Date
Drilled
	 • 	

5/80
5/80
5/80
5/80
5/80
5/80
5/80
5/80
5/80
5/80
5/80
6/80
5/80
5/80
MA
8/80
8/80
8/80
8/80
5/80
NA
Casing bize >
cm (in)
	 	 •
GRAY
10.2 (4)
10.2 (4)
20.3 (8)
10.2 (4)
20.3 (8)
20.3 (8)
10.2 (4)
10.2 (4)
10.2 - (4)
10.2 (4)
10.2 (4)
10.2 (4)
20.3 (8)
10.2 (4)
NA
10.2 (4)
10.2 (4)
10.2 (4)
10.2 (4)
20.3 (8)
NA
U UdJ. i^v|- -• -
m (ft)
	 	 	
SITE
39.6 (130)
40.2 (132)
42.7 (140)
44.2 (145)
35.7 (117)
36.0 (118)
34.7 (114)
35.1 (115)
36.0 (118)
31.1 (102)
36.0 (118)
*NA
34.7 (114)
37.2 (122)
NA
39.6 (121)
22.9 ( 75)
11.3 ( 37)
32.0 (105)
36.9 (121)
NA
m
__ 	 • —



33.5 - 39.6
34.1 - 40.2
18.3 42.7
38.1 44.2
11.3 35.7
11.6 36.0
28.7 34.7
29.0 - 35.1
29.9 -' 36.0
25.0 31.1
29.9 36.0
NA
10.4 -
31 .1
33.5 -
16.8
2.7
25.9
12.5

34.7
37.2
NA
39.6
22.9
11 .3
32.0
36.9
NA

(ft)
— — — — — —

—

(110 130)
(112 132)
( 60 140)
(125 - 1*5)
( 37 - 117)
( 38 118)
(94 114)
( 95 - 115)
( 98 - 118)
( 82 - 102)
( 98 - 118)
( 34 -
(102
(110
( 55
( 9
( 85
( 41

114)
122)
130)
75)
37)
105)
121)

HANCOCK SITE
10112
1021 1
10232
10413
10521
10541
10542
10721
10731
10821
10842
10931
10932
1 1032
20112
20243
20711
20721
20842
21141
21152
21234
21323
30312
40231
40311
40331
40421
4/80
4/80
NA
NA
5/80
NA
NA
4/59
1/82
2/68
NA
1/82
NA
NA
5/80
4/80
NA
5/80
NA
5/80
1/82
3/61
NA
3/60
NA
NA
5/80
NA
10.2 (4)
10.2 (4)
NA
NA
20.3 (8)
NA
NA
32/4 (12.75)
10.2 (4)
21.9 (8.625)
NA
10.2 (4)
NA
NA
20.3 (8)
10.2 (4)
NA
20.3 (8)
NA
20.3 (8)
10.2 (4)
16/8 (6.625
NA
25.4 (10)
'NA
NA
20.3 (8)
NA
43.2 (142)
46.6 (153)
NA
NA
31.4 (103)
NA
NA
32.3 (106)
28.7 ( 94)
37.2 (122)
NA
26.8 ( 88)
NA
NA
47.5 (156)
54.3 (178)
NA
32.6 (107)
NA
36.9 (121)
29.0 ( 95)
29.9 ( 98)
NA
35.7 (117)
NA
NA
34.7 (114)
NA
37.1 -
40.5 -

25.3


23.8
16.5
24.1

14.6


35.4
48.2

26.5

24.7 -
12.2
22.3

22.9


28.7

43.3
46.6
NA
MA
l\H
31 .4
NA
MA
l\ A
30.8
28.7
36.3
NA
26.8
NA
NA
47.5
54.3
NA
32.6
NA
36.9
29.0
29.9
NA
35.1
NA
NA
34.7
NA
(122
(133

( 83


( 78
( 54
( 79

( 48 -


(116
(158

(158 -

( 81 -
( 40
( 73

( 75


( 94

142)
153)

103)


101)
94)
119)

88)


156)
178)

178)

121)
95)
98)

115)


114)


*NA   Data  Not Available
                                      62

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Multi-depth  Well--
     Four  wells  (6895-A through 6895-D)  were  drilled within 0.7 m (2 ft)  of
each other at  the Gray site using the rotary  drilling method (Bonner 1978).
The  wells were  completed to depths of 11.3 m (37  ft), 22.9 m (75 ft),  32.0
m (105 ft),  and  39.6 m (130 ft).  PVC casing, 12.7 cm  (5  in)  diameter was
installed to  the top of  the  desired interval  and cemented in place.   The
cement plugs were subsequently drilled  out  and 10.2  cm  (4 in) diameter,
perforated  PVC liners were installed in the well sections   to be sampled
(Figure 25).  A  concrete pad was poured  around the top   of each  well  to
protect  it  from surface  contamination.   The  well casings were  cut  off
approximately  20.3 cm  (8 in) above  ground and covered  with locking  PVC
caps.   Sampling intervals are given in Table 7.  The sampling section   of
well 6895-A was  entirely  in the underlying bed rock.  Consequently, low
permeability presented considerable sampling  difficulty.
         TABLE 7.  SAMPLING INTERVALS FOR MULTI-DEPTH WELL  (6895)
	GRAY SITE	

     Well Designation                      Sampling Interval

          6895-C                                  9 -  37 ft
          6895-B                                 55 -  75 ft
          6895-D                                 85-105 ft
          6895-A                                 110 - 130 ft
Water Level Recorder  Wells—
     Five  wells  were constructed  at each  site  to obtain continuous water
level  records.   These wells   were drilled   by the  rotary method.   A
perforated PVC casing,  20.3 cm (8 in), was set  with a very fine gravel pack
from bottom of the casing to the surface.  The  lower  6 m (20 ft)  of  the
casing  was perforated.   A  1 .2  m x  1 .2  m  (4  ft x 4  ft) concrete pad was
poured around  the   exposed casing.  Typical  well   construction details  are
shown  in  Figure 26.   The casing was cut  off  10.2  cm  (4  in)  above the
surface of the pad.   Initially,  a locking metal  box  was placed over  the
water  level recorder  (Type  F  continuous water  level recorder,  Leopold
                                   63

-------
•12.7  cm
 (5")  ID.
 PVC casing
                       •grout
        (a.) Initial Step
                                                                10.2  cm (4") ID.
                                                                PVC Liner
                                            (b.)  Completed Well
  Figure  25.   Two-Step Construction Sequence  Used  for Multiple Depth Well
                                      64

-------
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Figure 26.  Typical  Rotary  Drilled Well Used to Obtain Water  Levels

            and Water  Quality Samples
                                    65

-------
 Stephens, Stephens,  Inc., Beaverton, Ore.).  This proved   unsatisfactory
 due  to  problems with  both sand  in the recorder  and alignment of   the
 recorder's counterweight.    Subsequently,  1.2 m x 1 .2 m x  1 .8  m   (4  ft  x  4
 ft  x 6  ft) sheds were built over the wells and the recorders  were placed on
 shelves 1.2 m  (4  ft)  above the well, in order to additionally protect  the
 recorders from sand.   The  well casing was covered with three and- one-half
 mesh screen to deter  animals from falling down the wells.  After  several of
 the  continuous water  level  recording wells received  direct  recharge due to
 flooding conditions  from heavy rains,  0.6 m (2 ft)  PVC casing  extensions
 were placed on all  continuous recording wells.  Completion data  for  these
 wells is given in Table 6.
      Originally, it  was planned to perform pumping tests on the recording
 wells to determine  aquifer  properties.  However, when  this was  attempted at
 the Gray site  (well  6885),  the perforations proved  to be inadequate to
 allow pumping at a  sustained rate.   At  the Hancock  site, the  saturated
 thickness was  too shallow (3 m) to permit  yields sufficient for a pumping
 test.
 Non-Recording Observation Wells—
      Wells used  for the purpose of monitoring ground-water quality and depth
 to  water at a specific  point in time,  but not  equipped  with continuous
 recorders,  were termed non-recording observation  wells.  At  both sites
 these wells included  those  installed by  Texas  Tech University  (TTU)  and
 irrigation  wells existing prior  to the  project.   Wells installed by  TTU
 were  drilled  using  the  rotary method. A 10.16  cm (4  in)  diameter  PVC casing
 was  installed in a 12.7 cm (5  in)  diameter  hole and the annulus  was packed
 with  fine gravel  from the bottom  of the well to the surface.  The casing
 contained  perforations in the lower 6 m.   Concrete pads, 1 .2 m  x  1 .2 m (4
 ft x 4 ft), were  poured around  the  casings to  deter  surface water contami-
 nation of the wells.  The casings were  cut off  15.2  cm (6 in) above the pad
 and covered with  PVC caps equipped  with locks.  Only  the  reservoir  moni-
 toring  wells,  installed  by LCCIWR,  had  the casing  cemented to  deter
ground-water contamination  by surface water  short  circuiting down the  side
of the well casing to  the ground  water.
     Existing wells  used  for monitoring  included both  abandoned wells and
active,  irrigation wells.  Abandoned  irrigation wells were  used  for
                                  66

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monitor ing  purposes  only at the  Hancock farm.  These  wells  were  abandoned
over the years because  of the decreasing amount of available ground water
and the  importation of  irrigation  water  due to the  project.  Those wells
selected for monitoring had their pumps removed and were fitted  with metal
lids  with  locks.   All  other existing wells in the area beneath  a  pivot had
their pumps pulled and  casing removed or cut  off 1 .2  m (4  ft)  below the
surface  before being  backfilled with-chunks of concrete to  within  3 m (10
ft) of the surface followed by top soil until level.  Installation records
were not  vailable  for many  of the  existing wells.    The  existing wells
utilized steel casing 10.2 cm (4 in)  to 61  cm (2 ft)  in diameter. The zone
between the casing and  well hole was packed with gravel from  bottom  to sur-
face.  Small concrete pads were sometimes utilized for  motor  supports. Tur-
bine  and submersible  pumps  were used in these wells. Turbine  pumps often
dripped oil into the  wells.  A pump covered  the entire well  hole of an
active  irrigation well; therefore, no depth to water measurements could be
made.
Reservoir Monitoring  Wells—
     Monitoring wells were  installed  in  the  southeast corner  of each
reservoir in compliance with  the  City of Lubbock's  Wastewater  Discharge
permit  requirements.   These specifications required that the wells be
located within the runoff drainage moats surrounding  each reservoir.   At
each  reservoir a  22.2 cm   (8 3/4  in)  hole was drilled to  the  first clay
(Red Beds) past the ground water  using a mud  rotary  drilling  rig.  The
wells  were cased  with  10 cm  (4 in) PVC pipe.  The pipe was perforated from
approximately 10 m (30  ft)  above the ground-water table to  the  bottom of
the  well.   Gravel was  used to pack the annulus from  the bottom  of the well
to the top of the  perforations. One meter (3  ft)  of  blow sand  was  packed
above  the gravel. The  wells  were cemented from the sand packing  to  the top
of the well including a 38 cm (15 in) casing, one meter (3 ft)  above ground
level  and  a1mx1m(3ftx3 ft)  concrete  pad.   The wells  were then
developed with recirculating  water until clear of drilling debris.  Figure
27 shows the typical  construction of a reservoir monitoring well.  Table 8
gives the completion  data for each of the reservoir monitoring  wells.
                                   67

-------
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Figure 27.  Cemented Reservoir Monitoring Well

                          68

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                        TABLE  8.   RESERVOIR MONITORING WELL COMPLETION DATA
ON

Well Number
1U932


Depth of Well
Depth to Acquifer
Gravel Pack Interval
Perforated Interval
Cemented Interval

Diameter of Hole
Diameter of casing

(m)
26.84
16.78
11.59-26.84
14.64-26.84
0-11.59
(cm)
22.32
10.16

(ft)
88
55
38-88
48-88
0-38
(in)
8 3/4
4
10831

(m)
28.67
15.86
13.42-28.61
16.47-28.67
13.42
(cm)
22.23
10.16

(ft)
94
52
44-94
54-94
0-44
(in)
8 3/4
4
21152

(m)
28.98
13.12
10.68-28.98
12.20-28.98
0-10.68
(cm)
22.23
10.16


(ft)
95
4
35-95
40-95
0-35
(in)
8 3/4
4

-------
Water Sampling
Ground water Sampling—
     Ground  water  was sampled  three  times yearly  throughout the study;
spring after pre-irrigation (May), late summer after  irrigation  (Septem-
ber),  and winter  (January).   At  each sampling period  depth  to  water
measurements were made just prior to taking water samples.  Measurements
were obtained by using  a water level indicator   instrument (Model DR-760A,
Soil Test,. Inc., Evanston, Illinois).  A conductivity  sensor was  lowered
down  the well hole until contact  with water  was made,  evidenced by an
audible signal from  the hand held instrument  (combination cable spool  and
conductivity detector) and the glow  of  the  water  indicator light mounted on
the instrument.  At that time,  the number of feet  of pre-measured and marked
cable which had  been lowered down the well  was read at a mark even with the
top of the exposed well casing.
     Existing  wells with pumps were  sampled  at the  faucet or  opening
closest to the pump.   The faucet was rinsed by hand with the water  passing
from  the faucet.   The water  was allowed to run for five minutes before
filling sampling containers.   After  sampling, the  labeled sample containers
were  placed into  ice chests  for shipment to the LCCIWR laboratory within
one to eight hours.  Once the  samples were  received at the laboratory,  the
samples were analyzed or preserved immediately according to procedures out-
line on page 82.
     Initially, a portable  submersible  pump was used  on all the  wells
having no pumps.  The pump was lowered  3 m  (9 ft)  or more .below the  water
level, then  pumped  for ten minutes or until the pump ran dry, whichever
came  first.   The casing  would  refill  with water,  then be  pumped  for
samples.   At the  Hancock farm  where  the depth  of water was shallow,  the
pump had  to be lowered to a depth just  above  the  bottom  of the well. When
the well  was pumped,  sand was stirred  from  the bottom and pumped with the
water.  When  the pump was stopped to allow  the casing to refill with water,
the sand  in  the hose would settle onto  the pump's impellers, freezing them
in such a way  that the pump could not be  restarted.   There was no way to
clean  the  pump in the field.   The same  problem occurred on many of the Gray
farm wells.   Placing  screens on the  pump  inlet and additional well develop-
                                   70

-------
ment procedures did not  solve  the problem.  Consequently, a bailer was
substituted  for  the  submersible pump.
     Wells without  pumps were sampled  using a 7.6 cm (3 in)  diameter, 122
cm (4 ft)  long polyvinylchloride (PVC) bailer with a neoprene check valve
connected  to a  0.6 cm  (1/4-inch)  diameter cotton  rope.   The bailer was
cleaned between  wells by immersion in  ethanol followed by a  distilled water
rinse.  The  bailer  rsmoved approximately 41(1 gal)  of water each  time it
was withdrawn from the well.  Five to  15 bails of water, depending on depth
of  water  in the well  saturated zone, were  wasted  before  samples were
obtained.  At  the Gray farm where the water  table was high,  samples were
obtained  immediately after wasting.  At the Hancock farm, there was only a
few feet of water standing in the wells. Consequently, agitation  of the
water  during bailing  caused sediment in  the bottom of  the  well to be
suspended, leading to erroneous water  quality results. Similar wells having
pumpa normally  do  not  have a resuspension of particles. To  alleviate the
particulate problem, wells were allowed  to settle for  several  hours  between
wasting and sampling.
     Ground-water samples were collected from the organic non-contaminated
well  in a manner so  that there  would be negligible priority  organic
contamination.    Initially  an air driven, glass pump connected by 0.6 cm
(1/4 in) diameter Teflon tubing, was used  to  draw ground-water  samples.
Due  to the slow sampling  rate, the  inability to pump out  the  well before
sampling,  and continual  breaking of the  fragile glass  pump when  lowering it
39.6  m (150 ft), the  use  of the pump was replaced by a  stainless steel
bailer.  Using the stainless steel bailer  the organic non-contaminated
wells  were sampled in  the  same manner as the  monitoring wells  without
pumps.  Water samples  for extractable priority organic  compounds were
poured into  boric  silica quartz glass  containers with screw  capped  teflon
lined  lids.   Volatile organic  compounds  analysis  was conducted  on
ground-water samples which were poured  in 20 ml boric silicate  glass vials
with screw caps  which  were teflon faced  having neopreme septums.  The
capped, vial  containing  the sample was checked for air bubbles.  If  air was
observed in  the  capped vial, a new sample was collected  and the  procedure
was repeated.
     A trial well sampling run was made  to  determine whether or  not the
                                  71

-------
 bailing procedure  allowed representative  sampling  of  the  aquifer-   The
 monitoring well at Reservoir #1 was selected for  the  test because of  its
 fluctuating nitrate  levels.  The well was bailed  31  times  and  samples  taken
 from the first (four percent of well volume),  twentieth (85 percent  of  well
 volume), and thirty-first  (132 percent of well volume)  bail full.   Waiting
 periods were not necessary  between bailing and  sampling in order  to allow
 the  well to recharge.  Because of the time  it took to lower  and  raise  the
 bailer  (3-5 min) the well  recharged  with 4 L (1 gal) of water  from the
 aquifer as evidenced  by  no reduction  in measured  depth to  water  The
 nitrate concentration  in the first, twentieth  and thirty-first samples  were
 4.92,  5.44 and 5.38 mg/1, respectively.   The results indicate that there
 was no  appreciable  difference in  nitrate concentration with increased
 bailing.
 Seeps and Springs  at Gray Farm—
     A  walk-through survey of the canyon from 50th  Street to  the  east  side
 of the  study area Farm-to-Market  Road  ( FM)  1729  was undertaken during
 February,  1981.  Seventeen  sites were  found where  water was or had been
 flowing from the study site into the surface stream  in  Yellowhouse Canyon.
 Four  of these sites were  used to convey overflow from holding  ponds for
 surplus water  from the Gray farm;  the other 13 were  seeps  and/or  springs.
 Surface flow from  each of these locations was measured  with a  V-notch weir,
 mounted on  a plywood support.   A berm was placed  to channel   flow through
 the  weir-  Eventually most  of the  berms were reinforced  or replaced by sand
 bags.  In addition to the 17 sites where  the  weirs  were installed,  other
 sites  showed  signs of  seepage,  as evidenced by  a  luxurious growth of
 vegetation,  but  were spread over an area  too large  to allow channeling
 through a  weir.  One of the  largest seeps was in a side canyon whose head
 was immediately  south of observation well 6888.   Manual  measurements of the
 flow through the weirs and  of  the  water level in  this  well were made weekly
 from April  1 through August 5,  1981. Measurements were  terminated when the
 landowner asked  that measuring  equipment  be removed.
     The quality of water from  the seeps  and springs was monitored  at the
 same  frequency   as the wells during  1980  and 1981.   Monitoring of  the seeps
 and springs was  discontinued  after 1981  due  to  altercations with land-
owners  in the  canyon.   Grab  samples were  obtained  from the seep or spring
                                  72

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as it  flowed over  the  weir.  After  the samples were  collected  in  the
labeled sample containers, they were packed in  ice chests for shipment  to
the LCCIWR  laboratory.  Samples were received  at  LCCIWR within one to eight
hours  after sample  collection  and immediately  analyzed  or preserved
according  to procedures presented on page 279.  Water samples obtained  for
extractable and  volatile organic analyses were  collected  in glass contain-
ers in the  manner  previously outlined.

Applied Water Sampling—
     To monitor the. water applied to the farms and research plots, sam-
ples were obtained from the effluent pumped from the  City into the  pipe-
lines  to  the farms,  effluent water applied to  the land and well water used
for irrigation.   The water  sampling locations  of these samples were 1)  the
Hancock and Gray effluent  pump stations at  the Lubbock sewage treatment
plant; 2) distribution can 4 at the end of the  Hancock farm pipeline  prior
to water distribution to the reservoirs and over  the farm; and 3) distribu-
tion cans leading  from the reservoirs to the farm.
     Samples were  obtained  by  compositing  grab  samples  and by  using
indiscrete composite samplers  (ISCO, Model 1580, Instrument  Specialities
Company, Lincoln,  Nebraska). The composite samplers sampled 100 ml of water
each 15 minutes  over a 24 hour period.   A total of   9.6 L  (2.5 gal)  was
collected  each sampling period.  Composite samplers were used whenever it
was possible to  use  one  sampling  location to represent the water  being
applied to  the  farm.   For example,  by sampling the  final sump  at  the
Lubbock sewage treatment plant, the wastewater being  applied to the Gray
farm  and  wastewater being shipped to the Hancock farm could be monitored.
Samples from distribution can 4 at the Hancock  farm represented water being
applied directly from  line  and that flowing  into the reservoirs.   If  one
reservoir was the  predominant source of applied water  to  the  farm,  then  a
composite  sampler  was used to sample the water  flowing  from the reservoir
and being applied  to the farm.  The composite samplers  were  kept  cool  in
the field  with  crushed  ice  surrounding  their  10 1  (2.5 gal) sample con-
tainers.  The composite samples were transported to the  LCCIWR lab  where
the composite sample was shaken until homogenous, then  split into smaller
sample containers.   Water  samples  were either analyzed immediately  or
                                 73

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preserved according to procedures presented on page 279.
     In several  instances during  the monitoring  period  more than  one
reservoir was used as a source of applied water. Consequently, in order to
obtain a sample of water representing  the applied water,  it  was necessary
to  pull  a grab sample of water from each reservoir.  The grab samples were
obtained from sampling taps in the  top of  the  distribution cans at each
reservoir-   The distribution cans  distributed the wastewater flowing from
the reservoirs or pipeline to the farm.  After grab samples  were obtained
from  the reservoirs, they  were composited  into a single container  in
proportions  equal to each reservoir's  contribution to the applied water  for
that  day.  The composited  sample was then  placed in  an  ice chest  and
transported  to the LCCIWR  lab.  At the lab  the sample  was shaken  until
homogenous then split into aliquots  for analysis.
     To document that 24 hour composite samples and grab  samples from  the
distribution cans,  leading  from the Hancock  farm reservoirs,  could be
representative of the water  in the  reservoirs,  a reservoir survey  was
performed.   The largest reservoir,  Reservoir 1,  was monitored  twice to
determine reservoir stratification.  Reservoir 1 is 40 ha x 4.8 m (100 ac  x
16  ft)  containing 1 .5 x  16^m-^ (1200 ac ft).  A survey of the reservoir  was
made June 16,  1982.  The  reservoir was sampled  on  a grid  pattern (Figure
28) at  61 cm  depth  intervals in  each  zone.   Because of  wind,  it  was
impossible to maintain  a  stationary position;  consequently, dissolved
oxygen, conductivity and  temperature measurements were made from surface to
bottom as the boat drifted  across a zone.  Water samples for nitrate/
nitrite analysis were taken at 0.9 m (3 ft)  and 4 m (12 ft) depths  at  three
locations.  The data in  Tables 9 and 10 indicate that  Reservoir 1 is  a
completely mixed reservoir.   The  only  type of stratification  appeared  to be
an increase  in dissolved oxygen in the top 61  cm of the  reservoir-   A
second survey  of Reservoir  1  was  performed September 10, 1982.  Samples  for
conductivity,  ammonia and total organic carbon (TOC) analysis were  obtained
from the  0.3 m  (1 ft),  1.8  m  (6 ft)  and 2.7 m (9 ft)  depths from the  north,
middle and south portions of  the  reservoir.   As shown by the  data in  Table
11 it appears that  the  reservoir  was completely mixed.   Only the  ammonia
measurement suggests a higher  concentration Ln the center of  the reservoir
near the  location of the  wastewater  inlet.
                                 74

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           1 — 12 : Sampling  Grid  Quadrants
               T : Utility Pole
               O : Sampling  Locations
           	= Path  of Boat
Figure 28.  Sampling Grid for Reservoir #1
                            75

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  TABLE 9.  NITRITE PLUS NITRATE (N02/N03) CONCENTRATIONS  AT  1  M and 4 M
                  FOR RESERVOIR 1 LOCATIONS 2, 7, AND  10
	AS SHOWN IN FIGURE 11	

Sampling Location            2                  7                   20


Depth of Sample                           ND2/N03 (mg N/l)

  1  m (3 ft)                 0.01                0.04                0.04

  4 m (12 ft)                 0.03               0.03                0.05
                                 76

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TABLE 10.  VARIATION OF DISSOLVED OXYGEN,  TEMPERATURE
 AND SPECIFIC CONDUCTANCE WITH DEPTH IN RESERVOIR 1

''Location Dissolved Oxygen Temperature Specific Conductance
and Depth (mg/1) (°C) ( mhos/cm)
1-2
1-4
1-6
1-8
1-10
1-12
1 -Bottom
5-2
5-4
5-6
5-8
5-10
5-12
5-Bottom
10-2
10-4
10.6
10-8
10-10
10-12
10-Bottom
2-2
2-4
2-6
2-8 NO
2-10
2-12
2-Bottom
6-2
6-4
6-6
6-8
6-10
6-12
6-Bottom
0.4
0.4
0.6
0.6
0.4
0.4
0.3
3.6
0.3
0.4
0.3
0.4
0.4
0.3
2.2
0.5
0.4
0.3
0.3
0.3
0.25
0.5


PROBE DATA



0.4
0.3
0.1
0.1
0.1
0.1
0.4
23
23
23
23
23
23
23
23
23
23
23
23
23
23
23
23
23
23
23
23
23
24
24

AVAILABLE — DRIFTED INTO ZONE 6.
Note Adjustment in DOs


24
24
24
24
24
24
24
2100
2100
2100
2100
2100
2100
2100
2100
2100
2100
2100
2100
2100
2100
2100
2100
2100
2100
2100
2100
2090
2100
2100





2100
2100
2100
2100
2100
2100
2100
                                                   (Continued)
                     77

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Table 10,  continued
1 Location Dissolved Oxygen
and Depth (mg/1)
7-2
7-4
7-6
7-8
7-10
7-12
7-Bottom
7-Bottom
12-2
12-4
12-6
12-8
12-10
12-12
12-14
0.4
0.3
0.2
0.1
0.05
0.05
0.05
0.05
r.o
0.75
0.75
0.65
0.65
0.55
0.55
Temperature Specific Conductance
(°C) ( mhos/cm)
24
24
24
24
24
23
23
23
24
24
24
24
. 24
24
24
2100
2100
2100
2100
2100
2100
2100
1950
2100
2100
2100
2100
2100
2100
2100

  Feet  x  0.3048  = meters
                               78

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TABLE 11.  RESERVOIR 1  SURVEY OF SPECIFIC CONDUCTANCE, AMMONIA
          AND TOTAL ORGANIC CARBON,  SEPTEMBER 1982


South



Middle



North



Sample
Depth
(m)
.3 (1 ft)
0.9 (3 ft)
1 .8 (6 ft)
2.7 (9 ft)

0.9 (3 ft)
1.8 (6 ft)
2.7 (9 ft)

0.9 (3 ft)
1.8
2.7
Specific
Conductance
( mhos/cm)
2070
2090
2060
2100

2090
2080
1060

2070
2070
2070
Ammonia
(mg N/l)
<0.01
<0.01
<0.01
<0.01

<0.01
0.03
0.14

0.08
<0.01
<0.01
Total Organic
Carbon
(mg C/l)
12.5
17.5
18.6
15.3

16.4
13.3
11 .1

18.6
20.1
20.3
                             79

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    The  results of the reservoir  surveys  indicate  that  Reservoir  1  is  a
completely mixed system. Dissolved oxygen (DO)  concentrations  in  the upper
61  cm  of the water column ranged from 0.4  to  3.6 mg/1  with an average of
1.2 mg/1.  At depth  greater than 0.5 m (2 ft)  the DO  level  ranged  from 0.1
to  0.75 mg/1.
    The  conclusion which  may  be drawn  from the study was that  water
quality data obtained  from grab  samples or 24 hour composite  samples,
taken  at the distribution can receiving reservoir water,  was representa-
tive of the water quality in the reservoir and  bulk of the water  applied
to  the farm from the reservoirs.
Perched Water
     Examination of the baseline data from  the Hancock  site at the end of
1981 showed minor response  in the water level  to the  heavy  rainfall events
which occurred during October,  1981.   This fact, together with the extreme
depth to water [21-36 m (70-129 ft)]  led to  the decision to monitor  the
more  shallow zones for perched water tables  which  might  result  from the
application of large amounts of effluent.   The  project design called  for
excessive irrigation to occur  at both the  LCCIWR experimental farm plots
and at the Texas Tech  University (TTU)  plots.  Consequently,  aluminum
access  tubes 5.1 cm (2 in) in  diameter were  installed  to  a depth suffic-
ient to detect the uppermost perched  layer with a neutron probe. Initially
five  tubes were to be installed at the TTU  site and  nine at the LCCIWR
site (Figure 29).  The tubes at  the   TTU site  were installed during  Sep-
tember-November, 1982 without  difficulty.   However, approximately  18
holes were augered at the LCCIWR site.   In each hole dense rock  was  en-
countered at about the 8 m (25  ft)  depth  which could  not be penetrated by
the auger. Rotary drilling with  both  air and water,  as  well as  a larger
auger, which used air to  remove the  cuttings was attempted.  An initial
test of  the permeability of the  rock  indicated that  it  might be  suffic-
iently permeable to prevent the formation  of  a perched water table. How-
ever,  a  second test demonstrated that only the  top few centimeters of  the
rock were  permeable.  Both tests used  the falling head  method (Brakensiek
1977).   Three  tubes were successfully installed at the LCCIWR site.  Neu-
                                 80

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                                                                      LCC#4
                                            L.
                                           'LCC#8
                   LCC#9
                      Plot 1
                  TTU#3
                                        TTU#1
Plot 3
         TTU#5
                                    Plot 2
                                     TTU#2
                                       •
Figure 29.  Location of Neutron Access Tubes,  LCCIWR and TTU Research
            Areas, Hancock Site

                                   81

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tron  readings were  made on a  weekly basis  at  15 cm  (6  in) intervals
through October 15,  1983,  using  a Troxler neutron probe, Model 1256.
Laboratory Operations  - Waters
Laboratory Handling  and Preservation of Water Samples--
    After being logged onto sample receiving forms,  samples were placed in
a  4°C,  walk-in refrigerator or the samples were passed to the analyst by
whom they were to  be  analyzed.   Samples were  analyzed  within the  time
frames  specified in  Table  A.1  (Appendix  A).  Preservation methods were
generally limited  to  pH control,  chemical addition, refrigeration,  and
freezing. Table  A.1  summarizes methods employed for preservation  of water
samples.
Water Analyses-
    Water  samples were analyzed  for priority organic pollutants, other
organics,  minerals,   trace metals,   other inorganics,   and  indicator bac-
teria.   During the  two baseline years and  the irrigation monitoring per-
iod, water samples were analyzed for the 104 parameters  listed in  Table
12.   The number of parameters  was reduced for  portions of the  1982 and
1983 monitoring periods.   The reductions included:  1)  having a complete
analysis (104 parameters) made on the 10 continuous  recording wells and on
the wastewater streams used for  irrigation;   and 2)  reducing the number of
parameters analyzed  on all other samples by dropping  Ba, Co, Cr,  Cu, Pb,
Hg, Mo,  N-i, Se,  Ag, and Tl. The number of metals analyzed was reduced  in
the non-recording wells because  it  was decided in a joint meeting  between
LCCIWR and EPA RSKERL  staff that  the dropped  metals  were insignificant  in
concentration according  to  baseline data,  unlikely to increase  signifi-
cantly due to metal loadings expected on .the  farm, and  would be monitored
in  the continuous water level  recording well  which should  be representa-
tive of  the aquifer. A complete  analysis program,  similar to that   for  the
baseline  samples, was  performed  for  the last  sampling period,  fall-winter,
1983.
Analytical Procedures  for Waters—
    Because there were approximately  104 analyses performed  on each sam-
ple,  conservation  and preservation  of sample  was of  prime importance.

                                 82

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                         TABLE 12.  WATER QUALITY ANALYSES
Alk (mg/1 CaC03)
TOC (mg/1)
Conductivity (ymhos/cm)
TDS (mg/1)
pH
Cl (mg/Cl-/l)
TKN (mg N/l)
N02/N03 (mg N/l)
NH3 (mg N/l)
Total P (mg P/l)
Ortho P (mg P/l)
Org. P (mg P/l)
BOD (mg/1)
COD (mg/1)
SO'2 (mg  SO'/l)
Total Coliform/100 ml
Fecal Coliform/100 ml
Fecal Strep/100 ml
Salmonella/300 ml
Al (mg/1)*
As (mg/D*
Ba (mg/1)*
Ca (mg/1)*
Cd (mg/1)*
Co (mg/D*
Cr (mg/D*
Cu (mg/D*
Fe (mg/1)*
Pb (mg/D*
Mg (mg/1)*
Mn (mg/1)*
Hg (mg/1)*
Mo (mg/D*
Ni (mg/1)*
K (mg/D*
Se (mg/1)*
Ag (mg/1)*
Na (mg/D*
Tl (mg/D*
Zn (mg/1)*
Anthracene (yg/1)
Atrazine (yg/1)
Benzene (yg/1)
Benzeneacetic acid (yg/1)
4-t-butylphenol (yg/1)
Carbontetrachloride (yg/1
4-chloroaniline (yg/1)
Chlorobenzene (yg/1)
Chloroform (yg/1)
2-chlorophenol (yg/1)
1-chlorotetradecane (yg/1
Dibutylphathalate (yg/1)
2,3-d.ichloroaniline (yg/1)
3,4-dichloroaniline (yg/1)
Phenathrene (yg/1)
Dichlorobenzene (yg/1) m,p,o
Dichloromethane (yg/1)
2,4-dichlorophenol (yg/1)
Diethylphthalate (yg/1)
Diisooctylphthalate (yg/1)
Dioctylphthalate (yg/1)
Dodecanoic acid (yg/1)
Ethyl benzene (yg/1)
Heptadecane (yg/1)
Hexadecane (yg/1)
Hexadecanoic acid  (yg/1)
Methylheptadecanoate (yg/1)
Methylhexadecanoate (yg/1)
1-methylnaphthalene (yg/1)
2-methylphenol (yg/1)
4-methylnaphthalene (yg/1)
Naphthalene (yg/1)
4-nonylphenol (yg/1)
Octadecane (yg/1)
Phenol (yg/1)
Propazine (yg/1)
ct-terpineol (yg/1)
Tetrachloroethylene (yg/1)
Toluene (yg/1)
Trichloroethane (yg/1)
Trichloroethylene (yg/1)
*Total and Dissolved Metals
                                      83

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Table A.2 summarizes  the  methods of analysis used by the lab.  The methods
were specific for the types   of samples- and sample load experienced during
this project.  In many instances,  several references  are listed  for one
parameter, since most of  the  final methods of analysis, were developed from
portions of  various  methods.  The analytical  methods  employed  required
small quantities of sample, were fast, were accurate and precise.
SOILS
Soil Sampling
    Soil  cores  were   obtained  with a Gidding's soil coring and sampling
machine (Model GSRP-S, Gidding Company, Fort Collins, Colorado).  During
the first sampling period (March 1981) and final sampling period (November
1983) 1 .8 m (6 ft) cores  were obtained using  a  10.2 cm  (4 in) diameter,
1.2 m  (4 ft) long coring tube with a quick relief bit.  Cores were taken
to only 0.91  m (3 ft) depth during the intermediate sampling periods.
    In the  field, the core  was  divided  into  0.3 m (1 ft) sections on a
board brushed off between samples.  Each 0.3  m  (1  ft)  section was  thor-
oughly mixed and portioned into sample containers.   If several cores  were
composited to make a  single  sample,  then a  portion of  each thoroughly
mixed section was put into the same container corresponding to that depth.
At several sampling locations, the soil was so hard that a 0.9 m (3 ft)  to
1.8m  (6 ft) core could not be obtained.  In those cases, a coring auger
was used  to obtain samples at the desired depth.   Since  the auger  mixed
the soil collected  from various depths and took less sample, the augered
samples were considered one sample.
    The containers used for the soil samples were similar to the ones used
for water.  In the field, a portion of each sample was  put into a  glass
teflon lined screw  cap  jar for priority organic analysis.  The remainder
of the sample was put  into a 10.3 cm x 25.4 cm (8 in x 10 in) or 27.9 cm x
40.6 cm  (11  in  x 16  in)  sterile polyethylene  bag and sealed with a wire
twist.   The  samples were  immediately placed in ice chests and transferred
to the LCCIWR lab by 4:00 p.m. that day.  Once the samples were received
at the  LCCIWR lab,  the jars of soil were placed  in a freezer.  Immediately
prior to  volatile organic analysis, an aliquot of soil was obtained from
                                 84

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the soil sample contained  in  the glass jar- and placed in a Headspace® vial
for analysis.   The soil  in the  polyethylene bag was divided as follows:
    1.    A portion was separated into another sterile container for micro-
         biological analysis
    2.    A second portion   was  weighed directly into an ammonia extracting
         solution
    3.    A third portion  was poured into drying pans  to be air dried and
         and ground
    4.    The remaining portion  was  set in a 4°C cold box until needed
    Soil samples representative of the  farms were obtained by randomly
designating sampling locations (Figures 30  and 31) and compositing three
cores from within these  locations.   The  same  locations were sampled during
1980 through  1983-   By returning to the same location, it was theorized
that differences noted  in  soil  characteristics due to sampling variability
would be reduced.
    Sampling locations  for the  demonstration  area (Figures 32 and 33) were
determined by  first dividing  each  farm into  65 ha (quarter-section).  On
the Hancock farm,  each pivot encompassed approximately 65 ha (one quar-
ter-section).  Each field on the Gray farm  was approximately 65  ha (one
quarter-section).  The  quarter-sections were then divided into four 16.25
ha (40  ac) blocks and each block assigned  a  number.   Finally, a  random
number  table was used to randomly  select which block within a 65 ha (quar-
ter-section) was to be sampled. The cores within each  block were  pulled
and composited  at 0.3  m  (1 ft)  increments  to  make one sample for each
depth.  Soil samples were cored  just after  harvest for  cotton (November)
and twice a year for double cropped areas (April and November).
    A special  effort was made to obtain  soil  samples  from each different
type of farming  practice.  For  example, soil  cores were obtained from
non-irrigated,  furrow irrigated, flood irrigated, and  sprinkle irrigated
areas of the farms.
Laboratory Operations -  Soils
Soil Sample Preservation—
    Soil  sample preservation  methods employed were dependent on the par-
ameters for which the soils were analyzed.  The soils, brought in  from the

                                   85

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CD
ON
           Figure 30.   Grid for Random Selection of Soil and Crop Sampling Locations, Gray Farm

-------

                       Reservoir
                        Playa Lake

                    1 cm = 0.27 km
Figure 31.   Grid  for Random Selection of
Soil  and Crop Sampling Locations, Hancock
Farm

-------
                                      23143W
                                    I 22114
                                       18133 Y  17161
                                      02141

                                      01141
   Reservoir
-i-i Playa Lake
•  Sampling Site
                  1 cm = 0.27 km
Figure 32.  Soil Sample Location,
          Hancock Farm

-------
                                                                             •  Sampling Site
                                                                                Water
                                                                                = 0.27 km
21163  19164
 J  (ffii>
 ^   \t,','!'fy
Figure 33.   Soil Sample Locations,  Gray Farm

-------
 field  in plastic bags  or bottles or glass jars,  were preserved by three
 methods.  Soil samples were stored at 4°C until  analysis  occurred  where
 those  soils for which  microbiological  assay and wet chemistry analyses
 were made on a field  moist soil sample.  Soils for  which priority organic
 pollutants were to  be  measured were  frozen in  their glass  containers
 immediately upon receipt.  Soil samples analyzed for metals,  physicals and
 most  other inorganics  and  organics  were  dried,  ground, and  stored in
 plastic bags at room  temperature.  A portion of each sample,  regardless of
 analyses to be performed,  was taken within 24 hours after  sampling and the
 subsample was stored  for no more  than two days  in a plastic  bag at  4°C
 before being analyzed for  percent moisture.   Percent moisture  was a neces-
 sity for reporting soil data on a dry weight basis. Before a  subsample was
 removed  from  its container, the entire sample was well mixed  by shaking,
 kneading or stirring  until large chunks were broken and the sample appear-
 ed homogenous.   Table A.3 gives the  recommended  sampling  container,  stor-
 age temperature,  holding time, and method of pretreatment  by  category  of
 parameters for which the sample was to be analyzed.  Holding times for the
 parameters were determined from the literature and  by laboratory testing.
 For each category,   the recommended holding time  was  just less  than that
 time at which values  for the parameters of concern  began to change due  to
 excessive storage time.
    Soils analyzed for most minerals, metals,  physicals and nutrients were
 preserved by drying and grinding.  Drying a sample to less  than  five  per-
 cent moisture substantially  negated interactions between chemical  ions,
 organics and microbes (Black 1965).   The object of  drying  a sample  is  to
 dry the  sample in  the least  amount of time under the least harsh condi-
 tions.   Preferably the sample should be air  dried (until the sample is not
 sticky and can  be ground  without balling,  approximately five percent  mois-
 ture content)  at  about 20-25°C and 20-60 percent  humidity.  A  forced  air
 drying cabinet was  used to  dry the  soil  samples in  two days at  no warmer
than 40°C.   After drying, the  sample  was ground to  pass a  2 mm  sieve  and
 stored in  a plastic  bag  at room temperature  and  humidity.  If  upon grind-
 ing the soil  sample,   it  was noted that  the moisture content  was higher
than five  percent,  then the open  sack of  ground soil was placed in the
                                 90

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drying cabinet  for  24 hours, then reclosed.
Soil Analyses—
    Soil samples  were  analyzed for the  parameters  shown  in  Table 13.  To
trace the constituents  of the wastewater through the land treatment pro-
cess,  the same  parameters  analyzed for waters were  analyzed  for soils. In
addition, soil  samples  were tested for those parameters  used  to  (1)  char-
acterize soil  types;  (2)  measure assimilation capacity of the soil for
various-parameters;  and (3) relate  the constituents of soil to  plant
availability.   Soil samples from the  baseline years  and final sampling
period (winter  of 1983)  were analyzed for the complete  list of parameters.
The  1982 soil  samples  had  only the top three, 30 cm sections analyzed for
pH, conductivity, potassium, total Kjeldahl nitrogen,  total phosphorus and
priority organics.  3ustifications  for  reduction in  analysis were that
there was a backlog in  sample analysis, changes due  to  one year of irriga-
tion  wer_e not expected at depths below  one meter (3  ft),  and the state
discharge permit required only these analyses  except priority  organics.
Priority organics  analysis was retained  because there was  no analytical
backlog  for gas chromatography analysis.
Soil  Analytical Procedures—
    There were no  standard  methods for the analysis  of  soils.  For each
parameter, there are usually several different methods of extraction and
analysis of the extract,  each giving  different  results.   It is common
practice  among  soil scientists to use the procedures that fit their par-
ticular circumstances and cite the  procedure for which the results are
based on.  Consequently, results of separate investigations can be compar-
ed  only if the referenced analytical procedures were  the same.  The ac-
cepted books of referenced  analytical procedures were written in the 1940s
and  1950s and  did  not  contain adequate procedures  for  atomic absorption,
gas chromatography  or spectrophotography.    In  addition, the procedures
were not complete in the preparation of extracts, standards,  and analysis.
Therefore,  LCCIWR  lab  tested many  procedures  and mixed procedures in
order to obtain  analytical  procedures:  (1) with a high  degree of accuracy
and procedures;  (2)  that are relatively fast;  (3)  which are adapted to
modern  instrumentation; and (4) that are detailed and  complete. Table A.4
                                 91

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                            TABLE  13.
                                           QUALITY ANALYSES
Alk (mg/g Ca2C03)
TOC (mg/g)
Conductivity (ymhos/cm)
IDS (mg/g)
PH
Cl~ mg/g Cl~ Total
TKN mg/g N  Total
N02/N03 (mg/g N)
NH3 (mg/g N)
Total P (mg/g P)
Ortho P (mg/g P)
SO-2 (mg/g  S)
CaC03 (mg/g CaC03)
Cat ionic Exchange
Anionic Exchange
Organic Matter
Buffer Capacity
Solution Cations (mg/g)
Sulfur (mg/g)
Specific Gravity
Texture
Bulk Density
Consistency
Color
Humus (mg/g)
Total Coliform/g
Fecal Coliform/g
Fecal Strep/g
Actinomycetes/g
Fungi/g
Al (mg/g*)
As (mg/g)*
Ba (mg/g)*
B   (mg/g)*
Ca (mg/g)*
Cd (mg/g)*
Co (mg/g)*
Cr (mg/g)*
Cu (mg/g)*
Fe (mg/g)*
Pb (mg/g)*
Mg (mg/g)*
Mn (mg/g)*
Hg (mg/g)*
Mo (mg/g)*
Ni (mg/g)*
K  (mg/g)*
Se (mg/g)*
Ag (mg/g)*
Na (mg/g)*
Tl (mg/g)*
Zn (mg/g)*
Acenaphthylene (yg/1)
Anthracene (yg/1)
Atrazine (yg/1)
Benzene (yg/1)
Benzeneactic acid (pg/1)
4-t-butylphenol  (yg/1)
Carbontetrachloride (yg/1)
4-chloroaniline  (yg/1)
Chlorobenzene (yg/1)
Phenanthrene (yg/1)
Chloroform (yg/1)
2-chlorophenol (yg/1) m,p,o
1-chlorotetradecane (yg/1)
Dibutylphthalate (yg/1)
2,3-dichlorotetradecane  (yg/1)
3,4-dichloroaniline (yg/1)
Dichlorobenzene (yg/1)   m,p,o
Dichloromethane (yg/1)
2,4-dichlorophenol (yg/1)
Diethylphthalate (yg/1)
Diisooctylphthalate (yg/1)
Dioctylphthalate (yg/1)
Dodecanoic acid (yg/1)
Ethylbenzene (yg/1)
Heptadecane (yg/1)
Hexadecane (yg/1)
Hexadecanoic acid (yg/1)
Methylheptadecanoate(yg/1)
Methyhexadecanoate (yg/1)
1-methylnapthalene (yg/1)
2-methylphenol (yg/1)
4-methylphenol (yg/1)
Napthalene (yg/1)
4-nonylphenol (yg/1)
Qctadecane (yg/1)
Phenol (yg/1)
Propazine (yg/1)
a-terpineol (yg/1)
Tetrachloroethylene (yg/1)
Toluene (yg/1)
Trichloroethane (yg/1)
Trichloroethylene (yg/1)
 •Total and Available  Metal Analysis
              92

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lists the  references  for the procedures used  by  LCCIWR.  In most instances
several references  are listed for  a  parameter  denoting that procedures
from those references were mixed to obtain  final, complete, favorable pro-
cedure.
CROPS
Crop Sampling
     The  purpose  of crop  sampling was to  obtain  plant samples  which
represent  each farm,  crop, and type of irrigation.   The  crop samples  were
divided  into  specific  plant  parts  (i.e,  seed,  stem,  leaves, etc.).
Sampling locations  for crop samples were determined  in a manner similar to
that  for  soil samples.  The two farms were  divided  into  approximately 65
ha areas.  Each pivot  or  field encompassed approximately  65 ha (one. quarter
section,  150  acres).   The 65 ha  were subdivided  into  4 ha (10  acre)
sub-blocks and each block was assigned  a  number, 1  through 16.   The
sub-blocks were further  divided into quadrants. Four -to five sub-blocks
were sampled  from  each  block.   A  random  number generator was used  to
initially select  the sub-blocks and  quadrants  to  be  sampled.  The same
sub-blocks were sampled  each year, but not  necessarily the same quadrants.
Figures 34 and 35  show the crop sampling locations.
       Crop samples  were  collected  at  harvest  time  when the  crops had
developed maximum   maturity.   Normally, harvest  occurred  mid-October
through January.   Some portions of the farms  had two  crops grown per  year.
These  "double cropped"  areas  were harvested  and  sampled twice a year;
mid-October through January and April through mid-May.
    At sampling time, crop samples were obtained  for laboratory and  yield
tests.  For laboratory analysis, all the plants  within a square meter area
in each quadrant were removed and composited  into sterile, plastic bags to
obtain one plant sample  per block (field or pivot).   During 1981 the  roots
were  cut  from the  plants and composited separately.  No root samples were
obtained during 1982  and 1983 because: (a)  the microflora  attached to  the
root  could not be differentiated from that of the soil clinging to the
root and,  (b)  the roots of all crops  are commonly  plowed into the  soil
after  harvest, thereby  returning to  the soil the constituents of the
                                 93

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                       00019 A       *   V
                       A A    A  j\^ A  A A
                                      00018
                                    A00015
                                    A A
              A      A
              00006 A
                     Reservoir
                     Playa Lake
                  A  Sampling Site
                 1 cm = 0.27 km
Figure 34.  Crop Sample Locations,
          Hancock Farm
                                          /

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                                                                                Sampling Site
                                                                                Water
                                                                                = 0.27 km
Figure  35.   Crop Sample Locations,  Gray Farm

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roots.   Crop samples  for  yield  tests were  obtained form the same sub-
block locations as samples obtained  for laboratory analyses; however,  the
sub-block  samples were not composited  into one  sample  per  block.   To
reduce the  bulk of crop  brought into the  lab,  only  three or  four sub-
blocks per  block were harvested.   At the lab the grain sorghum plants were
divided into  grain and stalk and  leaves.  Cotton plants were divided  into
stalks  and leaves,  lint and seed.  The plants parts were then dried  and
weighed.  Yields of grain,  seed,  lint and  foliage per hectare (2.5  ac)
were  then  calculated.  Yields obtained  by repetitiously harvesting  two
square  meter areas  sometimes  varied  from the  yields obtained  by  the
farmers.   The farmers' yields were derived by dividing  the total  gin or
grainery weight of farm  product by the number  of acres  from  which  the
product  was  harvested.   The  farmers'yields  were used  in calculating
portions of the economical data. All other data concerning mass  balances,
yields, etc.,  used the yield data  based on harvesting two  one-meter  square
samples.
 Laboratory Operations
    In the laboratory,  aliquots for bacteriological examination  were
first obtained aseptically from  the bags containing  the  field samples.
The  whole  plants  for bacteriological  analyses were immediately divided
into plant  parts,  cut  into pieces 10 cm  (4  in)  or  smaller,  placed  in
separate sterile  bags, and placed in a 4°C refrigerator until analyzed.
The remaining  plant sample was divided into its plant parts (seed,  stalk,
etc.), dried,  ground, and stored in plastic bags for chemical analysis.
Crop Sample Preservation—
    The crops, brought  in  from the field  in sterile plastic  bags, were
preserved by  two methods.  Those crops for which microbiological assay  and
wet chemistry  analyses must  be made on a field moist sample were stored  in
their respective containers  at 4°C until analyzed.  Crop samples analyzed
for metals,  physicals and  most other inorganics and organics were  dried,
ground and  stored in  plastic bags  at room temperature.  A portion of each
sample  (plant part),  regardless of  analyses to be performed, was taken
within 24 hours after sampling for moisture determination.  The  subsample

                                 96

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was stored  for no more than two days in a plastic  bag  at 4°C before ana-
lyzing percent  moisture.  Percent moisture was a necessity for  reporting
all crop  data  on  a dry weight basis.  Before a subsample was removed from
its container,  the entire sample was well mixed  by  shaking, kneading  or
stirring until  the sample appeared homogeneous.
Crop Analyses—
     The analyses  (Table 14)  performed on crop samples  were determined by
the type of plant  and  plant part  (Table 15).  Those parameters   such  as
metals  and nutrients,  which could  be  translocated  from the soil to all
parts of the plant, were analyzed on all plant tissue  samples.  Bacteria,
yeast  and fungi, which could contaminate exposed  surfaces of crops, were
analyzed on all samples.  Analysis of crop roots were  discontinued  after
1981 because: (1)  microbes  in or on the root surface could not be discern-
ed  from that in the soil clinging to the roots; and  (2)  all crop roots are
plowed  into the soil  each year; consequently any chemicals absorbed in the
roots would be released  into the  soil and could be  analyzed  in  soil
samples.  Certain  other  parameters which were specific to a crop and plant
part and which are commonly used as crop quality indicators, were analyzed
only  for those samples.   During the 1982 and 1983 sampling periods crop
samples were pulled  from the  specified demonstration areas and yields were
obtained.  The samples  were processed in the lab and analyzed for min-
erals,  nutrients and  bacteria.   Analysis of  the  same  priority  organic
pollutants analyzed  in  water and soil samples was  never performed on crop
samples. Standard  methods for gas  chromatography  screening of  priority
organics in plant tissues do not exist. With the aid  of EPA, many methods
of  extraction and  cleaning  the samples  were tried  without success.   The
ultimate conclusion  was  that plant tissue contains  many organic natural
occurring, unidentified compounds and that organic  peaks of interest  can
be  discerned only after  extensive  sample  cleanup  and by using  a gas
chromatograph/mass spectrophotometer instrument.  Because of  the  large
number  of crop samples,  it  was not  practical to analyze the crops for
priority organics.
                                 97

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         TABLE 14.  CROPS ANALYSIS
 pH                                   B  mg/g
 TKN mg/g N                           Ca mg/g
 NH3 mg/g N                           Cd mg/g
 Total P mg/g P                       Co mg/g
 Oil mg/g                             Cr mg/g
 Protein mg/g                         Cu mg/g
 KCN mg/g                             Fe mg/g
 Fatty Acid mg/g                       Pb mg/g
 Sulfur  mg/g S                        Mg mg/g
 Starch  mg/g                         Mn mg/g
 Niacin  mg/g                         Hg mg/g
 Fiber mg/g                           Mo mg/g
 Biotin  mg/g                          Ni mg/g
 Total Coliform/g                     «  mg/g
 Fecal Coliform/g                     Se  mg/g
 Fecal Strep/g                        Ag  mg/g
A1 m                                 Na mg/g
As m                                 Tl mg/g
Ba m                                Zn mg/g
                    98

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                TABLE 15.  CROP ANALYSIS  PROTOCOL
                              COTTON

Lint, Seed, Burs, Stems:
     TC, FC, FS
     TKN, TP, S
     K, Ca, Mg, Na, Zn, Mn, Fe, B, Al,  Cd,  As

Seed:

     Protein, Cl~, Oil

                       GRAIN  SORGHUM  (HILO)

Grain, Stalk, Leaf:
     TC, FC, FS
     TKN, TP, S, Cl-
     K, Ca, Mg, Na, Zn, Mn, Fe, B, Al,  Cd,  As

Stalks, Leaf:
     HCN, Fiber

Grain:
     Protein, Starch,  Oil

                         ALFALFA, BERMUDA

Whole Plant:
     TC, FC, FS
     TKN, TP, S, Protein,  Cl~
     K, Ca, Mg, Na, Zn, Mn, Fe, B, Al,  Cd,  As
     Fiber

                       SOYBEANS, SUNFLOWERS

Leaf, Stem, Seed:
     TC, FC, FS
     TKN, TP, Cl-
     K, Ca, Mg, Na, Zn, Mn, Fe, B, Al,  Cd,  As

Seed:
     Protein, S, Oil

                           WHEAT, DATS

Leaf, Stem, Seed:
     TC, FC, FS
     TKN, TPS,  Protein, Cl-
     K, Ca, Mg, Na, Zn, Mn, Fe, B, Al,  Cd,  As

Seed:
     Starch
                                99

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Analytical Procedures—
      Like  soil methods  of  analyses, there  are no standard methods  of
 analyses for plant tissue.   Applicable  methods   were extracted  from  many
 sources and tested.   Table A.5 gives  the methods  of analysis for  crop
 samples.
 IRRIGATION RECORDS
     Documentation of  how much, when and where effluent water was  applied
 was necessary for the demonstration and research  efforts.   The records
 aided in the interpretation of soil and crop quality  data  as  well  as  crop
 yield data.  The records were  also used in  assessing the economics of
 domestic water  reuse  through farming by knowing the  water  usage by farm-
 ers,  cost of delivering and using the water,  farming costs  and money
 returns  of field  and government programs.  Finally,   the irrigation
 records were used in the  interpretation of the health  effects  data  (Camann
 et al 1985). The exposure of the participants to agents of  disease in the
 effluent water was based  on  where, when and how much wastewater  was spray
 irrigated.
     A simple form (Figure  B.I,  Appendix  B)  was  devised  on which  each
 farmer  recorded daily  the amount of water pumped through a  pivot and  the
 location of the  pivot in  the  field.   Each of the farmers   was supplied
 with  a pad of these  forms which they carried  in  their trucks.   Monthly,
 the forms were  collected  from the farmers.   A transparent circle, the  size
 of the pivot and marked in degree  units around  its  circumference,  was
 placed over the pivot  figure.  The position of the  pivot was  then given a
 location in degrees  and a direction of movement,  plus ( + )   for  clockwise
 and minus (-)  for counterclockwise.   The   pivot number, location, direc-
 tion  of movement, gallons applied, and date could then be entered into the
 computer.
    Figures  B.2 and B.3 show how  the form  was to be filled out and how
 some  were turned in,  respectively.   In many  cases, when the farmer  put
 down  a percent speed  instead  of the flow meter readings,  the  reason was
 simply a flow meter  failure.  There were a number  of problems  with  the
 flow  meters themselves, and also the  ability during long periods of oper-
 ation to actually get to the center of the pivot to  read the  meters  each
                                 100

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day.  However,  by knowing  the  design hydraulic  capacity of the pivots
(cubic meters  per minute flow), amount  of  time the pivot operated and  the
amount  of  land  irrigated within that  specified time, the amount of water
applied  during  the day (m^)  and hydraulic  loading to the land (mVha)
could be calculated.   A computer program was developed  to compute  the
hydraulic  loading based  on providing the  starting and final position of
the pivot machine.
    Overall this  system allowed  adequate records  to  be obtained as to
which pivots were operated on certain days and a comparison of irrigation
application and mass  balances.   This  system  worked well enough to now be
used by the farmers  to-help keep  track of percent  water used on their
acreage for dividing lake pump costs on a  use  basis rather than an acreage
base.
ECONOMICS
The economics of land treatment were   monitored  through operation  and
maintenance cost records provided by the City  of Lubbock  and the  farmers
utilizing the land  treatment system.
     The  city  supplied yearly summaries of the cost of treating the water
supplied to each farm  and  the cost  of-operation and maintenance of  the
pump station delivering  water to the Hancock farm.  Most of these costs
were broken into monthly subtotals.  This  allowed comparisons to be made
between growing and  non-growing seasons  and  different modes of  water
distribution on  the  farm operation  (i.e., irrigation  with water direct
from the city, and  only from the reservoirs).
    Yearly, the  farmers turned in  their financial statements including
operation and maintenance costs of the center pivots, electrical costs of
their share of the  reservoir pumps, farming costs, and  monetary returns.
Normally,   these records  were  completed  at the same time they prepared
similar information  for tax  purposes.
    Several problems  were  encountered  in obtaining  and analyzing  the
requested data.   First, crops harvested during the year may be stored  and
sold  the following year  when commodity  prices could be higher.  Conse-
quently, the records including the farming cost and return on investment
for  a  year may  have  taken  two  years  to  obtain.  Second, when a disaster
                                 101

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struck  (i.e.,  excessive rain, drought,  hail  or  early  freeze)  and  no  crop
yields were obtained, government disaster programs  or crop insurance had
to be  taken into account.   Third, government sponsored  farming programs
such as "Payment  In  Kind" (PIK) paid the  farmer  for  not farming  certain
amounts  of acreage.  Finally, the farmers did  not  keep  the same  type of
records. When working  with a  group  of  farmers on  economic  data, many
statements  were   encountered   from  individuals  who  turn in  everything
from  interest, labor, withholding and depreciation   to those who gave
a bare  minimum of  information.   As shown in  Figures  B.4  and B.5, the
form  originally  submitted to the farmers had   ten   categories  for ex-
penses and nine for  income.  Several times, discussions were held with the
farmers on  how the  forms should  be  completed.   After  receiving the
first set of completed  economic records from the  farmers,  it was obvious
that one set of records or one  farmer's operation  should not  be  compar-
ed directly to  that  of any other farmer's.  Figures  B.4, B.6, and B.7  give
examples of how divergent these reports were.  Conferences with the farm-
ers did not help  clarify the situation since the  records were based on how
they kept their personal records.  There was no way   to force  those,  who
who were not willing,  to rearrange  their data  into  a  previously specified
format. For this  reason,  categories from the  original  form were consoli-
dated  into more  encompassing categories  (Figure  36).  Therefore, some of
the finer details  may have been lost, but  overall  comparisons  should be
more accurate.
STATISTICAL ANALYSIS
    Quality data  are presented  in terms  of  arithmetic mean and standard
deviation.   The skewness and median values  are also provided for all water
quality  data.  Due to the  special variability  in the soil data, the co-
coefficient of variance is provided for the soils data.  The Waller-Duncan
test was  used  to objectively  corroborate the  differences in the water
quality results.   The Waller-Duncan test  incorporates probability  and the
degrees  of freedom to determine  if significant  differences exist between
any possible pair of means.   All significant differences were  determined
at an  a = to 0.05.
                                 102

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                        Equipment  Purchase
         Interest        or Depreciation
                               Tires and
                               Repairs to
                               Machinery
                               Gas, Oil,
                                Grease
                      Equipment
                                         Gas, Oil
                                         Repairs
      Seed
       and
    Fertilizer
Chemicals &
    and
  Spraying
Hoeing and
 Chemical
 Weed Control
Salaries
  Labor
 Social
Security
                "Seed,  Fertilizer,
                    Chemical
                                              1 Labor
    Irrigation Expense
       Fuel,  Repair
        Irrigation
          Expense
Figure 36.  With These Categories Pulled Together, More of  the  Farming
            Operations Can be Compared from Tenant to  Tenant
                                    103

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                               SECTION 6
                          RESULTS AND DISCUSSION

WASTEWATER EFFLUENT
Hydraulic Distribution
     On  February 19, 1982,  wastewater effluent from Lubbock's  Southeast
Water Reclamation Plant  (SeWRP) was pumped to the Hancock farm.   The total
hydraulic flow produced by SeWRP from February 19 to December  31,  1982  was
10.96  x  106 m3.   From  January 1, 1983 to October 31, 1983  19.29  x  106 m3
wastewater was discharged  by  SeWRP.
     As  previously stated,  the pump capacity in conjunction with  the man-
agement of water within  the SeWRP made it impossible to transport  water  to
the  Hancock farm  for more  than 16 hours each day.   Furthermore,  odor  and
operational problems  associated with irrigating directly with effluent from
SeWRP necessitated  the use of the reservoirs at the Hancock  farm as polish-
ing lagoons prior to  irrigation.   Since the  same pipeline distribution
network  was used  to provide water to the center.pivot irrigation  machines
and transport water to the reservoirs, main pipelines had to be dedicated
to either irrigation  from reservoir  or transporting  water  to  the  reser-
voirs.  Increased head losses resulting from closing of valves to accom-
plish  irrigation solely from reservoir aggravated the system total dynamic
head against which  the pumps must operate.
     Consequently, the  Hancock  farm received only  20 percent (4.13 x  10^
m3) of  the total  effluent  produced  from  February  through  December 1982.
SeWRP  pumped 59 percent of the total  effluent (12.52 x 106 m3) to  the Gray
farm  and  20 percent (4.29  x 106 m3)  to Southwestern Public Service (SPS)
during the same time period.  In 1983  the Hancock farm and  SPS  received  19
and 21 percent (3.74 x 106  m3 and 4.14  x 106 m3),  respectively, of  the
total effluent  discharged from January 1  through October.  Figures 37  and
38 present the variation  in flow produced by SeWRP and the average daily
flow rate per week  to each consumer  from February  1982 through  October
1983.
     The  1982 average hydraulic loading pumped to the Hancock farm  was 42.5
cm (16.7  in).   During the same time frame  (February  through  December)   the
                                  104

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o
Ui
1.00
6.00
11.00
          16.00
                                                21.00     26.00     31.00
                                                     WEEK  IN  1982
                                                                                                          SOUTHEAST HfiTER RECLflM.  PLflNT
                                                                                                          GRflT FORM
                                                                                                          HRNCOCK FflRH



                                                                                                          SOUTHWEST PUBLIC SERVICE
                                                  36.00      41.00      46.00      51.00
      Figure  37.   Hydraulic  Flow  to  Consumers  in 1982

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o
ON
          1.00
6.00
11.00
                                         16.00
21.00     26.00     31.00
     WEEK  IN  1983
                                                                                                     SOUTHEflST HRTER RECLflH. PLHNT
                                                                                                     GRflT FflRM
                                                                                                     HflNCOCK FflRM

                                                                                                     SOUTHWEST PUBLIC SERVICE
                                                             36.00     11.00     46.00      51.00
           Figure 38.   Hydraulic Flow to  Consumers  in 1983

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Gray  farm  received  103.5 cm (40.7 in).  The average hydraulic loading  to
the Hancock farm in  1983,  from January  1 to October 31, decreased slightly
to 38.6  cm (15.2 in).   Similarly, the  Gray farm was irrigated with  94.2  cm
(37.1 in) of effluent.
     The arithmetic mean  effluent flow rate produced by SeWRP was not  sig-
nificantly different ( ct =  0.05)  in 1982 and 1983.  Furthermore,  the  differ-
ence in average monthly flow  rates to the Hancock farm during 1982 and  1983
were not statistically  significant (a = 0.05).  The hydraulic flow to the
Gray farm, however, differed  significantly from 1982 to 1983.   A higher
mean flow  rate  was  received  at the Gray  farm  in 1983  (January through
October) than  in 1982 (February through December).  The difference was a
result of the combined  decreased flow to SeWRP and to  the  Hancock farm  in
1983.  In 1983 the Hancock farm  was  irrigated with water pumped  solely  from
the  surface reservoirs  at  the farm,  whereas  in  1982,  irrigation prior  to
planting (prewater)  and  40-45  percent of the summer irrigation was accom-
plished directly from  the  distribution  line  with  water pumped  from
Lubbock.
Effluent Quality
     Wastewater reuse  for  agronomic  purposes can be employed  with almost
any  type of waste which is amenable  to  biological treatment  (Deemer 1978,
Pound et.al. 1981).   Treatment efficiencies of land application  systems can
be quite high when designed  and  operated properly  (Table 16).  Constituent
removal efficiencies  will vary depending on the concentration  of the  con-
stituent in the applied wastewater and  hydraulic loading rate.
     During  the project  period, treated wastewater was monitored at  four
locations to characterize  the quality of irrigation water
     1)  the effluent from trickling filter Plant 2;
     2)  secondary effluent entering the Hancock farm;
     3)  secondary effluent pumped to the Gray farm; and
     4)  water pumped from the reservoirs on the Hancock farm.
Effluent from  trickling  filter Plant  #2 was monitored from September  1980
to February 1982. Water pumped  to the  Gray farm consisted of effluent  from
trickling  filter Plant #1 ,  trickling filter Plant #2,  and the activated
sludge plant.   Samples  of  the waste  stream to the Gray farm were collected
                                  107

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                   TABLE 16.  DESIGN EFFICIENCIES AND EFFLUENT QUALITIES OF CONVENTIONAL AND ADVANCED

                                      WASTE TREATMENT PROCESSES (Loehr et al.  1979)
o
oo

Design Removal Efficiency (%) Effluent Quality (mg/1)
Treatment Process
Conventional and AW Treatments
Preliminary Treatment
Primary Settling
Activated Sludge
Trickling Filter
Filtration
Activated Carebon
Two Stage Lime Treatment
Nitrification-Denitrification
Land Application Systems3
Irrigation
Overland Flow
Infiltration/Percolation
BOD3
0
20-40
75-95
75-90
50
60
-
-
98+
92+
85-99
SS ' P N BOD5 SS
0 0 0 210 230
50-65 - - 140 110
20 25
30 35
72 - - 10 5
60 - - 4 2
50
90 -
98+ 80-99+ 85+ 4 5
92+ 40-80 70-90 18 18
98+ 60-95 0-50 30 5
P N
11 30
-
-
-
-
-
0.5
3
2 6
2-7 3-9
4 15-30

      a  Influent  from preliminary treatment.

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from August  1982   to   September 1983.  Once secondary  effluent   was  trans-
ported to the Hancock  farm  in February 1982,  water  samples  were obtained
from the flow splitter  box  as the flow entered the Hancock farm.  Character-
ization of the waste stream  at  this location  was used to determine mass
loadings of various  constituents  to  the farm.   Sampling of  discharged
effluent from Plant #2  was  discontinued after wastewater was  pumped to the
Hancock farm. Arithmetic  mean values of the water  quality constituents  of
each irrigation  water  source is  provided in Table  C.1.  Median  concentra-
tion values were  used  in  computations and data interpretation when  the data
exhibited a high  degree of  skewness  (S).
     During  1980 and  1981, Lubbock's SeWRP was producing an effluent from
the trickling filter  system (Table  17) which had a composition  equivalent
to  a  typical medium   untreated domestic  wastewater  (Tchobanoglous  1979).
This  poor quality effluent was mainly attributable  to the  malfunctioning
of  the  anaerobic  digestion  process.  Effective liquid-solid phase  separation
was  not achieved in  the  second stage digester.  Consequently,  the  suspen-
sion recycled from the anaerobic  process to the head works of the trickling
filter  plant contained high levels  of ammonia,  suspended  solids and car-
bonaceous material.   From June  1980  to February 1982, the  average  effluent
total organic carbon  (TOC)  produced from trickling filter  Plant #2 was
117.7  mg/1.   Total  Kjeldahl Nitrogen  (TKN) concentration  averaged 38.59
mg-N/1  of which  67  percent was  ammonia-nitrogen (25.95  mg-N/1)   and  33
percent  was organic  nitrogen. Due to high organic  mass loadings  and  subse-
quent heterotrophic  organism activity, the trickling filter system  was not
nitrifying ammonia to  nitrate.  Approximately 57 percent of the  total phos-
phorus  (14.43 mg/1)  present in  the  effluent  from Plant #2 was  orthophos-
phate  phosphorus (PO^). During the  spring of 1982, SeWRP  placed on-line
additional anaerobic  digesters  and  rehabilitated the primary clarifiers  and
rotary distributors of the  trickling filter plants.
     The City of  Lubbock's  wastewater discharge permit  for  SeWRP required
the  plant to produce  an effluent  with a 30-day-average  5-day  biochemical
oxygen  demand (8005)  not greater than 45 mg/1.  During the project monito-
ring  period from February 1982 through October  1983 the effluent 6005
quality from SeWRP ranged from  a monthly high of 260 mg/1  to a monthly low
of 27 mg/1:
                                   109

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          TABLE 17.   CHARACTERIZATION  OF  EFFLUENT  PRODUCED BY
SOUTHEAST WATER RECLAMATION  PLANT  FROM JUNE  1980  THROUGH- JANUARY 1982

Parameter
Alkalinity (mg CaC03/l
Specific Conductance (ymhos/cm)
Total Dissolved Solids (mg/1)
pH
Chloride Ion (mg/1)
Sulfate Ion (mg/1)
Total Kjeldahl Nitrogen (mg N/l)
Nitrite plus Nitrate Nitrogen (mg N/l)
Ammonia Nitrogen (mg N/l
Total Phosphorus (mg P/l)
Orthophosphate Phosphorus (mg P/l)
Organic Phosphorus ( mg P/l)
Chemical Oxygen Demand (mg/1)
Total Organic Carbon (mg/1)
Concentration
Average
337
2216
1695
7.54
468
315
38.59
0.29
25.95
14.43
8.36
5.15
302
118

Standard
Dev iation
34
290
537
0.21
55
43
15.23
0.30
6.69
4.27
2.03
4.20
136
45
                              110

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1982
mg/1
143
260
198
139
108
.128
i30
76
69
171
63
86
1983
mg/1
71
120
105
65
30
39
49
27
43
3"1
63
49
                                 Average Monthly  Effluent 8005
                                 _Produced  by  Lubbock  SeWRP
              Month

            January
            February
            March
            April
            May
            June
            July
            August
            September
            October
            November
            December
     A higher  quality waste stream was pumped to the  Hancock and Gray farms
in 1983.  Average  TOC levels  at the terminus of the force main (Table C.1)
were 46 percent less  than the average concentrations measured in Plant #2
effluent samples obtained  from the previous (June  1980  through 1981) sam-
pling periods.
     No statistically significant differences  (a =  0.05) were observed in
TKN levels measured  in  the waste streams from Plant #2  (38.59 mg-N/1)  and
at the  terminus of the  force main  (41.70  mg-N/1).   As SeWRP1 s effluent
reached the Hancock  farm,  62  percent of the TKN was ammonia-nitrogen  (25.80
mg-N/1).   Ammonia-nitrogen was not significantly  different (a = 0.05)  from
the concentration measured in Plant  #2's effluent.   Therefore,  the data
indicate  no nitrogen  transformations through the force main. Total phos-
phorus  (TP) and organic phosphorus (Org P) levels  (11.82 mg/1 and  1.6 mg/1)
contained   in water   samples  obtained   from the  terminus of  the force
main  did decrease significantly from baseline (Plant  #2) effluent concen-
trations.   Orthophosphate   phosphorus  (PO^)   levels  measured at  both
locations  were  statistically  equivalent.  Consequently,  the decrease in
TP appears to be a result of a decrease in organic phosphorus mass loading
from  trickling filter Plant #2.  The improved anaerobic  digestion  capacity
                                  111

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and solids-liquid separation of digested sludge was probably the major con-
tributing factor to  the  decrease in organic phosphorus levels in Plant #2's
effluent.
     As  anticipated,  the bulk (71 percent) of the nitrogen contained in the
water  entering  the Hancock farm   (41 .77 mg-N/1)   was  lost   within  the
reservoirs.  Average effluent  TKN concentration was 11.74  mg-N/1.  The
median nitrite  plus nitrate  (N02 + N03) level in the reservoir discharge
stream was 0.27 mg-N/1.  Figure 39 presents the nitrogen cycle prevalent  in
waste  stabilization  ponds.  Nitrification of ammonia to nitrite and nitrate
does not normally occur  in stabilization ponds (Ferrara and Harleman  1978,
Pano .and Middlebrooks 1982, Ferrara and  "Avci 1982).  Insufficient nitrifiers
exist  in the upper aerobic zone of the pond.  Low nitrifier population  can
result from inhibition  by algae,  lack  of  aerobic  surface area to facili-
tate attachment  and  growth, or adsorption of  organisms  to particulates
which  settle into the  anaerobic  zone   (Ferrara and  Harleman  1978,  Stone
et al  1975).   Sporatic   checks of dissolved  oxygen (DO)  concentration
within the  water column of  reservoir #1  indicated  1  mg/1 or less  of DO  in
the upper 61 cm.   No dissolved  oxygen was measured  below 61  cm.  Stoichio-
metrically  the nitrification  process  requires  4.57 mg 02  for each mg  of
ammonia oxidized   (Christensen and Harremoes 1978).   Nitrification  was most
likely not  a major  contributor to the decrease in TKN.  Ammonia  nitrogen
in water exist  as ammonium ion  (NH4+)  and  dissolved  ammonia gas (NH3 ).  The
concentration  of the volatile  NH3  present in water is a function    of  pH,
temperature, and  concentration  of total  ammonia.  With water temperatures
varying from 10 to 21° C, Table  18 indicates a maximum of about 7.4 percent
NH3q present in the reservoir water  column at  an average pH of  8.3. Loss,  of
NH3  to  the atmosphere results in continued  dissociation  of ammonium
nitrogen to  dissolved ammonia gas.  With hydraulic  residence  time generally
greater  than 100 days,  and substantial  wind mixing  of the reservoirs, sig-
nificant quantities of ammonia  nitrogen  can-be lost  due to volatilization.
Therefore,  the most probable  mechanisms for loss of nitrogen within  the
water column in the reservoirs  were  ammonia volatilization  and  ammonia
assimilation in biomass  and sedimentation.
                                 112

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                              Ammonia Volatilization
                                                                                Denitrification
  Organic Nitrogen
                        Mineralization
Ammonia Nitrogen
                        N i t r if icat ion
Nitrate Nitrogen
                            Organism Growth
                                              Organism Growth
Net Loss To Sediment
   Figure 39.  Nitrogen  Cycle in Waste Stabilization Ponds (Ferrara  and  Avci 1982)

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      TABLE 18.  PERCENTAGE or FREE AMMONIA (AS NH,,  IN FRESH WATER

PH
7.0
7.1
7.2
7.3
7.4
7.5
7.6
7.7
7.8
7.9
8.0
8.1
8.2
8.3
8.4
8.5
Ml vrtrUiiNb pn MIML
10UC
0.19
0.23
0.29
0.37
0.47
0.59
0.74
0.92
1 .16
1.46
1.83
2.29
2.86
3.58
4.46
5.55

	 	 " -""

Temperature u
0.27
0.34
0.43
0.54
0.68
0.85
1 .07
1.35
1.69
2.12
2.65
3.32
4.14
5.16
6.41
7.98
0.40
0.50
0.63
0.79
0.99
1.24
0.56
1.05
2.45
3.06
3.83
4.77
5.96
7.36
9.09
11 .18
0.55
0.70
0.88
1 .10
1.38
1.73
2.72
2.72
3.39
4.24
5.28
6.55
8.11
10.00
10.17
14.97

    Algae growing  in  alkaline, hard water prefer bicarbonate rather than
carbon  dioxide as a carbon source  (Wetzel 1975).  The enzyme-catalyzed  up-
take of bicarbonate produces a  strong base:
                        HC03^=±C02 + OH~                              (D
Ruttner (1963) noted that algae which utilized bicarbonate  exerted  a  sig-
nificant effect on water pH.   This effect was also observed in the Hancock
reservoirs.  The average pH of  8.30 was significantly  ( a = 0.05) greater
than the effluent pH (7.76)  produced by SeWRP.
     Domestic wastewater contains  phosphorus in three  forms:  1)  organic-
ally bound  phosphorus; 2) condensed  phosphorus; and 3) orthophosphates.
Organically  bound phosphorus is normally the  least abundant of  the  three

                                  114

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forms and  exist  in ester and anhydride configurations  (R-OPC^PC^) and as a
phosphogen  (R-NPQ^) (Ryczak  et al 1977).   These organic  compounds are
components of  proteins, phospholipids,  nucleic acids and bacterial  cell
mass.   Condensed phosphates  consist of two or more  phosphorus atoms in a
ring or chain  structure.
     Sources  of condensed phosphates are detergents and metabolic by-prod-
ucts from  the  breakdown of human waste.  In an aqueous environment  these
inorganic   phosphate  compounds  slowly  hydrolyze  to   orthophosphate phos-
phorus. Hydrolysis of condensed phosphates is affected by  temperature  and
microbial concentrations  (Loehr 1974).   Aerobic biological wastewater
treatment  breakdown  condensed phosphates to orthophosphates.  Data present-
ed  in  Table C.1 indicate approximately 85 percent of the total phosphorus
contained  in  the effluent (11.82  mg/1) pumped to the  Hancock  farm  was
orthophosphate (8.43 mg/1).  Assimilation of orthophosphate phosphorus by
biomass for cell synthesis and adsorption  of orthophosphate to solids fol-
lowed  by   sedimentation decreased PO^ through the Hancock reservoirs from
an  average level of  8.43 mg/1 to 4.85 mg/1. Total phosphorus concentrations
were reduced by 47 percent  from 11.82 mg/1 to 6.31  mg/1.  Orthophosphate
removal in the reservoir account for about 65 percent  of the decrease in TP
(Table C.1).
     The  wastewater effluent  pumped to  the  Gray farm was significantly
affected by the activated sludge plant.  The nitrate-nitrogen concentration
averaged  3.45 mg/1  (Table C.1).  Since nitrification  in the trickling fil-
ter  plants was inhibited by high organic mass  loadings,  nitrate-nitrogen
was produced in the activated sludge  process  which had a hydraulic and
solids residence time of 8-10 hours and 4-10 days,  respectively.   Further-
more,  the higher  treatment  efficiency  of the   activated  sludge  plant
decreased   the TOC levels to an average of 52.6 mg/1.   Uptake of phosphorus
by  suspended biomass, also,  significantly reduced the average TP concen-
tration (9.18  mg/1)  in the waste stream pumped to the  Gray farm.
     As previously indicated, the sewage treated by the SeWRP was primarily
derived from domestic sources with less than 30 percent  contributed  from
industrial  sources (Section  4).  Trace  metal  levels contained in SeWRP
effluent (Table  C.1) reflected this low industrial  wastewater flow and pre-
sented  no potential phytotoxicity  problems (Table C.2).  Table 19 summar-
                                 115

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TABLE 19.
CONCENTRATION OF TRACE ELEMENTS IN TREATED WASTEWATER
Element
As
B
Cd
Cr
Cu
Hg
Mo
Ni
Pb
Se
Zn
Wastewater
Range*
(mg/1)
<0. 005-0. 023
0.3-2.5
<0. 005-0. 22
<0. 001 -0.1
0.006-0.053
<0. 0002-0. 001
0.001-0.018
0.003-0.60
0.003-0.35
0.004-.35
Effluent
Median*
(mg/1)
<0.005
0.7
<0.005
0.001
0.018
0.0002
0.007
0.004
0.008
0.04
Median Concentration (mg/1)
SeWRP
<-0.005
0.027
<0.0005
O.Q60
<0.047
<0.0004
<0.003
0.065
0.032
<0.005
0.133
Hancock
Reservoir
<0.005
0.038
<0.0005
0.006
<0.033
<0.0004
<0.003
0.007
<0.005
<0.005
0.066

* Chang
and Page, Land Treatment of Wastewater,
TABLE 20. WATER SALINITY SCALE (U.S.
Vol. 1, pp.
GEOLOGICAL
47
SURVEY)


Class

Dissolved
(milligrams
Solids
per liter
Fresh
Slightly saline
Moderately  saline
Very saline
Briny
                                      0  -   1,000
                                   1,000  -   3,000
                                   3,000  -  10,000
                                 10,000  -  35,000
                                     over  35,000
                             116

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izes the  concentration ranges of specific trace  metals measured in treated
wastewaters.   No  significant differences (a =  0.05)  in trace metal and min-
eral levels were  determined between any irrigation  water source from Febru-
ary 1982 to October 1983.
     The data  indicate that minerals, particularly  sodium (Na), may create
salinity and sodic  problems within the upper soil  profile.   According  to
the Water Salinity Scale  presented in Table  20,  the effluent pToduced by
SeWRP was slightly  saline (Dissolved solids from  1000  to  3000 mg/1).   The
low hydraulic loading  to  .the Gray  and  Hancock farm (20 to 60 cm) could
create accumulation of salts within the upper  soil  profile.  Without proper
salt management,  salts could pose future phytotoxicity problems to farmers.
The sodium absorption ratio (SAR)  of the effluent  stream from trickling
filter  Plant #2  averaged 9.84.  Evaporation and  transpiration remove water
from the soil,  thereby concentrating calcium and magnesium  carbonates  in
the soil solution and  eventually  resulting  in formation of calcium and
magnesium carbonate precipitates.  Reduction of these  cations from the soil
solution increases  the SAR.  Accounting for calcium  and magnesium carbonate
precipitation, the  adjusted SAR for  Plant #2 effluent  was 21.6. Irrigation
water  with an adjusted  SAR  above ten may create  severe water penetration
problems and development of alkali soils (Stromberg  and  Tisdale 1979,  EPA
1981,  Loehr et al  1979). Proper management of  salts contained in the irri-
gation water was  viewed  as  the most  important  task  which  would govern  the
long term success of the land  application system.
     Organic contaminants present  in wastewater  originate from diverse
sources.  Dissolved and  particulate  organic materials are released from
human metabolic activities  and excretion; metabolic  by-products from  bac-
terial  decomposition of  organic waste;  algal  and fungal excretions; and
metabolic by-products,  infiltration and inflow,  and  industrial wastes.
Certain  priority organic  contaminants can cause  (or are suspected causes
of) irreversible  biological effects including cancer  (carcinogenesis) ,
transmissible genetic damage (mutagenesis) , and  birth defects (teratogene-
sis).   Currently, there are severely limited toxicological data for organic
compounds;  therefore, a great deal of uncertainty  exists about the health
risk of low-level chronic exposure (Pettygrove  and  Asano  1984, Majeti  and
Clark 1981).  Feiler 1979 presented  information which  indicates trace
                                 117

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organic  concentrations  are effectively reduced by conventional wastewater
treatment. Table C.1  presents  the mean concentrations of  priority  organic
pollutants isolated  from  SeWRP's effluent.  Tables C.3 and C.4 present pri-
ority organic pollutants  measured in municipal wastewater  treatment  plant
effluents in Orange  County, California, Dayton, Ohio, and Cincinnati, Ohio.
The data indicate the-variety  of trace organics existing in treated  waste-
water depending on source.  Since  agriculture is the major .industry in the
Lubbock area, herbicides  (e.g., atrazine and  propazine)  and by-products
produced  from the d'ecomposition  of herbicides (e.g.,  2,3-dichloroaniline
and 3,4-dichloroaniline)  existed in the SeWRP's  effluent.   Carbon tetra-
chloride,  chlorobenzene, and diethylphthalate levels exceeded the respec-
tive organic concentration range  shown in  Tables C.3 and  C.4.  A mean
anthracene  concentration  of  6.1  yg/1,  4.0 yg/1 and 8.4 yg/1 contained  in
the effluent from Plant #2; wastewater pumped  to the Gray farm; and efflu-
ent  at  the  terminus  of the force main exceed  range  of concentration (0.16-
0.68 ppb)  reported by-Overcash (1983).  Remaining organics  which were com-
mon  to  trace  organics  listed in  Tables  C.3 and  C.4 were  well within
reported  general  concentration ranges.
     The  average  fecal coliform concentration  in  the waste  stream  pumped  to
the center pivot  irrigation machine  exceeded EPA guideline throughout the
study period.   The guidelines  state:
        "Biological treatment  by ponds or  inplant   processes  plus
        control of  fecal coliform   count  to less  than  1,000  MPN/
        100  ml  -  acceptable for controlled  agricultural  irrigation
       except  for human  food  crops  to be  eaten raw."  (USEPA,  1981)
The actual  flow-weighted average  fecal coliform concentrations of the
applied wastewater during  the  four major  irrigation  periods were:
                                     Fecal  coliform  concentration
                                 colony  forming  units  (cfu)/100 ml
              Spring.1982                     4,300,000
              Summer 1982                        840,000
              Spring 1983                          5)2OQ
              Summer 1983                        120,000
    During system operation, the fecal coliform concentration  of the waste
                                118

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stream  from  SeWRP and  the discharge  from the storage reservoirs  greatly
exceeded  EPA guidelines,  especially in 1982.  The effluent  BOD5  concentr-
ation produced  by  SeWRP  did not satisfy Texas permit requirements  until  May
1983.  The system,  however, was operated below hydraulic design  capacity  in
1982 and 1983.
FARMING OPERATIONS
Hancock Farm
     During 1980 and  1981 the Hancock farm was mostly dryland farm.  Approx-
imately 13 percent of the land was  irrigated with water  from the  Ogallala
aquifer.  Cotton was  the major crop grown.  Agricultural yields  for  Hancock
farm in 1980 varied from less than  112 kg/ha (100 Ib/ac) to 415  kg/ha (370
Ibs/ac).   During  the  1980 growing season the high temperature  for  30 days
exceeded 38°C (100°F).   Temperature in conjunction with  low  precipitation
(less  than 47  cm)_ reduced yields.   Base yields provided by Agricultural
Soil Conservation Service (ASCS), Lubbock, Texas, for the Lubbock  area  (10
year average) were approximately 337 kg/ha (300 Ib/ac).
     Cotton yields in 1981  ranged from 118 kg/ha (105 Ib/ac)  to 314 kg/ha
(280 Ib/ac).   In  1981  crops were planted; lost  due  to hail  in May;  and
replanted by the first  of June.  Additional rain and hail (12.5  cm)  in June
reduced crop stands.  Normal growing season for cotton  on the South Plains
is  120  days.  Any gain  in  yield  incurred by  replanting  to increase  the
population would  have been offset by a shortened growing season  (60 to  90
days).  After the early spring rains, soil moisture was  fairly normal until
September and  October when some yield (estimated 15 percent) was lost  due
to  late hail storms.
     Prewatering of fields  with  effluent began in February 1982.   Center
pivots  were operated  using  effluent directly from SeWRP.   Pivot operation
was subject to the diurnal  variation of water pumped by  SeWRP.  Application
of summer irrigation  under  these conditions was labor intensive  until July
when the  use of  reservoir 1  and  final adjustments on  automation made  the
system more manageable.
     Rainfall  and associated hail during  the month  of June  (Figure  40)
destroyed over 8.09 x  105 ha (2  x 10$  acres)  of the cotton  crop in  the
South Plains.   Only 16.2 ha (40 ac) of cotton remained beneath pivot 14.  In
                                  119

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          o
          o
                                                                           O Lubbock Airport
                                                                           O Normal Precipitation
                                                                           A Hancock Farm
                                                                           -j- Gray Farm
K3
O
          1.00       6.00       11.00      16.00      21.00      26.00      31.00
                                     MONTHS  (JUNE 1980-SEPT  1983)
       Figure  40. Precipitation During Project Period
36.00
m.oo

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addition,  wheat and  oats  double crop areas suffered severe damage and yield
loss (i.e.,  pivot 15 oats was  never harvested  and Pivot  6  had 50 percent
loss) .   The majority of  the  farmers planted grains to partially recuperate
financial  losses.  Tenant farmers  at the Hancock  farm planted approximately
552 ha (1365 ac)  of  grain sorghum,  162 ha (400 ac) of sunflowers,  and 257
ha (635 ac)  of soy beans  (Figure G.1).  The amounts of water pumped through
the  center  pivot irrigation machines in 1982  are presented in Table 21.
Operational  problems from plugged  screens  and  valves, plus complaints  of
odors  resulted  in  less  and  less use  of  irrigation  direct from the line.
Figures G.2, G.3, and G.4 show the sources of irrigation  water  in  July,
August and September 1982.   A water mass balance  indicated only two percent
of the water could not be accounted  for from February 19,  1982 to January
1, 1983 (Table D.1)  .
     Even with the nearly disastrous winter crop  production (double cropped
areas), the farmers planted portions of the farm  in oats  or wheat in  late
fall 1982 (Figure  G.5).  Durham  wheat was planted on portions of pivots 7
and  10 in February 1983 and was  grown  for  seed  production and not for human
consumption.   The  lack of crop  growth  on double cropped areas, was the
first  indicator  that nutrient uptake by crops  grown during  the summer  had
depleted the  available nutrients  within the root  zone. Furthermore,  actual
average nitrogen mass loading  to   the farm   was 58.5   kg/ha,  which  was
less than  design  loading of 120 kg/ha.  In  spring 1983,  several farmers
applied dry fertilizer [ranged from  68 kg/ha (150  Ib/ac) of 14?o N-6?o P-6% K
to 91  kg/ha (200 Ib/ac) of 20?o N-10?o P-5?o  K] to the soil or liquid fertili-
zer  through the  pivot [36 kg/ha (80  Ib/ac) of  20?o  N-5?o P-5?o K. Sulphur  was
applied beneath  pivots  15,   14,  and 11 to  determine if salts might be
inhibiting germination.   Since  nitrogen  was  incorporated into  the  soil
beneath several  irrigation machines, nitrogen  was  applied to soil irrigated
by pivots 15,  14, and 11  to remove nitrogen as  a   confounding factor during
the  sulfur test.  Table G.1 presents yield and  other data for these strips.
The  only difference attributable to  fertilizer  application, which may be of
interest, was the increase in plant   population  in every case where sulfur
was  applied.   Salts may  have  inhibited plant germination or burned  the
epicotyl during germination.
     During  the summer  of 1983,  less than  2.5  cm  (1  inch)  of rain was
                                  121

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Pivot #
1
2
3
4
5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
1ABLL 2

1 . IUI AL W,
	 -
Prewater
cm (in)
7.49
6.38
6.38
3.73
6.99
4.83
6.60
6.22
7.06
5.28
4.75
3.76
5.00
4.45
4.29
4.17
5.08
7.04
2.54
2.79
6.53
-4.34
2.95
_ 2.51
2.51
1.47
2.75
1.90
2.60
2.45
2.78
2.08
1.87
1.48
1.97
1.75
1 .69
1 .64
2.00
2.77
1.00
1 .10
2.57
1 .71
H I Lr\ MrrL-.-n-u' i^ iui"~ — 	 	 . —
** * ~—i
	 	 . 	 . 	 • 	
Summer Irrigation
cm (in)
	 • 	
5.74
14.12
5.89
19.43
4.80
7.82
13.08
8.36
7.32
7.85
19.05
16.74
11 .25
6.47
21 .82
10.52
12.07
11.46
13.18
12.73
10.41
10.44
2.26
5.56
*2.32/ % pivot = 4.64
7.65
1 .89
*3 ,08/ % pivot = 6.16
5.15
3.29
2.88
3.09
7.50
6.59
4.43
2.47
8.57
4.14
4.75
4.51
5.19
5.01
4.10
4.11

Total
cm
13.23
20.50
18.16
23.16
11 .79
20.47
19.69
14.58
14.38
13.13
23.80
20.50
16.26
10.72
26.06
14.68
17.15
18.49
15.72
15.52
16.94
14.78

1982
(in)
5.21
8.07
7.15
9.12
4.64
8.06
7.75
5.74
5.66
5.17
9.37
'8.07
6.40
4.22
10.26
5.78
6.75
7.28
6.19
6.11
6.67
5.82

* Pivots 3 and 6  were  planted one-half oats  and  one-half summer crop.  When
oat crop was lost,  that  half of  pivot was  left summer  fallow and rceived no
irrigation.  Therefore,   the actual applied  irrigation is double the calcu-
lated amount in this table.
                                   122

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recorded  from  the end of June  through mid-October.  Table 22  shows  the
irrigation per  pivot for 1983.  The projected  1983 hydraulic loading was
expected  to  range from 38  to 41  cm  (15 to 16  inches/year).  The  irriga-
tion schedule  for pivot 15 (Figure 41) was  designed to  irrigate this
amount.   SeWRP's effluent,  except for  few minor quantities, was  pumped to
the reservoirs  prior to transport to the center pivot irrigation machines.
Nutrients  such  as  nitrogen decreased by  an average of 71 percent from  30-45
ppm to 5-7 ppm  (Table C.1),  thus  greatly reducing supplemental  fertiliza-
tion  anticipated  in the irrigation water-  Irrigation of cotton was  ceased
at the end of August.  At the completion of  irrigation, less than  1 m of
water  existed  in the reservoirs.  A  frost occurred in mid-September  and
halted cotton fiber growth.   Subsequent  regrowth did  not  increase lint
yields.
     Figure  G.6  shows  the  crops  grown in  1983 at the Hancock farm.   The
ASCS  ten year   average for   irrigated  cotton  in  this area was  393  kg/ha
(350 Ibs/ac).

Gray  Farm

     Secondary treated effluent from SeWRP was delivered  to the  Gray  farm
through three pipelines to   three  storage   reservoirs  (Figure 4).   The
ponds had a surface area  ranging from 0.2 ha  to  24.3 ha and an  average
storage depth of one  meter.   The  estimated  usable storage capacity was
250,000  m^.  Consequently, the ponds could  have  stored  less  than  0.25
hectare-cm per  hectare  of irrigated  farmland.  The estimated hydraulic
retention time of the ponds was 10  days.  Irrigation methods employed at
the farm were flood, row water, and center pivot irrigation machines.
     Prior  to  1982,  with 75 to  80 percent of the farm planted in  cotton,
water was applied  to the cotton areas in  early spring, February through
April (prewater);  and in the summer from June through August.  An  estimated
70 cm of water was applied  to the land  designated  for  cotton planting
(Table 23).  Any other irrigation (the remaining six months), with no stor-
age, had  to be  put on winter crop or grazing area (Figure 42).  From  two to
4.5 m/yr  was applied to these areas in order to keep the main economic  crop
(cotton)  at maximum production.   Figure  G.7 shows the areas and respective
                                 123

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lAbLL LL . lUlttL NMll-i\ ni i

Pivot No.
1






5
6
7
8
9
10
11
12
13
14
15
16
17
18
19
20
21
22
	 	 ~ Total
(cm)
20.0
34.0

27.0

48.0

40.9
50.0
31.8
26.9
38.4
29.0
29.2
31.0
33.3
22.9
43.9
35.3
29.2
29.0
30.2
17.5
20.6
27.4

1983
(in)
7.9
13.4

10.6

18.9

16.1
19.7
12.5
10.6
15.1
11.4
11.5
12.2
13.1
9.0
17.3
13.9
11.5
11.4
11.9
6.9
8.1
10.8
124

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N>
    E
    o
    .g
    '«*3
    CD
    O)
    t   2-
                                                                                 COTTON
                                                                             A   MILO-SOYBEAN
                                                                            •• •  WHEAT - OATS
                                                            AUG ' SEP  '  OCT  ' NOV  '  DEC
                                                 1983
           Figure 41.  1983 Design Hydraulic Loading to Pivot #15 by Crop

-------
r-o
OS
        Figure  42.   Winter 1982 Crop and Grazing Areas at Gray Farm

-------
methods of application.
               TABLE 23.   GRAY  FARM  HYDRAULIC LOADINGS/CROP

Approximate loadings applied based on
number of potential operation during the
Season
Prior
1982
1982
1983
Flood Cotton
1 2
(kmd)(mgd) (cm)(cm)
to
53 14 70 65
38 10' — —
38 10 — —
Milo
1
(cm)
—
70
70
maximum output of center pivot and
growing season
Wheat
1
(cm)
465
230
207
Soybeans
1
(cm)
—
70
—
Alfalfa
1 1
(cm)
—
70
70
(cm)
—
55
55

 '  Row or flood  irrigation areas.   Row  water crops  are based on one pre-
   water application and six summer  time applications.
 2  Center pivot irrigation — Pivots are nozzled to deliver 15 cm/21 days,
   over six months application time  (seven  on alfalfa). This yields hydrau-
   lic loadings of 90 cm  (105 cm  on alfalfa).  Because only  enough pivots
   are on hand  to irrigate one-half of  the acreage at any one time,  these
   loadings must be halfed to 45 cm/yr .and  52 cm/yr, respectively.
      In February 1982 the farm was  purchased by the Vladic family.  The new
 landowner immediately took action  to  turn the farm into cattle grazing and
 the production of alfalfa hay.  In  the spring of 1982 the  Vladics planted
 over  506 ha (12-50 acres) in alfalfa (Figure G.8), 304 ha (750 ac) of wheat
 (Figure G.9,  and 121 ha (300 ac) of soy beans (Figure G.10).  During  this
 year  between 30  and 40 percent of this land had a poor alfalfa stand and
 required replanting.
     Due to  the time of year the  alfalfa was planted, severe weather con-
 ditions after planting,  and excessive weed  growth, a low yield and  poor
 quality  hay resulted.   The major  factors limiting proper water management
 were hydraulic  limitations  of the  center pivot   irrigation machines  and
 inadequate  storage.
     After the  poor crop  of 1982, no further expansion of the hydraulic
distribution  system  or capital expenditures  were  made.   The alfalfa  crop
was watered  with  whatever  equipment was available.  The inability to apply
enough water  through the existing center pivots  was a limiting  factor  to
                                 127

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crop production.  Highly  efficient haying  operations with no  irrigation
limitations,  strive to attain a 28 to 30  days  harvest  frequency.   With one
month between cuttings, the towable center pivots could not supply suffi-
cient water  for two fields (approximately 49 ha  each). Without the  capital
to purchase  more center pivot  irrigation machines, the Vladics had two
options:
     1)   Water both 89 ha  (120 acres)  fields  with one towable pivot;  thus
         apply only 10 to 15 cm   (four to six inches)/cutting.   The entire
         alfalfa  area  could be   harvested;   however,  drastically reduced
         yields   (50 percent or more)  would have  resulted.  This alterna-
         tive also  forces the  harvesting equipment  to cover   the entire
         alfalfa  area.
     2)   Keep the center pivot  on just one field until 25 to 30  cm  (10 to
         12  in) have been applied and a good growth  (30 to 41 cm) has been
         been achieved for harvest.  Then the  towable  pivot  could be moved
         to  the other field.  This type of watering schedule  would reduce
         the  areas the  harvest equipment had  to cover in one month;  how-
         ever, it would  have reduced harvesting  on a particular  field to
         every other cutting.  This policy would greatly decrease the total
         year's harvest (50 percent or more).
The second  alternative was the alternative taken by the Vladics.

HYDROGEOLOGIC INVESTIGATION
     An  objective of  expanding  the  Lubbock land treatment system was to
relieve  the  hydraulic and  nutrient mass overloading experienced  at the
Gray land  application site.  Prior  to diverting treated wastewater to the
Hancock  farm, the  Gray  farm received up  to 57,000  m3/day  of  SeWRP
effluent  which was used to irrigate  approximately 1200  ha (Wells  et al,
1979).   This was an  average  (over the  entire farm) hydraulic  loading of
1.7 m.   Reported annual consumption by the type of crops grown at the  Gray
farm varied  from 133 cm for  cotton  to 219 cm  for alfalfa (FAD, 1977).
Consequently,  water not consumed  by crops accumulated  in  surface impound-
ments, percolated  to the ground water, evaporated,  or exited the farm as
surface  runoff.  Estimated  useable storage at the Gray farm was  250,000 m3
(203  ac  ft) which provided a storage detention  time  of  about four  days.
                                 128

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Consequently, management was a severe problem  at  the Gray farm.
     Water  percolation to the ground  water created a  ground-water  mound
beneath  the Gray  farm.   Depth  to  water ranged  from 4.6  m (15  ft)  to
22.8 m (75  ft).   Ground-water levels in wells  north of  the Gray farm  moni-
tored  by the Texas  Department  of  Water Resources and  the High  Plains
Underground Water Conservation District No. 1  ranged from  25.5 (83.5  ft)
to  29.5  m  (96.7 ft).  Degradation of ground-water quality beneath a land
application site depends on such  factors as hydraulic application  rate,
schedule of application,  crop uptake  of chemicals,  soil profile charac-
teristics,  concentration  of constituents in the irrigation water,  and
climate  (Hook and Kardos 1978,  Iskandar and  Wright 1983, Bole et al 1981,
Hinesly, Thomas  and  Stevens 1978,  Oldham 1975). Ground-water quality
beneath  the Gray  farm was degraded  due to  water management problems and
inappropriate cropping patterns.  Literature does not provide information
evaluating the  effects  of hydraulic  and chemical mass reduction on the
soil, water, and crops characteristics of an environmentally degraded  slow
rate land  application site.  The objectives  of  the hydrogeologic investi-
gation were as follows:
      1.  Determine the effect of  slow rate  irrigation  of secondary treated
         wastewater on  ground-water-quantity   and quality beneath the Han-
         cock farm which had no previous history  of wastewater irrigation,
         and
      2.  Determine  the effects  of reducing   hydraulic  and chemical  mass
         loading at the Gray  farm on ground-water quantity and quality.
Water Level Data
      Table  24  gives January water levels for  wells which were part of the
State of Texas  and/or U.S. Geological Survey (USGS) water levels measuring
program  which are located in the vicinity of  each farm.  State well loca-
tions are indicated on Figures D.I and D.2.
Gray Farm Depth  to  Water Measurements—
     Water  levels measured  in the  observation  wells  on the Gray farm are
shown in  Figures D.3  through D.6.   The figure  on  the left ordinate scale is
the  average depth  to water in the well based  on  all measurements; the well
number designation  is to the right of the trace.  Each small division is
                                 129

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                                           TABLE 24.  JANUARY WATER  LEVELS  IN  STATE  WELLS
                                    Data  from  Publications of  Texas Department  of Water Resources
                                 and Files  of High  Plains  Underground  Water  Conservation District  //1
CD

Well No.
Elevation of
Land Surface
Depth to Water
1979
1980
1981
rn (ft)
1982
1983
1984
GRAY AREA
26-301
26-603
27-102
27-201
27-204
27-402
974.8
963.2
961.6
958.0
•957.1
958.0
(3198)
(3160)
(3155)
(3143)
(3140)
(3143)
28.5
4.2
N/A
29.1
28.9
22.9
(93.5)
(13.8)
N/A
(95.5)
(94.8)
(75.2)
28.3
3.0
25.5
28.6
28.6
N/A
(93.0)
(9.9)
(83.7)
(93.9)
(93.7)
N/A
28.6
3.9
25.5
29.5
29.3
22.6
(93.7)
(12.9)
(83.5)
(96.7)
(96.0)
(74.3)
28.5
4.5
25.8
28.8
28.4
22.3
(93.6)
(14.6)
(84.6)
(94.5)
(93.3)
(73.0)
27.9
6.0
24.8
28.2
28.0.
21 .7
(91.0)
(19.8)
(81.5)
(92.4)
(91.9)
(71.2)
27.7 (91.0)
3.8 (12.6)
24.7 (81.2)
27.6 (90.5)
27.7 (90.9)
21.8 (71.4)
HANCOCK AREA
34-801
34-901
35-704
35-707
35-801
42-301
42-602
43-501
43-502
968.0
961.3
956.8
952.8
945.8
961.6
951.9
941.8
944.3
(3176)
(3154)
(3139)
(3126)
(3103)
(3155)
(3123)
(3090)
(3098)
45.7
44.8
41 .1
40.1
26.7
33.5
27.3
21.6
23.9
(149.8
(146.9)
(135.0)
(131.6)
( 87.7)
(109.9)
( 89.5)
( 70.9)
( 78.5)
44.9
43.9
41.1
40.0
26.7
33.3
26.6
21 .9
23.8
(147.4)
(144.1)
(134.7)
(131.2)
( 87.5)
(109.3)
( 87.2)
( 71.9)
( 78.1)
45.4
45.2
42.2
40.8
26.7
33.7
27.4
22.0
24.1
(148.9)
(148.4)
(138.4)
(133.8)
( 87.5)
(110.7)
( 89.9)
( 72.2)
( 79.2)
45.5
45.0
42.1
40.9
26.8
33.6
27.3
22.1
24.1
(149.4)
(147.7)
(138.1)
(134.3)
( 87.8)
(110.4)
( 89.7)
( 72.4)
( 79.2)
45.1
45.4
42.5
40.5
26.8
33.8
27.5
21.8
23.7
(148.0)
(149.1)
(139.5)
(132.8)
( 87.9)
(110.8)
( 90.3)
( 71.5)
( 23.7)
44.5 (145.9)
43.2 (141.6)
41.3 (135.6)
40.1 (131.5)
27.0 ( 88.6)
32.8 (107.6)
25.7 ( 84.3)
21.0 ( 68.9)
.23.3 ( 76.4)

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30.5 cm  (1  ft).  Table  25  shows the initial,  minimum, maximum and ending
depth-to-water  measurement.
     Figure 43  presents ground-water level contours  beneath  the Gray farm
in December 1981.   Flow occurs from the Gray site toward the  north,  east,
and  south.  During  1981, the quantity of flow to the  north  and east was on
the  order  of 1.28  m3 per  day per meter of boundary  or about 6166 to 7400
m3/day  (5  to 6 ac-ft/da).   Water losses   of 4316  m3/day (3.5 ac-ft/da)
occurred  through  the canyon walls  on the south,  and  withdrawals  by the
City of Lubbock  averaged  4563 m3/day  (13.7 ac-ft/da). Using an average
delivery rate of 56,775 m3/day (15 MGDT, the required  evapotranspiration on
1052 ha (2600  ac)  was  40,821 m3/day  (33.1 ac-ft/ da) or  142.2 cm/yr (56
in)/yr).  Potential annual   evapotranspiration  were  calculated  as  170.2
cm/yr (67 in)(Ramsey et  al 1983).  This site appears to  have been in hydro-
logic balance.
     During May and June  1982,  a total precipitation  of 34.82 cm (13.7 in)
was  recorded at the Gray  farm  (Ramsey et al 1983) which was 74 percent of
the  average precipitation  for the area.  The ground-water  levels in wells
6880, 6884, and 6892 measured  in Dune rose 9.1 m, 5.4  m, and 7.3 m, respec-
tively. These  wells  probably experienced recharge due to  flooding as a
result  of the very large  rainfall.  During 1983 there  appeared to be  some
indication that water  levels in the observation wells  dropped.
     In  1982 only 25 percent of SeWRP's total effluent  (16.65 x 106 m3) to
be used  for irrigation was transported to the  Hancock farm.  From January
1,  1983 to October 31,  1983, the Gray farm received 11.41 x 106 m3 which
was  75  percent of the total effluent applied to land  and 3.74 x 10^ m3 was
pumped to the Hancock farm.  Consequently,  the  decline in  ground-water
level beneath  the  Gray  farm  probably  was only slightly  affected by the
transfer of water  to the  Hancock farm.  The change in  cropping pattern to
alfalfa may have been  the  major  contributing factor to  the decrease in
ground-water level.   The  trend was noticeable only during 1983 (a drought
year) and may not  be sustained in the future.
Hancock Depth to Water Measurements—
     Hydrographs for the  22 observation wells at the Hancock site are shown
in Figures D.7  through D.11.  Table 26 presents the initial, minimum, maxi-
mum  and ending depth-to-water measurements.  Irrigation pumps on the  farm,
                                 131

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TABLE 25.   STATISTICS  OF  DEPTH  TO  WATER  IN  OBSERVATION WELLS
               AT GRAY SITE  DURING PROJECT

Depth to Water
Well No.
6880
6881
6882
6883
6884
6885
6886
6887
6888
6889
6890
6891
6892
6893
6896
6895A
6895B
6895C
6895D
7000
Initial
19.9
21.5
22.9
18.9
8.5
8.2
15.2
10.7
19.8
13.7
4.6
5.1
8.5
12.1
12.6
13.8
7.9
7.7
7.7
6.9
(65
(70
(75
(62
(28
(26
(50
(35
(65
(45
(15
(16
(28
(39
(41
.3)
.6)
.0)
.0)
.0)
.8)
.0)
.0)
.0)
.0)
.0)
.7)
.0)
.6)
.3)
(45.3)
(25.8)
(25.4)
(25.3)
(22.8)
Minimum
10.61
21.3
22.3
18.6
5.3
5.0
15.2
10.7
19.8
13.2
3.4
4.1
3.4
10.1
3.6
9.7
5.9
5.9
6.1
5.9
(34
(34
(73
(61
(17
(16
(50
(35
(65
(43
(11
(13
.9)
.9)
.0)
.1)
.3)
.4)
.0)
.0)
.0)
.3)
.3)
.4)
(11.0)
(33.0)
(11.9)
(31.7)
(19.4)
(19.5)
(19.
(19.
9)
3)
m (ft)
Maximum
19.9
22.1
25.6
21.0
10.7
10.1
16.7
13.2
21 .3
14.4
5.8
6.1
12.2
12.1
15.0
13.8
8.3
8.3
8.7
8.3
(65
(72
(84
(68
(35
(33
(54
(43
(70
(47
(19
(20
(40
(39
.3)
.5)
.1)
.8)
.1)
.0)
.7)
.2)
.0)
-4)
.1)
.0)
.0)
.8)
(49.1
(45
.3)
(27.2)
(27,
.2)
(28.4)
(27.2)
F inal
17.7
21.5
22.2
18.9
9.2
8.4
16.5
12.8
21.2
14.3
4.3
5.6
8.9
11.3
12.8
9.8
8.0
8.0
8.2
7.9
(58.1)
(70.5)
(73.0)
(62.0)
(30.2)
(27.6)
(54.1)
(42.0)
(69.5)
(46.9)
(14.0)
(18.5)
(29.2)
(37.0)
(42.0)
(32.0)
(26.2)
(26.2)
(26.8)
(26.0)
                               132

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Figure 43.  Water Level Contours in feet, December, 1901, Gray Farm

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TABLE 26.   STATISTICS OF DEPTH TO WATER  IN  OBSERVATION  WELLS AT
                       - - - - -  ~ - -^ ,- 1^.,,r-,T)Lir, n n n -j £- p -j-

Well No.
10112
10211
10521
10721
10731
10821
10842
10931
10932
11032
20112
20243
20711
20721
20842
21141
21152
21234
21323
30312
40231
40331


Initial
34.0
37.0
24.2
25.9
24?7
21.9
26.9
21.5
20.6
28.4
35.7
41.5
31.4
27.4
30.5
27.4
26.3
26.3
29.6
32.0
30.2
29.6
(11.1.4)
(121.5)
( 79.3)
( 85.0)
( 81 .0)
( 72.0)
( 88.1)
( 70.4)
( 67.7)
( 93.1)
(117.0)
(1.36.0)
(103.0)
( 90.0)
(100.1)
( 90.0)
( 86.2)
( 86.3)
( 97.1)
(105.0)
( 99.0)
( 97.0)
nniNuui.



Uepth to water in v i *-/
Minimum Maximum F
27.9
36.5
22.9
19.1
19.0
18.9
20.6
17.4
13.4
27.2
33.7
41 .5
31.1
24.8
25.3
25.0
22.0
22.7
29.0
31.4
29.6
28.2
( 91.6)
(119.9)
( 75.0)
( 62.6)
( 62.4)
( 67.7)
( 62.0)
( 57.0)
( 43.9)
( 89.3)
(110.7)
(136.0)
(102.0)
( 81.3)
( 83.0)
( 81.9)
( 72.1)
( 74.4)
( 95.0)
(103.1)
( 97.0)
( 92.7)
34.4
40.3
25.8
28.1
25.2
27.3
27.3
21.5
20.7
28.7
36.1
44.6
32.4
29.5
30.7
27.7
26.3
26.6
30.2
32.4
30.8
29.6
(113.0)
(132.1)
( 84.8)
( 92.2)
( 82.8)
( 72.0)
( 89.7)
( 70.5)
( 67.9)
( 94.3)
(118.3)
(146.3)
(106.3)
( 96.7)
(100.8)
( 91.0)
( 86.4)
( 87.3)
( 99.1)
(106.3)
(101 .0)
( 97.0)
32.6
36.6
22.9
19.1
1.9.0
18.9
24.9
18.3
15.5
27.4
34.2
41 .6
31.2
24.8
28.0
25.0
22.4
22.7
29.0
31.5
29.8
28.9
inal
(106.8)
(120.0)
( 75.0)
( 62.6)
( 62.4)
( 62.0)
( 81.8)
( 59.9)
( 51.0)
( 90.0)
(112.2)
(136.4)
(102.2)
( 81.3)
( 92.0)
( 82.0)
( 73.5)
( 74.4)
( 95.1)
(103.4)
( 97.7)
( 94.8)
                            134

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except  for  those adjacent to the City of Wilson, were removed  during  the
winter of 1980  in  anticipation of the new water supply.
     The 1981  crop  was  farmed dryland.  The hydrographs indicate little or
no change in water levels occurred during this period. In 1981  ground-water
flow  occurred  toward  both  the north and the south from  a ridge through  the
center of the property (Figure 44).  Flow to the south was at  a velocity of
about  0.152 cm/day  (0.005 ft/da)  and to the north at about 5.79  cm/day
(0.19 ft/da).  Flow  into the region  from the west was part of  the regional
flow; the divergence was caused by the  position of the Slaton  Channel.   The
remaining saturated  thickness  was less  than 6.1 meters (20 ft).   Depth   to
water  varied  from    24.4  to  36.6 m  (80 to  120 feet).   Considering   the
thickness  of the  unsaturated zone and the propensity  for clay  layering,
there was little likelihood that  treated effluent would reach the water
table during the life of the project.   Rather, water applied  in  excess  of
the  root zone capacity would be intercepted by a less  permeable layer  and
create,  at least temporarily,  a perched condition. This  would  lead to a
pronounced  lateral  flow  until the "edge" of the less  permeable layer  was
reached.  Downward migration would again commence until   another  layer  was
encountered.  Thus, the point of contact with- the water table  may be quite
distant  from the point of  application of the water.
      Precipitation  (19.7  cm)  during June 1982 caused the moat  areas  around
each  of  the  storage  reservoirs to fill  beyond  capacity.   These  areas  had
been excavated outside the original playa lake boundaries to  provide stor-
age  for  the  natural  runoff.  These newly excavated areas offered  an excel-
lent  opportunity for natural recharge to occur.   Almost instantaneous
(within  two months)  ground-water  rises were  recorded  in  wells  10931   and
10932.  These  wells  were  located approximately 250 m (800 ft)  apart.  Well
10931 was located on the edge  of an  area which had been  dredged out by  the
landowner just  to the  east  of  the Hancock property to provide  extra storage
for the surface runoff.  According  to TDWR's  permit  requirements, well
10932 was drilled  within the dredged out "moat" on the southeast side of
Reservoir 1. A  cement  plug  was poured around the upper  12.2 m  of the well
casing.   Water level measurements in February and April were  relatively
constant at 20.7 m (6.8  ft) to water.
     During June 1982  surface  runoff contained in the moat did  not submerge
                                  135

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                    Reservoir
                    Playa
                 1 cm = 0.27 km
CONTOUR ELEVATIONS IN FEET
    (.3048 METERS/FT)
Figure 44.  Water Level Contours,  December
          1981, Hancock Site

                              136

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the top  of  the well, however,  later  examination suggested that water had
entered the  hole outside the casing by  piping  underneath the concrete  pad.
The actual  recharge from the precipitation  event was reflected in the more
gradual rise (approximately 30 cm  in 18  months), beginning at about  that
time  and continuing until  the  end of  the measuring period (September/
October 1983).  This trend was evident in  each  of the wells except 10112.
This  well,  located in the northeast corner of the property, experienced a
rise (1.86 cm)  in  the fall of 1982 and  a  gradual decline during the summer
and  fall of 1983.  Pumping by nearby irrigation wells probably account for
this behavior.   Something of the same pattern  was seen in well 20112 on the
north boundary of the east-west center  line.  A water balance (Table D.1)
indicated ground-water recharge from surface runoff contained in the  moat
areas surrounding the reservoirs and  through  coarse material along the
fringes of playa  lakes most likely caused the  water level rises beneath the
farm. Irrigation amounts  during the  study period were far less than crop
evapotranspiration rates, and consequently do  not appear to be a source  of
ground-water recharge.
Soil  Moisture Studies
      Hydrographs of the weekly  soil  moisture measurements made with the
neutron  probe at  the  TTU research  site and  the LCCIWR  site are shown  in
Figures D.12  through D.16  and  Figures  D.17  and  D.18, respectively. The
depth of the observation  below the ground level is shown on the  right
ordinate and  the average  soil  moisture (percent, by volume) on the left
ordinate. The average value was closely related to the soil texture;  finer
textured soils exhibit  a larger  average  moisture content than do the
coarser soils.  The range of moisture variations was quite  small except  in
the surface zone.
     The natural  variation in radioactive  decay rate causes a variability
in the soil  moisture measurements.   This phenomenum was  measured in the
field in two successive measurements of the  soil moisture in TTU #3 (Figure
29)-  The elapsed  time required to collect the two sets  was approximately
two hours.  The maximum difference was  2.49  percent at  the 0.3 m (1 ft)
level, followed by 0.84 percent at the  4.3 m (12 ft) level.  The mean  dif-
ference  was 0.23  percent, with a standard deviation of 0.44 percent.   Thus

                                 137

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it appeared the readings  were repeatable  to  approximately ± 1 .0  percent
about  95   percent  of the time.  Because the  objective  of the neutron  stud-
ies was to  detect  the  formation of a perched saturated zone  which might
lead  to  horizontal streaming, two tests  were conducted  using  LCCIWR #4
(Figure 29).  A berm about  15 cm (6 in) high was constructed at  an  approx-
imate  radius of 1 m (3.5 ft) around the access tube.   The  area  inside the
berm was flooded and soil moisture measurements  made  as quickly  as  possi-
ble. The time required  to obtain one measurement at each 15  cm  (6  in)  depth
interval was slightly in excess of one hour.   The results of each  test are
shown  in  Figure 45- The  first test covered a period of  just  over  three
days; the second test lasted about  36  hours.   The average soil  moisture
during  the test is shown on the left side  and  the soil depth  on  the  right
side.  A comparison of  these averages to the  long term  averages for  LCCIWR
#4 shown  in Figure 46 revealed the profile  was wetter  during  these tests.
A measurement prior to  the  second  test was not  obtained. This  may  have
accounted for the slightly  higher average readings  on the  second  test.
Based on the average readings, there was significant  wetting down  to about
3 m  (10  ft) at this site.  The layer of finer textured  soil at the 3.95 to
4.10 m (13.0 to 13.5 ft) depth retarded the  flow causing some  increase of
soil  moisture in  the  coarse  material  in  the  3.4  to  3.7  m (11  to 12 ft)
zone.  It was not  possible in either  test to see a  "wave" or "slug",  of
water moving through the profile.
     Attempts  to  correlate rainfall with increase in  soil  moisture in the
upper meter were  only marginally satisfactory.    TTU #5 was in  a natural
surface  drainage  path, and experienced  ponded water  just  a  few inches away
after some irrigation events.  Measurements  at the 30 cm (1  ft) measurement
were  influenced by the nearness of the soil  surface;  however,  the  0.5 m
(1.5 ft)  measurements showed little evidence  of  flooding.   This  level,  in
fact, remained  quite dry.
     The expected  general trends were:   the  upper level became wetter dur-
ing  December to  April or May and exhibited  a drying  trend through the sum-
mer and fall months.  A measurement about the middle  of  March,  1983, showed
a sharp decrease  in soil moisture within the  0.6 to 1.8  m (2 to 6  ft)  zone
in the TTU #3,  0.4  to 4.3 m (1.5 to 5.0  ft)  zone in TTU  #4 and  0.6 to  4.3 m
(2.0 to 5.0 ft)  zone in TTU #5.  Less than 2.5 mm (0.1  in) of precipitation
                                  138

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             Test #1
Test  #2
32.9
qn 7
3D . /
qn q '
3U . 3 ,
OQ R
C.J.Q
OR II
 1 a . 1
CD 1 Q ?
"^ 1 ^J * *^
fc- pn U

^  	 »...* 	 A 	 	 7.U
                                          1.8
                                        19,
                                            8
                                               w
                                                            *
                                                            1.0
                                                                  c
                                                                  o
                                                                  •M
                                                                  <0


                                                                  0)
                                                                  V)

                                                                  O

                                                                  O
                                                                  Q.
                                                                  0)
                                                                  Q
            Ti me ( hrs)
Ti me  ( hrs)
Figure 45.     Water Content  (Percent by  Volume)  During flooding  Tests
              August 1983, LCCIWR #4
                               139

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           A  A	•
           • -*^L. "•»••«• *»»
                                                    0.33
                                                          CC
                                                          LJ
                                                          
-------
occurred prior  to  this  sudden change.  The neutron probe measurements above
the cited zones showed  no  change;  and little, or no change was noted  below
the zone.  If these  changes  in soil moisture measurements were omitted,  the
soil moisture measurement  in the period just preceding and  just following
the moisture fluctuation gave no hint of a change.  Some instrument mal-
function might have  been  suspected had only one hole been affected.
     If,  in  some  sense,  these  measurements reflect changes in water con-
tent, it is safe to  conclude that  changes below about 3.0  m (10  ft) were
below  the detection  level (^ 1%) of the neutron probe method employed in
plots  TTU #1 ,  TTU  #2, TTU #3, and TTU #4.  Nonetheless, TTU #5 exhibited
what appeared to be  a  "wave" or "wetting front"  moving  through  the soil
beginning at the  0.6 m (2.0 ft) level early in April and progressing down-
ward to  the 7.6 m (25.0 ft)  level  by the middle of May.  The hydrograph of
average water content in the sampled profile of each neutron tube is shown
in  Figure 47.  The similarities between the hydrographs were not apparent;
therefore, the soil moisture transient was not a function of precipitation
events.   Irrigation on the TTU  plots is given in Table D.2 and D.e. It does
not appear  that the lack of correlation,  as shown in Table 27, was due to
the irrigation schedule.

        TABLE 27.  CORRELATION MATRIX FOR WATER CONTENT IN TEXAS TECH
              UNIVERSITY  PLOT OBSERVATION SITES, HANCOCK FARM


TTU 1
TTU 2
TTU 3
TTU 4
TTU 5
TTU 1 TTU 2 TTU 3
1 0.481 0.790
1 0.629
1


TTU 4
0.376
0.426
0.541
1

TTU 5
0.505
0.465
0.354
0.354
1

     Based  on  the results  obtained during this study,  the neutron soil
moisture measuring device  was  not  a  useful research tool.  It may indicate
the  moisture content in  a general way, but  was not precise enough to allow
indicated changes to be associated with a cause.
                                 141

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    24.3
    22.8
    23.4
TTU«1

 S  22.8
 4-*
 c
 o
 o
 o>  25.9
 W
 o
 O)
 (0
    21.2
 •  24.3
    24.5
TTU«5
LCC«4
LCC*8
 LCC«9
          SONDJFMAMJJASO

             1982               1983
Figure 47.  Variation of Average Water Content as Indicated by the
                       Neutron Probe
                            142

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Groundwater Quality
     The hydrologic  data   indicates a general  ground-water   elevation de-
crease of 30 cm beneath  the Gray farm and a gradual rise (approximately 30
cm  in  18 months)  in  the ground-water level beneath the Hancock  farm.  Asso-
ciated with this  ground-water recharge  could be an  alteration  in water
quality. Ground-water  quality beneath the Hancock and Gray  farms  was  moni-
tored from June 1980  to  October 1983.  The baseline data collection period
extended from  June  1980  to  February 1982.  The SeWRP diverted  effluent to
the Hancock farm on  February  19, 1982.  Therefore, the time  from  February
1982  to October  1983  is  referred  to  in the text  as the  irrigation data
collection period.
Hancock  Farm—
     Several  well water  samples contained  levels  of  contaminants  which
exceeded or equaled  drinking  water maximum constituent levels, MCI, (Table
28) as  set forth by  the State of Texas (1980) and National  Interim Drinking
Water  Regulations (U.S.  EPA 1977).   Primary concern was focused  on applied
water constituent levels  exceeding  the reported drinking water  MCI.   These
parameters were nitrate-nitrogen (1x103), Se, ^g, Fe and Mn.
      With  regard to   drinking water sources, Se exposure in its chronic
form  is associated  with  dental caries, jaundice, skin eruptions,  chronic
arthritis, abnormal  finger and toenails, and  subcutaneous  edema (Kowal
1983).  Selenium is  readily available in alkaline soils and  easily taken up
by  plants.  High levels of selenium  in crops  grazed by animals  may pose
potential toxicity  problems.  Selenium is essential for  animals and most
likely humans (Loehr  et al 1979).   Suggested  maximum  Se concentrations
which will avoid Se  toxicity  to animals are less than four  to five ppm.
     Several hundred  milligrams of  silver consumed per kilogram of body
weight can cause anemia  and possible death.  The primary  effect  in humans
is a permanent blue-gray discoloration of the skin and eyes.
     The major human health   risk with high levels of nitrates  in drinking
water is the development of  methemoglobinemia in infants less  than about
three  months of  age.   An  infant's  partially developed capacity to secrete
gastric acid allows  the  gastric pH to rise to  a  level which  promotes the
growth  of bacteria   which  reduce nitrate  to nitrite  in the upper gastro-
                                 143

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TABLE 28.  PERCENT OF HANCOCK EARM WELL WATER SAMPLES WHICH EXCEED
  OR EQUAL DRINKING WATER STANDARDS EOR THE EOLLOWING PARAMETERS

Total Number of Wells = 27
Maximum Constituent Level

Date
07/22/80
10/30/80
11/11/80
01/26/81
03/27/81
06/11/81
10/29/81
11/18/81
01/18/82
06/14/82
09/22/82
11/10/82
02/15/83
03/14/83
05/09/83
07/20/83
09/15/83
No of Wells
Sampled
12
7
16
23
2
24
2
22
27
27
25
2
7
12
27
1
27
Percent Exceeding or Equaling Drinking Water Standards
Parameter
AS
0
0
0
0
0
0
0
5
0
0
0
0
0
0
0
0
0
BA
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
CD
17
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
CR
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
PB
8
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
HG
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
N03
8
0
25
0
0
13
0
27
4
11
12
0
57
8
15
0
7
SE
0
29
0
0
0
4
50
18
19
15
0
0
0
0
15
0
11
AG
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
                                                                     (continued)

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Table 28, continued
Recommended Secondary Constituent Levels
Percent Exceeding or Equaling Drinking
Parameter
Date
07/22/80
10/30/80
11/11/80
01/26/81
03/27/81
06/11/81
10/29/81
11/18/81
01/18/82
06/14/82
09/22/82
11/01/82
02/15/83
03/14/85
05/09/83
07/20/83
09/15/83
No. of Wells
12
7
16
23
2
24
2
22
27
27
25
2
7
12
27
1
27
CL
0
0
0
0
0
0
0
9
0
4
0
0
0
0
4
0
7
CD
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
FE
25
14
0
22
0
4
100
73
85
96
92
100
0
0
59
0
89
MN
67
71
25
30
100
42
50
45
52
52
44
100
0
0
30
0
48

S04
0
0
0
0
0
4
0
0
0
4
8
0
14
0
4
0
4
Water Standard

IDS
8
0
0
0
0
4
0
0
4
7
0
0
29
0
7
0
11

ZN
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0

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intestinal  tract (Kowal  1983).  Nitrite is adsorbed into the bloodstream
and oxidizes the  ferrous Fe to  ferric state  in  hemoglobin.   The  ferric
state of Fe  is  incapable of transporting oxygen to the body's cells.
     During  the baseline period, Fe and Mn levels  in the ground water  con-
sistently exceeded recommended secondary constituent levels of 0.3 and 0.05
mg/1, respectively.   Iron and Mg can  cause corrosion and  pipe blockage.
Aesthetically,  these-minerals affect the appearance of water and can  impart
a metallic taste  to the  water-  Furthermore,  Fe and Mg can  cause staining
of laundered goods  and   manufactured  products.   Table  C.5  provides the
well codes from which water was extracted containing Fe and  Mg exceeding
primary drinking  water standards.
     In well drained soils the majority of  Fe on occurs as ferric  ion and
and only small  quantities of  ferrous ion are present.  Generally, Fe min-
erals  in  the soil of the High Plains of Texas are predominately magnetite
(Fe304)  and hematite (Fe203).-  When  soils become saturated  or otherwise
subject to anaerobiasis, ferric ion is reduced to  ferrous oxidation state.
The  reduction process is associated with biochemical  reactions occurring
within  the soil profile.  Solution of the ferrous  compounds occurs once the
insoluble ferric oxides are reduced to the ferrous ion.  Similarly,  manga-
nese dioxide, which is quite insoluble in water,  is reduced from an oxida-
tion state of IV  to II under anaerobic conditions  and solution  occurs.
     Nitrogen—Table C.5  presents  the specific Hancock  wells which con-
tained  water  of  such   quality   that  certain   drinking   water   stan-
dards were exceeded during certain ground-water sampling  periods.  The fre-
quency  of exceeding drinking water standards  is also presented.   The  infor-
mation  reflects an increase in nitrate-nitrogen levels equal to or above 10
mg/1 nitrogen  in wells 21152, 10112, 10731,  10931, 10821  and  10932  during
the project   monitoring  period.  Statistically significant  ( a = 0.05) in-
creases  only occurred  in  wells 21152,  10731, and 10932  (Table C.6).  As
indicated by the  frequency information, wells 21323, 10112, and 10821  only
exceeded  nitrate standards  once during the monitoring  period. Therefore,
the data were somewhat skewed resulting in an increased standard deviation
and  increased  risk of  a  Type II error  (i.e., the researcher accepts the
null hypothesis,  that there is no difference  between means  and  the alterna-
tive is  true).   Well 20842 maintained a high median nitrate-nitrogen level
                                  146

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of 9.61  ppm during  the  baseline  period and 10.70 ppm from February 1982 to
October 1983 (Tables C.7 and  C.8).  Conversely, several  well  water samples
(20112, 21141,  30312,  21234)  showed  a statistically significant decrease in
nitrate concentrations and  contained levels below drinking water standards.
     Figures C.1  through  C.6  show  the variation of  nitrate concentration
in the ground water  beneath  the  Hancock  farm from June  1980 to October
1q83.   As  stated  previously  in the  hydrogeologic investigation, a possible
scenario for the rise  in elevation  beneath the farm was the percolation  of
rainfall surface runoff captured  in playa lakes or moat areas surrounding
the wastewater  storage reservoirs to the aquifer. Delineation of high  pre-
cipitation months  on the  nitrate  graphs does support the hypothesis that
leaching of nitrates to  the ground  water may be associated with rain events
(e.g.,  21152,   10731, 10931, 21323, 20842, 10112, 10931).  Only well 21323
did not exhibit a  corresponding increase with  ground-water  elevation  with
nitrate nitrogen increase.  Hydrographs  indicating a  rise in water eleva-
tions was measured in  November  of 1982  and not in July.  Continuous  hydro-
graphs showed a general  increase  in  saturated  thickness of the ground water
beneath the farm in  August.  Nitrate levels  in well  21323 rose  in  July
1982.
     Another scenario  which must  be considered is the possible leakage of
water stored in three  reservoirs. Figure C.6 illustrates  the variation  of
ground-water nitrate  levels  in reservoir  monitoring wells 10932 (reservoir
1), 10731 (reservoir 2), and  21152  (reservoir 3"> .  Superimposed on  this
graph  are  the  months  when  each reservoir  was  approved  for operation by the
Texas Department of  Water Resources  and placed in operation.  Wastewater
effluent was pumped  by SeWRP  to
     1.   reservoir  1  on April  13,  1982;
     2,   reservoir  2  on September  2, 1982: and
     3.   reservoir  3  on October  14, 1982.
     Due to  the heavy precipitation in May and June and the lack of avail-
able storage in reservoir 1,  an emergency  request for permission to  trans-
port water to reservoir  3 was sent  to the  Texas Water Commission. Reservoir
3 had 30 cm of  clay  liner initially  installed  and 90 percent of the  bottom
had an additional  30 cm  of  clay.  On July  1 water was pumped into reservoir
3 and was discontinued on July  26,  1982.   A volume of 348,107 m-' was stored
                                 147

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in resei
       irvoir  3.   On  3uly 26 water was pumped  from  reservoir  3  to  the  land
for irrigation.   Reservoir 3 was drained and installation  of the additional
30 cm of clay  was  completed by the end of August.
     Degradation  of water quality in well 21152 was  observed  prior to any
transport  of  SeWRP effluent  to the reservoir.   No  degradation  in water
quality was observed in reservoir  1  until five months after  it  received
Lubbock's  effluent stream.   An increase  in  nitrate-nitrogen levels was
measured in well  10731 within one month after Reservoir 2 was  placed on-
line. Based on the hydrologic data which indicates a general rise in ground
water approximately two  months after  the precipitation  in  May  and  June
1982,  it  is highly  probable  that high  nitrate  levels in  wells  21152,
10731, and 10932   were the result  of leaching nitrate by percolation of
surface runoff in  the moat area encompassing reservoirs  2 and  3.
     Average total Kjeldahl nitrogen (TKN)  concentrations in  the ground
water ranged from  <0.10 to 24.89 mg/1 (Tables C.I and C.8). The  majority of
well water samples contained less than 1 ppm TKN.  During  the  baseline per-
iod  six  wells contained water with average TKN levels greater than 1 ppm
(Table C.7).  Figures C.7 through C.12 show the variability  in the data.
Only the median TKN values of wells 20711  (2.85 mg/1 TKN), 20842 (1.53 mg/1
TKN), and 40231 were greater than T ppm. Only one well  (30312) exhibited  a
significant (a =  0.05)  change in TKN from  the baseline period  through the
irrigation period.  Average TKN levels in ground water  collected from  well
30312  increased  from 0.85 mg/1 to 24.89 mg/1.  Well 30312  was  a victim of
gross contamination by an accidental discharge  from an  adjacent  riser which
flowed  directly  into the well.  The rise in TKN levels in wells 10721 and
20711  (Figure C.7)  measured in 1982,   may have  resulted  from  surface
runoff   flowing directly  into the well or   through rodent  burrows under-
neath concrete pads.  In general, organic nitrogen comprised the major com-
ponent of the  TKN.
     Average  ammonia-nitrogen levels varied  from 0.03  to 15.15  mg/1 during
the ground-water monitoring period.  As expected, the highest  ammonia  con-
centration was  measured  in well 30312  in October 1982.    Figures  C.13
through C.17 present the variation in  ammonia in the  Hancock  wells  from
June  1980  to  October 1983.   Ammonia-nitrogen increases measured  in wells
10721 and 20711 were probably due to  surface runoff caused  by the  heavy
                                 148

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precipitation  in  May  and  June entering the well. The composition of nitro-
gen species present  in well  10721, 20711, and 30312 changed from the base-
line period to the irrigation period.  The average percentages of the TKN
in the  ammonia  form  during the irrigation  period in well waters collected
from well  10721 and  20711  were 85 and 76, respectively.  During the base-
line monitoring period,  the  average percent ammonia for  well  10721  was  17
and 9  percent  for  well 20711. Surface runoff was transporting mineralized
nitrogen from the  upper  centimeters of the soil profile to the wells.
     Phosphorus—Phosphorus removal is accomplished by several mechanisms:
plant  and  microbial  uptake, soil adsorption, and chemical precipitation.
Phosphorus  bound in  organic  forms  is mineralized to inorganic forms  fairly
rapidly in  soils (Enfield  and Ellis 1983).  Inorganic phosphorus is retain-
ed in the soil  profile by  adsorption  and precipitation  mechanisms.  Slow
rate irrigation systems have demonstrated almost complete removal  of phos-
phorus (Christman  1972,  Hook, Kardos and Sopper 1973, Anderson 1978, US EPA
et al 1981, Walker and Demirjian 1978, Pound et al 1983, Loehr et al 1979).
     Figures C.18  through  C.22 present the variation of  total phosphorus
(TP)  from  June 1980  to October   1983.  In general, the data  appear to be
highly variable.  No significant differences (a = 0.05)  in  TP were  deter-
mined  between the  irrigation and baseline monitoring periods. During the
baseline monitoring  period,  average TP levels measured in the ground water
ranged  from 0.19  mg/1 to  0.58 mg/1 (Table C.9).  The average  ground-water
TP concentration from  February 1982 through October 1984  ranged from  0.02
mg/1 to 0.41 mg/1  (Table C.10).  The data indicate a decreasing  trend in
TP from baseline through irrigation.  This decrease was primarily  due  to a
decrease in organic  phosphorus  in  the ground  water.  Total phosphorus
levels in well  10211 rose  drastically in June 1982 to 4.06 mg/1. The topog-
raphy  around  the  well was  relatively  flat and at a  higher elevation.
Surface runoff  flowed  away from this area; consequently,  the surrounding
area was not susceptible to  flooding.  Located approximatelly 2 m from this
well was a  ditch maintained  by the County to collect surface runoff  from
country roads.  During heavy precipitation events migration of percolate
water from  the  ditches  through  soil profile  could leach  phosphate phos-
phorus  to  the gravel packing surrounding the well casing and subsequently
to the ground water  or directly to the ground  water.   Figure C.23 shows
                                  149

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that orthophosphate  phosphorus (P04)   concentration   did  increase  to  3.38
mg/1 in June   1982  and comprised  83  percent   of  the   TP   concentration.
Average  orthophosphate phosphorus concentrations measured  in  water  samples
collected from well 10211 during the irrigation period (Table  C.10) were
significantly (a = 0.05)  greater  than  average   levels   measured   during
the baseline  monitoring period (Table C.9).  Furthermore, there appeared to
be  an  increase in TP and P04 (Figures C.23  through C.29)  in  most wells in
June 1982.   During the baseline period ground-water PO^ levels  ranged  from
<0.01  to 0.22 mg/1.  From February 1982 to October 1983,  the majority of
water  samples analyzed contained less than  0.10 mg/1  orthophosphate phos-
phorus.
     Organic  Carbon--Each water  sample  was  analyzed  for  chemical  oxygen
demand  (COD)  and  total organic carbon (TOC) to  determine organic contamina-
tion of the ground water.  Figures C.30 through C.33 present  the  COD data
obtained June 1980 to October 1983.   The variability of  the COD data was
greater than  the  variability of the  TOC data.   Consequently,  only water
extracted from well  20243  contained COD  levels which decreased  signifi-
cantly  from the- baseline period through the  irrigation  period.   Well 20243
was a  newly  constructed  well and soil organic matter plummeting into the
well boring during construction probably  caused the  relatively  high  COD
(337.9  mg/1) measured during the baseline period.  Similarly, construction
of wells 20721, 20712, 10211, 10112, 21141 and  40331 most likely was  a  fac-
tor in  their  respective initial ground-water  COD concentrations. Median COD
concentrations during the baseline and  irrigation periods  ranged  from  4.1
mg/1 to  94 mg/1  and 3.8  mg/1 to 88 mg/1,  respectively  (Tables  C.9 and
C.10).  When the farm  was irrigated,   only  well   40231   contained water
with an average or median COD greater than 40 mg/1  (Table C.10).
     Figures  C.34 through C.40 present  the TOC  data obtained from  June  1980
to  October  1983.  A significant  (a=  0.05) decrease in  TOC  levels  was
observed in water samples collected from wells  10112,  10211, 20112,  20243,
20721,  21141, 10232, 40231, 21234, and 10541   (Table  C.6).  As previously
stated,  the  first six wells were newly constructed wells  for the project
and TOC  increases probably resulted from construction  activities.   Source
of ground-water organic contamination may  be  oils and  other lubricants  from
pumps and motors.  Prior  to 1981   most of the   existing  wells  on the  farm
                                 150

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were used  to provide  crop  irrigation.  From the end of 1980 through  1981,
all irrigation   pumps   and motors  were removed  from the farm wells  (e.g.,
10232,  40231, 21234, 10541,  21323, 30312,  20711, 10821, 10842,  and  10721).
In summary,  since  June  1980  the ground water beneath the Hancock farm has
shown a decrease in  TOC concentration.
     Minerals — Prior to transporting SeWRP's effluent to the Hancock  farm,
the average  total   dissolved  solids (IDS) in the ground water  beneath the
the  farm  ranged from  363  mg/1 to  989  mg/1  (Table C.7).   Figures C.41
through  C.45  present the  IDS data  for specific Hancock wells.   Initial
IDS levels measured  in  newly constructed wells 40331 (969  mg/1)  and 20112'
(827 mg/1)  were probably an  artifact of well construction and  development
(Figure C.44).   Average  IDS values  in well  water  collected  from 10821
dropped  significantly  ( a =  0.05)  from 902 mg/1  (baseline period)   to 674
mg/1  (irrigation   period).    Significant  increases  in  IDS  levels  were
measured in wells  10731 and  10721  (Figures C.41 and C.45).   The  increase  in
ground-water TDS  in well 10731   was probably   due to  leaching of salts
from the  soil  profile by percolate water produced by the  heavy precipita-
tion events in  May and  June  1982.  Removal of an old irrigation line from
well 10721  and subsequent  backfill of the trench may have produced  a more
porous media thereby creating  a pathway for water in the upper soil  profile
to  migrate to well  10721. The increase in TDS levels in reservoir monitor-
ing well 10721  was measured in  October 1982  which was within one month
after  the reservoir was placed in service.  As previously  stated, continu-
ous hydrographs indicate the ground-water levels beneath the farm began  to
rise in August  1982.
      TDS concentrations observed  in Hancock wells 10232 and 40421 exceeded
1000 ppm once during the irrigation  period (Table C.7).  A drastic rise  in
TDS concentrations (1199  ppm) was detected  in  well 10232 in April 1983
(Figure C.42).  TDS levels measured in the well prior  to  and after April
1983 ranged from 595  to 677  ppm  and 559 to 611 ppm, respectively.   A more
gradual increase in  ground-water  TDS concentration was measured in well
40421  (Figure  C.42) from  the spring 1981 (659 ppm) to October 1983  (1104
ppm). The data  indicate a step increase in concentration  in October 1981
(852 ppm)  and another step increase  in September 1982 (948 ppm).   These
stepped or ramped  increases  may be associated with precipitation events  in
                                  151

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August-September  1981  and May-June 1982.
    IDS in the  ground  water consisted primarily of Na, Ca, Mg, and K salts.
The ground-water hardness varied from hard (150-300 mg/1 as CaC03) to very
hard  (greater  than   300  mg/1 as CaC03). Excluding  the reservoir monito-
ring wells,  Ca  ion concentration  in the well water ranged from 24.0 to 55.8
mg/1  and   contributed   approximately one-third  of the total hardness dur-
ing the baseline  period.  Recirculat ion water  used to  develop reservoir
wells 21152  and 10731  was not completely purged prior to obtaining  the one
sample collected  in January 1982.   Consequently,  Ca levels in reservoir
wells  21152 and  10731 were 150.0 mg/1 and 138.0 mg/1, respectively, (Table
C.11)  which  were  more  than two times the levels measured  in  the remaining
24 wells.   Once the wells were sufficiently bailed Ca levels  decreased  to
65.5 mg/1   in well 21152 and 67.8 mg/1 in well 10731 (Table C.12).   Well
water   from 10721  exhibited a significant ( a = 0.05)  increase in average
Ca concentration  from  47.8  (baseline) to 117.8 mg/1 during the  irrigation
period which corresponded  to the TDS rise.  In addition,  the gradual in-
crease in  TDS resulted from statistically  significant increases in Mg, Mn,
 K, and Fe salts  (Table  C.6).
     Comparison of baseline and irrigation period average sodium adsorption
ratio (SAR)   for  the  water  extracted from each  well indicate a general
change in   composition   of salts.  From  June 1980  to February  1982,  the
average  adjusted  SARs  (SARacj j) of the ground water ranged from 3.0 to 8.4
(Table 29).   To  prevent the creation of sodic  soils,  irrigation  water
should have an  SARatjj  below six  (Stromberg  and  Tisdale  1971).  Eleven
wells contain water with average SARacjj less than six. Increasing problems,
however, may occur with  SARadj from six to nine. Computed SARad; values for
ground water obtained  from 24 wells were between six and nine.  Therefore,
no severe   problems with water  penetration  were  indicated  by the data.
During the  irrigation  monitoring period, SARadj values ranged from 2.1  to
11.0  (Table 29).  The  high average SARadj exhibited  by well 30312  was a
result of the effluent contamination experienced in spring  1982.   Average
sodium levels  increased from an average baseline level of 105.5 mg/1 to an
average level  of 180.8  mg/1.  Associated with  this increase in  Na  was a
decrease in  Ca  and Mg  concentrations.  Whereas, approximately 60 percent of
the wells  demonstrated an increase in Ca and Mg, and Na  was  reduced  in  79
                                  152

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                  TABLE 29.  SODIUM ADSORPTION'RATIO FOR HANCOCK FARM WELL  WATER

Well No.
10112
10211
10521
10542
10931
20112
20243
20721
21141
40331
10232
10721
10821
10842
11032
20711
20842
21323
30312
40231
40421
21234
40311
10541
Average
Cation Concentration (meq/1)
Calcium
B*
2.00
1.94
1.82
1.43
1.20
2.56
3.11
2.31
2.68
2.48
1.65
2.39
2.79
1.38
2.04
2.58
1.74
2.30
3.34
2.49
2.13
2.07
1.94
1.28
I**
1.88
1.88
1 .88
1.96
2.05
2.14
1.90
1.84
2.86
2.24
2.78
5.89
2.21
1.45
2.58
2.86
2.66
2.89
2.76
3.18
3.58
2.14
3.13
1.74
Maqnesium
B
3.25
2.98
1.75
2.28
3.06
3.84
2.83
2.34
3.75
4.02
3.39
4.44
5.43
2.94
4.30
5.39
3.37
5.20
5.75
4.88
4.51
4.20
4.16
2.71
I
2.78
2.78
2.32
2.98
3.60
3.71
2.46
3.16
4.43
3.98
3.34
9.16
3.66
3.05
4.36
5.15
4.34
5.43
3.72
5.39
5.69
3.94
5.20
2.82
Sodium
6
3.13
3.78
2.06
5.22
4.48
4.12
6.01
4.30
5.21
6.45
5.22
4.12
6.39
5.40
4.12
3.08
3.54
6.83
4.58
4.18
5.35
2.35
6.32
4.93
I
2.75
2.99
3.06
4.43
4.62
3.21
3.76
4.78
4.24
4.36
4.58
5.15
4.09
4.43
3.08
2.91
2.17
4.62
7.86
3.76
4.45
1.50
5.22
3.74
Average Sodium Adsorption Ratio
No n- ad justed
B
1.9
2.4
1.5
3.8
3.1
2.3
3.5
7.8
2.9
3.6
3.3
2.2
3.2.
3.7
2.3
1.5
2.2
3.2
2.2
2.2
2.9
1.3
3.6
3.5
I
1 .8
2.0
2.1
2.8
2.7
1.9
2.5
3.0
2.2
2.5
2.6
1.9
2.4
3.0
1.7
1.5
1.2
2.3
4.4
1.8
2.1
0.9
2.6
2.5
Adjusted
B
4.4
5.5
3.3
8.4
6.8
5.5
8.4
6.4
6.7
8.3
7.3
5.3
7.7
8.1
5.3
3.6
5.1
7.7
5.5
5.5
6.7
3.0
8.3
7.7
I
4.1
4.6
4.4
6.4
6.5
4.6
5.5
6.9
5.3
5.8
6.0
5.1
5.8
6.9
3.9
3.8
2.9
5.5
1 1 .0
4.5
5.2
2.1
6.2
5.8
	
*B =  Baseline Period
**I  =  Irrigation Period
*SAR  ,. values  presented  in Appendix  H.

-------
percent  of  the wells during the  irrigation period.  Therefore, in 18 wells
the SARacji was lowered during the irrigation period.
     Ground  water Fe concentration increased  significantly  (  oc = 0.05)  in
wells 10931,  10721, 20711,  30312,  and 21234 (Table C.9).   Each of these
wells existed on the farm prior  to the project  and were constructed  with
cast Fe  casings.  As the ground-water level increased in these wells,  con-
tribution of ferrous oxides from  the casing  may  have contributed  to the
higher Fe levels.   In addition,  wells 10931,  10721, and 21234 were  sub-
jected to increases in ground-water level exceeding 2 m.   Consequently,
ferrous  ion  most likely was leached from the soil  profile.   In  general, the
ground water beneath the  farm  contains Fe  at concentrations exceeding
drinking  water recommended secondary constituents  limits  (Table C.5).
     Similarly,  Mg levels  rose  significantly in wells  10721  and 30312
(Table C.6).   Significant decreases in Mg occurred in the reservoir moni-
toring wells 21152 from 0.465 mg/1 to 0.064 mg/1  and 10731  from 0.650  to
0.08 mg/1.   As previously  stated,  higher  levels of most salts  in the
reservoir monitoring wells during the baseline  period resulted from well
construction and development.
     Major  anions associated with the cations were chloride (Cl)  and  sul-
fate (504). Significant (a  - 0.05)  increases in Cl ion  were observed  in
wells  10721  and 10731.   Chloride ion  concentration  decreased  in wells
10821 and 30312  which was  contaminated with effluent in  the  spring 1982.
During the baseline  period,  -chloride levels   ranged  from 22 mg/1 (0.6
meq/1) to 246  mg/1  (6.9 meq/1)  and  from 17 mg/1 (0.5  meq/1) to 345 mg/1
(9.7 meq/1)  from February 1982 to October 1983.   Table  30 indicates that
chlorides present  in the ground water would cause no foliar  injury  to
crops grown  on the Hancock farm which were primarily cotton, sorghum, and
alfalfa.
     Prior  to transporting  SeWRP's  effluent to  the Hancock farm, the
ground-water sulfate concentration ranged from 32  mg/1 to 243 mg/1.   During
the irrigation  period,  wells 10931  and 10731  exhibited   significant  in-
creases  in  average  S04 levels  from 93 mg/1 to 208 mg/1  and  32 mg/1 to 161
mg/1, respectively.  Ground water collected  from  wells  10721,  10821, and
30312 had significant decreases in S04 levels (Tables C.7  and C.8).  With
the  significant  decrease in Cl (201 to 86 ppm) , S04 (243 to  147 ppm)  TDS
                                  154

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(902 to 674  ppm), and Mg  (66.2 to 44.7  ppm)  in  well 10821, some surface
runoff  may  have entered the well during the heavy precipitation in May  and
3une 1982.
TABLE 30.   RELATIVE TOLERANCE OF SELECTED CROPS  TO  FOLIAR INJURY
                 FROM SALINE WATER APPLIED BY  SPRINKLERS3
	(Pettygrove and Asano 1984)
          Na  or  Cl concentrations (meq/l)D  causing  foliar injury0
       <5               5-10               10-20                 >20

Almond Grape
Apricot Pepper
Citrus Potato
Plum Tomato
Alfalfa
Barley
Corn
Cucumber
Saf flower
Sesame
Sorghum
Cauliflower
Cotton
Sugarbeet
Sunflower

(a)
(b)
(c)
Susceptibility based on direct adsorption of salts through the leaves.
The concentration of Na or Cl in meq/1 can be determined from mg/1 by
dividing the equivalent weight for Na (23) or Cl (35.5).
(meq/1 = mg/1/equivalent weight)
Foliar injury is influenced by cultural and environmental conditions.
These data are presented only as general guidelines for daytime
sprinkler irrigation.
     Trace Metals—Almost complete removal  of  trace metals occurs in soils
suitable  for slow rate  land application systems  (EPA, 1981).  At soil pH
values above  6.5, most trace metals are retained in the soil profile  and
are  insoluble components.   Consequently,  trace metal  removal is normally
not considered in the design of slow rate systems (EPA,  1981). Mechanisms
governing  the removal of  trace  metals are filtration (suspended forms),
ion exchange, precipitation, surface adsorption and volatilization  (Page
et al  1981,  EPA 1981, Brown 1978).   Adsorption  of cationic heavy metals
(i.e., Pb,  Cd, Zn,  Cr (III), and Cu)  increases with increasing  pH  (Brown
1978).   Surface adsorption of anionic heavy  metals, such as Cr (VI), As,

                                  155

-------
 and  Se,  however,   decreases as  pH  increases.   Anionic metals  adsorb  most
 readily at pH levels of four  or below.  At  pH values  greater  than  five,  pre-
 cipitation is  an  important  mechanism  of   removal of cationic heavy metals
 from solution; whereas, precipitation of anionic  heavy metals is  negligible
 at pHs  between one and nine.
     Several  trace metals present in the  ground  water varied significantly
 during  the project monitoring period (Table C.6).   The discussion was
 focused on concentration variations in  Cr,  Pb,  Mo,  Se, Cu,  and  Cd.
     During the baseline period,  average Cr levels  in  well water  beneath
 the  Hancock farm ranged from <0.005  ppm to 0.031 ppm (Table C.11). Exclud-
. ing the average levels measured in wells'20711  (0.011  ppm), 10932 (0.031
 ppm),  and 10542  (0.018 ppm),  Cr concentrations ranged from <0.005 ppm to
 0.009  ppm with 16 of the 27  wells containing water  with <_ 0.005  ppm Cr.  A
 significant (a  =  0.05) increase in  Cr  was measured  in well 10542 (from
 0.018 ppm to 0.076 ppm).   Figures C.46 through C.47 illustrate  the varia-
 tion  in Cr in  the  ground water  throughout the  project monitoring period.
 Sufficient information was not available to explain  the rise in  Cr  in  well
 10542 (Figure C.46) in September 1983.
     Construction and  development of  wells 10731 and 21152 caused initial
 Pb concentration in the water samples obtained in January 1982 to  be  0.011
 ppm  (Figure C.48).    From  February 1982  to October 1983,  lead  concentra-
 tions averaged 0.008 and 0.005 ppm in wells 10731 and 21952, respectively
 (Table  C.12).  Average lead  concentrations ranged from <0.002 ppm  to 0.022
 ppm (well 10211) during the baseline  period and 0.003 ppm  to 0.021  during
 the  irrigation period (Tables C.11 and C.12).  In June 1982 an  increase in
 Pb (Figure 49) exceeding the  drinking water  criteria of  0.05 ppm  was de-
 tected  in well 10521  (0.052 ppm Pb).  Possible surface erosion of soil  into
 the well casing or through the gravel packing surrounding the casing caused
 this  pulse rise in Pb.  Dissolved Pb concentration in wells 10542, 10721,
 20711,  21323,  20212,  20721, 21141, and 40331 was  quite variable during the
 project monitoring period (Figures C.48 through C.50).
     Generally  molybdenum (Mo) concentration in ground water  beneath the
 Hancock farm  decreased  from the   baseline  period  through the  irrigation
 period  (Figure 50).   As shown, the  data   was quite  variable  during the
 baseline period.   Significant decreases  (a = 0.05) in Mo  concentrations
                                   156

-------
CD
z:
a
cr
   i.oo
 June 1980
                                      PO
                                                               KEY	
                                                           D Well 10731
                                                           O Well 21152
                       O
            6.00
                    11.00
16.00     21.00     26.00
   MONTH SHMPLED
                                                         1
                                                       31.00
                                    O
                                                                        O
                                                                       -B-
36.00     HI. 00
     October 1983
Figure 48.   Lead Concentration in  Well  Water  over  Time,  Hancock  Ferm
03,
  8
                                                              KEY
                                                           D  Well  10521
  _          III         I        I
   1.00      6.00      11.00     16.00     21.00     26.00
 June 1980                          MONTH SflMPLED
                          31.00
                                   36.00     41.00
                                         October 1983
Figure  49.   Lead Concentration in  Well  Water over Time, Hancock  Farm
                                  157

-------
oo
      CM

      o
    o
    *—I
    *
      o
      CM
      CO
      1—I
       •
      o
    a
      CM
    O
      00
      o
      o
                                                        KEY	


                                                     D  Well 10112


                                                     O  Well 10211


                                                     A  Well 10541


                                                     0  Well 10821


                                                     C3  Well 10842
       1.00

    June 1980
6.00
  I

11.00
16.00      21.00       26.00

    MONTH  SRMPLED
  i           i            i

31.00      36.00       m.OO

                October 1983
     Figure 50.  Molybdenum  Concentration in Well Water over Time,  Hancock Farm

-------
were  measured  in wells 10931 and 20721  (Table C.6).
     As  stated  previously, the Se concentration in several wells  exceeded
or equaled  drinking water  maximum contaminant levels  during  the baseline
period (Table  C.5) .  Table C.6 shows no statistically  significant  changes
occurred  in Se levels.  Wells 20721, 40331,  20712,  10821,  and  20112 had Se
level increases  after water  was pumped  to  the  Hancock  farm  (Figure 51).
Precipitation  and adsorption mechanisms for  removal of  Se  in alkaline cal-
careous  soils  are  negligible (Brown  1981, Page  1981,  Loehr et  al  1979);
consequently,  Se  is most readily available under these  conditions.  There-
fore, increased percolation of water during or  after  heavy precipitation
events  in May 1982 may  have  leached  Se to the ground  water obtained in
wells 20721  and 20112.   Furthermore, Se  increases  in wells 50331,  10821,
30312,  and  40311  during the baseline period may have been associated with
precipitation  events.
     Copper is readily adsorbed in alkaline, clay/clay loam soils such as
exist at the Hancock farm.  Even in acid soils Cu is strongly retained and
barely  migrated  to the subsurface (Loehr et al 1979).  Average Cu  levels
ranged from <0.005 to 0.032 ppm (Tables C.11  and C.12).  Soil containing Cu
entering the reservoir monitoring wells 21152, 20731,  and  10932 during well
construction and development caused  Cu levels  in  these  wells  of  0.011,
0.027 and 0.032 ppm, respectively. From February 1982  to October 1983  aver-
age Cu levels  ranged  from <0.005  to  0.126 ppm  (Table  C.12).   A  gradual
rise  in Cu concentrations  was experienced in  well 40421 located in the
southeastern  corner  of  the  farm.  This  atypical,  gradual Cu  increase
commenced in  the spring  1981  and appeared  to continue  to  October 1983
(Figure 52).   Since  Cu was   the only  parameter which  significantly
increased,  it  was  difficult  to develop a scenario to  explain this occur-
rence.  The majority of ground-water samples  contained less than  0.01 ppm
Cu.
     During the baseline period, average ground-water  Cd levels ranged  from
<0.0005 ppm to  0.004 ppm  (Table C.11) and <0.0005 to 0.003 ppm  (Table  C.12)
during  the irrigation  period.  No statistical   significant differences
occurred in Cd  concentrations in  ground water  beneath the farm  between
baseline  and  irrigation periods.  Several wells (approximately 50 percent)
exhibited a pulse  in Cd in samples collected  in November 1981 (18th  month)
                                   159

-------
   OJ
    •
   O
4
I

O

 *

,-~. o
  I CM
    LU CD
    CO -•
ON   ^
o   Z
    CO
      CO
      O
      O
                                                                            KEY

                                                                         D  Well 20721

                                                                         O  Well 40331

                                                                         A  Well 20112
                   I
       1.00
     June  1980
                                      I           I     ,      I
                                     16.00       21.00       26.00
                                         MONTH  SflMPLED
             6.00       11.00      16.00      21.00      26.00      31.00
                                       MONTH SflMPLED

Figure  51.  Selenium Concentration in Well Water over Time, Hancock Farm
  I           I
36.00      41.00
     October 1983

-------
                                                                     KEY	

                                                                 D  Well 21323

                                                                 O  Well 40311

                                                                 A  Well 40421
   KOO
June 1980
6.00
11J)0
16.00      21.00      26.00
    MONTH SflMPLED
31.00
36J)0      41.00
     October  1983
Figure 52.  Copper Concentration in Well  Water over Time, Hancock Farm

-------
and January 1982 (20th  month)(Figure  53).   Ground-water Cd  was not an
agricultural or  public health problem during both  monitoring periods.
     As previously stated, trace metals were not a major concern  due to  the
limited industrial wastewater contribution to SeWRP's sewerage load  and  the
ability  of the alkaline  calcareous soil profile to adequately  remove  and
render relatively insoluble most trace metals.  Increases in  ground-water
Se concentrations appeared  to be associated with rainfall events  and  the
ineffectiveness  of the alkaline, calcareous soils  to absorb  the element.
     Priority Organic Pollutants — Tables 'C.13 and C.14 present  the  types
and associated average  concentration trace of organic compounds measured
from June 1980  to February 1982 and from February  to October 1983. In gen-
eral,  slow rate land  application of organic compounds contained  in  munici-
pal wastewater  should  pose no hazard to ground water, soil  microbial com-
munity and vegetation (Overcash 1983,  Davidson  et al 1980).  The  ground-
water  data confirms this statement.  Significant increases in  dibutylphtha-
late  were observed in wells 21323, 30312, and 40311.  In  addition,  water
obtained  from wells 10112, 10211, 10842,  21323,  30312,  and 10541  contained
significantly  higher levels of diethylphthalate   during.the  irrigation
period than the  baseline monitoring period.  Phthalates are  used  as  plasti-
cizers in polymers and  migrate quite readily  to the surrounding environ-
ment.   Well 10542 was  constructed with a stainless steel casing and  sampled
with  a stainless steel bailer. An average of 51 .6 ppb diisooctylphthalate
was measured during the baseline period and <2.0  ppb was measured  during
the irrigation period (Tables C.13 and  C.14).  Consequently,  the presence
of phthalates in the other water samples  may have  been an artifact of  using
a PVC  bailer or contamination from plastics that  were prevalent  throughout
the analytical laboratory.
     Wells  10521, 10331, 10721, 30312, 10931, 10821, and 10731 exhibited a
pulse  increase in atrazine in 1983 (Figure 54).  Atrazine was  used to kill
weeds  and grasses  in borrow ditches,  and around center pivot  irrigation
machines.  In addition,  patches  of  weeds  surrounding  playa   lakes or
extending into  fields  were treated with atrazine.   Atrazine  has a  low  solu-
bility in water  (0.0033 g/ml water at 27°C) and  leaching from soil probably
is limited by  adsorption  on certain soil constituents (Davidson  et  al
1980).  Therefore, atrazine increases were most  likely a result  of  trans-
                                 162

-------
   o
   ID
  o
  in
O
«—i
*
  o
53-
CD
88,
^-' O
Qo
   o
   •—l
    «
   o
   o
   o
               KEY	
           D  Well 11032
           O  Well 20711
           A  Well 20842
           0  Well 21234
           £3  Well 21323
                I
  1.00
June 1980
Figure 53
 I           I           I          I
n.OO      16.00      21.00     26.00
               MONTH SflMPLEO
              6.00       11.00      16.00      21.00      26.00      31.00
                                       MONTH SflMPLED
             Cadmium concentration in  Well Water over  Time, Hancock Farm
36.00
      1
     41.00
October 1983

-------
   O
   O
   O'

   CO
   O
   O
   If)'
   C\J
   O
   O
   o1
   CM
QQ
Q_

Q_
  o
  o
UJ -
    -1
  in
  o
  o.

  in
  o
  o
                KEY


            D  Well 10821


            O  Well 10931


            A  Well 21234


            •+  Well 40231


            X  Well 11032
   1.00

 June 1980
  I           I           I

16,00      21.00      26.00

    MONTH SflMPLED
              6.00       11.00      16^0       21.00       26.00      31.00





Figure 54.  Atrazine Concentration in Well Water over  Time,  Hancock  Farm
  I

36.00
      1

    41.00

October  1983

-------
port of  soil  particulates bearing  herbicides  into the well  casing or
through the gravel packing surrounding the  casing.   Average  atrazine  con-
centrations  in  wells 10521,  10931,  10721,  30312,  and 10731 were all less
than 2.0  ppb during the baseline period  and 13.9  ppb,  2.5  ppb,   11.9  ppb,
10.8 ppb,  and  12.6 ppb, respectively,   from February 1982 to  October 1983.
What appears to have been a pulse input of-herbicide drastically   affected
the average concentration of atrazine  in the well  water.
     Water in  well 10541 experienced a propazine pulse (17.3  ppb)  measured
in  September  1983 (Figure 55).  Propazine is a herbicide commonly used for
the control of weeds in grain sorghum production.   Similar to  atrazine,
propazine has a low solubility (practically insoluble  in water, Merck
Index,  1968) and  is readily adsorbed into certain  soil  constituents. Conse-
quently,  propazine increases in well 10541  were  probably  due to migration
of particulates containing propazine into the well.     Table  C.6  indicates
which wells  exhibited significant  ( a = 0.05) increases or decreases in
specific  organic  compounds during the  irrigation period.  The statistical
analysis  for the  reservoir monitoring  wells (i.e.,  21152, 10731,  and 10932)
is extremely misleading since only one water sample  for each  well  was  col-
lected during the baseline period.  Variation in  certain organics may have
been attributable to precision of the  particular extraction  and  GC  proce-
dure employed  (Section 4, Methodology).
     Bacteriological  data--  Bacteriological  indicator organisms, total
coliform  (TC), fecal coliform (FC) and fecal Streptococci  (FS)  were meas-
ured to determine potential contamination by  pathogenic organisms.  Table
C.15 presents the average levels of indicator organisms measured  from 3une
1980 to February  1982.  Only water collected from  wells 10821 (an  existing
well) and 10932  (reservoir 2 monitoring well,  cement  sealed) contained no
indicator  organisms.  Well 10541 contained no fecal  coliform. In  addition,
only one  water   sample of  five  collected from  well   40311  contained TC
and FC  organisms.  Therefore, indicator organisms  were isolated  in  water
from more than 85 percent of the wells during the  baseline monitoring per-
iod.  A small  biochemical study identified the FS   organisms to  have  been
possibly  S.  faecalis subspecies 1iguefaciens and  not  of human source.
Theoretically, fecal contamination of water from  a  human source  would pro-
duce a  FC  to   FS ratio of greater than four.  During the baseline monitor-
                                 165

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       o
       o
       O'
       CM
       O
       O
       CO'
ON
    CD
    O-
    Q-
    LU
    
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ing period,  water collected from  seven wells had  average  FC:FS ratios
greater  than  four.  Eight wells contained water with FC:FS ratios less  than
1.0 which  is indicative  of fecal contamination from an animal  source.   A
potential  source  of Salmonella, FC  and FS was  most likely  rodents which
burrowed  beneath concrete pads surrounding well casings.   Contamination
from rural waste  disposal systems appeared limited due to the sparseness  of
domiciles  on  and  surrounding  the farm.   An additional interesting fact was
the high frequency of bacterial contamination of the wells during the base-
line  period  (Table C.15)   which indicates a continual source or survival
of bacterial  forms.  Salmonella was detected in 10521, 10931, 20212, 20243,
40331, 10232, 20711 and  30312 in November 1981. Precipitation events total-
ing 18.08  cm  were measured  at Lubbock  International Airport in  September
and October 1981. Percolation of water through soil macropores and/or  rock
fractures  could transport bacteria and viruses  for great distances (McNabb,
Dunlap,  and Keeley 1977).
     Table C.16 presents the  average TC, FC, and FS concentrations measured
in ground-water samples  from  February  1982 and  October  1983.  Significant
increases in TC  and FC  were  detected  in well 10521 in June 1982, which was
probably due  to increased percolation  or direct contamination from surface
runoff  associated with  heavy precipitation in May 1982.  Detection of  Sal-
monella in water  samples decreased during the irrigation period.   The pres-
ence of Salmonella was measured in well 21323 in June 1982 and wells 10721,
10541 and  21152 in September  1983.  During the  baseline  period  bacterial
indicator organisms were  not detected in well 10821; however, TC and  FS
were measured in  over 60 percent of  the water  samples collected from the
well  in 1982 and 1983.  From February 1982 to October 1983, there was  an
increase in the number of ground-water samples having  FC:FS ratios less
than one compared to those  observed during the baseline period.
     In general,  very little  difference was observed between bacteriologi-
cal  data  obtained during  the baseline and irrigation monitoring periods.
Bacterial  indicator organism  data  did not appear  to provide an adequate
measure of ground-water pollution from human origin.  Recent studies (Hunt
et al 1979),   have also  questioned the use of  bacterial   indicators  for
monitoring  human contamination of waters.
                                   167

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Gray Farm—
      As previously  mentioned, land application of secondary treated  waste-
 water had been  practiced  at  the Gray farm since 1939.  Hydraulic and nutri-
 ent  overloading of the  farm had increased the quantity of ground water at
 the expense of  ground-water  quality.  Table 31 presents the percent of well
 water  samples  collected from the Gray wells which contained constituents
 equaling or exceeding drinking water standards.  Due to  improper  nitrogen
 management on the  farm, sufficient NQ^-N was leached to the ground water to
 create drinking water problems (>10 mg N/l) throughout the entire aquifer
 beneath  the farm.   The incidence of water samples containing Se concentra-
 tions greater than  the drinking water maximum constituent level (MCI) (0.01
 ppm) was less on  the Gray farm than observed on the Hancock farm.  As noted
 with the ground-water quality beneath the Hancock farm,  Fe and Mn   levels
 consistently equaled or exceeded recommended secondary constituent levels
 of 0.3 ppm and  0.05 ppm,  respectively.  Hydraulic overloading leached  salt
 from and through  the soil profile thereby increasing TDS, 5Q(± and Cl levels
 in the ground water above recommended  secondary  constituent levels  with
 regard to drinking  water  sources.  Sulfate is of concern due to its cathar-
 tic effect on humans.  Chlorides are normally not harmful to humans.   Con-
 centrations of chloride  exceeding 250 mg/1, however, give a salty taste to
 water.  Table C.17  delineates the specific Gray wells containing  water  of
 such  quality that certain  drinking water standards were exceeded and the
 corresponding frequency of violations.
      Nitrogen--The hydrographic data revealed that the aquifers saturation
 zone  ranged from  3 m to  21  m below the ground surface.  Therefore, the lag
 time between an environmental disturbance and a transient  response  in  the
 ground-water quantity and  quality was  relatively short  (within days).
 Furthermore, the  data indicate the ground water was moving from the  north-
 west to the southeast toward Yellow House Canyon. Consequently, there was a
 great deal of variation in data for each well during the entire monitoring
 period.
      A comparison  of baseline and irrigation information provided in Table
 C.17 indicates  a  decrease in the frequency of ground-water N03-N concentra-
 tions equaling  or  exceeding  10 mg/1 in wells 6880,  6882, 6888, 6892, 6856,
 6870,  6889, 6893, and 6884.   Prior to pumping water to the Hancock farm,
                                  168

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                             TABLE 31.  PERCENT OF GRAY FARM WELL WATER SAMPLES WHICH EXCEED
                             OR EQUAL DRINKING WATER STANDARDS FOR THE FOLLOWING PARAMETERS
VO

Total Number of Wells = 27
Maximum Constituent Level

Date
06/25/80
08/19/80
09/25/80
01/08/81
03/27/81
06/02/81
10/28/81
11/02/81
01/27/82
05/27/82
10/11/82
11/01/82
05/19/83
10/10/83
No of Wells
Sampled
11
9
24
25
1
24
19
3
25
23
20
5
25
25
Percent Exceeding or Equaling Drinking
Water Standards
Parameter
AS
0
0
0
0
0
0
0
0
0
0
0
0
4
0
BA
0
0
0
0
0
0
0
0
0
0
0
0
0
0
CD
9
0
0
0
0
4
0
0
0
0
0
0
0
0
CR
0
11
0
0
0
0
0
0
0
0
0
0
0
0
PB
0
11
0
0
0
0
0
0
0
0
0
0
0
0
HG
27
11
0
0
0
0
0
0
0
0
0
0
0
0
N03
73
100
79
84
100
83
74
33
84
74
55
60
60
52
SE
0
0
0
0
0
4
5
33
0
0
5
0
4
0
AG
0
0
0
0
0
0
0
0
0
0
0
0
0
0
                                                                                              (continued)

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Table 31,  continued
Percent Exceeding or Equaling Drinking
Water Standard
Parameter
Date
06/25/80
08/1 9/80
09/25/80
01/08/81
03/27/81
06/02/81
10/28/81
11/02/81
1/27/82
05/27/82
10/11/82
11/01/82
05/19/83
10/10/83
No. of Wells
11
9
24
25
1
24
19
3
25
23
20
5
25
25
CL
55
89
63
84
100
83
68
33
80
78
65
80
76
76
CU
0
0
0
0
0
0
0
0
0
0
0
0
0
0
FE
18
0
0
12
100
13
26
33
12
43
35
100
4
72
MN
82
0
4
8
100
13
26
33
16
17
15
20
16
12
S04
64
67
67
56
0
63
53
0
60
48
45
60
64
36
TDS
100
100
92
96
100
96
79
67
92
91
80
100
88
88
ZN
0
0
0
0
0
0
0
0
0
0
0
0
0
0

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the average  N03-N levels  ranged from 5.05  mg/1  (well 6890) to 35.89 mg/1
(well  6891) (Table C.18).  Figure 56  illustrates   that the  higher ground-
water  N03-N concentrations were experienced  in  areas which were row watered
or flood  irrigated and wells down gradient  from these  areas.  Once SeWRP's
effluent  was  pumped to the Hancock farm,  ground-water  N03-N levels beneath
the Gray  farm ranged  from 0.77  mg/1 (well  6890)  to  33:43  mg/1  (well
6894)(Table C.19).  Significant (a = 0.05) decreases in N03-N were measured
in wells  6889, 6886, 6856, 6857, and 6891  (Table  C.20).   Figures  C.56  to
C.59 demonstrate the variation in N03-N  levels throughout  the project
monitoring period.  During May and June 1982  a  total precipitation of 34.82
cm was recorded   at the   Gray farm.  Wells  6856 and 6857 are located  in
areas  where extensive leaching of nutrients  and salt from the soil  profile
occurred  due  to  overflow  from the effluent holding pond and expansion  of
the playa  lake area resulting from high  intensity and  prolonged precipita-
tion. Accumulation of nitrate nitrogen  within the upper soil profile was
negligible. Furthermore, saturated soil conditions inhibited mineralization
of organic nitrogen to ammonia and the nitrification process.  In addition,
the shallowness of the ground water «3 m  from  the ground surface)  reduced
the potential soil volume to leach constituents. Consequently, while in-
creased  water  percolation caused by  heavy precipitation in May and  June
1982 had  minimal effect on  the salt  concentration  in the  ground water
obtained  from wells  6856  and 6857,  a  significant decrease in  N03-N
occurred.
     Water samples collected on May 25, 1982 from well 6889 contained 1.76
mg/1 of N03-N.   Furthermore,  a comparison of the February and May water
quality  data shows a slight increase in TKN   (0.60 mg-N/1 to 1.20  mg-N/1)
and TP (0.04  mg  P/l to 0.34 mg P/l) .  The data indicates the possible con-
tamination of  the ground water in  well  6889 by surface  runoff.   Several
additional wells  such as 6880, 6890, 6886, and  6870 demonstrated a trend  of
decreasing levels of  N03-N in the  water  samples collected during the
irrigation period (Figures C.56, C.57, and C.59).   Well 6885 experienced a
significant  increase  in  ground-water  N03-N concentration  during the
irrigation monitoring period. This may have  resulted from increased  water
percolation due  to the proximity of the well to an earth ditch constructed
to transport effluent water for row watering certain  alfalfa portions  of
                                171

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Figure 56.  Nitrate Concentration (mg/1) in Well Water under Gray Farm,  Baseline Period,
            1981-1982.

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the farm  and  increase percolation of highway runoff.  Nitrate increases  in
well 6883  may  have  resulted  from similar factors.  Figure  57  presents the
average NG^-N levels observed during the irrigation period.   Comparison  of
the average  baseline and  irrigation monitoring period NG^-N data shows a
nitrate  decrease  in  17 of 27 monitoring wells and five wells  (6852, 6855,
6885, 6864,  and 6883) had  an increase in average N03-N levels.  Four  wells
(6880,  6884,  6892,  and 6896) were known to have been inundated due to sur-
face runoff.   Wells  6884, 6882, and 6896 were located in close proximity  to
playa lakes  or wastewater storage ponds.
     Water samples collected  from wells  6884 and 6892  have exhibited a
pulse in TKN  due  to  transport of surface runoff directly into  the well base
or  underneath the  concrete pad and through the gravel packing surrounding
the casing.   Figure  58 shows a TKN rise in the water  sample  from well 6884
in  October  1982.   This  well  was completely inundated with  water from the
adjacent  playa lake  during the  heavy  precipitation in- May  and June.
Similarly,  TKN levels rose in wells 6849 and 6864 in May  1982.   Well 6849
was adjacent  to a playa lake and well 6864 was located in an  alfalfa field
which was spray  irrigated.  In October 1981, well 6892 contained  water with
28.05 mg/1 TKN.   A  small spike in TKN (2.92 mg/1) was observed in October
1982.   Both  increases in TKN were measured in samples collected  during the
next sampling  periods  following heavy rainfall events. Statistically sig-
nificant  increases  in TKN concentrations during the irrigation period were
measured in  wells 6889 and 6893 (Table C.20) .  The increase in TKN levels
measured   in well  6893  (Figure 59) was first observed at the end of  May
1982  (7.88  mg N/l)   and continued  to the end  of the project monitoring
period.   Well 6889  experienced a TKN pulse which was measured in May  1983.
A total  of 11.08  cm  of precipitation occurred in May. Measured increases  in
TP  and  COD  indicate a relatively short path length through   the soil pro-
file  due  to  possible macropores,  fractures in rock, horizontal percola-
tion along  indurated layers  within  the soil profile, flow  directly into
wells or underneath  concrete pad  and  through  gravel, packing surrounding
well casing.   During the  baseline  period TKN concentrations varied from
0.28 mg/1  to  6.97 mg/1 (well 6892).  Once water was diverted  from the Gray
farm to the  Hancock farm,  average TKN levels ranged from  0.20 mg/1 to 765
mg/1 (well 6889)  (Table C.19).
                                  173

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--J
-p-
                                                                                    O Well

                                                                                   ->:-;-:- Ponded
                                                                                   --------- Water

                                                                                   '	• = 0.27 km
      Figure 57.   Average Nitrate Concentration (mg/1)  in Well Water under Gray  Farm, Past  Baseline,  1983

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           CM
•-J
                                                                                             KEY
                                                                                          D Well 6881
                                                                                          O Well 6883
                                                                                          A Well 6884
                                                                                          O Well 6885
            1.00
          June  1980
             6.00       11.00      16.00     .21.00      26.00      31.00
                                       MONTH  SflMPLED
Figure 58.  Total Kjeldahl Nitrogen  Concentration  in Well Water over Time, Gray Farm
36.00      11.00
      October  1903

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 §
 1.00
June 1980
6.00
11.00
16.00      21.00      26.00
    MONTH SRMPLEO
31.00      36.00      m.OO
                October 1983
Figure  59.  Total Kjeldahl Concentration in Well Water  over Time,  Gray Farm

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     During the baseline period,  average  NH3-N levels ranged from 0.02  ppm
to 2.05 ppm.  Average ground-water NH3-N  concentrations were from 0.01  ppm
to 6.96  ppm  from February 1982 to  October  1983.  Ammonia  appeared to con-
tribute more  to the  TKN  rises measured in wells 6884,  6889, and 6893
(Figures C.60  and C.61).  Effluent from the  SeWRP was  stored in the playa
lake adjacent  to 6884.  Ammonia was the primary nitrogen form in the  efflu-
ent from SeWRP.  Therefore, inundation of well  6884  with  water from  the
playa lake  should  have produced a major  NH3-N peak.  Whereas, TKN peaks
measured in  wells 6892 in October  1981  and 6849 in May  1982 resulted from
primarily  organic  nitrogen  contamination.   In October 1982 a rise  in  TKN
level in well  6892, however, was attributed primarily to  an increase  in
NH3-N.  Minor increases in NH3-N  levels were measured in wells 6849, 6852,
6856, 6864,  6880, 6868, 6870,  and  6883  in  September 1981  following heavy
rains in August  and September  (Figures  60  and 61).
     Phosphorus—Average  TP levels  in the ground water beneath the Gray
farm ranged from  0.10 to  3.49 ppm (well 6892) during the baseline  period
(Table C.21).  Precipitation events during August (15th month) and Septem-
ber  (16th  month)  1981 appeared to have caused a TP concentration increase
in wells 6886, 6880, and 6892.  Well 6892  (Figure 62) experienced a  signif-
icant rise  in TP  concentrations from 3.78 ppm  (3une 1981) to 12.30  ppm
(October 1981).  This corresponded  to an increase in  organic nitrogen  to
24.98 mg N/l. During the irrigation  period,  from February 1982 to  October
1983, ground-water TP  levels  generally remained relatively stable with
average concentrations ranging  from  <0.07  (wells 6852,  and 6864)  to 1.94
ppm (well  6887)(Table  C.22).  The inundation  of well  6884 (Figure  63)
caused an  increase in TP  to  1.84 mg/1.   Ground water collected from well
6887 contained increasing levels of TP  from  May 1982 (0.39 ppm)  to October
1983 (4.02  ppm).   A decrease  in TP  concentrations during the irrigation
period was  measured in  wells  6852, 6856, 6864,  6885, 6888, 6855, 6870,
6857, 6881,  6882,  and 6883.   Eighteen wells contained water which  dropped
in TP levels during the irrigation period. During the monitoring period  a
statistically significant decrease in  TP  levels was observed in water sam-
ples collected from well 6892  (Table C.20).
     Figures  C.63 through C.69   present the ground-water orthophosphate
phosphate (PO^.) data.  TP increases observed  in wells 6884 and 6887  in 1982
                                 177

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CD
                                                                                    KEY
                                                                                D Woll 6081
                                                                                O Well 6888
                                                                                A Well 6871)
                                                                                O Well o803
            t.OO        6.00       11.00       16.00      21.00      26.00      31.00
          June 1980                                 MONTH SflMPLEO
          Figure 60.  Ammonia Concentration in Well Water over Time, Gray  Farm
 r
36.00
      October 1983

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                                                                          KEY
                                                                      D Well 6849
                                                                      O Well 6852
                                                                      A Well 6856
                                                                      O Well 6864
                                                                         Well 6880
  J.OO
June 1980
6.00
11.00
16.00      2 J.OO      26.00
    MONTH SflMPLEO
31.00      36.00      UJ.OO
                October 1983
Figure 61.  Ammonia Concentration in Well Water over  Time, Gray Farm

-------
       o
       o
CO
O
                                                                            KEY
                                                                       D Well 6855
                                                                       O Well 6870
                                                                       A Well 6857
                                                                       O Well 6892
  1.00       6.00
June 1980
                              11.00
16.00      21.00      26.00      31.00
    MONTH SRMPLED
36.00      m.OO
     October  1983
     Figure 62.  Total Phosphorus Concentration in Well  Water over Time,  Gray Farm

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                                                                                    KEY
                                                                                D Well  6881
                                                                                O Well  6882
                                                                                A Well  6883
                                                                                O Well  6884
  J.OO
June 1980
6.00
11.00
16.00      21.00      26.00
    MONTH SflMPLED
31.00
36.00      m.OO
      October 1983
Figure 63.   Total Phosphorus Concentration  in Well Water over Time, Gray  Farm

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and  1983  resulted  from increases  in PO4  in  these  well water  samples
whereas,  the  increase in TP (12.30 mg-P/1)  in well  6892,  which was measured
in October 1981,  was caused  by an increase in organic  phosphorus (9.34
mg-P/1).   Ground water contained in well  6892, however,  experienced an
increase  in  PO^ in October  1982 which  was  the  next water sampling period
after the May/June 1982  precipitation.   Similarly, well  6886  showed an
increase  in  PO^ in October 1981 and  October 1982.  Ground-water  PO^ levels
in well 6880  increased in October 1981  to  1.15 mg P/l and remained  at 0.44
to 0.60  mg P/l throughout the remainder  of  the  project monitoring period.
Inundation of well 6892 and transport  of  soil into  the  well caused  tremen-
dous  increases in TP and  TKN which were primarily  organic forms.  PO^
increases in  well 6884 were due to flooding of the  well in  Dune 1982.
     Organic  Carbon--Both total organic carbon (TOC) and chemical oxygen
demand (COD)  were measured in well water  samples  to  determine the levels of
organic matter.  Ground-water COD measurements were  quite variable from June
1980  through October 1982  (29th month) and appeared to  stabilize during
1983 (Figure  64).  During the baseline  and  irrigation periods, average  COD
values  ran.ged from 27.2 mg/1 to 125.4 mg/1 (well 6887)  and 11.4 mg/1 to
100.3 mg/1 (well 6896), respectively (Tables  C.21  and  C.22).  Median  COD
values  were  from  12.1 mg/1  to 159.1  mg/1  (well  6887) from June 1980 to
February 1982 and 10.3 mg/1 to 46.9  mg/1  (well 6855) during the irrigation
period.   Approximately 80 percent of  the  Gray wells contained less average
COD in their  respective ground water during the  irrigation  period compared
to the baseline  COD concentrations.   Similarly, ground-water TOC  concentra-
tions, decreased from the baseline period  through  the irrigation  period
(Figure 65).
     Comparison of  baseline  irrigation TOC data show a significant TOC
decrease in water collected from wells  6857,  6854,  and  6855 (Table  C.20).
Water  collected from well  6884 which was inundated showed an increase in
COD  and TOC  (Figure  65)  during June 1982.  Well 6880,  which was  also
inundated, (Figure 66) experienced a  large  increase in  COD from 40 ppm to
209 ppm in May 1982.  Well ground-water elevation data  indicates  a  drop in
water  level  during this sampling period  in well  6880 (Figure D.3).  Suffi-
cient information was not available to  develop a  scenario about the  possi-
ble cause of  this COD increase.
                                  182

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CD
                                                                              KEY	
                                                                          Q Well 6885
                                                                          O Well 6890
                                                                          A Well 6864
                                                                          O Well 6882
                                                                             Well 6881
            1.00
         June 1980
6.00
            r          r
11.00      J6.00      21.00      26.00
               MONTH SRMPLED
  r
31.00
 T
36.00
    41.00
October 1983
         Figure 64.  Chemical Oxygen Demand Concentration  in  Well  Water over Time, Gray Farm

-------
                                                                  KEY
                                                              D  Well 6883
                                                              O  Well 6884
                                                              A  Well 6885
                                                              0  Well 6886
    1.00
June 1980
6.00
11.00
16.00      21.00      26.00
    MONTH SRMPLED
31.00
36.00      41.00
     October 1983
      Figure 65.  Total Organic Carbon  Concentration  in Well Water over Time, Gray  Farm

-------
CD
                                                                                       KEY

                                                                                   D Well t>888

                                                                                   O Well 6883

                                                                                   A Well 6880

                                                                                      Well 6886
          1.00
        June  1980
         Figure 66.
 T	r°	1	1	1	r
6.00        11.00      16.00      21.00       26.00      31.00      36.00      HI.00
                           MONTH SflMPLED                               October 1983
Chemical Oxygen Demand Concentration  in  Well  Water over Time, Gray Farm

-------
     Minerals — The  salt  management  procedure employed at the Gray farm
prior to  transporting water to the Hancock  was leaching.  The average con-
centration of total dissolved solids (TDS) in the ground water beneath  the
Gray farm varied from 1010 mg/1 (well  6890) to 2271 mg/1 (well 6893)(Table
C.18).   Surface runoff entering directly  into the well casing or along  the
gravel  pack surrounding the casing may have diluted TDS levels measured in
wells 6886, 6888, 6892, 6880, 6882, and 6884 during precipitation events in
August/September 1981 (15th  and  16th months) and May/June 1982 (24th  and
25th months)(Figure 67).  The erratic  variation of TDS  concentration  in
well 6882 may  have been attributable to  the proximity of the well to an
earthen  ditch and collection of highway  runoff.   During  the irrigation
period, average  ground-water  TDS were   from 723 mg/1 (well 6888)  to 2812
mg/1 (well 6893)(Table C.19).  Wells 6886  and 6888 experienced a signifi-
cant decrease in ground-water  TDS  levels  and a significant increase in  TDS
was measured in well 6895 during the irrigation period.
     Calcium, Mg,  K  and  Na salts  were  the primary  contributors  to  the
ground  water dissolved solids beneath  the  Gray  farm.  The  average ground-
water Ca levels ranged from 47.7 mg/1  (well 6893) to 161.7 mg/1 (well 6880)
during  the baseline period.  No significant  (a = 0.05)  differences  in
ground-water  Ca  concentration were determined  when comparing  the data
obtained prior to February 1983 and the data from February 1982 to October
1983.   A  comparison of average ground-water Ca  levels computed  for  the
baseline and  irrigation  p_eriods (Tables C.23  and C.24);  however, does
indicate  a slight  increase in Ca  levels  in 72 percent of the wells. Fur-
thermore,  Mg concentrations increased  slightly in 19 of 25 wells.  Average
Mg concentrations were from 21.8 mg/1  to  137.6 mg/1 from June 1980  to Feb-
ruary 1982 and from 38.5 mg/1 to 148.7  mg/1 during the irrigation period.
Water collected  from well  6884 contained the lowest concentration of Mg
during both monitoring periods.  Well  6888  had  a  significant (a =  0.05)
decrease  in ground-water  Mg  during the irrigation  period.  The  minimum
average ground-water hardness  was  368  mg/1 as CaC03 (very hard). Since  the
ground water beneath the farm was mined by the City of Lubbock and adjacent
farmers,  scaling problems in  transport system most likely existed  or will
occur in the  future. Associated with the  increase  in  Ca and Mg  in  the
ground water was a decrease in  Na levels  in 15 of 25 wells.  Calcium and Mg
                                  186

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 o
 o
                                        Precipitation Events
                                                        KEY	
                                                      Q Well 68B5
                                                      O Well 6806
                                                      A Well 68B8
                                                      O Well 6890
   1.00
June 1980
 Figure 67.
 6.00
11.00
 I           I           I
16.00      21.00      26.00
    MONTH SflMPLED
31.00
             I
36.00      41.00
      October
Total  Dissolved Solids Concentration in Well Water over Time,  Gray Farm

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were probably  replaced by other exchange cations, primarily Na, on the soil
complex.   The  combined reduction in Na and increases in Mg and Ca  produced
a decrease  in SARadj in  17 wells (Table 32).  During the baseline period
the average  SARadj of  ground water from 25 wells exceeded nine with well
6893 exhibiting the highest SARadj value of 23.9.  Flooding of well 6884
reduced  its  average SARadj value from 9.4 to 6.2.  Severe sodic problems
would  develop  in  the soils of  adjacent farms  which utilized  this ground-
water  source  for  irrigation.   Figure 68 presents the location  of wells con-
taining  water with SARadj  greater  than  nine.  As expected, areas on the
farm which were  historically  irrigated by flood or row water contained  the
higher Na levels.  In  1982 the cropping pattern was changed and alfalfa
became  the primary  crop  grown.  A more even and reduced hydraulic distribu-
tion of  water over the entire farm associated with higher evapotranspira-
tion reduced  leaching of Na  from the upper soil profile.
     During the  irrigation  period,  significant (a  =  0.05) increases  in
ground-water  Fe  concentration  were measured in wells 6884  and 6870  (Table
C.20). Furthermore, increase in the  number of  wells (i.e., 6855, 6888,
6889,  6890,  6848,  6849,  and  6883) containing water which had Fe concentra-
tions  equal  to  or exceeding drinking water standards was observed  (Table
C.17).   Saturated  soil   conditions in May 1982  caused reduction of  Fe  to
soluble  ferrous  iron and subsequent percolate water transported increasing
quantities of  ferrous Fe to  the ground water.  Data presented  in  Figure  69
substantiate  the  hypothesis that percolation resulting from heavy precipi-
tation  events  in  May (24th month) and August/September 1981  (15th and 16th
months)  leached sufficient quantities  of Fe to the  ground water  to ex-
ceed or equal  drinking  water  standards.  Due to the  rapid rise and  fall
of Fe  in  most  wells, the data  indicate a rapid recharge of the ground-water
table  and  transport of  Fe away from the well.  Transport time of percolate
in the  ground  water may  have been decreased by such factors as:
     1.   high ground-water  elevations
     2.   indurated layers within the soil profile, such as plow pans, clay
          lenses,  and caliche  layers
     3.   macropores with the  soil profile
     4.   rock fractures
     Each factor  cited may have influenced the transport of percolate water
                                   188

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                           TABLE 32.  SODIUM ADSORPTION RATIO'FOR GROUND WATER BENEATH GRAY FARM
CD

Parameter
Well No.
6848
6849
6852
6854
6855
6856
6857
6864
6870
6880
6881
6882
6883
6884
6885
6886
6887
6888
6889
6890
6891
6892
6893
6894
6896
Ca
(meq/1)
B*
4.83
4.43
4.40
4.54
4.80
4.38
5.16
5.00
4.92
8.07
4.04
5.49
4.08
5.56
3.94
3.79
5.54
2.79
5.51
3.28
4.56
5.27
2.38
3.46
6.10
I**
5.77
5.63
6.10
5.21
5.52
6.68
5.77
6.03
5.70
7.51
5.48
6.00
5.88
5.13
4.88
3.31
5.17
2.20
5.17
4.16
5.90
5.19
2.90
4.98
8.74
Mg
(meq/1)
B
7.39
6.97
6.85
7.06
7.31
7.26
7.33
6.95
5.66
6.13
6.58
5.74
6.56
1.79
- 7.25
5.74
6.95
7.78
8.46
5.16
8.74
6.28
7.74
5.17
11.32
I
8.19
8.54
8.04
7.75
8.77
8.42
7.71
8.33
6.14
5.28
7.07
5.66
8.05
3.17
8.06
4.63
7.16
4.40
8.15
7.18
9.21
5.71
10.59
5.60
12.23
Na
(meq/1)
B
13.75
13.72
14.42
17.47
15.02
12.94
15.18
12.54
13.35
3.17
7.80
4.76
5.62
6.95
10.97
7.07
5.89
7.84
8.29
6.06
6.71
11.60
20.69
10.87
6.16
I
12.45
9.60
14.72
15.99
15.52
12.19
14.72
12.69
11.32
1 .58
4.30
7.48
4.08
5.15
10.70
5.44
7.18
3.22
6.60
6.30
4.05
11 .15
27.73
9.00
5.33
SAR
(meq/1)
B
5.6
5.7
6.1
7.2
6.1
5.4
6.1
5.1
5.8
1 .2
3.4
2.0
2.4
3.6
4.6
3.2
2.4
3.4
3.1
2.9
2.6
4.8
9.2
5.2
2.1
I
4.7
3.6
5.5
6.3
5.8
4.4
5.7
4.7
4.7
0.6
1.7
3.1
1 .5
2.5
4.2
2.7
2.9
1.8
2.6
2.6
1 .5
4.8
10.7
3.9
1 .6
SARadj
(meq/T)
B
15.12
15.4
16.5
19.4
15.9
14.6
16. '5
13\3
14.5
3.2
8.2
5.0
6.0
9.4
12.0
8.0
6.2
8.5
7. "8
7.5
6.5
13.0
'23.9
12.5
5.5
I
12.7
9.7
14.8
17.0
16.2
12.3
15.4
12.7
12.7
1 .4
4.4
7.8
3.9
6.2
10.9
6.2
7.5
4.0
7.0
7.0
4.0
12.5
27.8
9.8
4. "5
             *SAR  ,. values presented  in Appendix  H.
                 aaj

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                                                                            O  Well
                                                                            -»:- Ponded
                                                                            ---" Water
                                                                               = 0.27 km
Figure  68.   Gray Wells  which Contain  Water with SARad.  greater than 9

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                                                                             KEY
                                                                         D Well 6885
                                                                         O Well 6886
                                                                         A Well 6887
                                                                         4 Well 6888
                                                                         X Well 6890
   1.00
June  1980
            I          T
16.00      21.00       26.00
    MONTH SRMPLED
             &.OD       n.on

Figure 69.   Iron Concentration in Well Water over Time,  Gray Farm
 r
31.00
 T
36.00
      I
    41.00
October 1983

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to the ground  water  contained in wells 6848,  6849,  6856,   6855, and 6890.
Ground-water elevations  in these wells were relatively shallow ranging from
three  to  nine meters from the ground surface.  A caliche  layer existed  at
depths of 45 to  110  cm beneath the soil surface.   Percolate  water  can  be
held  above  the caliche layer until it moves vertically through the indur-
ated layer or  the  water  can flow horizontally across the layers and  effect
the  flow  of  percolate  through the caliche layer at the Gray farm.  Pulse
ground-water Fe  concentration increases measured in wells  6888 and 6889
were  most likely governed  by soil profile characteristics  (factors 2,  3,
and 4 cited  above).
     Fewer wells  equaled or exceeded d-rinking water recommended secondary
constituent  levels for Mg from February 1982 to October 1983  (Table  31).  A
significant increase in Mg (5.52 ppm) was measured in well 6893 in  October
1982.  In addition,  Mn in water collected from wells 6884 and 6889 equaled
or exceeded  drinking water  standards  (0.05 ppm)  during the  irrigation
period.  Factors similar to those governing the transport of iron  to the
ground-water  table also affected the increase in ground-water Mn observed
in several wells.
     Major anions associated with  the salts were chlorides  and sulfates.
Average chloride concentrations ranged from  208  mg/1 (well  6890)  to 535
mg/1  (well  6854)  during the baseline monitoring  period and  154 mg/1 (well
6888) to 686 mg/1  (well 6896) during the irrigation period.   Based on
guidelines presented in  Table 30, use of the ground water beneath the flood
or row water irrigated area delineated in Figure G.17 for sprinkler  irriga-
tion of alfalfa  and  grain sorghum may cause  foliar injury.  A significant
(a = 0.05) rise  in chlorides from a minimum of 114 ppm to a maximum  381 ppm
was  experienced in  well 6890 during  the project monitoring period  Ground-
water chloride  levels in wells 6849,  6880,  6884, 6887, 6880,  6892, and
possibly 6889  were affected by precipitation events during  August/September
1981  and May/June  1982 whereby water  with a lower chloride  concentration
was  entering  the ground water.  Ground-water hydrographs  indicate wells
6880, 6884,  and  6892 were  inundate  wells during the project monitoring
period  (Figures D.3 and D.5).  Well  6849 which was in close  proximity to a
playa lake most  likely received some ponded water  either directly into the
well  or  as  a  result of a very short migration through the upper soil pro-
                                 192

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file to  the  gravel  packing surrounding the  well  casing.   Ground-water
chloride  levels  in  wells  6893,  6894, 6854, 6855, 6857, 6870, 6881, 7000 and
6883 were relatively  stable  throughout the project (Figure 70).
     Before effluent  was  pumped  to the Hancock  farm, average ground-water
sulfate  concentrations  varied  from 149 mg/1 (well 6894) to 795 mg/1 (well
6893).   Once  the hydraulic  loading was reduced, 148 mg/1 (well 6894)  to 399
mg/1 (well 6855)  was the range  of average ground-water  sulfate (50^)  con-
centrations measured  beneath  the Gray farm.  Significant 50^ decreases  were
measured  in wells 6881, 6889, and 6892.  A significant increase in sulfate
ion  was  measured in  well 6893.  A similar ground-water increase in sulfate
ion wasmeasured  in  well 6893.   Similar to ground-water  chloride levels,
sulfate  concentrations in  wells 6880, 6884, 6888, 6886, 6894, and possibly
6854 appeared to be affected  by  precipitation events.
     Trace Metals--Tables  C.23 and C.24  present the average trace metal
concentrations  in  the ground water beneath the Gray farm.  The majority of
trace metals  analyzed in  each water sample were at low concentrations.  This
was  anticipated since the  irrigation stream contained low levels of trace
metals and the soil matrix  had  the ability to remove most metals. Nonethe-
less, certain metals  did  increase significantly in the ground-water samples
obtained  from certain wells  and/or equaled or exceeded drinking water  MCls
and  warrant  discussion.   Therefore, the following discussion pertains  to
the variation of Pb,   As,   Se,  and Ag in the ground water beneath the  Gray
farm.
     Drilling muds used during the construction and  development  of new
wells at  the  Gray farm probably  introduced certain Pb salts into the well.
Lead  is  normally strongly  bound to soils; consequently, Pb associated  with
dust or eroded soils  entering the well from   the  surface  may have  caused
the  high concentration experienced in most well water samples collected in
June 1980 (Figure 71). The  increase in Pb measured in  almost every  well
in the fall   1983 was probably  due to  Pb associated with colloidal  matter
not filtered  from the water  sample.  Previous  heavy precipitation  events
did  not  produce any  detectable response in ground-water Pb concentration.
Average  Pb concentrations  ranged from <_ 0.002 ppm to 0.01 ppm (wells  6880
and  6881)  during  the baseline  period and from 0.003 ppm to 0.041 ppm  from
February  1982 to October  1983.   The data showed no potential public  health
                                  193

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  o
  o
                                                                       KEY
                                                                   D  Well  6854
                                                                   O  Well  6855
                                                                   A  Well  6857
                                                                   -f  Well  6870
                                                                   X  Well  6891
  1.00
June 1980
  Figure 70
6.00
11.00
                        1           T
16.00      21.00      26.00       31.00
    MONTH SflMPLED
                                                                    36.00      ill.OO
                                                                         October 1983
Chloride Concentration  in Well Water over Time, Gray Farm

-------
                                                                   KEY	
                                                                D Well 6885
                                                                O Well 6886
                                                                A Well 6887
                                                                   Well 6888
   1.00
 June 1980
6.00
11.00
16.00      21.00      26.00
    MONTH SflMPLED
31.00
36.00
      I
    41.00
October 1983
Figure 71.   Lead Concentration  in Well Water over Time, Gray Farm

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hazard.
     Water collected from well  6889 in May  1982 contained sufficient  As
(0.0547  ppm)  to  equal or exceed  the  drinking  water MCI of 0.05 ppm.  In
addition,  significant  (a =  0.05) increases in As were measured in  ground
water collected  from  wells 6889  and  6848 during  the  irrigation period.
Baseline  average ground-water As levels were from  <0.005 ppm to 0.009  ppm.
During the irrigation period, average As levels ranged  from  <0.005 ppm to
0.038 ppm  (well 6889).   Water extracted  from 23  of  25 wells contained
average  As levels less than or equal  to 0.010  ppm from February 1983 to
October  1983.  In May 1983, 11.08 cm of rain fell on the Gray farm. Anionic
metals such as As adsorbed onto the soil more readily at pH  levels of four
or less  and  surface  adsorption decreases with increasing soil  pH.   There-
fore, As could have been leached from soils  in  the  upper profile by perco-
late water.
     Similarly,  Se  an anionic heavy metal,  is more available at high pH
levels.   Contrary to  the numerous ground-water  Se concentrations exceeding
drinking  water  standards beneath the Hancock farm,  the water  beneath the
Gray farm had  Se  levels  well below the drinking  water MCI  of 0.01 ppm.
Except for water  obtained  from well 6896, all the remaining  wells contained
water with less  than  0.007 ppm Se.
     In general, ground-water Cr concentrations were less  than 0.005 ppm.
Therefore,  no  potential  public health problems  existed with  the  presence of
low  levels of Cr in the  ground water-  Average  Cr levels in the  ground
water ranged  from <0.005 ppm to 0.009 ppm and <0.005 ppm to  0.021 ppm (well
6894) during  the baseline and irrigation monitoring periods, respectively.
Particulates  containing  Cr probably entered  the well during  rain events in
May 1983 which caused elevated concentrations in wells 6882  and  6885.
     Sloughing of soil into well 6881  during construction and development
probably was  the  cause of  the increase in Cd to 0.019 ppm in  the water sam-
ple collected  in  June 1980 (Figure 72).  Slight Cd  increases were measured
in most  Gray wells  in  May 1983.  This small rise  may have  been associated
with transport of small  quantities of dust and  colloidal material contain-
ing  Cd  levels to the ground water during the  May  1983  precipitation or an
artifact  of sample  analysis.   Regardless  of the  slight  ground-water
impulses,  the  average Cd levels were less than  or equal  to 0.004 ppm  during
                                  196

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                                                                            KEY
                                                                        D  Well 6881
                                                                        O  Well 6882
                                                                        A  Well 6883
                                                                        +•  Well 6884
                                                                        X  Well 6885
  1.00
June 1980
6.00
11.00
16.00      21.00      26.00
    MONTH SRMPLED
31.00      36.00      m.OO
                October  1983
 Figure 72.  Cadmium Concentration in Well Water Over Time,  Gray Farm

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the entire project monitoring period.
     Currently  Co  is  not listed in the drinking water standards; however  Co
may be a carcinogen (Sawyer and McCarty 1978).  Since a signfiicant   (a =
0.05) Co increase  occurred in water collected from wells 6893 and 6855 dur-
ing the irrigation monitoring period, the Co data are being presented. From
June  1980 to February 1982, 24 of 25 wells contained water with average  Co
levels less than  or  equal to 0.006 ppm. Data  obtained  after water was
pumped to the Hancock farm, showed 11 of the 25 wells to contain water with
average Co levels  less than or equal to 0.006  ppm and 19  of 25 wells had
ground-water  average Co  concentrations less than or equal to 0.008 ppm.
Average ground-water  Co concentration in Well  6855 increased from <0.005
ppm to 0.030 ppm.  The higher Co levels were measured in water samples col-
lected in May 1983 and the fall 1983.  Since precipitation  events in 1981
and  1982 appeared to have little effect on Co and other  trace metals (ex-
cept As and Se)  it was difficult to develop a scenario defining what  caused
these  slight  increases in trace metals.  The presence of colloidal  matter
in  the water  sample analyzed  for  heavy  metals may  have  affected the
results. Nonetheless, Co and other trace metals in the ground water beneath
the Gray farm were at  levels which would pose  no toxicity problems  to
humans, crops or animals.
     As  observed  with  other trace  metals,  increases in  ground-water  Ag
concentration were measured in May and the fall 1983 (Figure 73).  Gener-
ally,  average  ground-water  Ag concentrations  were less  than  0.002 ppm
throughout the monitoring  period.  Statistically significant increases  in
Ag were only measured in water samples obtained from wells 6882 and 6891.
     In summary, the  data  shows trace metals  present in the ground  water
posed  no potential  public  health  risk.  Due to limited industrial  waste
discharges treated by SeWRP, and the ability of the soil matrix to remove
most trace metals, these results were anticipated.  With the alkaline  soils
which existed at the  Gray  farm, anionic heavy metals such  as As and  Se were
more  soluble  and consequently an  apparent association  was observed with
precipitation events  and slight As and Se increases in the ground water.
     Bacteriological data--Bacterial indicator organisms, TC and  FS were
assayed  in each water sample to determine the potential presence of  patho-
genic organisms.   Tables C.25 and C.26 provide the average indicator  organ-
                                  198

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VO
       O
       CO
    O
    »—1
    X
      in
    ~ r\i_
        1.00

     June 1900
                                               KEY

                                            D  Well 6840

                                            O  Well 6849

                                            A  Well 6852

                                               Well 6864

                                            X  Well 6870
6.00
11.00      16.00      21.00       26.00
               MONTH  SflMPLED
31.00   (   36.00       41.00

                October 1983
     Figure  73.  Silver Concentration in Well  Water Over Time,  Gray Farm

-------
ism concentrations measured  in  ground-water  samples  during  the  baseline  and
irrigation monitoring  periods.
     Salmonella  was isolated in  wells  6883,  6885, 6888  and  6892  during  the
baseline period.   Three of the  five Salmonella isolations  were measured
during the fall 1981.   In  1981  the  area which  encompasses wells 6883,  6885,
and 6888 was planted in-cotton.   With the  precipitation  in  August and Sep-
tember,  very little irrigation of  cotton  crop was conducted  after  mid Aug-
ust.  Increased water  percolation due to the  heavy precipitation  in August
and September 1981 probably transported  Salmonella to  the  water contained
in wells 6883 and 6885.  Associated with the  presence of Salmonella in well
6883 was an increase in FC concentration.  Well 6888 experienced  a  decrease
in ground-water IDS and NQ^-N at  the same  time Salmonella was isolated.  The
presence of Salmonella in  the well  appeared  to be related to  surface  runoff
entering directly into the well casing  or  along the  gravel  packed area sur-
rounding the casing.  Total  coliform and FC  increased in the  water  samples
obtained  from well 6888 during the fall 1981.  Furthermore,  Salmonella  was
detected in water samples  obtained  from wells  6888 and 6892  in June 1980.
From  February 1982 to October  1983 only one  water sample contained  Salmon-
ella.   This organism was isolated in water  from well 6884  which was col-
lected  in October  1984.  Increases in TC,  FC and FS were  also measured in
this water sample. These rises  in indicator  organism and Salmonella levels
were  a  direct effect of  the flooding  of  well  6884  during  June 1982.  Many
organisms can remain viable  in  the  soil for  several months  and  be eluted
into  the  ground  water (Dunlap  1968,  Gerba  et al  1975).  Changes  in ionic
strength of percolate  caused by precipitation  could  release  and  transport
coliform bacteria through  soils.
     The  data indicate wells 6848,  6849,  6852, 6854,  6855,  6856, 6857,  and
6864 experienced  little bacterial contamination during the  monitoring per-
iod.  Except for  well 6864,  these wells were located  in  areas  which were
row water or flood irrigated.   Statistical comparison of bacterial  indica-
tor levels during the  baseline  and   irrigation period shows  no  significant
(a= 0.05) differences for-all  wells except 6881.   One water sample  was
collected from well 6881  which was positive  for FC  in May  1982.  This high
level  of FC (3 x  10A counts/100 ml)  was a  result of  the  heavy precipitation
during May which  produced a significant  increase  in coliform  bacteria.
                                  200

-------
Fecal coliform to  FS  ratios  indicated  fecal contaimination primarily from
animals  (FC:FS <1 .0) .
Priority Organic  Pollutants
     The ground  water beneath the Gray  farm contained very low levels of
specific priority  organic  pollutants (POP)  assayed.   Tables C.27 and  C.28
show  the  average trace organic compound  concentrations of certain POPs in
ground water.   The majority  of POPs were less than their respective  detec-
tion  limits during  the baseline period. Diisooctylphthalate was present in
every well water  sample. Phthalates are  ubiquitous compounds in the  envir-
onment and consequently their  presence in  the water samples may have been a
result of water contamination  from PVC well  casing (wells 6880, 6881, 6882,
6883, and 6891),  or  phthalates in the laboratory. Well 6894 was constructed
with a stainless  steel  casing  and the average diisooctylphthalate   levels
measured   during   the baseline  period  was 35.3 ppb. Besides phthalates,
23.7 ppb and 29.2  ppb  were the average heptadecane concentrations measured
in  water  collected  from  wells 6849 and 6854.   In May 1983, the anthracene
level in water samples  obtained from 6882  was 14.9 ppb.   Besides this  one
sample,  the remaining  samples  from 6882  were <2.0 ppb.
     Statistical  analysis  of propazine levels obtained from wells 6884  and
6892  showed a significant increase in propazine concentration during the
irrigation period  (Figure  74). Propazine  was  a common  herbicide used  to
control  weeds in grain  sorghum crop production.  Consequently,  the small
increase in propazine  could  be attributable  to leaching the herbicide  dur-
ing  the  May-precipitation or  transport  of  a small quantity of particulates
containing propazine directly  into the well  or through the  gravel packing
surrounding the well casing.
     In  summary,  statistical comparison  of  trace organic compounds isolated
in the ground  water  beneath  the Gray farm  is presented in Table C.20.  Con-
tamination of  ground water by  priority organic pollutants was not a problem
during the study  period.   The  soil matrix  was  very efficient in removing
and  biologically  degrading  these organics.  Consequently, the organic com-
pounds in the  municipal effluent posed no  hazard to public health.
SOILS
     As  previously  mentioned, the soils  on the Hancock farm are primarily
                                201

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                                                   KEY

                                               D  Well  6883

                                               O  Well  6884

                                               A  Well  6885

                                                   Well  6892
  1.00
June 1980
  '           I           I            I
6.00        11.00       16.00       21.00       26.00
                            MONTH SflMPLED
                                                                         [
                                                                       31.00
  I            I
36.00       41.00
     October 1983
Figure 74.   Propazine Concentration in Well  Water Over Time, Gray Farm

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of the Amarillo  series.   Soil  types  found on the Gray farm are mainly Acuff
and Estacado loams.   Soils  on  both  farms were  formed  in  calcareous,  loamy
eloian deposits.  When  wastewater is applied to soils, a diversity of chem-
ical, biochemical,  and  physical  processes govern the  availability of nutri-
ents  and  metals to  plants,  the  mobility of nitrogen, phosphorus and metals
and the potential degradation  of ground-water  quality.
     If .soil  characteristics, such  as  topography, texture, drainage, color
of topsoil, and  past management  are  uniform throughout  a  field, each  com-
posite  soil sample  can represent four  to six  ha (Donahue et al 1971).  The
area irrigated by a  center  pivot machine was approximately 48.6 ha.  Assum-
ing the uniform  soil characteristics, 8 to 12  composite soil samples should
have been collected  to  provide a representative soil  analysis of the  area
irrigated by a  center  pivot machine.   During  each sampling period, a total
of 200 to 300 composite soil cores  would have  been required  to adequately
describe the soil characteristics of each farm.  Each 183 cm soil core would
have been divided into  30 cm sections and analyzed  for  various physical,
chemical and biological parameters  giving a total of more than 3000 samples
including quality controls.  The management and economic'limitat ions  asso-
ciated with handling and analysis of more than of 3000 samples per sampling
period dictated  the  reduction  of sample load  to a total  of 54 cores  for
both  farms collected  each  sampling period.   Consequently, sufficient sam-
ples were not collected to  adequately define the spatial variation  in  soil
characteristics  throughout  the entire farm.  In addition, nine farmers were
responsible for  the  agricultural practices employed  at  the  Hancock  farm.
Therefore crop  and soil management practices varied throughout the farm.
The only factor  relatively  constant  throughout the project  period  was  the
hydraulic loading applied  to  various portions of the farm. Thus, interpre-
tation of the Hancock soils  data was based on  three  average hydraulic load-
ings  (42.2 cm + 4.2, 52.2  cm  +_  3.8, and 68.9  cm +_ 5.4) received by various
portions  of the  farm. Soils  data  obtained from the  Gray farm will be dis-
cussed according to cropping patterns employed during  1981, 1982,  and
1983.
                                  203

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Hancock Farm
      Physical characteristics of the Hancock soils  beneath  the center pivot
 irrigation machines are presented in Table E.1.  The  soil texture within
 the upper 30  cm (1  ft) of the soil profile was  generally  sandy clay loam.
 Clay to clay loams dominated the soils from  a depth of 30 cm to  122 cm (4
 ft) within the profile.  The majority of soils from 122  cm  to 183 cm (6 ft)
 were clays.  An  apparent trend towards higher sand  and  silt concentrations
 in the  texture  analysis may be due to soluble salt increases from 1981 to
 1983.   This has  been cited (Black 1965)  as  one  possible interference in
 hydrometer type texture  analysis.  Soils  beneath center  pivots 19 and 20
 (northwestern corner) were primarily sandy clay loams  from 0 to  122  cm (4
 ft) (Figure 8).   The land beneath pivots 19 and  20 was  the highest surface
 elevation on the farm.  Consequently,  coarse material  remained  at  these
 locations while finer materials were  transported  by  wind  and surface run-
 off toward the playa lake areas.  Playa lakes on  and surrounding the  Han-
 cock farm  contained gray clays  which are  commonly called  Randall clays.
 The material within the playa lake  which was included  in the irrigation
 pattern of center pivot  18  (code number  23145)  was  typical  of Randall
 clays. The soil  texture within the soil profile of  the playa lake  included
 under  pivot 2  (code number  1141)  however,  changed during the study from
 grayish brown  clay (baseline) to  sandy loam or  sandy clay loams  (Fall
 1983).  This change in the upper 91  cm may have reflected the incorporation
 of solid waste,  produced by the local cotton gin,  into  the soil profile.
 This  practice is commonly employed   not only to  handle  a solid waste prob-
 lem but also to  improve the soil characteristics  for crop production.   An
 indurate layer  of calcium carbonate (caliche) existed within the soil pro-
 file at a depth  of 61 cm to 183 cm throughout the farm.
 Nitrogen—
      Nitrogen applied  to soils  is removed  from  the wastewater stream by
 adsorption, crop utilization, and gaseous nitrogen  losses by ammonia  vola-
 tilization and/or dinitrogen (N£)  and nitrous oxide evolution through the
 denitrification  process.  Nitrogen loss due  to ammonia  volatilization is
 increased in soils with high calcium carbonate concentrations, pH above 7,
                                  204

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low cation  exchange  capacity, low buffering capacity,  warm  temperatures,
decreased  soil  moisture and high ammonium concentrations at the  soil sur-
face (Fenn  1975,  Gasser 1969,  Fenn and Kessel 1974).   Soils at the  Hancock
farm were  alkaline and calcareous with pH values, within  the upper 183 cm,
of seven  to eight.   Cation exchange capacities (CEC)  were greater  than 20
meq/100 g  (average 22.4 meq/100 g -h 3.7) which were  characteristic  of the
clay/clay  loam  soils.  Due to the CEC value, volatile  ammonia  may  have been
adsorbed  onto clay material; thereby preventing the escape  of  ammonia from
the soil  matrix.   Most of the ammonia-nitrogen .was present  in  the  upper 152
cm of the  soil  profile.  The soil CEC value and pH levels, however, indi-
cated  that  volatilization most likely did not  contribute  significantly to
nitrogen  losses.
     The bulk  of  the  nitrogen  in the soil profile was  in the  organic  form,
which appeared  to  decrease linearly through the upper  15  cm of the profile.
Carbon to  nitrogen (C/N) ratios of the organic matter ranged from  3  to 47
with only  three percent of 235  cores having a  C/N ratio greater  than 20.
Generally,  a a C/N ratio  of  approximately 22 and a  N  percentage  of two,
mineralization  of  organic nitrogen  equals the  immobilization of organic
nitrogen  (Campbell 1978,  Loehr 1979).  Smaller C/N  ratios are associated
with net  mineralization and ratios higher than 22 indicate  net immobiliza-
tion.  The  average C/N ratios of the effluent pumped  to the  farm and from
the reservoirs  were 4.0 and 5.9, respectively.  Therefore,  net mineraliza-
tion of organic nitrogen predominated within the soil  profile.
     Tables  21  and 22  present the monthly amount of irrigation at  the Han-
cock farm  during 1982  and 1983.  Due to the low quantities  of  water  applied
to soil,  the soils were normally well drained resulting in  good soil aera-
tion within the  profile.  As  a result of adequate soil  aeration  and  alka-
line pH values, nitrate was the major inorganic nitrogen form (Tables E.2
to E.4).  Good aeration probably limited denitrification  within  the  upper
61 cm of  the profile.  The data indicate that sufficient  carbon sources may
have been available  for  denitrification (Tables E.5  to E.7).   Nitrate
lenses  were  detected within the lower 91 cm of several  soil cores (Figure
75).   Low moisture conditions in the semiarid climate of  the South  Plains
may have  inhibited decomposition of organic matter and  denitrification of

                                  205

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      o
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                                                  Hancock Farm
                                                                                      KEY
                                                                                   O Soil  Core 02003


                                                                                   O Soil  Core 05071

                                                                                   A Soil  Core 06043
                                           T
                                    T
                                                T
       0.00
      Figure 75.
0.03
0.07
0.21

  -i
                        0.10        0.1U        0.17


                      WTRITE + NITRATE (MG  N/G)'10


Illustration  of Nitrite+Nitrate Lenses in Hancock Soil, 1981
0.214
0.28

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N03-nitrogen .   With  approximately 20 cm of effluent applied in a two week
period,  Ryden  et al  (1981) observed maximum total denitrif ication and ^0
fluxes from  soils  within 24 to  36  hours after  irrigation  events.   This
quantity  exceeded the  annual hydraulic load to the farm.  Denitrification
may have been significant during heavy precipitation events experienced  at
the farm in  August/September 1981 and May/Dune 1982.
     A nitrogen  mass  balance for the three average hydraulic loadings  was
conducted  to delineate the major mechanisms  governing nitrogen losses.
Nitrogen inputs  to the soil  were primarily a result of effluent irrigation.
During  1983 several  farmers  may  have  used fertilizers but the types and
quantity  were  not available  for  incorporation  into the  mass balance.
Therefore,  nitrogen  input due to application of fertilizers was assumed to
be negligible.   An additional sources of nitrogen is through precipitation.
Inorganic  and  organic  nitrogen within the soil  profile  may be sources
and/or sinks of  nitrogen.  Nitrogen is lost by volatilization, crop uptake
and harvest, deep  percolation, and denitrification.  Nitrogen losses due to
volatilization were assumed  negligible and 10 percent of the inorganic pool
in the soil  profile was  assumed  lost due to denitrification.  The following
mathematical relationship presented by Mehran et al (1981) was used to com-
pute a nitrogen  mass  balance:
     Niorl  = Nlt-1  +  K(eir- Qir
                     r  +  (1-d)(1-e-km1t)NAor + (1-e-km2t)Nfn
          + (1-e-'
-------
             Qp  =  Amount of precipitation (cm/yr)
              e  =  Fraction of  nitrogen applied by irrigation entering the
                    soil profile,
              a  =  Runoff coefficient,
              g  =  Gas  loss coefficient for applied inorganic N
                  fertilizer,
              d  =  Gas  loss coefficient of applied organic N fertilizer,
              km-|,  km2> I20) values in the soil profile at the Hancock farm, NH3
nitrogen may adsorb on the soil matrix before it can escape to the  atmos-
phere  (Ryder 1981), Fenn 1975, Gasser 1969).  Ammonia volatilization prob-
ably was minimal within the soil profile.  Based on the  preceding  assump-
tion, equation (1)  reduces to  the following form:
          Nior|t = Nior|t-1 +  K(e.Cir.Qir + (1-a)CpQp)                 (2)
                                  208

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     The mineralization rate  constant (km3)  was  assumed to equal 0.0052
yr~^ (Mehran  et al 1981).  The values for the parameters used in equation
(2) are  presented in Table 33.  The amount of denitrified N^ was computed
by the  following expression:
               Nd = C(Nior|t)                                        (3)
         Where   C = denitrification coefficient (.10).

The amount  of nitrogen  taken up by  plants is presented in Table F.I.  A
weighted average of the nitrogen  uptake was computed  for each hydraulic
loading.
     Only the  cotton lint and/or seed from the cotton  and grain  producing
crops were harvested.  The remaining crop biomass was assumed to be  incor-
porated  into  the soil organic mass prior to the next  growing season.  The
coefficients used to determine  the mass of organic  nitrogen incorporated
into the soil after the first growing season are  also  presented in Table
F.2.
     Since  the  water  balance  indicated  no deep percolation of inorganic
nitrogen through the profile the amount of inorganic nitrogen present in
the profile  was calculated as:
               Nior|net   = Nior|t - Nd - Ncp                            (4)
       Where    N^or|   , = inorganic nitrogen  remaining in soil profile
                               (kg/ha-yr), and
                Ncp = Weighted  average nitrogen uptake  by crops, (kg/ha-yr).

     Figure  76  presents the  predicted and average measured  mass of  inor-
ganic  nitrogen within the  upper 183  cm  of the soil profile in the  fall
1983.   The spacial variability  of the data in  conjunction with the  error
associated  with the assumptions imposed on the model  have produced highly
variable results.  At the lowest hydraulic loading (42.2  cm) the processes
included in the nitrogen model appeared to describe the  majority of nitro-
gen transformation within the soils.  Crop nitrogen  uptake always exceeded
nitrogen mass input by  irrigation.  Increased nitrogen  loses due to deni-

                                 209

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                    Table 33
Input Parameters and Coefficients for Hancock Soils
               N Mass Balance Model




IS3
O




Parameter
1981 Inorganic nitrogen mass in 183 cm soil profile
1981 Organic nitrogen maaa in 183 cm soil profile
Annual hydraulic loading in 1982 and 1983
Nitrogen concentration in irrigation water
in 1982 and 1983
Amount of precipitation in 1982 and 1983
Nitrogen concentration in precipitation
Fraction of nitrogen applied by irrigation
Runoff coefficient
Mineralization rate constant
Denitrification coefficient
Average Hydraulic
Loading 42.2 cm
Symbol Value
Nior|t_i 270-9 k9-N/ha
Nor|t -j 9486.5 kg-N/ha
Qjr 16.2 cm and 26 cm
Cir 24.4 mg-N/1 and
12.4 mg-N/1
Qp 70.0 cm and 45.72 cm
Cp 1.2 mg-N/1
e 0.95
a 0.35
Km3 0.0052 yr'1
C 0.10
Average Hydraulic
Loading 52.2 cm
'Value
384.3 kg-N/ha
9605.0 kg-N/ha
19.6 cm and 32.6 cm
24.4 mg-N/1 and
12.4 mg-N/1
70.0 cm and 45.72 cm
1.2 mg-N/1
0.95
0.35
0.0052 yr-1
0.10
Average Hydraulic
Loading 68.9 cm
Value
327.9 kg-N/ha
9698.0 kg-N/ha
20.1 cm and 48.8 cm
24.4 mg-N/1 and
12.4 mg-N/1
70.0 cm and 45.72 cm
1.2 mg-N/1
0.95
0.35
0.0052 yr-'
0.10

-------
        N  in  Root  Zone  in  19U1
        N  from  Organic  N  in  Root  Zone
•"""""  N  Applied  in  Effluent
™l^1  Removed by Crop
^^^*  Denitrification
^^**  Measured level  in  Profile 1983
 ####  Difference between Measured  and
        Predicted   Potential  Leaching
400
300
^^
.c
w>
c
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|100


1 +
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100



200
300
400
, 42.2 cm , 52.2cm ,

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Figure 76. Inorganic Nitrogen in 183 cm Profile at the Hancock Farm
        211

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trification,  volatilization,  or possible  leaching were  not completely
accounted  for  in the mass balance at the 52.2 cm  irrigation loading. Miner-
alization  of  organic nitrogen may have been greater than estimated within
soils subjected to an average of 68.9 cm hydraulic  loading.  Increasing the
mineralization constant, km3, to 0.02 yr~1  (2 percent) yielded a predicted
inorganic  N mass in the profile of 302 kg/ha  compared to a measured average
of 277  kg-N/ha.   Generally, only one to three percent of the 
-------
  Q_ CN
  LU  •
  Q
                                  42.2 cm Hydraulic Loading
                                                                    KEY

                                                                   Q 1981

                                                                   O 1983
     0.00      0.02
                       0.05      0.07      0.10       0.12      0.15
                              INORGflNIC NITROGEN  (MG/G)  xlCT1
                                                                      0.17
                                                                                0.20
  Q_ CM
  uJ  •'
  CD ""
0.00.      0.02
                                   52.2 cm Hydraulic Loading
                                                                    KEY
                                                                   O 1983
                       0.05      0.07      0.10       0.12      0.15
                              INORGflNIC NITROGEN  [MG/G)     "1
Figure  77.   Inorganic Nitrogen  in  Hancock Soils

                                        213
                                                                      0.17       0.20

-------
                                       68.9 cm Hydraulic Loading
                                                                             KEY
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0.05       0.07       0.10       0.12       0.15

        INORGflNIC NITROGEN  (MG/G) *10''
0.17
0.20
    Figure 78.   Inorganic Nitrogen in Hancock Soils Receiving 68.9 cm Hydraulic Loading

-------
adsorption  of phosphorus by calcite  (Shukla  et  al  1971,  hiolford  and Mat-
tingly 1975).   Nonetheless,  the existence  of an  indurated caliche soil
(CaCQ.3 soils)  at  the  45  cm to 183  cm  depth in the  soil  profile supports the
hypothesis that phosphate-calcite reactions were  a major factor in the
removal of phosphorus from the soil solution.   The  soil profiles throughout
the farm denote a general  decrease in TP  from 1981  levels to 1983 levels
(Figures 80  and 81) .
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                                                                                  KEY
                                                                          D  1981


                                                                          O  1983
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Figure  81
O.OH
0.07
                                                                   0.22
                                         0.11        0. Ill        0.18

                                      TOTflL PHOSPHORUS  (MG/G)

                  Total Phosphorus  in Hancock Soils Receiving 68.9 cm Hydraulic Loading
0.25
0.29

-------
land.   Competing reactions by clay minerals, amorphous hydrous oxide and
calcite probably  limited the available phosphate to crops.  At depths  from
61 cm  to  183  cm  phosphorus most likely was  incorporated  in  relatively
insoluble  calcium forms (i.e., tricalcium phosphate and  hydroxyapatite).
Phosphorus  existing in these forms is not available to crops.   Phosphorus
may have also  existed as dicalcium phosphate (Labile P)  which will readily
dissolve,  should the solution P decrease, and  become available  to the
crop.
            TABLE 34.  PHOSPHORUS MASS BALANCE, HANCOCK FARM

Hydraulic
Loading
(cm)
42.2
52.2
68.9
Applied
P04-P
(kg/ha)
1982 1983
10.2 12.6
12.3 15.8
12.6 23.7
Applied P
(kg/ha)
1982 1983
13.7 16.4
16.7 20.6
17.1 30.8
Crop
Uptake
(kg/ha)
1982 1983
32.5 10.6
41.0 10.7
47.3 27-7
Soil
Profile
(kg/ha)
1982 1983
5235 4036
5687 4518
6272 4501
Unaccounted
Mass
(kg/ha)
-1186
-1155
-1744

Minerals—
     Salts contained  in the irrigation stream (approximately  1200  ppm) were
considered  a potential problem to crop germination  and  establishment, and
soil permeability.  The leaching requirement to reduce salinity  toxicity to
crops can be determined  by  the following expression (Texas Department of
Health 1981)
                              (ET - IR)
L =
      Ce
(5)
     Where
     Cm - Ce
L  = Amount  of water  required for leaching (cm),
Ce = Electrical conductivity of effluent (dS/m),
Cm = Maximum allowed  electrical conductivity of soil
     solution (dS/m),
IR = Infiltrated rainfall (cm), and
ET = Crop evapotranspiration (cm).
                                 218

-------
     The electrical conductivity  (Ec) of the effluent applied to the soil
was approximately  2  dS/m.   Maximum  EC of the soil solution  for cotton  and
alfalfa  ranges  from four  to  eight  dS/m at 25°C (Texas Department of Health
1981).   The  calculated  ET  for  cotton in the Lubbock area was 133.2 cm (Ram-
sey 1985).   In  1982, annual  precipitation recorded at the Hancock farm was'
70.24 cm.  Based on  water  balance calculations for the Hancock farm,  about
65 percent  of the rainfall  infiltrated the soil; therefore the value of IR
would have  been  about 45.6 cm.   Substituting these values into Equation (5)
produces a  leaching  requirement  of  approximately 29 cm (11.5 in).
     The estimated total water needs to satisfy the crop requirements  (ET)
and leaching  requirements (L),  were 162.3 cm.  the amount of irrigation to
achieve this water requirement was  the difference between 162.3 cm and  the
45.6 cm of  infiltrated  rainfall  for a total irrigation requirement of 116.4
cm (45.8 in).  During 1982,  however, less than 29 cm of  water was applied
to the  farm.   Similarly, from  January through October 1983, 46 cm of pre-
cipitation  was  recorded  which would  have yielded  a  computed leaching
requirement of  approximately  34 cm and a resultant total water need of 167
cm.  Therefore,  an estimated  138 cm (54 in) of irrigation  would have  been
required to satisfy the  crop ET and leaching demands.  Less than 51 cm of
water,  however,  was  applied  to the  land.  Consequently, salts were expected
to accumulate  within the soil  profile during both irrigation seasons.
     Tables E.8  to E.10 show  the  variation  of   total  dissolved   solids
through the  soil profile.   In  general salts accumulated in the upper 122 cm
of the  profile.   In  the double cropped areas  (68.9 cm hydraulic loading)
TDS levels  increased at the  152  cm  and 183 cm depths (Figure 82),whereas no
increase at  these  depths was  detected in soils irrigated with less amounts
of water (Figure 83).  Assuming  negligible crop uptake of salts, a mass
balances of  the  TDS  in  the soil  profile, indicated the majority of applied
salts  were  retained within  the  183 cm (Table 35) soil zone.  The amount of
TDS unaccounted  for  averaged  five to nine mg TDS/kg of soil, which was well
within  the  variability  of  the  data.
     Sodium salts composed  most of the salt load to the Hancock farm.  An
increase of  Na  was  measured   in the top 30 cm of the soil  (Figures 84 and
                                   219

-------
                                           60.9  cm Hydraulic Loading
     o
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                                                                                 KEY
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                            0.19       0.29       0.39       O.H8       0.58

                                   TOT  DISSOLV SOLIDS  (MG/G)
0.00
           0.10       0.19       0.29       0.39        0.48        0.58       0.68






Figure  82.  Total  Dissolved Solids in Hancock Soils Receiving 68.9 cm  Hydraulic Loading
0.78

-------
   Q-CW.
   LU •
   O
                                    ^2.2 cm Hydraulic Loading
                                                                  KEY
                                                                  D  1981

                                                                  O  1983
          	1	1	1	1	1	;	1—
      "0.00      0.10      0.19      0.29      0.39      0.48      0.58
                               TOT  DISSOLV SOLIDS  (MG/G)
                                                                  0.68      0.78
   i—o
   Q_ CM
   UJ  •
     "
                                   52.2 cm Hydraulic Loading
    	1	1	1	1	1	
0.00      0.10      0.19      0.29      0.39      0.18
                         TOT OISSOLV  SOLIDS  (MG/G)
                                                                     KEY
                                                                    D 1981

                                                                    O 1983
                                                             0.58
Figure  83.   Total  Dissolved  Solids  in  Hancock Soils

                                       221
                                                                       0.68
                                                                                0.78

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     TABLE  35.   MASS  TOTAL DISSOLVED SOLIDS MEASURED IN HANCOCK SOILS
Hydraulic
Loadings
(cm)
42.2
52.2
68.9
Mass TDS in Soils TDS Applied Unaccounted
(kg/ha) (kg/ha) for Mass
1981 1983 — 1982 1983 Total (kg/ha)
9,515 12,885 +3,370 1,944 3,120 5,064 -1 694 (
10,923 15,787 +4,864 2,520 3,912 6,264 -1400 (
8,917 15,488 +6,571 2,412 5,856 8,268 -1697 (
m)
Q%]
10%)

85).   As  the  total hydraulic loading increased  in the double cropped areas
(68.9 cm),  Na accumulated within the upper 61 cm.  As previously mentioned,
if there  is  buildup of Na in the soil profile, it may create sodic condi-
tions in  the  soil.  Assuming 60 percent of the  total Na  was exchangeable
(George  et al  1985) the exchangeable Na percentage (ESP)  was approximately
two in the  upper  30 cm in 1981 and was increased to a maximum of six in  the
double cropped areas.  Sodic soils have been arbitrarily defined as soils
having an ESP of  more than 15 percent exchangeable Na (Hausenbuiller 1972).
Future use of SeWRP's effluent without proper management of sodium in  the
soil   profile  may  produce  sodic  soil (ESP > 15) in the  upper 30 cm in
approximately six to seven years of system operation.
     Data variability (CV from 15 to 52) limited the usefulness of comput-
ing  a sodium mass balance.   Nonetheless,  a Na  mass balance  (Table  36)
indicated that  Na was retained in the soil profile.  The  unaccounted  for
mass  was  well within the variability of the data.
             TABLE 36.   SODIUM MASS  BALANCE ON  HANCOCK SOILS

Hydraulic
Loading
(cm)
42.2
52.2
68.9
Sodium Applied
(kg/ha)
1982 1983
502
607
623
791
999
1484
Sodium
1981
7386
6792
6891
in Soil Profile
(kg/ha)
1983
6630 -756
73'04 +512
8414 +1523
Mass
Unaccounted
(kg/ha)(error)
-2049 (24%)
-1084 (13%)
584 (6%)
                                  222

-------
CL. CN
                                    42.2 cm Hydraulic Loading.
                                                                      KEY
                                                                    D 1981

                                                                    O 1983
   0.00
             59.80     119.60
                                 179.HO     239.20     299.00
                                  SODIUM -  Nfl (MG/G)
                                                               358.80    418.60
Q_ CM
UJ  •"
O "
D
      w
       0.00
                  1
                                    52.2 cm Hydraulic Loading
                            1
                59 80     119.60
                                  1 - 1 - 1
                                 179.40    239.20    299.00
                                 SODIUM  - Nfl  (MG/G)
                                                                      KEY
                                                                     D 1981

                                                                     O 1983
	\	1	1
 358.80     418.60     478.40
Figure 84.
            Sodium  in  Hancock  Soils

                                        223

-------
                                            68.9 cm Hydraulic Loading
                                                                                   KEY
      o
      o
      o
      (O
   Q_ r*J
   LU  •'
   Q
M
-O
   V)
      o
      00.
     o
     3V
     O
     O.
D  1981


O  1983
       0.00
  i           r           i            i           i           i         ~
59.80      119.60      179.40     239.20     299.00     358.80      118.60
                        SODIUM -  Nfl  (MG/G)
               478.HO
     Figure 85.  Sodium in Hancock Soils Receiving 68.9 cm Hydraulic  Loading

-------
      Potassium  (K)  is  a  vital  element  in  plant  growth  and  is  removed  from
 the soil more than any other  element except nitrogen.  Wastewater K/N ratio
 of 0.9 or  greater  will  satisfy  the  K  nutrient  requirement  of forage  crops
 (Palazzo  and  Jenkins 1979).   The  average  K/N  ratio  in the wastewater ranged
 from CL.71  (pipeline)  to 2.43 (reservoir).   Consequently,  the majority of
 the  K applied,  if available  to  the  crop,  should  be  assimilated by  the  crop.
 The  potassium uptake for  the various crops produced  on  the  Hancock farm is
 provided  in Table F.4.   In calcareous soils,  however, calcium  competes  with
 K for entrance  into the  plant  (Potash  Institute of America, 1973).  Conse-
 quently,  calcareous  soils may require higher  available K levels.   Tables
 E.11  to  E.13 present the variation of  K  within  the soil profile.  Through-
 out  the  farm  K appeared to decrease within the soil profile-   A mass  bal-
 ance (Table  37) indicated  that  the  crops utilized more K  than provided in
 the  irrigation, water-  Since cotton plants are defoliated prior to harvest,
 leaf tissue  from cotton plants  were not  analyzed; consequently, the meas-
 ured  K content in cotton  was low  (Table F.4).  Analysis  of  remaining  crops
 include  leaf  tissue.
	TABLE 37.   POTASSIUM MASS  BALANCE,  HANCOCK  FARM	
Hydraulic     Applied  K    Weighted  Average    Soil Profile    Unnacounted
 Loading       (kg/ha)     Crop Uptake  (kg/ha)       (kg/ha)       for Mass
  (cm)      1982"   1983       1982    1983*      1982   1983      (kg/ha)

  42.2      31.6    50.7     107.0    44.8    111,782   69,265   -42,447  (38%)
  52.2      38.2    63.6     124.1    34.4    118,089   85,018    -3,304  (28%)
  68.9      39.2   95.2     159.2   262.5    105,173  67,934   -36,951   (35%)

*Cotton Leaf Tissue not  Analyzed
      Major  aions  associated  with  the  salts applied  to the soil were  Cl and
 804.  In general,  both  these  ions appeared  to  accumulate within the upper
 122  cm (Tables E.8 to E.10).  Chloride  ion concentrations measured  in' soil
 normally range  from 50 to 500  ppm  (Hausenbuiller 1972).  Average Cl levels
 ranged from 12 to 70 ppm  in  soil  samples  collected in  1981 and 38  to 162
 ppm  in soils  obtained in  the  fall of  1983  and winter  of  1984.   The majority
                                   225

-------
of soils  analyzed  contained chloride levels at the lower end of the normal
range.  Chloride  ions may be a substitute of fluoride in apatite.   A  lense
of Cl  was  detected between 91  cm  and  122 cm in the double cropped areas
receiving  the  greatest  amount of irrigation (Figure 86).  Both sulfates and
chlorides  increased throughout the  entire soil core at average hydraulic
loading of 68.9 cm.  Analysis of soils data obtained from areas receiving  a
total  irrigation during  the  project  of about  52  cm and 69 cm,  showed  a
lense  of  SO^  ion present at 152 cm and 183 cm.  With the existence of the
indurated  caliche  layer,  this SQ(± lense may be  associated  with gypsum
(CaS04).
Trace Metals —
     Due to the  low levels of metals in the wastewater, trace metals were
not considered to pose  a problem to crops or public health.   Tables  E. 11
to E.13~present the  average concentration of metals in the 183 cm soil pro-
file.  A mass  balance computed on the trace metals (Table 38) indicated the
change in  metal   levels from 1981 to 1983 was not attributed to irrigation.
Arsenic is  contained in defoliants applied to cotton; however, the mass of
As sprayed on the  crop was normally less than one to two kg/ha.  Therefore,
the mass accumulations  of As observed in the soils were probably  not total-
ly the result  of  application of defoliants.  The large coefficient  of vari-
ability obtained  for As, Ba, Cd, Co, Pb and other metals made it  difficult
to develop  scenarios explaining increases or decreases in specific  metals.
Priority Organics—
     The majority  of  samples analyzed  for  priority organics in  1981  and
1983 contained organic  compounds at levels below  detection  levels of  the
analytical  procedure (Tables E.14 to E.16).  Atrazine, common in  herbicides
used on the farms,  was  measured in some soil samples in 1981  but was  less
than  detection levels  in 1983.  Both 2,3-dichloroaniline and 3,4-dichloro-
aniline were detected in a few samples in the upper 30 cm  of soil.   These
organic compounds  were probably degradation products of the trifluralin
herbicide  which was  commonly used  on  the farm.   Benzene  and chloroform
within  the profile in 1981 and 1983 was most likely used as a solvent for
herbicides  sprayed  on the land.  The upper 61 cm of soil  contained higher
                                 226

-------
                                            60.9 cm Hydraulic Loading
      o
      o.

      CNI
      o
      ID
    31


    Q_ CM
                                                                               KEY
ho
|SJ
O
CO
      o
      CO
      o
      3"
      O
      O.
       *
      o
       0.00
                                                                              D  1981

                                                                              O  1983
               0.02
—!	1	1	]—
 O.OU       0.06       0.08       0.10
           CHLORIDES -  CL  (MG/G)
0.13
0.15
0.17
      Figure 86.  Chlorides in  Hancock Soils  Receiving 68.9  cm Hydraulic Loading

-------
Table 38.   Metals Mass Balance for Hancock Farm
	 	 	 . 	 	 	
Metal

42.2 cm
A3
Ba
Cd
Co
Cr
Cu
Tl
Pb
Ni
Se
Zn
52.2 cm
As
8a
Cd
Co
Cr
Cu
Tl
Pb
Ni
Se
Zn
68.9 cm
As
Ba
Cd
Co
Cr
Cu
Tl
Pb
Ni
Se
Zn
Total Mass
Applied
(kg/ha)
a

0.026
0.165
0.009
0.138
0.032
0.055
0.021
0.091
0.06
0.021
0.474

0.32
0.203
0.012
0.026
0.045
0.068
0.026
0.111
0.073
0.026
0.585

0.041
0.257
0.012
0.034
0.054
0.087
0.034
0.117
0.073
0.026
0.585
Soil Profile Mass
( kg/ha)
1981 1983
b

108.0

1.79
56.32
317.9
147.1
24.7
64.1
288.89
4.694


152.55
6815
1.750
62.26
377.65
140.95
22.62
71.77
184.8

1181.0

122.30
9532.9
1.37
56.37
218.35
143.08

4B.09
184.8

1181.0
c

170.4

2.13
91.87
206.3
93.9
22.6
81.3
172.82
6.4


124.30
1284
2.688
93.84
158.14
75.53
12.80
72.41
137.8

957.9

337.83
1566.1
2.65
118.37
200.00
81.29

124.43
137.8

957.9
i in Profile
(kg/ha)
deb

+62.4

+0.34
+35.55
-111.6
-53.2
-2.1
+ 17.2
-110.07
+1.706


-28.25
-5531
+0.938
+31.58
-219.51
-65.42
-9.82
+0.64
-47.0

-223.1

+215.53
-7966.8
+1.28
+62
-18.35
-61.79

+76.34
-47.0

-223.1
Unaccounted
Mass
(kq/ha)
e d a

+58.8

+0.331
+35.41
-111.6
-53.3
-2.1
+ 17.1
-110.13
+1.685


-2B.57
-5531
+0.926
31.55
-219.55
-65.49
-9.84
+0.53
-47.

-224

+215.49
-7967.1
+ 1.27
+62
-1B.40
-61.88

+76.22
-47.

-224
Percent Error
7--— 	 	 r- X 100
fb + a)

54

18
63
35
36
8
27
38
36


19
81
53
51
58 -
86
43
0.7
25

19

176
84
92
110
a
43

158
25

19
                  228

-------
levels of  benzene than  deeper soil zones analyzed.   In addition, benzene
levels  were  less  in 1983  than measured in 1981.   This decrease  may have
been due to biological  degradation of these compounds during  the growing
season.   Herbicides were  applied in the late winter or early spring.   Sam-
ples collected  in  1981 were obtained in March through  May after  application
of_herbicides.   Soil  sample collection in 1983  occurred  in  November 1983
through  February 1984.   Another solvent,  tetrachlomethylene and  carbon
tetrachloride,  was measured above detection limits in  1983.   Organic com-
pounds used as insecticides (i.e.,  acenaphthylene,  m-dichloroben-zene,
p-dichlorobenzene, and o-dichlorobenzene) were also isolated  in the  upper
30 cm of  soil  in  1981 .  Dichlorobenzene m and o were detected  to a depth of
61 and  91 cm,  respectively, in 1983.  Phthalates were  measured  throughout
the  soil  in 1981.   Several organic  compounds  (i.e., 4-t-butylphenol,
2-chlorophenol,  ethylbenzene , methylheptadecanoate , methy Ihex adeconoate ,
and  octadecane) were isolated during 1981  but were below their respective
detection limits  in 1983.
     The  mass  of  each organic compound applied to the farm  is presented in
Table E.33.   The mass of  each organic in the  irrigation stream  contributed
very little to  the mass detected in the soil profile.
Bacteriological  Data—
     Factors which affect the retention and survival  of pathogens in soils
include temperature,  soil moisture, pH, organic matter, biological  activ-
ity, cation exchange capacity, particle size, and clay content.  Bacteria
are removed in  soils  primarily by filtration.  Bacterial  indicator  organ-
isms existing  in the soil profile in 1981  and 1983 are presented in Table
E.17 to E.  19.   In the top 30 cm total coliform bacteria existed at  levels
greater than detection limits in 1983.  Irrigation with effluent apparently
did increase the concentration of coliform bacteria in the  upper  30  to 61
cm of the soil  profile.   Similarly, fecal streptococcus was  detected  in the
upper 91  cm at  levels greater than analytical limits in 1983 in  soils col-
lected  from areas  receiving 52.2 cm and 68.9 cm.
     Actinomycetes are ubiquitous throughout soils.  In alkaline,  dry soils
over 50  percent of  the  microbial population may consist of actinomycetes
                                   229

-------
(Alexander  1967).  Average  actinomycetes  levels  within  the  soil  profile
ranged  from  109 to 1012  counts per gram of soil.   During the irrigation-
period,  actinomycetes within the upper 91  cm  experienced a  one-to-two log
increase  in  concentration.   Since an increase  in actinomycetes normally
follows  increased  bacterial and mold  growth, the  rise in actinomycetes
indicated  a  general increase in biological activity  in  the  upper 91  cm.
     Fungi levels  were relatively constant in the  1981  baseline soil  sam-
ples  (5 x 1Q.3 to 2.4 x 10.4  counts/g) .   Irrigation  produced no apparent
effect on  fungi  concentrations.
Gray Farm
     Table E.20  presents the physical characteristics of the soils included
in the Gray  farm.  Unlike the Hancock  soils, the Gray soils  contained  a
higher  percentage of coarse  material throughout  the upper 122 cm of the
profile.  The predominate soil texture within the  upper 30  cm  of  the  pro-
file  was  sandy  loam.  Sandy clay loams existed  from a  depth of 30 cm to 91
cm.  As  with  the Hancock soils, the coarser material referred  to earlier
could be the  result of salts interfering with the  hydrometer texture analy-
sis.  Coagulation  by the salts can shift  the percent  sand up  by a small
amount  (Black 1965).  Soil  texture  at  depths greater than 122 cm varied
primarily  from clay to clay loams.   Similar to the soils obtained  from  the
Hancock  farm,  an  indurated caliche soil  was observed  at depths from 40 to
183 cm.  This indurated zone made the ability to obtain discrete 30  cm  soil
sections  to  a depth of 183 cm extremely  difficult.  Consequently, the  data
shows a  high  frequency of composite  samples  collected at  depths greater
than 91  cm.
Nitrogen—
     Average  nitrogen  levels measured in the  soil  profile beneath center
pivot machines are presented in Table E.21 and E.22.  This area  was  pre-
dominantly  cotton in 1981 and produced alfalfa in  1982 and 1983.   Nitrate
nitrogen concentrations were fairly uniform throughout the entire  183 cm
soil  depth  in  1981.  Analysis of  soils in 1983,  however,  indicated  a
decrease in  nitrate levels in the upper 91 cm (Figure 87),  which  resulted
from  greater N  uptake by  alfalfa.   Ammonia nitrogen  existed  primarily in
                                 230

-------
      8.
Gray - Sprinkler Irrigated


       KEY

    D  1981

    O  1983
                 I	1	1	1	1	1	\	
       0.00      0.03      0.06      0.09      0.12      0.15      0.18      0.21
                                NITRITE+NITRflTE  (MG-N/G) Mid'1
                                             0.24
      §_
    a:
    Q_r5_
    a'
     8
                                     Gray  Flood Irrigated
                                           KEY
                                          D 1981

                                          O 1983
           	1	1	1	1	1
      0.00       0.03      0.06      0.09      0.12      0.15
                                NITRITE+NITRflTE (MG-N/G)

Figure  87.    Nitrite  + Nitrate  in  Gray Soils

                                      231
                          0.18      0.21
                                             0.24

-------
the top 30  cm of soil.  No appreciable  change  in ammonia concentrations was
observed in  NH3  levels between  soil samples collected in 1981 and 1983.
The bulk of the soil nitrogen was  incorporated in organic matter.  Organic
nitrogen decreased almost  linearly  to  a depth of 91 cm to 183 cm (Figure
88).  A reduction of organic nitrogen from 1981  levels  was measured in
1983.   Carbon  to  nitrogen  ratios  varied from 9 to 17, which indicated no
mineralization of organic nitrogen should have occurred  in the soil  pro-
file.   A nitrogen  balance  was conducted on the soil profile.  At a pH of
7.9, two to three percent of the total  ammonia could have been lost through
volatilization  as  the water  was sprayed  from the center pivot machines.
Volatilization of ammonia within the soil matrix could have been about  five
percent.   Due  to  the soil  texture (i.e.,  sandy clay loam and clay  loam),
however, ammonia escaping the profile  may have been reduced by sorption of
ammonia to  the soil.
     Nitrogen losses  resulting  from the  denitrification  process  were
assumed to  be 30 percent of the total  inorganic  nitrogen  pool.  Nitrogen
uptake  by  alfalfa  in 1982  and 1983  was approximately 250 kg/ha and 260
kg/ha,  respectively.   Cotton harvested  in  1981  removed  about 50 kg/ha.
Increased  soil  moisture  levels  resulting from  frequent irrigation  most
likely  increased the  biological  activity  in the soil  and consequently
resulted in  greater mineralization of  organic nitrogen.  The annual  min-
eralization rate of organic nitrogen was  assumed to have  been two percent
which  was  in the  range   of one  to three  percent observed in other  soils
(Bremner 1967).  The values of parameters contained in  equation (2) are
presented in  Table 39.  Figure  89  presents the results of the nitrogen  mass
balance for the sprinkler irrigated  areas.   The mass balance indicates  that
nitrogen uptake by crops was the major mechanisms governing nitrogen
losses.  Deep percolation of inorganic  nitrogen  beneath  the center pivot
machines was probably not  a  major mechanism of nitrogen loss in 1982 or
1983.
     In the flood  or  row irrigated wheat areas which encompassed an  esti-
mated 100 ha, nitrogen losses due  to denitrification of inorganic nitrogen
was  assumed  to  be  30 percent  of  the  inorganic pool.  The annual hydraulic
loading to  the wheat area varied  from  approximately 230 cm  in 1982 to 207
                                 232

-------
Q_ CM
UJ  •'
a "
                                      Gray  Sprinkler

                                          KEY
                                         D 1981

                                         O 1983
  _           I         I          I         I          I
   0.00      0.09      0.19      0.28      0.37      0.4.7
                            ORGPNIC N  (MG-N/G)
                                                             0.56
                                                                      0.65
                                                                                0.7H
 Q- CM
 UJ  •'
 a •"*
   §
                                       Flood Irrigated
                                        KEY


                                       O1983
    „           I         I          I         I         I          I
     0.00      0.09       0.19      0.28       0.37      0.17       0.56
                              ORGflNIC N  CMG-N/G]


Figure  88.    Organic  Nitrogen  in  Gray Soils


                                      233
                                                                      0.65
                                                                               0.74

-------
            TABLE 39.  INPUT PARAMETERS AND COEFFICIENTS EOR N MASS BALANCE MODEL
              Parameter
Symbol
                 Value
Center Pivot Irrigation Areas
    1981 inorganic nitrogen mass in 183 cm soil profile
    1981 organic nitrogen mass in 183 cm soil profile
    Annual hydraulic loading in 1981, 1982, and 1983
    Nitrogen concentration in irrigation water
    Amount of precipitation in 1982 and 1983
    Nitrogen concentration in precipitation
    Fraction of nitrogen applied by irrigation
    Runoff coefficient
    Mineralization rate constant
    Denitrification coefficient
Row Water or Flood Irrigated Areas
    1981 inorganic nitrogen mass in 183 cm soil profile
    1981 organic nitrogen mass in 183 cm soil profile
   Annual hydraulic loading in 1981, 1982, 1983
   Nitrogen concentration in irrigation water
   Amount of precipitation in 1982 and 1983
   Nitrogen concentration in precipitation
   Fraction of nitrogen applied by irrigation
   Runoff coefficient
   Mineralization rate constant
   Denitrification coefficient
Niorlt-1
Niorlt-1
Qir

Qp
Cp
e
a
km3
C

 Niorlt-'
 Nor|t-1

 Cir
 Qp
 Cp
 e
 a
 km3
 C
                398.6 kg-N/ha
                10,359 kg-N/ha
                65 cm, 55 cm, 55 cm
                27.93 mg-N/l
                •60.5  and 48.4 cm
                1.2 mg-N/l
                0.97
                0.35
                0.02  yr~1
                0.30

               330.8  kg-N/ha
               9741.9 kg-N/ha
               465,230,207 cm
               27,93  mg/1
               60.5 and 48.4 cm
               1.2 mg-N/l
               0.97
               0.35
               0.03 yr-1
               0.30

-------
   500
   400
N in Root Zone in  19U1
N from Organic N in Root Zone
N Applied in Effluent
Removed by Crop
Denitrification
Measured level in  Profile 1983
Difference between Measured and

300
.c
\200
5
C
0)
§>100
±S


0
c
(0
O)

O
_c
100


200

300




















'



! !i
| g I
1 § •
^ 3 '
t^ Hk I
1 Si
f

1








1981 ' ' 1982
Predicted
I
I
3 ;
I i
I *<
g ^
Ik ^
i I
ii ^
3 I
i
Sa ^
• «
1
•


j
j
j
1
1
1
i
> ' ' 1983
11 > 1 1_- a >j ij j. v^ u aii<_i
1
1
t-
^
r
(•
f-
f-
j.
fr
t
t
t
(-
t
.
t
t
t
t
t












Figure 89.   Inorganic Nitrogen in 183 cm  Profile Cotton/Alfalfa
             Gray Farm
                               235

-------
cm in  1983.   The parameter values used in the nitrogen mass balance equa-
tion (2)   are  presented  in Table  39.   The results of the  nitrogen mass
balance  for  the irrigated  areas are presented in Figure 90.  Deep perco-
lation of nitrates to  the ground water remained a significant process for
the loss  of nitrogen from the soil profile in the flood or row water areas.
The ground-water  quality data also substantiate this conclusion.
Phosphorus—
     Similar  to  the Hancock farm, an indurated caliche soil  existed within
the soil  profile  at depths ranging from 41 cm to 183 cm.  Therefore, phos-
phate  calcite reactions  were probably an important mechanism for the
removal of phosphorus  from the soil solution.   Both TP and  organic phos-
phorus exhibited  a gradual decrease in concentration with  increasing depth.
     A total  phosphorus mass balance (Table 40)  showed annual  phosphorus
removal  by crops in  1981,  1982 and 1983  was less  than the mass  applied
through irrigation.  Only 33 percent of the TP was consumed by crops.  The
remainder was probably fixed  into the soil matrix.   As  noted  with cotton
produced  on the  Hancock farm, phosphorus uptake was less.than normal values
of 15  to  34  kg/ha/yr.  The unaccounted mass of 1026  kg/ha was  equal to an
average concentration  of about 0.04 mg-P/kg and within the variability of
the data.
     The  row  water  or flood irrigated  areas appeared to  have exhibited an
increase  in TP in the  soils (Tables E.23 and E.24).  Soil  sampling  method
may have  caused  an apparent increase in  TP (coefficient of variation ranged
from 17 to 139 percent).  The phosphorus uptake  by wheat (Table 40)  was
only 12 percent  of the estimated 1072 kg/ha applied from 1981  through 1983.
Fixation  of phosphorus may have been the major   mechanism which .governed
phosphorus removal from  the soil  solution.   Some  TP  removal was also
attributable  to  deep percolation of phosphorus.
Minerals—
     Total dissolved  solids in  the soil matrix beneath the center pivot
machines  increased gradually with  depth in 1981  (Table  E.25).   Whereas,
frequent  leaching of salts in the wheat areas produced a more  uniform TDS
concentration   throughout the entire soil profile  (Table 26).  A TDS mass

                                  236

-------
•••— N in Root Zone in 19U1

1200




1000



800




600


03
"0*400
C
200
'•z.

u
c
03
S>
o
c
200

400
600
ifSIOf! N from Organic N in Root Zone



















! K
^
-i
\\
• m
\\
IN Applied in Lr fluent
••••• Removed -by Crop
^"^^" Denitrification
^^^^ Measured level in Profile 1983
»» Difference
Predicted
between Measured and
- Potential Leaching
*
^
f
r
$
*
*
*
#
•)
t
*
•s
It
*
*
^
e
*
i
i
-
-)
-j
^
^ i :
1 | ^
'
i $
« ^
S i
j • •
i i
i i

i i
j j


(•
f.
r
t
t
I
i-














1 1981 ' ' 1982 ' ' 1 983 '
Figure 90.   Inorganic Nitrogen in 183 cm Profile Wheat Area Gray Farm



                               237

-------
TABLE 40.   TOTAL PHOSPHORUS MASS BALANCE ON GRAY SOILS


Irrigation
Mode

Spray

Flood or
Row Water
Total Phosphorus
Applied
( kg/ha. yr)
1981 1982 1983
93.8 50.5 50.5
I
671.0 211.1 190.0

Crop Uptake of
Phosphorus
( kg/ha. yr)
1981 1982
9. 26.

24. 54.

Total Phosphorus
in Soil Profile
(kg/ha. yr)
1983 1981
30. 6,059

Unaccounted
Mass
(kg/ha)
1983
5,163 -1,026

54. 6,101 10,368 +3,327



N>
CD



TABLE 41. MASS BALANCE


ON TDS IN SOILS


PROFILE ON GRAY FARM




Irrigation
Mode


Spray
Flood or
Row Water
TDS
Applied
( kg/ha. yr)
'1981 1982 1983
7,345. 6,215. 6,215.
52,545. 17,707. 13,391.

TDS in Soils Change in
(kg/ha)

1981
18,091 .
25,990.

Profile
(kg/ha)
1983
22,613. +4,522
23,391. -2,599

Unaccounted
Mass
(kg/ha)

-15,253
-86,632


-------
balance  indicated  flood and row irrigation and precipitation  leached salts
below a depth  of  183 cm during the  period from  spring 1981  through 1983
(Table  41).   The salts applied to cotton and alfalfa areas,  however, were
primarily retained  in  the soil profile.  A comparison of TDS levels  within
the  profile  in 1981  and  1983 showed  a  TDS concentration  increase  in the
soil from 91 cm to  183 cm beneath the alfalfa crops (Figure  91).   The pro-
file  TDS levels  shows little variation in TDS levels within the upper 91
cm.  Once percolate  reached the  indurated layer,  the vertical  hydraulic
conductivity  may have been  reduced.   Therefore,  more  soil moisture was
available for  alfalfa  consumption, and more salts were retained in the pro-
file.   Furthermore,  with  extended drying periods (about a month) between
irrigation periods,  capillary  action may have  transported  salts  into  the
upper  183 cm  of soil; thereby causing an increase in salt concentration.
In addition, some salts may have been leached to deeper soil depths.
     Increases in  TDS levels measured in 1983 did not appear  to be associ-
ated with increases  in Na ion  (Tables E.27 and E.28).  A slight increase in
the  average  Na concentration was measured at depths of  61 and 91 cm in
1981.  Based on a CEC  in the upper 30 cm of 22 meq/100 g,  an ESP of approx-
imately seven was  computed for Na in the top 30 cm beneath  the spray irri-
gated area.   Therefore,  Na levels  were maintained sufficiently  low by
leaching to prevent  sodic conditions (ESP <15) in the soil.  Similarly,  the
ESP value for  1981  and 1983 in the upper 30 cm  of  the flood  or  row  water
areas  was seven.   In 1983,  Na levels  within  the  soil  profile at depths
greater than 61 cm  were greater than average values measured in 1981  (Fig-
ure  92).  Table 42 presents  a mass balance on Na in the  183  cm soil core.
The variability in  data can explain a large portion of the unaccounted  for
mass  in the  cores extracted'  from the spray irrigated areas.  Deep percola-
tion apparently transported Na into the soil profile to depths greater than
183 cm.
     The  average K  to N ratio in the wastewater pumped to the Gray farm in
1982 and 1983  was 1.21.  Therefore, K would not inhibit the crop  utiliza-
tion  of the  N contained  in  the wastewater stream. Contrary  to Na levels,
(Table 42), K  mass  was more unaccounted for  in  soils collected  from  the
spray  irrigated  land than the wheat areas.  Some of this loss of K can be
                                 239

-------
   s_
 Q. rg
 UJ _;
Gray - Sprinkler Irrigated



     KEY
   0.00
              I
             0.15
                      0.30      O.H5      0.60      0.75
                            TOT  DISSOLV  SOLIDS  (MG/G)
                                                           0.90
                                                                     1.05
                                                                              1.20
Q_ CM
UJ •'
o
                                Gray   Flood Irrigated

                                       KEY

                                     D 1981

                                     O 1983
  _           I         I         I          I         1         I          I         I
   0.00      -0.15      0.30      0.145      0.60      0.75      0.90      1.05      1.20
                            TOT DISSOLV SOLIDS  (MG/G)


Figure  91.   Total Dissolved  Solids  in  Gray  Soils


                                  240

-------
 O

 to .
                                       Gray   Sprinkler


                                          KEY


                                          D 1981


                                          O 1983
    0.00
              82.00
                        1 Ell. 00
                                  216.00    328.00    410.00

                                     SODIUM  (MG/KG)
                                                                T

                                                               492.00
                                                                         574.00
                                                                                   656.00
 a. PJ
 LU
 o'
   3
    0.00
                                    Cray - Flood Irrigated


                                           KEY
              82.00
164.00     246.00     328.00    "ilO.OO

             SODIUM  (MG/KG)
                                                               492.00
                                                                         S74.00     656.00
Figure 92.   Sodium  in  Gray  Soils



                                       241

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                  TABLE  42.   SODIUM  AND  POTASSIUM  MASS  BALANCE  ON  GRAY  SOILS




N>
-P-
ho

Irrigation
Mode
SODIUM
Spray
Flood or
Row Water
POTASSIUM
Spray
Flood or

Mass Applied
(kg/ha. yr)
1981 1982 1983


2,460 1,458 1,458
17,596 6,095 5,486

139 90 90
990 375 337

Crop Uptake
( kg/ha. yr)
1981 1982 1983


000
000

30 170 90
305 262 262


Mass in
Soil Profile
(kg/ha)
1981 1983


9,809
8,862

84,902
69,547


10,402
12,813

66,620
71,595

Change in
Profile
(kg/ha)

+593 .
+3,951

-18,282
+2,048

Unaccount-
ed Mass
(kg/ha)

-4,783
-25,226

-18,210
+1 ,175
Row Water

-------
attributable to the spacial variation (coefficient  of variation of about 80
percent)  in the data obtained at depths of 121  cm  and greater.  Potassium
may have  been  leached deeper into the profile.
     Cotton grown beneath center pivots consumed  less  K than applied in
1981. Alfalfa,  however,  due  to its higher  N  requirement, utilized more K
than was  applied.  Wheat had ample K provided in  the  irrigation water  and
apparently removed it  from  the soil  solution.  Very  little K was unac-
counted  for in the mass balance conducted on  soil  samples obtained from the
flood irrigated areas.
     As  previously  stated, the major anions associated with the salts
applied  to the soils were chloride and sulfate.   Higher levels of chloride
ions were found  at depths  from 61 cm  to 183 cm than  in the upper 61 cm
(Figure  93).   Soil cores obtained in the late fall  of 1983 from the  flood
and  row  irrigated areas  contained less  Cl than  the baseline soil cores.
Chlorides may  have been increased in the profile  of soils collected  at  121
to  183 cm beneath the center pivot machines.  The  variability of the data,
however,  made  interpretation of the data very difficult.
     Sulfates ions  increased through the first  61 to 91  cm of the pro-file
and were  relatively constant at depths from  91  cm  to 183 cm (Figure  94).
With greater  quantities  of  irrigation on the wheat, larger quantities of
SO^  were leached past  the  183 cm depth.  Consequently,  a more uniform 50^
profile  was observed beneath the flood irrigated  areas.   In addition,  soil
samples  collected from  the  wheat  area in  1983 contained  less SO^ than
baseline  samples  (Figure 94).
     Mass balances  on Cl and  SO^  ions present  in the  183 cm profile are
provided  in Table 43.  The results support the  deep percolation of  anions
past the 183  cm  depth in the flood irrigated  areas during the period from
1981 through 1983.
Trace Metals—
     Table E.27  shows the variation of trace  metals within the top 183 cm
of the  soil profile in wheat areas.  Table 44 presents  the total  average
mass of  specific trace metals applied by flood and row irrigation.  Over a
three year period from 1981 through  1983, input  of  trace metals  through
                                 243

-------
   Q_ CM.
   UJ •
   o •"
                                         Gray - Sprinklar

                                            KEY

                                            Q19B1

                                            O 1983
      0.00
                0.01
                         0.08
                                   0.12      0.16       0.20
                                     CHLORIDES (MG/G)
                                                               0.24
                                                                         0.28
                                                                                  0.32
  Q_ <
  UJ
  a
  o
  CO ,
                                   Gray - Flood Irrigated


                                         KEY
    °°-00      0-01      0.08      0.12      0.16      020
                                   CHLORIDES  (MG/G)


Figure 93.    Chlorides  in  Gray Soils



                                   244
0.24
          0.28
                   0.32

-------
      S
                                          Gray - Sprinkler
                                              KEY

                                             O 1981

                                             O 1983
       0.00       0.03
                          0.07
                                    0.10      0.14      0.17
                                      SULFHTES  (MG/G)
                                                                0.21       0.2<4
                                                                                   0.28
       0.00      0.03
                                     Gray   Flood Irrigated

                                            KEY
                                           D 1981

                                           O19B3
                          0.07
0.10       0.11      0.17
   SULFflTES (MG/G)
Figure 94.    Sulfates  in  Gray Soils

                                      245
                                                                0.21
                                                                           I         I
                                                                          0.2U      0.28

-------
TABLE 43.   CHLORIDE AND 5ULFATE MASS BALANCE ON GRAY SOILS

Irrigation
Mode
CHLORIDE
Spray
Flood and
Row Water
SULFATE
Spray
Flood and
Row Water




Mass in
Mass Applied Crop Uptake Soil Profile
(kg/ha. yr)- (kg/ha. yr) (kg/ha)
1981 1982 1983 1981 1982 1983 1981 1983

3,029 1,
21,762 6,


2,048
14,648 4,


667 1,667
969 6,272 98


979 979
094 3,685 99


71
98


81
99


81 3,648 4,416
98 3,192 1,660


93 4,552 4,190
99 2,901 1,890


Unac-
counted
Mass
(kg/ha)

-5,443
-36,241


-4,194
-23,141



TABLE 44.
TRACE METALS MASS
BALANCE
ON SOILS COLLECTED

FROM FLOOD AND ROW IRRIGATION AREA

Trace
Metal
As
Ba
Cd
Co
Cr
Cu
Pb
Ni
Mass Applied
(kg/ha)
1 .887
26.96
0.276
0.358
4.820
5.167
2.962
4.235
Mass in Soil Profile
(kg/ha)
1981 1983
85.1
2351.
2.56
36.8
593.7
202.2
34.4
175.0
26.9
1267.
4.40
90.1
189.4
83.3
101.4
118.6
Change in Unaccounted
Soil Profile Mass
(kg/ha) (kg/ha)
-58.1
-1084.
+1.84
+53.3
-404.3
-118.9
+67.0
-56.4
-60.0
-1111
+1.56
+52.9
-409.1
-124.1
+64.3
-60.6
                             246

-------
irrigation  to the soil was low.  Compared to  the  concentration of metals in
the soils,  the concentration of metals in the crop  tissue was negligible.
Anionic metals  such as As and Cr (VI)  probably  were transported by perco-
late to depths greater than 91 cm within the  alkaline  soils. In addition,
Ba, Cu, and  Ni  possibly  leached beyond  the 91 cm soil  depth.  Possible
accumulation  of  Cd,  Co and Pb occurred in the upper 91  cm of soil  in  the
flood  irrigated areas.   Special variability had the most impact on the
unaccounted for  trace metal mass measure in 1981  and 1983.
Priority Organics—
     The majority  of soil samples  analyzed for specific priority organic
compounds,  contained  levels below their  respective  detection limits (Tables
E.29 and E.30).  Furthermore, the frequency at which the concentration of an
organic compound at  each depth interval  exceeded its  detection limit  was
generally  low  in  1981 and  1983.  Basically, the same organic compounds
which were  prevalent  within the soil profile  at the Hancock farm predomi-
nated the  soils  collected  from the Gray  farm.
     In both  the spray and fl.ood irrigated areas, solvents such as benzene
and chloroform  existed throughout the 183 cm soil  profile in 1981.  Benzene
levels decreased to  levels barely exceeding detection  limits in 1983.  In
1983,  however,  chloroform levels appeared to have increased from baseline
levels. Furthermore, the  chloroform concentration  increased with depth.
     Similar to the finding  present in the  discussion of Hancock soils,
carbon tetrachloride  and tetrachloroethylene  were not  measured .at concen-
trations  above  detection limits  in 1981,  but were  detected at  levels
exceeding  analytical  limits in practically all samples  collected from flood
and spray  irrigated areas  in 1983.   Carbon tetrachloride concentrations
were relatively  constant  within  the  entire soil  profile and in samples
collected  throughout the farm.  These  finding may reflect sample contami-
nation during soil  collection, handling, and  analysis.
     Chlorinated aniline compounds  such as  2,3-dichloroaniline and 3,4-
dichloroaniline may  have  been derivative of herbicides or fungicides.
Trifluraline, which  was commonly used would not have been applied to either
the wheat  or  alfalfa  areas.   Unless  pulses of  fungicides used  for  seed

                                  247

-------
treatment  were discharged into the wastewater stream and were undetected,
sufficient  information was not available to delineate the source of chlori-
nated anilines  in  the Gray soils.  In general, 2,3-dichloroaniline was more
prevalent at  soil  depths  from 91  cm to 183  cm  beneath  the  center pivot
machines in  1983  than in 1981.  Furthermore, less chlorinate  anilines were
detected in the flood irrigated soils.
     Acenaphthylene and the various dichlorobenzene forms in  the soils may
have been derived  from application  of insecticides.  These  organic com-
pounds  existed primarily  in  the upper 61 cm of the soil profile.   Except
for acenaphthylene and m-dichlorobenzene levels  in the top 30 cm of soil
beneath  center pivots in  1983, acenaphthylene  and the dichlorobenzenes
decreased in  1983  to approximately the detection  limits  for  the specific
organic.
    • Phthalates are  fairly ubiquitous in  the  environment,  consequently
scenarios describing the sources of  these compounds- in  the  soil samples
were difficult to develop.   Dibutylphthalate  and  diethylphthalate were
detected at various depths  within  the 183 cm profile in 1981  and 1983.
Higher  concentrations o'f dibutylphthalate were measured in soils  which were
subjected to  flood irrigation (27 to 135 ppb) than spray irrigation (28  to
42 ppb).
     Within the flood irrigated area, 20 of 36 organics measured  were below
detection limits throughout the entire core in 1983; whereas,  in  1981 only
five compounds were not detected above analytical limits.  Only 12  and 15
organic  compounds  of a total of 36 assayed were not measured  above detec-
tion limits within the entire profile beneath center pivot machines  in 1981
and 1983, respectively.   Therefore,  greater  soil water moisture in  the
flood irrigated areas may  have enhanced biological degradation of these
organic  compounds.
     The presence of  trace organics in the soil profile in  1981  and 1983
may have been directly related to  the mass loadings of  specific organic
compounds through  flood irrigation land growing wheat (Table 45). Decreased
organic  mass  loadings by spray irrigation of land producing alfalfa, how-
ever,  reduced  the potential  of residual levels   of priority   organic com-
pounds  in 1983  derived solely from irrigation.

                                 248

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TABLE 45.  MASS OF PRIORITY ORGANICS APPLIED TO GRAY FARM

Flood Irrigat
Priority Detection
Organic Limits Mass Applied
Compound Concentration ( g/ha) in
(ppb)
Acenaphthylene <20
Anthracene <20
Atrazine <100
Benzene <1
4-t-butylphenol <10
Carbontetrachloride <1
4-chloroanil ine <100
Chlorobenzene- <1
Chloroform <1
2-chlorophenol <10
l-chlorotetradecane <2D
Dibutylphathalate <20
2,3-dichloroaniline <20
3,4-dichloroaniline - <20
Dichlorabenzene M <10
P <10
0 <10
2 ,4-d ichlorophenol
Diethylphthalate/ <20
Hex ad ecane
Ethylbenzene <1
Heptadecane <10
Methylheptadecanoate <20
Methylhexadecanoate <20
1-methylnaphthalene <10
2-methylphenol <10
4-methyl phenol <20
Naphthalene <10
Octadecane <20
Phenol <10
Propazine <100
a-terpineol <10
Tetrachloethylene <1
Toluene <1
Trichloroethane <1
Trichloroethylene <1
1981
227.9
283.6
506.2
51.2
237.2
372.
1348.5
51.2
46.5
395.2
227.8
1339.2
395.2
269.7
265.0
297.6
539.4
358.0
302.2
60.4
348.8
390.6
585.9
316.2
283.6
404.6
144.2
200.0
488.2
930.
376.6
223.2
88.4
316.2
55.8
1982
57.5
92.
906.2
253.
117.3
73.6
303.6
23.
89.7
218.5
170.2
2911.8
112.7
165.6
179.4
85.1
269.1
158.7
372.6
43.7
158.7
103.5
94.3
59.8
59.8
165.6
471.5
195.5
193.2
476.1
432.4
52.9
25.3
115.
23.
1983
51.8
82.8
815.6
227.7
105.6
66.2.
273.2
20.7
80.7
196.6
153.2
2620.
101.4
149.0
161.5
76.6
242.2
142.8
335.3
39.3
142.8
93.2
84.9
53.8
53.8
149.0
424.4
176.0
173;9
428.5
389.2
47.6
22.8
103.5
20.7
ion
Calculated
Concentration
30 cm of Soil
(ppb)
79.0
107.4
552.3
124.6
107.8
119.9
451.2
22.2
50.8
189.9
129.2
1610.3
142.8
136.9
142.0
107.6
246.2
154.6
236.7
33.6
152.4
137.6
179.3
100.7
93.1
168.5
243.7
133.9
200.4
429.9
280.8
75.9
32.0
125.3
23.3
Spray Irrigation
Calculated
Mass Applied Concentration
(g/ha) in 30 cm of Soil
1981
31.8
39.6
70.8
7.2
32.2
52.0
1B8.5
7.2
6.5
55.2
31.8
187.2
55.2
37.7
37.0
41.6
75.4
50.0
42.2
8.4
48.4
54.6
81 .9
44.2
39.6
56.6
20.2
28.0
68.2
130.0
52.6
31 .2
12.4
44.2
7.8
1982
13.8
22.
216.7
.60.5
28.0
17.6
72.6
5.5
21.4
52.2
40.7
696.3
27.0
39.6
42.9
20.4
64.4
38.0
89.1
10.4
38.0
24.8
22.6
14.3
14.3
39.6
112.8
46.8
46.2
113.8
103.4
12.6
6.0
27.5
5.5
1983
13.8
22.
216.7
60.5
28.0
17.6
72. 6
5.5
21.4
52.2
40.7
696.3
27.0
39.6
42.9
20.4
64.4
38.0
89.1
10.4
38.0
24.8
22.6
14.3
14.3
39.6
112.8
46.8
46.2
113.8
103.4
12.6
6.0
27.5
5.5
(ppb)
13.9
19.6
118.2
30.0
20.9
20.4
7B.2
4.3
11.6
37.4
26.5
370.2
25.6
27.4
28.8
19.3
47.9
32.0
51. 6
6.8
29.2
24.4
29.8
17.1
16.0
31.8
57.6
28.5
37.6
83.8
60.8
10.9
5.7
23.2
18.8
                        249

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Bacteriological  Data—
     The average  concentration of bacterial indicator organisms, actinomy-
cetes, and  fungi present  in  the soil profile in 1981  and  1983 on the  Gray
farm  are presented  in   Tables E.31 and E.32.  Total coliform (TC), fecal
coliform (FC)  and  fecal streptococcus (FS) were primarily retained  in  the
top -30  cm  of  soil.  Soil  core 23132  in the flood  irrigated area had the
highest concentration of  indicator organisms  in  the  upper 30 cm of soil.
In 1983, core 23132 also  was the  only core containing  TC, FC, and FS to
depths of 122  cm.   The location from which this core  was  extracted  was  in
close  proximity to riser pipes fitted with alfalfa control valves used for
flood irrigation  on  this particular  portion  of land.   Consequently, a
deeper  portion  of the upper profile  was saturated due to the increased
hydrostatic pressure  experienced at the riser's discharge.  Therefore,  high
bacterial  counts  in this soil possibly were associated with deep percola-
tion resulting from poor  flow distribution with the irrigation system.
     Fecal  streptococcus was  detected  at  greater  concentrations in the
spray irrigated  areas in  1983 than in 1981.  Certain  soil  samples obtained
from the flood irrigated  area contained concentrations of  TC and FS exceed-
ing detection  limits  at depths of 183 cm.
     Fungi  and  actinomycetes  concentrations within the soil profile  were
relatively  constant throughout the farm and the monitoring period (Tables
E.31  and E.32).   Changes in hydraulic loading or cropping patterns did not
appear to affect  the number of actinomycetes  or fungi present  throughout
the entire  183 cm  soil core.
CROPS
Hancock Farm
Crop Yields—
     Comparisons  of  crop analysis were difficult because of the inconsist-
ency in agricultural  practices employed at the Hancock  farm (Figures  G.1,
G.5 and G.6).  In 1982  the Hancock farm was planted in three crops:  sun-
flowers,  soybeans  and milo.  For late planted crops,  sunflower yields  were
in the  normal range  recorded for the High Plains, 1124 to 2247 kg/ha (1000

                                  250

-------
to 2000  Ibs/ac).   Pivot 7 was replanted due to poor germination  and  yielded
1612 kg/ha (1435  Ib/ac).   The best  sunflower  seed yield was  2647 kg/ha
(2356 Ib/ac)  from the land irrigated  by Pivot  17.   Soybean production
ranged from 2036  kg/ha  (30.2 bu/ac)  under Pivot 19 up to 2697  kg/ha (40
bu/ac) on Pivot 2 which was  within the High Plains soybean  range of  1685 to
2697 kg/ha (25  to 40  bu/ac)  cited by Texas A & M Extension Service.  Milo
yields  were less than expected.   Primarily, this was due  to  lateness of
planting and also possible delay in  flowering from watering at   early boot
stage.   In addition, some  herbicide damage, due to treating the land with
Trifluralin (Treflan®) in expectation of growing cotton, may have  lowered
yields.   Milo  yields  ranged  from 3307 kg/ha (2943 Ib/ac)  beneath Pivot 9 to
6691 kg/ha (5955  Ib/ac)  under Pivot 19.  Texas A & M Extension  Service
reported milo  yields  for the High Plains of 3933 to 5618 kg/ha.
     1980, 1981 and 1983  cotton yields obtained from the Hancock  farm are
presented in  Table  46.   A  definite  improvement  on  crop  production was
experienced in  1983.  Regardless of  irrigation, an increase  in  production
was  anticipated   since 1983 was the only year during the study  when  a nat-
ural disaster  did not affect crop planting and establishment.  In  general,
cotton  production in 1983  exceeded average yields obtained  from irrigated
land in Lubbock County.  Average crop yield  per  center pivot machine,  as
determined from   four one-meter square samples, is presented  in Table 46.
Differences between values recorded  by farmers and researchers were  due  to
sampling procedure and the fact that every boll was picked  from  plants once
the sample was  brought to the laboratory.  Consequently higher  yields were.
projected for  crops  grown beneath each pivot than actually recorded  at the
cotton gin.  1983 crop yields may have been limited due to  nutrient  short-
ages, boll worm   infestation,  and  cooler weather in  September, which may
have limited cotton fiber production.
Crop Quality—
     Comparisons were  conducted  on 1981 and 1983 cotton  stalk and seed
quality data and  1982 and 1983 milo  data. Defoliants were applied  to the
cotton  crop prior to stripping the cotton;  consequently,  leaf  tissue from
cotton plants  was not available for  analysis.  Milo plants were  sectioned
                                  251

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                                          TABLE 46.   COTTON YIELDS,  HANCOCK  FARM
N>

Tenant
Farmer A
Farmer B
Farmer C
Farmer E
Farmer F
Farmer G
Farmer H
Farmer I
Ha.
56.7
87.8
120.2
171.2
100.8
82.2
116.1
87.4
1980*
Ac . kg/ha
140
217
297
423
249
203
287
216
Lubbock County***
70
137
234
100
85
417
393
109
156*
Ib/ac
62
122
208
89
76
371
350
97

Ha . Ac . .
56.7 140
143.3 354
172.0 425
213.7 528
100.8 249
82.2 203
116.1 287
87.4 216

1981*
Kg/ha
222
118
178
131
274
316
196
246
373*
Ib/ac
198
105
158
117
244
281
174
219

Ha.
56.7
142.5
65.6
207.2
50.6
82.2
116.1
29.9

Ac.
140
352
162
512
125
203
287
74

Lubbock County***
1983**
Kg/ha
615
579
676
560
740
572
353
597
(312)*
395**
Ib/ac
547
515
602
498
659
509
314
531



          * Dryland
         ** Irrigated land
        *** Texas A & M Extension Service, Lubbock, Texas

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into stalk  (including  leaf),  whole head  samples  in  1982, and pure grain
samples  in 1983.
     Cotton — Table  47 presents the concentration  ranges of elements found
in cotton stalk and  seed.  Elements such as Ca, K,  Na, Fe, Ba, Cr, and Pb
apparently accumulated more in the stalk than in  the  fruit; whereas,  N,  P,
Cd existed  at  higher levels in the seed.   The elemental analysis of the
cotton  plants is  provided  in Table F.5.
    TABLE 47..  RANGES  OF SPECIFIC ELEMENTS PRESENTED  IN THE CROP TISSUE
                       OBTAINED FROM HANCOCK FARM

Element
Ca
K
Na
Fe
Ba
Cr
Pb
N
P
Cd
Stalk (mg/g)
5,000-95,000
5,000-30,000
200-11 ,000
33-800
3-30
<.5-3
<.2-5
2,000-18,000
700-3,000
<.05-.7
Seed (mg/g)
1 ,000-16,000
3,000-13,000
<3-5,000
<. 5-150
3-17
<.5-1.5
<.2-2
8,000-47,000
5,000-12,000
<.05-2.5

     Previous work  (Giordano &  Mays 1977)  showed  Cd to be higher in leaf
tissue than  in stalk or seed tissue.  Arsenic was  never  at  concentrations
in the detectable range  in either seed or  stalk and Cu proved to be very
dynamic.   In  1981  eleven crops were analyzed  where Cu concentration  in  the
seed  was  lower  than levels measured in the stalk.  Only four plants con-
tained higher Cu concentrations  in  the seed than  measured in the  stalk
tissue.   This trend was reversed in 1983 with 10  out of 11 samples showing
an apparent accumulation of Cu in the seed.  It  should  be  noted also  that
the overall  concentration  of Cu in the stalks dropped in the range of 80
percent while, at  the same time,  Cu concentration in  the  seed stayed  the
                                  253

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same  or  possibly  even increased.   This would indicate that when Cu became
depleted in the soil, any available Cu was transported to the seed.
     Through comparison of concentrations of specific elements from year  to
year for the  same  crop  parts,  any accumulation  in crops  may denote  an
increased availability from effluent irrigation.   Conversely, depletions  of
certain elements in the crop tissue may indicate  a limitation of available
macro or micro nutrients in the  soil solution. A summary of depletions and
accumulations of nutrients and metals  are compiled in Table 48.
          TABLE 48.  ELEMENTAL SHIFTS  IN COTTON TISSUES OBTAINED
                      FROM HANCOCK  FARM 1981  vs.  1983

Concentration
1981 > 1982
TKN
°TP
Ca
Ca
K
Na
Na
Cd
Cd
Cu
Pb
Pb
Stalk
Stalk
Stalk
Seed
Stalk
Stalk
Seed
Stalk
Seed
Stalk
Stalk
Seed
Concentration Concentrations
1981 1983 1981 < 1983
TKN
TP
K
Fe
-Fe
Ba
Cr
Cu
Cu



Seed
Seed
Seed
Stalk
Seed
Seed
Stalk*
Seed*
Seed**




 *0verall the same  but  one  or  two  sharp  rises  or  drops  show  inconsistency
  in trend
**Pivots 3 and 11 show  substantial drops but overall  trend is  same  or a
  little increase.
     Comparison  of the 1981 and 1983  cotton crop tissue  analysis indicated
that a majority of  the  elements  assayed  remained  relatively  constant  in the
seed  tissue.  Corresponding  stalk parts  showed decreases  in element con-

                                 254

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centration  levels  from  1981 to 1983.  The availability of certain elements
in the  soil  solution may have been reduced in 1983 compared  to 1981.  For
example,  the  P  levels  for  seed and stalk for 1981 to 1983 are presented  in
Table F.5.  A  64 percent decrease in phosphorus concentration can cause  a
reduction in  yield (A  & L Labs Soil and Tissue Analysis Handbook).   Phos-
phorus  levels  in the  cotton stalks  decreased  by 6 to  70  percent, or  an
average  of  51 percent.   This magnitude of phosphorus reduction in the  crop
may cause limitations  in growth, flowering and yield. Phosphorus is import-
ant  to the  plant in many ways:  photosynthesis, hastening maturity,  stimu-
lating  blooming  and seed formation,  and stimulating early root growth.
Inhibition  of early root development produces a cyclic effect:  the  less  P
available to the crop,  the  less root growth; the less root growth,  the  less
P picke'd  up by   the roots, etc. (Inter-American Labs 1978).   If the  seed  P
levels  are compared (Table  F.5), there was almost no drop in their concen-
tration  (less than three  percent) from 1981 to 1983.  If the P levels was
low enough to  reduce  flowering and seed formation, the phosphorus available
would  have  been translocated to the seed and the concentration would  have
stayed  practically the  same.  Consequently,  the mass of P (Concentration  x
Yield) removed  by the  crop would have been  reduced.  As stated previously,
P uptake  by  cotton in  1983  was less than anticipated.
     Grain  Sorghum (Milo)—Table 49 presents concentration  ranges of  spe-
cific  elements   measured in sorghum  tissue.   Elemental analysis of  milo
stalk and seed samples  obtained from the Hancock farm are provided in Table
F.6.   Arsenic levels  in collected stalk samples were less than 0.5 mg/g  in
1983 compared  to values  ranging from <0.5 to 1.12 mg/g  in 1982.  More  Cd
existed  in  the  stalk  and leaf tissue (0.14  to 0.46 mg/g) than was detected
in the  seed  «0.05 to  0.3 mg/g).  This phenomenum agreed with results pre-
sented by Giordano and Mays (1977).  Furthermore, Cd levels in the stalk
were lower (0.06 to 0.16 mg/g) in 1983 than  in 1981.
     In summary, no  accumulation of trace metals appeared to have resulted
from land application  of the City  of Lubbock's wastewater.  The overall
decrease  of nitrogen  and  phosphorus in tissues from 1981 to 1983 was  par-
tially  due to  the failure of the irrigation  stream to meet  crop nutrient
                                 255

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requirements.   Originally, irrigation  was expected  to provide  sufficient
N and P to  satisfy crop need; however, due to odor problems, the  effluent
was  transported through  the reservoirs before  application to the soil.
Nitrogen concentrations in the irrigation water were reduced from 42 ppm to
approximately  12  ppm by passing the effluent through the reservoirs.  The N
reduction,  in  conjunction with a 50 percent reduction in the total  hydrau-
lic loading resulted in a N deficiency in many of the fields.  Since N is a
translocatable nutrient, it will be taken from older tissue in a plant  and
put  into the  newer tissues.  This was consistent with N accumulation in the
seed as shown  in  Tables F.5 and F.6.
          TABLE  49.  CONCENTRATION RANGES OF SPECIFIC ELEMENTS IN
            GRAIN  SORGHUM TISSUE COLLECTED FROM HANCOCK FARM

Element
Ca
K
Na
Fe
As
Ba
Cd
Cr
N
P
Stalk
(mg/g)
4,500-7,500
12,000-28,000
175-1 ,100
200-600
<.5-1 .1
7.5-17.0
0.06-0.46
0.8-2.4
2,500-12,000
650-1,200
Seed
(mg/g)
170-1,200
2,000-6,000
50-200
4-115
<. 5-1.0
2.0-3.0
<.05-0.3
<.5-1.3
11,000-17,000
2,400-2,900

Gray Farm
Yields-
     Crop analysis  and comparison for the Gray farm was complicated by a
change in ownership  and management which caused a complete change  in  crop-
ping  pattern in 1982  and  1983.  Cotton yields  prior to 1982 equaled or
exceeded irrigated Lubbock County  yield averages of 434  to 457  kg/ha in
                                  256

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1980 and  1981,  respectively.   A  summary  of  yields  from the Gray farm (1982
and 1983)  are  presented  in  Table  50.
      TABLE 50.   CROP YIELDS  OBTAINED  FROM  GRAY  FARM  IN 1982 AND 1983
                                  (KG/HA)

1982
Location***
1
2
3
4
5
6
10
11





Crop
Soybeans
Soybeans
Soybeans
Alfalfa**
Al f al fa
Alfalfa
Alfalfa
Alfalfa





Yield
3387
2325
2512
1312
1912
1575
1837
1688





1983
Location***
1
15
16
5
8E
13
14
7E
11W
4
12
10W
10E
Crop
Wheat*
Wheat
Wheat
Alfalfa**
Alfalfa
Alfalfa
Alfalfa
Alfalfa
Alfalfa
Alfalfa
Alfalfa
Alfalfa
Alfalfa
Yield
1884
1786
737
1790
2005
1290
2140
1965
1765
2040
2064
1430
1779

  * Fall sampling of vegetative  growth  —  wheat  used only for grazing
    (no grain harvested)
 ** This was one cutting  of alfalfa —  in  1982 there were two cuttings and
    in 1983, three to four cuttings.
*** Locations correspond  to cropping areas delineated  in Figure 35.
    Alfalfa yieldsin1982 (establishment year) ranged  from  1.8 to  2.7  met-
ric tons/ha (2 to 3.0 tons/ac)  which was  relatively low compared  to a nor-
mal range of 5.4 to 7.0 metric tons/ha.  The  yield  reduction was  partially
due to  1)  delays  in watering,  thereby  delaying regrowth; 2) poor stand
establishment; and 3) weed competition.  Weed competition also affected the
quality  of the hay  harvested;  thus lowering the crop's marketability.  In
addition, some fields were left  with excessive growth  in the fall to.pro-
                                  257

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vide pasture  for cattle.  This practice produced two detrimental effects:
1) a loss of one cutting of alfalfa, and 2)  grazed areas could not be
watered  because of high probability of crown damage to  the alfalfa plants
resulting from  cattle mashing the crowns into wet soils.   In the winter of
1982, the farm  grazed approximately 3,000 head of mixed breed calves weigh-
ing from 159 to 318  kg  (350 to 700 Ib) .
     Soybeans  were  planted  three  rows per  bed with a  Tye® grain drill.
Variations in stand  may have  been due to salts or planting when field con-
ditions  were  less  than  optimal.  Soybean yields averaged 2494 kg/ha  (37
bu/ac).   Wheat  yields from the Gray farm were difficult to determine since
no grain  harvest was  planned and forage harvest was accomplished by graz-
ing .
     1983 alfalfa  yields on the Gray farm were again reduced by delays in
watering which  reduced  the number of cuttings (see discussion on Farm Oper-
ations).   Normally, five  to seven cutting of alfalfa are expected in  the
Lubbock  area (Texas  A & M Extension Service).  The Gray farm produced three
to four  cuttings.   Alfalfa yields were slightly improved  over 1982 values;
however, this was due  to  1982 being  the seeding  and crop  establishment
year.
Crop Quality—
     Crop analysis  for 1981 was  almost all  cotton with one milo and  one
wheat sample collected.   In 1983 three wheat and eight, alfalfa samples were
obtained from the farm  for analysis.  The results of the  elemental analysis
of crop  samples are  presented in Tables F.7 and F.8.  The  data was for only
a single  year; therefore  any  comparisons over  time could not be accom-
plished.  Comparisons were made between specific  elements  in crop tissue
obtained  from  the Gray farm  to normal concentration values cited in liter-
ature and levels measured in  crop tissue from  similar crops grown on the
Hancock  farm.
     Cotton—In 1981  cotton tissue,  the K, Na, Ca and Ba accumulated more
in the  stalk  than  in  the  seed and N, P,  and Cd were at  higher concentra-
tions in the seed.   This  trend was similar to the distribution of elements
in cotton tissue collected  from the  Hancock farm.  Certain trace metals
                                  258

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(Cr, As  and  Pb)  were  below detection limits (less than 0.5 mg/g).  In cot-
ton produced  on  the  Gray  farm more  Cu was measured in the seed than in  the
stalk.   Large differences existed in Na and Ca concentrations in the crop
obtained  from the Gray and Hancock  farms.  Higher Na uptake by crops at  the
Hancock farm  may have  resulted  from a reduction in soil water availability.
As soil moisture decreases, the concentrations  of salts  in soil solution
increase  and  more salts are transported  into the plant.  With irrigation,  a
higher percent available  water  may  be present in the soil profile and  salts
in the soil  .solution  are diluted.  Soil analysis of the Gray farm shows it
to be higher  in  salts.  Salt data,  however,  was computed  on a dry weight
basis; therefore did not  show  the effect of higher or lower water avail-
ability on soil  solution  concentration.  A comparison of data to  some nor-
mal  values outlined  in A & L  Labs Soil and Tissue Handbook indicated  the
only elements not within  a range of 50 percent of the average values to  the
average  levels  cited  in  the A  & L  Handbook were Ca at the Gray farm and Na
in the Hancock cotton.
     Milo, Wheat, and Alfalfa—When the single milo and wheat samples were
compared to  normal  levels (as  specified by the A & L Handbook) the only
major difference was the-high  concentrations of Ca in the  crop tissue.  In
1983,  alfalfa  tissue contained Na at higher levels  than normal  cited
values.  Despite higher concentrations  of  Na  and Ca  in  the crop  tissue,
potential toxic   trace  metals   did not  appear  to accumulate  in the crop
tissue.

ECONOMICS
     The  economics attributable to the  Hancock farm portion of the Lubbock
Land Treatment System can be divided  into construction  costs, operational
costs and revenues.   An economic analysis was conducted to determine the
costs and revenues accrued by  the City,  landowner, and tenant farmers.
Construction Costs
     The Hancock farm portion  of the  Lubbock Land Treatment  System was con-
structed, excluding land acquisition  cost,  with monies  from EPA (88 per-

                                   259

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cent),  the  City  of Lubbock (10 percent),  and the Lubbock  Christian  College
Investment  Corporation (LCCIC)(two percent).  The Hancock farm  system was
built  on private farm land (1478 ha)  leased to  the  LCCIC.  Table  G.2 gives
the  construction costs including  engineering fees  and  construction
contracts.   The land acquisition cost was the  actual 1978  purchase price
of the  land.   The  construction  cost was  $6,421,071.78  and  the  land
purchase price  $1,460,000.00 ($988/ha  or $400/ac)  for  a system total of
$7,881,071.78.   The main categories of money expenditure  (>$400,000)  were
engine-ering  design ($405,607), pump station  and  force  main construction
($2,658,554),  reservoir construction  including  pumps  ($1,691,209),  and
farm distribution system  including  pivots and distribution  pipeline
($1,433,801).
    Two possible  scenarios  will be  presented in  this portion  of  the
report.  Scenario. 1 will consider the system  construction costs being
borne by the  municipality and land cost will be  paid  by a private institu-
tion.  The  second scenario will assume the municipality paid  for construc-
tion and land costs.  Construction and land cost were amortized over  a 20
year period  at an interest rate of 10  percent.   The  situation' proposed  in
scenario 1  would  result  in  the annual  cost  to the City for  system  con-
struction of  $754,219.08/yr-  With scenario 2  the  annual capital cost
would increase by $925,710.68/yr.
    The Hancock  farm received 4,128,213 m3 (11 x 108  gal) of effluent  from
February through  December  1982 and  3,744,393 m3  (10  x 108 gal)  from
January  through October 1983.   Assuming that  the   City could have main-
tained  those   flows for a  12 month period,  the 1982 flow would have  been
4,503,505  m3/yr (12 x  108 gal/yr)  and  the 1983  flow  would have been
4,493,271 m3/yr (12 x 108 gal/yr).   Based on scenario 1  the  1982 and  1983
amortized cost for system construction per 1,000 units of effluent  pumped
to the  Hancock  farm would have been  $167/1000 m3/yr  ($0.63/1000 gal).   If
the City did  purchase the land, then  the  amortized construction  cost  per
1000 units  of effluent pumped would  have  been $205/1000  m3/yr  ($0.78/1000
gal)/yr). Federal cost sharing is 85  percent for innovative  and  alterna-
tive technology.   Therefore,  1983  amortized  construction costs to the
municipality in scenario  1  would have  been  $25/1000  m3/yr  ($0.10/1000

                                 260

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gal/yr).   With  cost  sharing, annual construction and  land  cost  would have
been about  $31/1000  m3/yr ($0.12/1000 gal/yr).  Land  acquisition affected
the amortized  capital cost by approximately 24 percent.
Operational  Costs
    The City's operational cost were associated with providing electricity
to pump motors,  maintenance of pump station and force  main,  and  treatment
of wastewater transported  to the Hancock farm.  LCCIC  was financially
responsible  for  maintenance  of the reservoirs,  reservoir  pump  stations,
distribution  lines  and  building site modifications.  The  tenant  farmers
paid for maintenance  of the pivots, electricity for the pivots  including
booster  pumps,  electricity for the reservoir pumps and  farming  costs such
as tractor maintenance, fuel, seed, hired labor,  and  equipment  expendi-
tures.   In  addition,  the tenant farmers paid Standefer and Gray, Inc. a
service charge of  $51.87/ha/yr  ($21/ac/yr)  for  land  irrigated  with the
City's  effluent water.   The farmers'  rent to LCCIC was  one-third of their
gross crop yield.
    The  1982  and  1983 operational costs expended by  the City and  associ-
ated with the  farm are  in  Table G.3.  Table G.4 gives  the farm operational
cost  for the  baseline period (1980 through 1981) during  which no waste-
water was pumped to the Hancock farm.
    The  1982  and  1983 Hancock system operational costs were $641,945.03
and $625,268.90, respectively.  Based upon the farm receiving 4,128,213 m3
(10.9  x  108  gal)  in 1982 and 4,493,272 m3  (11.9 x 108) in  1983,  the
system's operation  and  maintenance  (0 &  M)  cost  was   $156/1000 m-5
($0.59/1000 gal)   in 1982 and $139/1000 m3 ($0.53/1000  gal) in  1983.  The
City's  portion of the  0 & M cost was $71/1000 m3 ($0.27/1000 gal)  in 1982
and $58/1000 m3 ($0.22/1000 gal) in 1983.  The farm's  portion of the 0 & M
cost  in  1982  was  $84/1000 m3 ($0.32/1000 gal) and $81/1000  m3 ($0.31/1000
gal) in 1983.   Table  51 indicates  that the  0  &  M costs for the  Hancock
system  were in the  range normally  experienced  by  slow  rate  systems of
comparable size (EPA  1980).  The  City's expenses showed an increase in
operations cost of $31,846.19 in 1983 while the farmers  had  an operational
cost increase  of $15,170.06.  The farmers operational  cost  increase  from
1982  to  1983  was  due  to .an $18,548 increase  in seed, fertilizer and
                                 261

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        TABLE 51.  0 & M COSTS OF LAND  TREATMENT  SITES (EPA, 1982)
                     Preapplication
                    Treatment 0 & M
                          Costs*
                    Landtreatment
                     0  &  M  Costs*
Total Treatment
  0 & M Costs*
16 Sites

Cost/1000 m3
Mean
Standard Deviation
Cost/1000 gal
Mean
Standard Deviation

$13-361
132
85

$0.05-1 .37
0.50
0.32

$0.6-165
22
24

$0.002-0.62
0.08
0.09

$67-525
157
125

$0.25-1.99
0.59
0.47
Above costs based on:
Flow m-Vs
  Mean
Standard Deviation
0.0022-0.3505
    0.056
    0.09
Flow MGD   .           0.05-8.0
   Mean                  1.28
Standard Deviation       2.05
bCost reflects fourth quarter 1983 dollars
                                   262

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chemicals  and a  $37,505 increase  in  irrigation expenses, primarily
electricity.   The irrigation expense  increase was  offset by $45,053
decrease  in  farm  improvements.  Improvement  costs occurred from materials
or labor  put  into  the  operation and  improvement of  the  Hancock system
other than  routine farm operating expenditures.  The 1982 match included
terracing the fields  for runoff  control,  existing  roads improvement,
installation of roads  to the pivot control  boxes at the center  of the
pivots,  removal  of abandoned farm houses to  enable pivots  to make a  full
circle,  repair  of pivots after two consecutive  tornadoes,  installation of
sprinkler drags, conversion of automatic end  gun  valves to.manual valves,
repositioning of pivot  flow meters,  replacement of inline screens  at the
pivot inlets,  and  removal of abandoned  wells.   The 1983  match included
field terracing,  maintenance of reservoir dikes, abandoned farm  house
removal,  screen  replacement, and installation of  thrust blocks under  each
pivot booster pump.  The 1980 and 1981  farm operational cost (Table G.4)
were within  $14,000 of each other, with the  average being $221 ,336 .62/yr .
Comparison  of the average baseline system operational cost (Table  G.4)  to
the post baseline  system, operational cost (Table  G.3) shows an increase in
system  operational cost  of $420,608.41  for  1982  and $403,932.28 for  1983.
Since the operational  cost categories reflecting routine  farming (i.e.,
interest,  depreciation, repairs, tires,  oil, gas,  seed,  fertilizer,
chemicals and labor) were approximately the  same  from  1980 through  1983,
the  increase was primarily  due to initiation  of wastewater flow  to the
Hancock  farm.
    The  farming  expenses  are shown in  detail  in  Tables G.5 and G.6  for the
baseline period  and irrigation period,  respectively.   There was a  great
deal of  variability between  farmers  in the  expenses reported and  total
farming  expense  per acre.  Part of the variability was due to the farmers
having  different ages  of equipment  and thus  operational costs; planting
various  quantities of  crops which differed in production costs; uniqueness
of individual  farmers  in  their effort  at farming; farmers farming the same
crop in  different  manners; method by which the  farmers  kept their finan-
cial records;  and  one  portion of the farm receiving natural disasters that
the rest of  the  farm did  not.  The expense data is not  reported in  finer
detail  (i.e,  repairs,  gas,  oil, seed,  chemicals, labor, depreciation,
                                 263

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electricity,  etc.) because of the high degree of variability in which this
data was received.   Most of this information was taken from checkbooks and
income  tax  records; therefore, the record keeping systems for each farm
operator  were inherently different.   For  this  reason, many  of  the
financial  categories requested from the farmers were combined (Figure 15).
Even with  these larger accumulations of the data base, (Tables  G.5  to G.6)
comparisons  should  only be made from year to year,  or baseline to  irriga-
tion, for  a  specific farmer and  not  between  farmers.  Nonetheless,  the
tables  substantiate the increase in farm operational  cost  (Table G.6)  due
to initiation of  irrigation.   Of  the over $400,000 increase in  system
operation,  approximately $107,190 (26 percent)  of the  increase was born
solely by  the tenant farmers;  $28,859 (seven percent)  by  the landowner  and
LCCIC; and $276,221  (67 percent)  by the City.  As previously mentioned,  the
City's operational expenses were accrued from the maintenance of the pump
station at  the  city and  pipeline to  the Hancock  farm; treatment of the
sewerage prior to its being pumped to the farm;  and cost  of electricity
for  the pumps at the pump station.  Of the City's $276,221 (67 percent)
average 1982-1983 increase in system operation, $266,098  (64 percent)  was
for treatment of  the sewerage; and $9,758 (three percent) was for mainten-
ance and electricity.
    During 1982 the  City paid  $291,778.00 (45  percent)  of the new system's
operational  expenses and $259,931.81  (42 percent)  in 1983.   Based upon  the
farm  receiving  4,128,213 m3 (10.9 x  108 gal) of effluent  in 1982  and
4,493,272 m3 (11.9 x 108 gal) in 1983, the City's  portion of  operational
cost for the  Land Application  System expansion was $71/1000 m3  ($0.27/1000
gal)  and  $58/1000  m3 ($0.22/1000 gal)  in 1982 and  1983,  respectively.
Negating the  treatment  of the sewerage going  to the Hancock farm,  the
City's  increase  in operational expenses, due to  initiating  the  Hancock
system, was  approximately $2/1000 m3/yr ($0.01/1000 gal/yr)  of effluent
pumped to  the farm.   If  the  Hancock system  was owned by  the City  and
operated  under  a tenant  farmer arrangement, the City's operational cost
would  have  increased  by approximately  $28,145/yr  ($6/1000  m3/yr  or
$0.02/1000 gal/yr)  for an average total of $304,000/yr ($68/1000 m3/yr or
$0.26/1000 gal/yr).  The  increase  in  City operational cost due  to  farm
ownership  possibly may have been offset by farm revenues.
                                 264

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Farming  Revenues
     Revenue is  the money obtained through the sale of crops  or  government
 farm programs.   Government  farm programs are programs in which the  farmer
 is paid  for  not growing  a crop (i.e.,  payment in kind,  PIK) , a support
 price for his  yield if  the  market value falls below the guaranteed  price,
 and  partial  payment  for lost yield due to disaster (i.e.,  flooding, hail,
 early freeze, and drought).   For  a privately  owned and operated land
 treatment  system, farm  revenues  must offset  annual construction  and
 operational costs.  Table 52 gives the 1980-1983  revenues for the  Hancock
 farm and the  distribution of those  revenues  between the  landowner and
 tenant  farmer.   A  common farm rental rate paid to land owners for a  south-
 west Texas farm is  one-third of the  gross yield,  including  government
 programs.  The land owner pays  land  payments  and  taxes out of his one-
 third  and  the tenant  farmer pays  all  farming costs,  except  major land
 improvement programs.  Gross revenue data  (Table 52) shows a definite
 increase in  crop revenue  and government support for the farm through the
 project period 1980-1983.   From 1980 through 1983  the gross  farm  revenue
 ranged  from. $367,605  to $815,672 with government  support  ranging from 27
 percent of the total  in 1980 to 34 percent in 1982.  The 1981 gross farm
 revenue  ($440,521)  was nearly the  same as the  1982 gross farm revenue
 ($453,322).  The Hancock farm was a dryland farm  with little  or  no  ground
 water for irrigation  prior  to 1982.  In 1980 cotton and grain sorghum were
 raised  utilizing rainfall and any available irrigation water.  In 1981  all
 of the  irrigation  wells were pulled as part of the  construction  effort and
 there was a drought causing the farm to be designated part  of the disaster
 area.   Effluent water was not available for  irrigation until February
 1982; but torrential  rains  and hail in late spring  made it impossible to
 raise  a  cotton  crop and  alternative crops were replanted.  The farm was
 again stipulated as part of the disaster area.  Finally, 1983 was  a good
 year with  the arrival of  irrigation water, no natural disasters, and the
 existence of  the PIK  program.  Consequently, the  steady increase in  gross
 farm revenue  was due  to  a combination of economic variability among the
 tenant  farmers,  inflation,  disaster payments, government support, alterna-
 tive cropping  and  a good year in 1983.  Obviously,  crop market price has a
 major affect  on  revenue.  Cotton prices were $1.51/kg ($0.685/lb) in 1980,
                                 265

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$1.02/kg  ($0.465/lb) in 1981, $1.13/kg ($0.513/lb)  in  1982,  and $1.31/kg
($0.593/lb)  in  1983.
                    TABLE 52.  HANCOCK FARM REVENUES

Year
1980
1981
1982
1983
Revenues
Crop Government
Revenue Support
$268,307 $ 99,298 (27%
293,065 147,456 (33?^
299,258 154,064 (34?o
583,342 234,330 (28%
Total
Revenue
)* $367,605
) 440,521
) 453,322
) 815,672
Revenue Distribution
Owner Tenant
1/3 2/3
$122
146
151
271
,535
,841
,107
,891
$245
293
302
543
,070
,681
,215
,781

*Government  Support to Farmers as Percent  of  Total  Revenue
     Table  53  is a summary of the gross income of  the individual  tenant
farmers 'by  year-   Table G.7  gives a more  detailed examination of the
tenant farmers' gross income by delineating  sources of revenue.   The  data
show  that  not only the farm as a whole,  but  also each tenant  farmer had a
definite  increase in  gross  income  throughout the project (1980-1983).
Again, the  high  variability  in gross  income between farmers exists for
many of the  same reasons as the variability in operational  cost  of the
individual  farmers, such as variation  in crops, uniqueness of individuals
in farming  effort, variation in amounts of applied  water,  fertilizer,
rainfall,  hail,  pests,  inflation, and  means by which records were kept.
Records on  farm revenue are usually  more accurate than  records  on  farm
operational  costs because the cotton gins and grain elevators  keep records
of how much  each farmer produced and how  much he was paid for  his  produc-
tion.  Government support accounted for  approximately 26 to 40 percent of
the farmers' total farm revenue  in  1980, 1981, and 1982.   From  1982 to
1983 the  crop  revenue more than doubled ($199,505.40 to $543,781.55) while
government  support (PIK) decreased by half ($102,709.56  to $49,239.65).
The federal payments (PIK)  in 1983  represented  only 8.5 percent of the
farm's total gross income. The gross cotton  revenue from the Hancock  farm
is compared to  the gross  cotton revenue for Lubbock County  in Table 54.
                                 266

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                 TABLE 53.   SUMMARY OF GROSS INCOME OE TENANTS

Earmer A
Earmer 3
Earmer C
•Farmer D
Farmer E
Earmer F
Earmer G
Farmer H
Earmer I
Earmer 3
Earmer K

1980
$110.97
69.67
64.39
68.41
57.61
49.71
67.17
98.10
43.40
151 .07
63.47
Total Gross
1981
$123.80
98.16
86.07
96.20
94.91
80.92
'97.70
107.03
79.83
Left
Left
per Acre
1982
$154.94
125.47
109.29
Left
116.57
102.37
130.00
143.01
146.22
Left
Left

1983
$207.57
188.97
196.60
Left
216.92
302.33
213.38
158.97
254.27
Left
Left

*Total/acre x 2.47  = Total/hectare
 Left = Farmer no longer farmed on Hancock farm
    TABLE 54.   LUBBOCK COUNTY,  TEXAS GROSS COTTON REVENUE vs. HANCOCK FARM

                              Lubbock County             Hancock Farm

1980 Dryland              $206.96/ha ($83.79/ac)       $207.58/ha ($84.04/ac)
1981 Dryland              $335.44/ha ($135.85/ac)     $224.05/ha ($90.70/ac)
1982 Irrigated            $249.77/ha ($101.12/ac)           No Cotton
1983 Irrigated            $453.13/ha ($183.69/ac)     $571 .77/ha ($231.48/ac)
*Lubbock County data from personal communication with Jackie Smith,
 Texas A & M Extension Service, Lubbock, Texas.
                                   267

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1983 was  the only year  in which  the farmers  were not hailed out. This
factor,  in conjunction  with  availability of-effluent  water  for  irrigation,
produced  more revenue  per hectare  from the Hancock  farm ($571.77/ha or
$231 .49/ac)  than  the  Lubbock  County average ($453.13/ha or .$183.69/ac).
Net Costs
    A positive cost  benefit  relationship should exist between  the cost of
construction and  operation  of the land treatment system and the benefit to
the owner or operator of  the land treatment site.   The financial balance
sheet for  the Hancock farm  portion of  the Lubbock Land Treatment  System
and the  Hancock farm  as a separate entity is shown -in Table 55.  The table
shows that the Hancock  system had a negative net balance of $702,661.81  to
$1,103,687.57 each  year of  the project.  The system net cost per 1000 m3
of effluent pumped  to  the Hancock  farm was $267.35/1000 m3 ($1.00/1000
gal) in 1982 and $161.28/1000 m3 ($0.61/1000 gal) in 1983.  The reduction
in system  cost in 1983  was  primarily due to the increase in revenues.
    In  the Lubbock land treatment situation, the Hancock farm was private-
ly owned utilizing tenant farmers.  The balance sheet for the Hancock farm
(Table  55) shows  the  farm had  a -$10,751.88, +$48,603.64, -$60,644.59, and
+$286,535.24 balance  in years 1980-1983, respectively.  The tenant farmers
as a group  and  the  land owner should have made a net profit in 1981 and
1983, but  by comparing  the gross farm  revenue distribution (Table  52)  to.
the  farm  operational cost  (Tables G.3 and G.4), it appeared that the farm
owner could  not make  land payment by $41,265.  in 1980,  $16,959 in  1981,
and $45,063 in 1982; but gained $84,171 in 1983. Therefore, the landowner
has experienced a four  year  net loss of $19,116.  Using the same tables as
for the owners  net  income, it is evident that  the tenant farmers as a
group netted $30,514  in 1980,  $65,564  in 1981, and $202,364 in 1933;  but
lost $15,584 in  1982.   The farmer's operational  cost did  not include
living  expenses;  consequently, the four year average  farm net was $70,715.
If each of  nine  tenants received an equal share of the profit (which does
not occur),  then  each tenant  would  have received $7,857/year for  their
families to  live  on.
    A comparison of the shift  in  tenant farmers income between pre- and
post- irrigation  periods  is  given in Table 56.  The table shows in general
that the  years the farmers  had irrigation water (1982 and 1983) they made
                                   268

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                                              Table 55

                                           Balance  Sheet
 Total Hancock System
ON
MD
(c)
(d)

(a)
(b)

)
\
D
1980
Cost/yr Construction $751,265.00
Land Acquisition 163,800.00
Cost Operational - City -0-
Cost Operational - Farm 214,555.88
Total Cost 1,129,620.90
Revenues 367,604.91
Balance $(-)762 ,01 5.97
Net Cost/1000 gal Treated
1981 1982
$751,265.00 $751,265.00
163,800.00 163,800.00
-0- 291,778.00
228,117.36 350,167.03
1,143,182.40 1,587,010.03
440,521.55' 453,322.44
$(-)702,660.81 $(-)l03,687.59
$1 .00
1983
$751 ,265.00
163,800.00
259,932.81
365,337.09
1,540,334.90
815,672.33
$(-)724,662.57
$0.61
Hancock Farm
Land Acquisition
Operational - Farm
Total
Revenue

$163,800.00
214,555.88
378,355.88
367,604.00

$163,800.00
228,117.36
391 ,917.36
440,521 .00

$163,800.00
350,167.03
513,967.03
453,322.44

$163,800.00
365,337.09
529,137.09
815,672.33
       Balance
$(-) 10,751.88    $(+)  48,603.64   $(-)  60,644.59   $(+)286,535.24

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                                 Table 56

                   Comparisons of Shift in Farmers' Income
                       Pre-effluent to Post-effluent

Farmer A
Farmer B
Farmer C
Farmer D
Farmer E
Farmer F
Farmer G
Farmer H
Farmer I
1980 + 1981
Net Average
$ Income/ acre*
-5.22
+2.82
-0.59
-9.83
-0.96
-9.01
+15-. 72
+42.30
+25.58
1982 + 1983
Net Average
$ Income/ acre*
+ 66.58
+ 56.57
+ 0.32
	
+ 21 .40
+105.20
+ 15.34
- 44.79
+ 89.05
Pre to Post
Irrigation
$ Net/ acre/ yr*
+ 71.37
+ 59.39
+ 1.22
	
+ 22.36
+114.21
+ 9.63
+ 2.49
+ 63.48
*$/acre x 2.17 = $/hectare
                                270

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more net  income  per hectare than the baseline period (1980  and  1981)  when
there was  no  effluent  water applied.  All of  the  farmers had  a positive
four year  average net  income primarily due to the  income received  in  1983.
The tenant farmer's net  income  is given in further detail in Table G.8.
    Scenarios  for city  funding the Hancock extension of the Lubbock Land
Treatment  System  are given  in Table 57.  Option 4, where'the City  paid  for
approximately 15 percent of  the  construction  cost,  and  pays  for  the
treatment  and pumping  of the wastewater to a private farm was  in  reality
the  case  of  the  Hancock site.  Under this situation the City  would have
had costs of $112,690, $112,690,  $404,468  and  $372,623  in  1980-1984,
respectively. The City's cost per 1000 ITK pumped to the Hancock  site  would
have been $98 ($0.361/1000 gal)  and $83 ($0.31/1000 gal)  for 1982  and
1983,  respectively.   The only  scenario  in  which the  City  would have
covered its cost  and made money was Option  2  where the  City  would have
constructed the facilities  on land bought by the City under  a construction
grants program (15 percent  City match) and operated the s'ystem  using City
personnel.  Under this  situation, they would have netted $15,789  in  1980,
$75,144 in 1981,  and $2,541 in  1983.  Only in 1982 would  they  have had a
deficit ($492,551).  An  option  not shown is where  an individual  construct-
ed the land treatment   system on privately  owned  land and  the  City paid
for  treatment and pumping cost  of the wastewater to the site.   Under such
a situation,  the  deficits to the private  individual would  be  similar to
those  of  the City in Option  1.  This option would not be  feasible  for a
large system  such as Lubbock's  because the economic deficit  ($750,000/yr)
would be prohibitive for the first 20 years.
                                  271

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                                          Table 57
                          City's Net  Cost  in  Variations in Funding
                     Hancock  Extension  of  Lubbock Land Treatment System

Option 1

Option 2

Option 3

Option 4


$/yr
$/1000 m3
$/yr
$/1000 m3
$/yr
$71000 m3
$/yr
S/1000 m3
1980
-762,016

+ 15,789

- 15,950

-112,690

1981
- 702,661

+ 75,144

+ 8,112

-112,690

1982
-1,103,688
-267(1 .00)*
-492,551
-119(0.45)
-279,441
-67(0.25)
-404,468
-98(0.36)
1983
4724,662.5]
-161($0.60)»
+2,541
+0-56(0.00)
-128,021
-28(0.11)
-372,623
-83(0.31)
*(    )   = $71000 gal

Option 1 = City constructs .and operates Hancock site, "no  matching fund

Option 2 = City constructs Hancock site with matching  funds (15%) and operates
           system

Option 3 = City constructs Hancock site with matching  funds (15%) on City owned
           land farmed by tenant farmers

Option 4 = City constructs Hancock site with matching  funds (15%) on privately
           owned land operated by landowner or tenant  farmers
                                    272

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     Land Treatment.  Edited  by  I.K. Iskandar.  John Wiley & Sons, Inc.
     New York.  1981 .  444 pp.

44.  Metcalf, L. and Eddy, H.P.   Wastewater Engineering: Treatment, Dis-
     posal, Reuse.  2nd Ed.  George Tchabanoglous, ed.  McGraw-Hill, New
     York.  1979.   p. 920.

45.  Oldham, W.K.   Water Pollution Potential of Spray Irrigation by Using
     Secondary Effluent.  Environmental Protection Service, Economics and
     Technical Review Report  EPS 3-PR-76-1.  Ontario, Canada.  1975.

46.  Overcash, M.R.  Land Treatment of Municipal Effluent and Sludge:
     Specific Organic Compounds.  In:  Utilization of Municipal Waste-
     water and Sludge on Land.  University of California, Riverside,
     California.  199 pp.

47.  Page, A.L., Chang, A.C., Sposito,  and Mattigod, S.  Trace Element in
     Wastewater:  Their effects  on plant growth and composition and their
     behavior.in soils.  In:   Modeling Wastewater Renovation:  Land Treat-
     ment.  Edited by I. K. Iskandar.  John Wiley & Sons, Inc.  New York.
     182 pp.
                                  276

-------
47.  Page,  A.L., Chang, A.C., Sposito, and Mattigod, S.  Trace Element in
     Wastewater:  Their effects on plant growth and composition and- their
     behavior in soils.  In:  Modeling Wastewater Renovation:  Land Treat-
     ment.   Edited by I. K. Iskandar.  John Wiley & Sons, Inc.  New York.
     182 pp.

48.  Palazzo, A.J. and Jenkins, T.E.  Land application of Wastewater:
     Effect on Soil and Plant Potassium.  In:  J. Environ. Qual. Vol. 8,
     No. 3.  1979.

49.  Pano,  A. and Middlebrooks, E.J.  Ammonia nitrogen removal in facul-
     tative wastewater stabilization ponds.  J. Water Pollution Control
     Federation.  Vol. 54, No. 4.  1982.  344 pp.

50.  Pettygrove, G.S. and Asano, T. (ed).  Irrigation with Reclaimed
     Municipal Wastewater - A Guidance Manual.  Report No. 84-1 wr,
     California State Water Resources Control Board,  Sacramento.  1984.

51.  Potash Institute of America.  Plant food utilization.  PIA, Atlanta,
     Georgia.  1973.

52.  Pound, C.E., Griffes, D.A. and Crites, R.W.  Utilization of Municipal
     Wastewater and Sludge on Land.  University of California, Riverside.
     1983.   53 pp.

53.  Pratt, P.P., Biggar, J.W., Broadbent, F.E., Focht, D.D., Lund, L.J.
     and Tanji, K.K.  Nitrate in Effluents from Irrigated Lands.  Univer-
     sity of California.  Technical Report NSF-RA-770308.  National Techni-
     cal Information Service.  U.S. Department of Commerce.  Springfield,
     Virginia.  1977.

54.  Ruttner, E.  Fundamentals of Limnology.  3rd ed. University of Toronto
     Press, Toronto.  1963.  p. 295.

55.  Ryczak, R.S.  "A Review of Phosphorus Removal Technology."  Tech.
     Report No. 7706.  U.S. Army Medical Bioengineering Research and
     Development Laboratory, Fort Detrick.  Fredrick, Maryland.  1977-

56.  Ryden, J.C.  Gaseous Nitrogen Losses.  In:  Modeling Wastewater Reno-
     vation; Land Treatment.  Edited by I. K. Iskandar.  John Wiley &
     Sons,  Inc.  New York.  1981.  277 pp.

57.  Sawyer, C.N. and McCarty, P.L.  Chemistry for Environmental Engineer-
     ing.  Third Ed.  McGraw-Hill Book Co.  New York.  1978.

58.  Scarseth, G.D.  Man and His Earth.  Iowa State University Press.
     Ames,  Iowa.  1962.  p. 143.                 —

59.  Shukla, S.S., Syers, J.K., Williams, J.D.H., Armstrong, D.E., and
     Harris, R.F.  Sorption of Inorganic Phosphate by Lake Sediments.
     Soil Science Soc. Amer. Proc.  35:244-249.  1971.

                                   277

-------
60.  Stecher,  P.G., ed.   The Merck Index.  Eighth Edition.  Merck &  Co.,
     Inc.  Rahway,  New Jersey.   1968.

61.  Stone, R.W.,  et al.,  "Upgrading Lagoon Effluent for Best Practicable
     Treatment."  Jour.  Water Poll.  Control Fed., 47, 8, 2-Q19.  1975.

62.  Stromberg,  L.K. and Tisdale,  S.L.  "Treating Irrigated Arid- Land
     Soils with  Acid- Forming Sulphur  Compounds."  Tech, Report No.  24, The
     Sulphur Institute,  Washington,  D.C.  1979.

63.  Stumm, W.  and  Leckie,  J.O.   Phosphate exchange with sediments;  its
     role in the productivity of surface waters.  Proc.  Fifth Inter.
     Water Pollution Research Conf., Pergamon Press.  1970.

64.  Thomas, R.E.   Federal  Incentives  and Requirements Influencing Waste-
     water Reuse.   Water Reuse.   Edited by E. J. Middlebrooks.  Ann Arbor
     Science Publishers, Inc.  Ann Arbor, Michigan.  75 pp.

65.  Torpy, M.F.,  Gearhear,  R.A.,  Spendlove,  J.C., and Spendlove, R.S.
     Field technique measuring  virus decay and potential aerosol hazard
     from wastewater sprinkler  irrigation.  PRWG139-2, Utah Water Research
     Laboratory, College of Engineering, Utah State University, Logan,
     Utah.  1975.

66.  Walker, J.M.  and Demirjian,  Y.A.   Muskeogon County, Michigan's Own
     Land Wastewater Treatment  System.  International Symposium, State of
     Knowledge  in  Land Treatment  of  Wastewater.  Vol. 1.  U.S. Army Corps
     of Engineers.   CRREL.   Hanover, New Hampshire.  1978.  417 pp.

67.  Webber, L.R.  and Leyshon,  A.J.   Soil changes due to effluent irriga-
     tion.  In:   Spray irrigation  of treated  municipal wastewater.  Papers
     presented  at  Harrison  Hot  Springs, B.C.  and Kelowna, B.C.  Environ-
     mental Protection Service,  Department of Fisheries and the Environ-
     ment, Ottawa,  Ontario,  Canada.   1975.

68.  Wetzel, R.G.   Primary  productivity.  In:  B.A. Whitton (Ed.) River
     Ecology.   Univ. Calif.  Press.  Berkeley, California.  1975.

69.  Williams,  R.B.  Wastewater  Reuse  - An Assessment of the Potential
     and Technology.  Water  Reuse.  Edited by E.G. Middlebrooks.  Ann Arbor
     Science Publ., Inc.  Ann Arbor, Michigan.  87 pp.
                                   278

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                                 APPENDIX A
          Sample  Preservation and  Analytical  Methods
                                     Table A.1
                     Water  Sample  Preservation Methods
Parameter Container
Physical Properties
Conductance
PH
Total Dissolved Solids P1
Metals
Dissolved P
Total P
Mercury Dissolved P
Inorganic, Non-metallics
Alkalinity P
Chloride P
Ammonia-Nitrogen P
Total Kjeldahl Nitroqen P
Nitrate plus Nitrite Nitrogen P
Dissolved, Ortho-phosphate P
phosphorus
Preservative Maximun Holding Time

Cool, 4°C 24 hrs
Determine immediately
upon arrival at lab
Cool, 4°C 24 hrs
Filter in lab 6 months
HN03 to pH <2
HNOj to pH <2 6 months
Filter in lab 6 months
HN0.3 to pH <2
Cool, 4°C 24 hrs
Non required 7 days
Cool, 4°C 24 hrs
2 ml ^50^ per liter
to pH <2
Cool, 4°C 5 days
2 ml H2S04 per liter
to pH <2
Cool, 4°C 4 weeks
2 ml H2SOi, per liter
to pH <2
Filter in Lab 24 hrs
Cool, 4°C
(Ref)

EPA




EPA
EPA
EPA

LCCIWR

Hydrololyzable
Total Phosphorus
Sulfate
Cool, 4°C                 5 days
2 ml H2S04 per liter
to pH <2

Cool, 4°C                 5 days
2 ml ^SOt, per liter
to pH <2

Cool, 4°C                 24 hours
                                                                                       ri'A
TOC
Priority Orqanics Pollutants   G2
2 ml  H2SQ;, per liter
to pH <2

2 ml  H2S04 per liter
to oH <2

Extract Base/Neutrals and
Acids within 48 hours.
Freeze extract.  Volatiles
are stored immediately in
airtight glass vial with
Teflon lined rubber suptum.
Cool, 4°C.
                                                                  5 days
                                                                  5 days
Fed . Reg .
Vol. 44,
No. 233
  Plastic
  Glass
                                         279

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                                    Table A.2

               LCCIWR  Analytical Procedures for Water  Analysis
Parameter
    pH
Conductivity
Total Dissolved Solids
Alkalinity
Chloride
Sulfate
Total Kjeldahl Nitrogen
Ammonia
Nitrates/Nitrites
           Method  of Analysis Reference

EPA.  1979.   Methods for Chemical Analysis of Wat8i
and Wastes.   EPA  600/4-79-020.  Method 150.1.
pp. 150.1-3 to  150.1-3.
EPA.  1979.
and Wastes.
pp. 120.1-1.
Methods  for  Chemical  Analysis of
EPA-600/4-79-020.   Method  120.1.
EPA.  1979.   Methods for Chemical Analysis of Watei
and Wastes.   EPA 600/4-79-020.  Method 160.1.
pp. 160.1-1 to  160.1-2.

EPA.  1979.   Methods for Chemical Analysis of Water
and Wastes.   EPA 600/4-79-020.  Method 310.1-1.
pp. 310.1-1 to  310.1-3.

EPA.  1979.   Methods for Chemical Analysis of Water
and Wastes.   EPA 600/4-79-020.  Method 325.3.
pp. 325.3-1 to  325.3-3.

EPA.  1979.   Methods for Chemical Analysis of Watei
and Wastes.   EPA 600/4-79-020.  Method 375.4.
pp. 375.2-1 to  375.2-5.
EPA.  1979-  Methods for Chemical Analysis of
and Wastes.  EPA 600/79-79-020.  Method 351,2.
pp. 351.2-1 to  351.2-5.
EPA.  1979.   Methods for Chemical Analysis of Watei
and Wastes.   Method  350.1  (Colorimetric,  Automated
Phenate)  pp.  350.1-1  to 350.1-6.

Technicon AutoAnalyzer Methodology — non-referenM
procedure for  preparation  of Alkaline Phenol solu-
tion .

EPA.  1979.   Methods for Chemical Analysis of Watei
and Wastewater.   EPA 600/4-79-020.  USEPA, Environ-
mental • Monitoring  and  Support Laboratory, Cincin-
nati, Ohio.

Technicon AutoAnalyzer II.  1973.  Nitrate and
Nitrite-Nitrogen  water and wastewater.  Industrial
Method 100-70W.   Technicon Industrial Systems,
Tarrytown,  New York.
         280

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Table A.2,   continued

     Parameter
            Method of  Analysis  Reference
                          EPA.  1979.  Methods for Chemical Anlysis of Water
                          and Wastewater.  EPA 600/4-79-020.  USEPA, Environ-
                          mental Monitoring and Support Laboratory, Cincin-
                          nati, Ohio.
Total Phosphorus
Orthophosphorus
Organic Phosphorus
Total Organic Carbon
Chemical Oxygen Demand
Total Coliform  Bacteria
Fecal  Coliform  Bacteria
Fecal  Streptococci
Salmonella
EPA.  1979.  Methods  for  Chemical  Analysis of Water
and Wastes.  EPA  600/4-79-020.   Method  365.1.
pp. 365.1-1.to 365.1-7-

EPA.  1979.  Methods  for  Chemical  Analysis of Water
and Wastes.  EPA  600/4-79-020. Method 365.1.
pp 365.1-1 to 365.1-7-
EPA.  1979.
and Wastes.
365.1-7.
Methods for Chemical Analysis of Water
EPA 600/4-79-020.  pp. 365.1-1 to
Beckman Model 9158 Total Organic Carbon Analyzer
Operation Manual  (1980).

EPA.  1979.  Methods for Chemical Analysis of Water
and Wastes.  EPA-600/4-79-020.  Method 415.1.
pp. 415.1-1 to 415.1-3.

QIC.  Standard Ampule Method  for Chemical Oxygen
Demand Test.  Oceanography International Corpora-
tion, 512 West Loop, College  Station, Texas.

EPA.  1978.  Microbiological Methods for Monitoring
the Environment.  EPA 600/8-78-017.  pp. 108-123.

EPA.  1979.  Microbiological Methods for Monitoring
the Environment.  EPA 600/8-78-017.  pp. 124-128.

EPA.  1978.  Microbiological Methods for Monitoring
the Environment.  EPA 600/8-78-017.  pp. 135-138.

Kaper, 3.B., G.S. Sayler, M.M. Bablini, and R.R.Col-
well.  1977. Ambient-Temperature Primary Nonselec-
tive Enrichment for Isolation of Salmonella spp.
from an Estaurine Environment.  Applied and Envir-
                          onmental Microbiology.
                          April  1977.
                        Vol. 33, No. 4, pp. 829-835.
                                  281

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Table A.2,   continued

     Parameter                        Method of Analysis  Reference


Metals                    EPA.  1979.  Methods for Chemical  Analysis  of Water
                          and Wastes.  EPA 600/4-79-020.   Section 200.

                          Perkin-Elmer.  1976.  Analytical Methods  for Atomic
                          Absorption Spectrophotometry.   303-0152.  Perkin-
                          Elmer Corporation, Norwalk, Connecticut.

                          Perkin-Elmer-  1980.  Analytical Methods  for Furnace
                          Atomic Absorption Spectroscopy -  B010-0108.  Perkin-
                          Elmer Corporation, Norwalk, Connecticut.

                          Perkin-Elmer -  1982. Analytical  Methods for Atomic
                          Absorption Spectrophotometry. •  Perkin-Elmer Corpora-
                          tion, Norwalk, Connecticut.

Priority  Organics         Federal Register.  Base/Neutrals,  Acids,  and Pesti-
                          cides. Vol. 44.  No. 233.  pp 69540-68547.
                          Monday, December 3, 1979.
                                 282

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                                   Table A.3

                 RECOMMENDATIONS FOR SOIL SAMPLE PRESERVATION
Parameter
Priority
Organic
Pollutants
Pretreatment Container
Glass jars with
none Teflon faced
screw caps
Temperature
freezing
0°C
Holding
Time
35 days
Indicator
Bacteria
    none
Sterile, wide
mouth autoclavable
polyethylene bottle
with screw cap
                                             Cool
                                              4°C
                30 days
                for 24?o
                moisture
                 soils
                14 days
                for  5%
                moisture
                 soils
Nitrates
                   none
                Plastic  bag
                             Cool
                           4°C
                12 hours
Nitrate
Extract
Place known
weight of
soil in 1 N
Capped glass
Erlenmeyer flask
  Cool
7 days
Metals,
Physicals
All other
Organics
and
Inorganics
Dried and
ground to
pass 2 mm
sieve
Plastic bag
Room temp,
   21 °C
                                                           Indefinite
                                       283

-------
                                    Table A.4

                  LCCIWR  Analytical  Procedures  for  Soil  Analysis
   Parameter

Sample Preservation by
Drying and Grinding

Soil Extraction by
Water
Percent Moisture
Jackson, M.L.
pp. 30-36.
     Method Reference

Soil Chemical Analysis (1958.
USDA "Soil Survey Laboratory Methods and Proce-
dures for Collecting Soil Sample", Soil Service
Investigations Report No. 1 (April 1972) pp. 7-8.
U.S. Dept. of Agriculture, Soil Conservation Ser-
vice, Washington, D.C.

USDA "Diagnosis and Improvement of Saline and
Alkali Soils", (August 1950).  Agriculture Hand-
book No. 60.  pp. 85, 88.

Meyer, R.E. and A.F. Sears.  "Soil Science Labor-
atory Manual" (1978).  Exercise IV-Soil Moisture,
Dept. of Agronomy, Texas Tech University,
Lubbock, Texas.

USDA "Diagnosis and Improvement of Saline and
Alkaline Soils" (1954).  Agriculture Handbook No.
60, p. 107.  U.S. Dept. of Agriculture, Soil Con-
servation Service, Washington, D.C.

USEPA.   1979.  Methods for Chemical Analysis of
Water and Wastes.  EPA 600/4- 79-020.   Method
160.1.  pp. 160.1-1 to 160.1-2.

USDA.  "Soil Survey Laboratory Methods  and Pro-
cedures  for Collecting Soil Samples" (1972).
Soil Survey Investigations Report No.  1, pp. 57-
60.  U.S. Dept. of Agriculture, Soil Conservation
Service, Washington, D.C.

USDA.  "Diagnosis and  Improvement of Saline  and
Alkaline Soils"  (1954).  Agriculture Handbook
No. 60.  p. 102.  U.S. Dept. of Agriculture,
Washington, D.C.

Jackson, M.L. Soil Chemical Analysis (1958).
pp. 41-56.

Black, C.A., et  al., Methods of Soil Analysis
(1965).  pp. 914-926.

USEPA.   1979.  Methods for Chemical  Analysis of
Water and  Wastes.   EPA 600/4-79-020.   Method
150.1.   pp.  150.1-1  to 150.1-3.
      284

-------
Table A.4  ,  continued
Texture
Alkalinity
Carbonate


Sulfur


Sulfate
Chloride
Black, C.A., et al.  Methods of Soil Analysis
(1965).  pp. 299-309, 371-373, and 374-383.

USDA.  "Soil Survey Laboratory Methods and Proce-
dures for Collecting Soil Samples" (April 1972).
pp. 14-16.-  U.S. Dept. of Agriculture, Soil Conser-
vation Service, Washington, D.C.

Meyer, R.E. and A.F. Sears.  "Soil Science Labora-
tory Manual" (1970).  Exercise III — Mechanical
Analysis.  Dept. of Agronomy, Texas Tech Univer-
sity, Lubbock, Texas.

Black, C.A., et al., Methods of Soil Analysis
(1965) .  pp.. 545-567.

Black, C.A., et al., Methods of Soil Analysis
(1965) .  pp. 945-947.

USEPA.  1979.  Methods for Chemical Analysis of
Waters and Wastes.  Method 310.1.  pp. 310.1-1
to 310.1-3.

LCCIWR Methods Manual, Vol. 1, Water and Waste-
water Analysis (1983).Lubbock Christian Col-
lege Institute of Water Research.  Lubbock, Texas.

Black, C.A., et al., Methods of Soil Analysis
(1965).  pp. 1387-138F:

Jackson, M.L.  So il Chem ic al An alys i s (1958).
pp. 322-324.

Jackson, M.L.  Soil Chemical Analysis (1958).
pp. 263-266.

Technicon Corporation.  "Sulfate in Water and
Wastewater" (1972).  Industrial method #226-72W.
72W.  Technicon Industrial Systems, Tarrytown,
New York.

Black, C.A., et al., Methods of Soil Analysis
(1965).  pp. 947-948.

Jackson, M.L.  Soil Chemical Analysis (1958).
pp. 261-263.

USEPA.  1979.  Methods for Chemical Analysis of
Water _and Wastes.  EPA-600/4-79-020.  Method 325.3,

-------
Table A.4,   continued
Conductivity
Total Dissolved Solids
Cation Exchange Capacity
Color
Particle Density
Percent Porosity
Bulk Density
Jackson, M.L.
pp. 234-251.
Soil Chemical Analysis (1958)
Chapman, H.D. and P.P. Pratt.  Methods of
Analysis for Soil, Plants and Waters (1961) .
pp. 17-19.  Div .  of Agricultural Sciences,
University of California.

EPA.  1979-  Methods of Chemical Analysis of
Water and Wastes.  EPA 600/4-79-020.  Method
120.1.  p. 120.1-1 .

Jackson, M.L.  Soil  Chemical Analysis (1958).
p. 256.

Chapman, H.P- and P.F. Pratt.  Methods of
Analysis for Soil, Plants and Waters (1961).
pp. 234-239.  Div- of Agricultural Sciences,
University of California.

USEPA.  1979.  Methods of Chemical Analysis of
Water and Wastes.  EPA 600/4-79-020.  Method
160.1 .  pp. 160.1-1  to 160.1-2.

USDA.  Diagnosis  and Improvement of Saline and
Alkali Soils (1954TAgriculture Handbook No.
60, pp. 100-101.   U.S. Dept. of Agriculture Soil
Conservation Service, Washington, -D.C.

Black, C.A., et al.   Methods of Soil Analysis
(1965).  pp. 899-900.

Meyer, R.E. and A.F. Sears.  "Soil Science Labo-
atory Manual" (1970).  Exercise I — Soil Color,
Texture, Structure and Consistency.  Dept. of
Agronomy, Texas Tech University, Lubbock, Texas.

Munsell Soil Color Charts (1975 ed) .  Munsell
Color, Macbeth Div.  of Kollmorgen Corp.,
Baltimore, Maryland.

Meyer, R.E. and A.F. Sears.  "Soil Science Labora-
tory Manual" (1970).  Exercise II -- Soil Density
Relationships.  Dept. of Agronomy, Texas Tech
University, Lubbock, Texas.

USDA.  Diagnosis  and Improvement of Saline and
Alkali Soils (1954)~Agriculture Handbook No.
60, p. 122.  U.S. Dept. of Agriculture, Soil
Conservation Service, Washington, D.C.

       286

-------
Table  A.4,    continued
Total  Kjeldahl  Nitrogen
Exchangeable Nitrate
and Nitrite Nitrogen
Organic' Nitrogen
Exchangeable Nitrogen
Total Phosphorus
LCCIWR Methods Manual, Vol. 1, Water and Waste-
water Analysis.  1983.  Lubbock Christian College
Institute of Water Research, Lubbock, Texas.

Black, C.A., et. al., Methods of Soil Analysis
(1965) .  pp. 1149-1178.

Jackson, M.L.  Soil Chemical Analysis (1958).
pp. 183-184.

USEPA.  Methods for Chemical Analysis of Waters
and Wastes (1979) .  EPA 600/4-79-020.  pp. 351.2-1
to 351.2-5.

Black,.C.A., et al., Methods of Soil Analysis
(1965).  pp

USEPA.  Methods for Chemical Analysis of Waters
and Wastes (1979).EPA 600/6-79-020.pp. 353.2-1
to 352.2-1/

Determinations of  Exchangeable Ammonium Urea,
Nitrate and Nitrite in a Single Soil Extract",
Agronomy Journal,  Vol. 69, January-February
1977.

Technicon Corporation.  "Nitrate and Nitrite
Nitrogen in Water  and Wastewater" (1973).
Industrial Method #100-70W.  Technicon Indus-
trial Systems, Tarrytown, New York.

Black, C.A. et al., Methods of Soil Analysis
(1965).  pp. 1179-1191 .

USEPA.  Methods for Chemical Analysis of Water
and Wastes (1979) .  EPA 600/4-79-020.
pp. 350.1-1 to 350.1-6.

Onken, A.B. and H.D. Sunderman.  "Colormetric
Determination of Exchangeable Ammonium, Urea,
Nitrate and Nitrite in a Single Soil Extract",
Agronomy 3ournal,  Vol. 69, January-February
1977.

Jackson, M.L.  Soil Chemical Analysis (1958).
pp. 169-172.

USEPA.  Methods for Chemical Analysis of Water
and Wastes (1979).EPA 600/4-79-020.pp. 365.1-1
to 365.1-7.
       287

-------
Table  A.4,   continued
Ortho Phosphorus
Organic Phosphorus
Total Coliform Bacteria
Fecal Coliform Bacteria
Fecal Streptococci
Actinomycetes
Fungi
Metals
Black, C.A. et al., Methods of Soil Analysis
(1965).  pp. 1043-1044.

USEPA.  Methods for Chemical Analysis of Water
and Wastes (1979).EPA 600/4-79-020.pp. 365.1-1
to 365.1-7.

Black, C.A. et al., Methods of Soil Analysis
(1965).  pp. 1467-1472.

USEPA.  Microbiological Methods for Monitoring
the Environment (1978THEPA 600/8-78-017-

Black, C.A. et al., Methods of Soil Analysis
(1965).  pp. 1467-1472.

USEPA.  Microbiological Methods for Monitoring
the Environment (19787^EPA 600/8-78-017.

Black, C.A. et al., Methods of Soil Analysis
(1965).  pp. 1467-1472.

USEPA.  Microbiological Methods for Monitoring
the Environment (19"78~T  EPA/8-78-017.

Black, C.A. et al., Methods of Soil Analysis
(1965) .  pp. 1498-1501.

USEPA.  Microbiological Methods for Monitoring
the Environment (1978) .  EPA 600/8-78-017.

Black, C.A. et al., Methods of Soil Analysis
(1965).  pp. 1502-1505.

Black, C.A. et al., Methods of Soil Analysis
(1965).  pp. 1019-1021.

USEPA.  Methods for Chemical Analysis of Water
and Wastes (1979)EPA 600/4-79-020.
p. METALS-6, Section 4.1.

Perkin-Elmer Corporation.  Analytical Methods
for Atomic Absorption  Spectrophotometry (1976).
Part No. 303-0152.  p. AY-5.1-2.  Perkin-Elmer
Corporation, Norwalk,  Connecticut.

USEPA.  Methods for Chemical Analysis of Water
and Wastes (1979) .  EPA 600/4-79-020.  Section

200'    288

-------
Table  A.4, ,  continued
Organic Carbon
Humus
Organic Matter
Priority Organics
Perkin-Elmer.  Analytical Methods for Furnace
Atomic Absorption Spectroscopy (1980).B010-
0108.  Perkin-Elmer Corporation, Norwalk, CT.

Perkin-Elmer-  Analytical Methods for Atomic
Absorption Spectrophotometry (1982).Perkin-
Elmer Corporation, Norwalk, Connecticut.

Black, C.A. et al., Methods of Soil Analysis
(1965).  pp. 1372-1376.

3ackson, M.L. Soil Chemical Analysis (1958).
pp. 214-219.

U.S. Federal Government.  Federal Register^
(1979).  "Base Neutrals, Acids and Pesticides",
Vol. 44, No. 233, pp. 69540-69547.  December 3,
1979-

Perkin-Elmer Corporation.  "Instruction Manual
for Sigma  Series  GC Console" .  Perkin-Elmer Cor-
poration Data Handling Systems Dept., Norwalk, CT,

Perkin-Elmer Corporation.  "HS6 Head Space  Samp-
ler for the Sigma Series and F22 Gas Chromato-
graphs —  Operator's Manual.  Perkin-Elmer  Cor-
poration,  Norwalk, Connecticut.
                                    289

-------
                                  Table A.5
                           Crops Analysis Methods
     Parameter
Crop Sample Preparation
                                                     Method Reference
Percent Moisture
Cotton Seed Delinting
Total Kjeldahl
Nitrogen, Ammonia and
Protein
Total Chloride

Total Sulfur

Oil

Total Phosphorus
Total Coliform,
Fecal Coliform and
Fecal Streptococcus
                                  Physical
    Horwitz, W., ed.  1970.  Official methods
    of analysis of the association of official
    analytical chemists.  Association of Offi-
    cial Analytical Chemists, Washington, D.C.
    Methods 3.076 and 7.053

    Chapman, H.D. and P.F. Pratt.  1961.
    Methods of analysis for soils, plants, and
    waters. Division of Agr- Sci., Univ. of
    California, Riverside, California.
    Method 2-3.

    Hopper, N.  1981.  Unpublished.  Dept. of
    Plant and Soil Sciences, Texas Tech Uni-
    versity, Lubbock, Texas.

    Issac, R.A. and W.C. Johnson.  1976.
    Determination of total nitrogen in plant
    tissue using a block digester.  3. of the
    Association of Official Analytical Chem-
    ists 59:98-100.

    Walker, R.O., ed.  1980.  Official and
    tentative methods of the American Oil
    Chemists'  Society. American Oil Chemists'
    Society, Champaign, IL.  Methods Aa 5-38.

    Chapman.  1961.  Method 8-2.

    Horwitz.  1980.  Method 3.063.

    Walker.   1980.  Method A.4-38.

   Horwitz.  1980.  Method 3.066.

Microbiological

    J. of Food Protection 41:336-340.  1978.

    Applied and Environmental Microbiology,
    36:831-838.  1978.

    Applied Microbiology,  32:63-69.  1964.
                                   Water  Pollution G.   25:605-609.  1953.
                                     290

-------
Table A.5, continued


                                   Metals

Total  Metals                        Perkin-Elmer.   Perkin-Elmer  Manual  of
                                   Analytical Methods  for  Atomic  Absorp-
                                   tion Spectrophotometry".   pp.  AY5-1  and  2
                                     291

-------
    Pivot
                             Week of
                                                                                        19
N>
Date:


Time:


FM*


GTD+
   Comments:
                                PIVOT LOCATION AND IRRIGATION RECORD

                          (Please record position of end tower each day)
                                                                                                    13
                                                                                                    O
                                                                                                    o
                                                                                                    O
                                                                                                    Q>
                                                                                                    T
                                                                                                    n>
                                                                                                    o
                                                                                                    o
                                                                                                    o
                                                                                                    -5
                                                         -a
                                                         •a
                                                         a
                                                         i—i
                                                         x

                                                         CD
   * Flow Meter Reading

   + Gallons to Date
Signature:
 Figure  B.1.   Pivot Location and Irrigation Record Form

-------
   Pivot
           -^05-
                                                                          of 3-v3/1983
                           PIVOT  LOCATION AND IRRIGATION  RECORD
                     (Please record  position of end tower each day)

                    -/Sto      -Vo       -3/0
hO
MD
Oate:  3/3//fo    V/2^3    V/3yfc,    V/V/fe    V/£/fo    V/7/63


                                                                 3-,
   Time:


   FK*


   GTD+
                   33/77
    Comments:
e
* Flow Meter Reading

- Gallons to Date
. _ A
                                                                      9/3O
                                                                                ex
                                             Signature:
     Figure B.2.  Example of  Properly Prepared  Irrigation Record

-------
                                                                         Week of-;
                             PIVOT LOCATION AND IRRIGATION RECORD
                       (Please record position of end tower each day)
 Date:
 Time:

 FM*

 GTD+
 Comments:
 *  Flow Meter Reading
 +  Gallons to Date
Signature-ly
Figure B.3.  Example of Inadequately Prepared Irrigation Record

-------
MONTH  / / /O-^	VR 83
                                         EXPENSES PAID BY CASH AND CHECK
                      ITCM DCSCWIPTIOM
                      SHOW IBS BU TON
                       NUMBt* 1TC
                                                      SAL ABIES
                                                             SOCIAL
                                                            sccu*'1™
                                                            WITMMLLO
CHCMICALS
POISON A
SPRAYING
            ^
                                                                     99
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                                                                             Us.
                     Tv
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K)
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    y/5? A/^;
         Jojkt
                                                                    Ho&(*
                                                                                                      a?
                                                                                                              5o
Figure B.4.   Original Sheet with 10  Columns for Expenditure Cat-ries. (Filled  out daily by  check
               number)

-------

•
J
4
•
•
7
a
o
10
it
NO
vO Ia
ON
13
14
19
t«
17
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19
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at
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as
24
29
MONTH . ^.JtiA.irh — J 	 _^=Wi 	 .1 R 	 U_w> / CLX"^v^ ^\
s


























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COMPANY
neccivco FROM


























ITCH DESCRIPTION
• HOW UB3 BU TONS
NUMBER, ETC

























TOTALS
1
TOTAL CASH
RECEIVED
7/fi2fl



















































1




















































3
cattle




















































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COTTON
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10



















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Figure B.5.  Original Sheet with Nine Areas of Income  (Done as a yearly lump sum)

-------
        JNTHijQ-^. I ~
                                              EXPENSES PAID BY CASH AND CHECK
MD
MUNTMWtAarti 1 	 ^feri

























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CHEMICALS
POISON a
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SO/3

























on

























       Figure B.6.  Some  Categories Changed to Pit Personal  Records (Yearly Lump Sum)

-------
        MONTH_<3-yy.'
                                                   EXPENSES PAID BY CASH AND CHICK
                                                                                       /-<=.,-/


^

Fe

AAcx

Ap

MX

A.-





















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SHOW LBS BU TON
NUMBCn ETC

























TOTALS
*OTAL CASH
EXPENDITURE
19 .IV

,33O(»

/753

2532^

4931

6,593
•4.2/0

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'
12,388

754,0

383

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     Figure  B.7.   Expenditures  on a  Monthly  Basis

-------
                                                             Table C.1

                                          Simple  Statistical Values  of  the  Quality  of
                                          Effluent Applied  to Land Treatment Sites
                                                              AHITIMETIC;  .TiANS
                                                                   AND
                                                            STANDARD DEVIATIONS
K)
Source* ALKALINITY
COHOUCTIVITT
IDS
SG CAC03A BG/L
10000 AT" 337. 2216. 1695.




10004



90000




90001





SD
S
DO

AT
SD
S
no
AT
SD
S
no

»T
SD
S
no


( 34.)
<-0.07>
342.

342.
( 54.)
< 1.1 9>
343.
283.
( 31.)
< 0.22>
285.

299.
( 30.)
<-0.09>
303.

TOTAL P
tource- BG P/L
»»•««»•»*»•»*••»•«*•»*•«•
( 290.)
< 0.18>
2130.

1969.
( 160.)
<- 1 . 45>
1975.
1818.
( 155.)
<-0. 13>
1825.

2093.
( 341.)
< 2.53>
2085.

ORTHO P
BG P/L
( 537.)
< 3.00>
1635.

1190.
( 107.)
< 0.76>
1180.
1130.
( 66.)
<-1. 17>
1146.

1241.
( 56.)

1246.

OBG. P
1G P/L
PH

7.54
(0.21)
<-1.05>
7.57

7.76
(0.36)
< 1.43>
7.70
7.88
(0.21)
< 0.09>
7.86

3.30
(0.52)
<-0.01>
8.30

COD
BG/L
CL
S04
1G/L BG/L
468. 315.
( 55.)
<-1 . 62>
470.

139.
( 71.)
< 1.83>
328.
303.
( 25.)
<-0.82>
306.

360.
( 18.)
< 0. 10>
359.

TOC
MG/L
( 43.)
<-0. 1 7>
311.

208.
( 46.)
<-0.05>
208.
178.
( 29.)
<-0.65>
179.

200.
( 52.)
<-2.66>
215.



TOTAL N
BG N/L
33.59
(15.23)
< 1.40>
35.42

41.70
(19.99)
< 0.75>
33.49
24.43
( 6.97)
<-0. 15>
25.78

11.74
( 8.20)
< 0.70>
12.38



NU2/N03
NH3

HG N/L MG H/L
0.29 25.95
( 0.30)
< 1.03>
0. 16

0.71
( 1.66)
< 3.57>
0.07
3.45
( 2.65)
< 0.41>
3.08

0.66
( 1.27)
< 2.95>
0.27



( 6.69)
< 0.42>
25.42

25-80
(10.70)
< 0.80>
25. 59
16.72
< 6. 10)
<-0. 25>
18. 54

8.24
( 6.41)
<-0. 04>
8. 38



Cu
c-t-
rc
-5
-0
c
fa
_J.

"<
o
^
OJ
Cu
13
Q.

^
CQ
C
rt>
CO

                                                                                                                                          "O
                                                                                                                                          -a
       10000  AT    14.43          A.36         5.15         302.4         117.7
              SD   ( 4.27)        ( 2.03)       ( 4.20)        (135.6)        (45.1)
              S    < 1.47>       < 0.60>      < 0.56>       < 0.32>      <  0.69>
              HO    14.16          8.32         4.73         284.0         114.3
       10004
       90000
       90001
AT    11.82
SD   (  3.63)
S    <  0.63>
(ID    11.13

IT     9.18
SD   (  1.36)
S    <  1.02>
HD     8.77
              AT
              SD
              S
              no
       6.31
     (  2.32)
     <  0.41>
       5.92
  8.43
( 1-71)
< 0.23>
  8.29

  7.28
( 1-13)
< 0.59>
  7.22

  4.85
( 2-20)
<-0.17>
  5.37
  1.60
( 2.20)
< 1.58>
  0.49

  0.55
( 0.58)
< t.19>
  0.43

  0.61
( 1. 19)
< 2.47>
  0. 19
 325.6
(290.2)
< 1.84>
 237.5

 175.0
( 71.8)
< 1.25>
 160.5

  75.1
( 29.0)
< 0.09>
  61.3
  64. 1
(37.3)
 0.88>
  51.9

  52.6
(29.5)
 1.44>
  44.3

  20. 8
(  6.4)
-0.32>
  20. fl

-------
          Table  C.1,  continued
            Source           TOTAL TOLIFCRMS
             ******•**•*•••**#••**•#*•*#*•***«
             10000  »V           27326016.
                    SO        (   16447465.)
                    S         <        0.45>
                    HD           27000000.
             10004   AV
                    SO
                    S
                    HO

             90000   IV
                    SO
                    S
                    BD

             90001   IV
                    SD
                    S
                    no
                         ?ECAL COLIPOBIIS
                 »**•**•*•****•** •*»**•***•
                             8852272.
                         {   5933719.)
                         <        1.19>
                             6600000.
   22639168.
(  13669506.)
<       1.38>
   23000000.

   26UOOOOO.
(  17608080.)
<       1.76>
   21000000.

    1054713.
(   3457580.)
<       4. 12>
     200000.
3576744.
3632128.)
    2.24>
3000000.

5010000.
4542747.)
    0.81>
2600000.

 109211.
 433929.)
    4.23>
   5000.
   PECAL STBEP.
*******•**********•***•**•***#*••
       281659.
    (   592418.)
    <      3.78>
       125500.

       243003.
    (   208804.)
    <      1.15>
       210000.

       295000.
    (   293115.)
    <      1.44>
       250000.

       151788.
    (   670406.)
    <      4. 13>
         1000.
o
o

-------
 Table  C.1,  continued
  flETlLS.  nrSSOL»ED(NG/L)




Sourc**
»•••**•
10000



10004



90000



90001



Source
10000



10004



90000



90001



****
IV
SD
S
HD
IV
SD
S
HD
IV
SD
S
HD
tv
SD
S
RD
•
IV
SD
S
HD
IV
SD
S
HD
IV
SD
S
HD
IV
SD
S
HD
<**********i
1.277
( 1.298)
< 1.56>
0.640
0.824
( 0.532)
< 0. 17>
0.631
1.026
( 1.409)
< 0.00>
1.026
0.844
( 1.113)
< 1.30>
0.279
Ha
34.8
( 7.6)
< 0.32>
35.0
24.3
(1.9)
< 0.73>
24.5
24.9
( 0.8)
< 0.0 >
24.9
27.4
( 1.4)
<-0. 17>
27.2
0.009
(0.006)
< 1.62> <
0.005
0.006
(0.002)
< 3.48> <
0.005
0.005
(0.0 )
< 0.0 > <
0.005
0.006
(0.003)
< 2.27>
0.005
nw
0.056
(0.025)
<-0.38>
0.060
0.057
(0.029)
< 0.34>
0.048
0.030
(0.028)
< 0.00>
0.030
0.057
(0.044)
< 1. 26>
0.045
0. 198
(0.130)
: i.32>
0.201
0.078
(0.067)
C 0.17>
0.084
0.037
(0.039)
: o.oo>
0.037
0.032
(0.062)
C 2.27>
0.010
HG
0.000
(0.000)
< 0.61>
0.000
0.000
(0.000)
< 1.00>
0.000
0.000
(0.0 )
< 0.0 >
*****
0.000
(0.0 )
< 0.0 3
0.000
1.278
(1.494)
< 2. 33>
0.78 1
0.220
(0.270)
< 1.77>
0.100
0. 100
(0.0 )
< 0.0 >
0.100
0. 186
(0.244)
< 2.27>
0.100
no
0.007
(0.004)
< 1.26>
0.006
0.003
(0.000)
< 1.00>
0.003
0.003
(0.0 )
< o.o •>
*****
0.003
(0.000)
< 1.00>
0.003
54.7
( 13.4)

53.
58.4
( 7.0)
< 0. 76>
57.
59.6
( 1-9)
< 0.0 >
60.
65.2
( 3.2)
< 0.99>
64.
HI
0.062
(0.065)
< 2. 19>
0.056
0.048
(0.056)
< 1.04>
0.006
0.010
(0.0071
< 0.0 >
0.01J
0.0 08
(0.009)
< 2. 27>
0.005
0.002
(0.002)
< 2.25>
0.000
0.012
(0.046)
< 3.88>
0.000
0.002
(0.002)
< 0.00>
0.002
0.000
(0.000)
< 1.00>
0.000
K
21.3
( 7.3)
< 0.52>
19.2
19.5
( 7.5)
< 1.74>
18.1
16.3
( 0.5)
< 0.00>
16.3
19.5
( 4.1)
< 1. 51>
19.3
0.006
(0.002)
< 4.05>
0.005
0.005
(0.000)

0.005
0.006
(0.002)
< 0.00>
0.006
0.005
(0.0 )
< 0.0 >
0.005
SE
0.015
(0.018)
< 2.58>
0.005
0.005
(0.000)
< 1.00>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.059
(0.035)
< 0.0 9>
0.052
0.030
(0.030)
< 0.66>
0.009
0.005
(0.000)
< 0.0 >
0.005
0.005
(0.000)
< 2.27>
0.005
1C
C.006
(0.003)
< 2.95>
0.005
0.005
(0.001)
<-3.88>
0.005
0.005
(0.0 )
< 0.0 >
0,005
0.005
(0.0 )
< 0.0 >
0.005
0.081
(0.064)
< 1.36>
0.072
0.024
(0.026)
< 1.32>
0.010
0.006
(0.001)
< 0.0 >
0.006
0.011
(0.017)
< 2.27>
0.005
Hi
378.4
(131.7)
< 1. 13>
358.0
318.6
1 50.9)
< 0.08>
317.5
265.0
( 1-4)
< 0.0 >
265.0
304. 1
( 43.9)
<-0.49>
308.0
0.731
(0.510)
< 0.89>
0.643
1. 187
(0.698)
< 0.84>
1.241
1. 185
(1. 196)
< 0.00>
1. 185
1.097
(1.064)
< 0.93>
0.615
TL
0.005
(0.001)
< 4.01>
0.005
0.005
(0.000)
< 1.00>
0.005
O.OOS
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
0.005
»*•»•***
0.018
(0.023)
< 2.89>
0.011
0. 130
(0.468)
< 3.87>
0.015
0.007
(0.0071
< 0.00>
0.007
0.002
(0.001)
< 2.27>
0.002
ZN
>$ fc # $^^>
0.104
(0.100)
< 1.34>
0.076
0.169
(0.087)
< 0.86>
0. 163
0.172
(0.170)
< 0.00>
0.172
0.102
(0.058)
< 0.59>
0.081

-------
Table  C.1,  continued
NETALS. TOTAL (NG/L)
Source *
                                 DA
                                                    CA
                                                              CD
                                                                       CO
                                                                                 CD
                                                                                           CU
                                                                                                     FE
                                                                                                               PB
10000 AT
SD
S
(ID
10004 AT
SD
S
no
90000 AT
SD
S
HD
90001 AT
SD
<^J S
S
Source*
10000 AT
SD
S
1000* AT
SD
S
BD
90000 AT
SD
S
no
90001 AT
SD
S
HD
0.650
( 0.0 )
< 0.0 >
*****
0.091
( 0.070)
< 1.03>
0.086
0.139
( 0. 129)
< 0.92>
0.084
0.136
( 0.136)
< 1.76>
0.09*
HG
45.0
( 0.0)
< 0.0 >
*****
27.0
( 9.1)
29.3
28.2
( 2.8)
< 0.26>
27. «
28.4
( 5.1)
30.2
0.034
(0.0 )
< 0.0 >
*****
0.006
(0.002)
< 0.83>
0.005
0.007
(0.003)
< 1.25>
0.006
0.006
(0.002)
< 0.75>
0.005
nw
• £4 ##4 frt44
0.045
(0.0 )
< 0.0 5
*****
0.025
(0.012)
< 0.06>
0.02*
0.035
(0.009)
<-0.09>
0.035
0.040
(0.019)
< 0. 72>
0.038
0.216
(0.0 )
< 0.0 >
*****
0.192
(0.082)
<-0.78>
0.197
0.387
(0.197)
< 0.58>
0.394
0.133
(0.090)
<-0.20>
0. 157
HG
kt •$• 4 #•# *#<
o.o
(0.0 )
< 0.0 >
0.0
0.000
(0.0 )
< 0.0 >
*****
0.0
(0.0 )
< 0.0 >
0.0
0.000
(0.0 )
< 0.0 >
0.000
0.822
(0.0 )
< 0.0 >
*****
0.034
(0.028)
< 1.36>
0.027
0.024
(0.015)
< 0.38>
0.018
0.053
(0.041)
< 0. 18>
0.038
.10
X* • • V •••#••
0.070
(0.0 )
< 0.0 >
• •*•*
0.003
(0.002)
< 1.57>
0.003
0.003
(0.000)
< 1.00>
0.003
0.003
(0.000)
< 1.00>
0.003
67.0
< 0.0)
< 0.0 >
****
47.5
( 16.81
si.
50.7
( 7.0)
< 0.1 4>
48.
54.3
( 10.5)
<-0.54>
54.
HI
49ttf*4ttfrt
0.061
(0.0 )
< 0.0 >
*****
0.062
(0.058)
< 1.1 5>
0.065
0.032
(0.047)
< 1.1 1>
0.006
0.018
(0.020)
0.007
0.005
(0.0 )
< 0.0 >
*****
0.001
(0.002)
< 1.76>
0.000
0.001
(0.000)
< 2.04>
0.000
0.000-
(0.000)
< 1.00>
0.000
K
## * » * tt ••#44
22.0
( 0.0)
< 0.0 >
*»»*
29.7
(10.7)
<-2.38>
32.4
33.9
( 5.3)
< 1.59>
32.9
30.2
{ 7.8)
34.0
0.003
(0.0 )
< 0.0 >
*****
0.004
(0.002)
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
SE
0.031
(0.0 )
< 0.0 )
*****
0.005
(0.0 )
< o.o •>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
G.036
(0.0 )
< 0.0 >
*****
0.067
(0.035)
< 0.31>
0.060
0.072
(C.048)
0.053
0.006
(0.001)
< 0.61>
0.006
AC
0.005
(0.0 )
< 0.0 >
*****
0.004
(0.00 Ml
< 0.62>
0.003
0.032
(0.002)
0.001
0.004
(0.001)
0.005
0.035
(0.0 )
< 0.0 >
*****
0.057
(0.051)
0.047
0.081
(0.044)
< 0.89>
0.064
0.051
(0.057)
< 1.45>
0.033
HA
384.0
( 0.0)
< 0.0 >
*****
225.3
< 81.5)
<-2.00>
235.0
238.9
I 33.0)
<-0.46>
252.0
255.7
( 55.5)
279.0
0.423
(0.0 )
< 0.0 >
*****
0.821
(0.470)
<-0.02>
0.770
0.627
(0.555)
< 1.25>
0.380
0.774
(0.773)
< 0.93>
0.360
TL
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
o.oos
0.049
(0.0 )
< 0.0 >
* ****
0.036
(0.029)
< 0. 50>
0.032
0.046
(0.014)
< 0. 16>
0.044
0.008
(0.008)
< 0.94>
0.005
ZK
** • * tt W
0.050
(0.0 )
< 0.0 >
*****
0.301
(0.527)
< 2.67>
0. 133
0.135
(0. 104)
< 0.48>
0.083
0.093
(0.108)
< 2.01>
0.066

-------
   Table  C.1, continued
    ORGMICS (PPB)
Source     ACKHAPHTBTLEHE  AHTHTtACENE/PHEHATHB EKE    ATBAZINE  DEHZENE/TRICHLOBOET UYL ENE
 »•***»••••»•«*••*«**«»»*•***»*«•*••«•••••••»•
 10000  AT         4.9               .  6.1
        SD      (  1.6)               (  7.5)
        S       < 1.51>             < 2.44>
        RD        5.00                2.00
                                                                                             BENZSKEACETIC ACID  tt-T- B UT VLPH ENOL
   1000*   AT
          SD
          S
          HO

   90000   AT
          SD
          S
          no
  90001
          AT
          SD
          S
          HD
                   4.9
                   6.0)

                  4! 55

                   2.5
                   1.1)
                  1.58>
                  2.00

                   3.2
                   1.5)
                  0.37>
                  2.00
              8.4
           (  12.8)
           <  2.79>
             3.20

              4.0
           (   2.6)
           <  0.86>
             2.95

              5.5
           {   6.9)
           <  1.73>
             2.00
Sojjrc^ CABBOI TETBACHLOBIDE   4-CHLOHOA!iiLi»E
   10000  AT
          SD
          S
          no

   1000*  AT
          SD
          S
          HD

   90000  AT
          SD
          S
          BD

   90001  AT
          SD
          S
          HD
                  8.0
               (  9.3)
               < 3.72>
                 5.00

                  4.7
               (  4.6)
               < 2.89>
                 4.70

                  3.2
               (  2.5)
               < 1.99>
                 2.00

                  3. 1
               (  1.6)
               < 0.28>
                 2.00
•**•*•*•****•*
            29.0
          ( 36.7)
          < 1.98>
           10.00

            17.1
          ( 38.9)
          < 5.10>
           10.00

            13.2
          ( 24.4)
          < 2.53>
            6.90

            42.4
          (140.7)
          < 4.10>
           10.00
10.9
( 17.4)
< 3. 18>
5.10
32.5
( 36.9)
< 2.09>
18.25
39.4
( 31.0)
< 0.61>
23.25
10.9
< 7.9)
< 0.70>
10.00
CHL010SZNZEHE
1. 1
( 0.3)
< >4.01>
1.00
1.3
( 1-9)
< 5.20>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1. 1
( 0.4)
< 2.80>
1.00
1.9
( 1-5)
< 1.83>
1.00
11.0
( 23.6)
< 2.47>
2.40
2.2
( 2.4)
< 2. 14>
1.00
CHLOBOFORd
1.0
( 0.1)
< U.25>
1.00
5.3
( 6-3)
< 1. 71>
2.70
3.9
( 3.6)
< 0.89>
2.65
1.9
( 2.3)
< 3.34>
1.00
16.6
( 0.0)
< 0.0 )
• *»••*
3.7
( 2.6)
< 0.00>
3.75
0.0
( 0.0)
< 0.0 >
0.0
0.0
< 0.0)
.< 0.0 >
0.0
2-CBtOBJ PHENOL
8.5
( 6.9)
< 0. 51>
6.55
7.3
( 16.6)
< 4.35>
2.00
9.5
( 15.0)
< 1. 41>
1.15
3.5
( 7.8)
< 3.95>
1.30
5. 1
( 8.0)
< 2.75>
2.00
19.6
( 69.3)
< 4.96>
2.45
5. 1
( 4.2)
< 0.52>
4.05
3.4
I 3.21
< 2.69>
2. 10
1-CHLOHOTETBADECA US
4.9
( 4.4)
< 1.49>
2.00
10.5
( 9. 1)
< 1.56>
8.65
7.4
( 4.5)
< 0.67>
6.20
6.5
( 11.11
< 3.63>
2.60

-------
 Table  C.1, continued
  8ourc«*OIBOTripH1TniL1TE  2.3-iici!LOB
         HO      8.80

  1000*
  90000
  90001
*V
SD
S
HO
AT
SD
S
3D
»»
SD
S
NO
103.9
(149.2)
< 1.62>
23.40
126.6
(114. 4J
< 0.45>
122.10
36.8
( 44.2)
< 2.44>
29.55
8.5
( 6. 1)
< 1.37>
6.15
13.3
( 19.3)
< 2.59>
5.00
4.9
( ».9)
< 2. 17>
3.30
3.5
( 1-5)

3.70
5.8
( 7.2)
< 2.28>
2.00
8.2
( 16.0)
< 4.46>
3.B5
7.2
( 5.8)
< 1.06>
6.15
3.2
( 1-9)
< 1.77>
2.35
5.7
( 6.9)
< 2.59>
2.60
11.2
( 29.6)
< 5.02>
4.70
7.8
( 5.3)
< 0.40>
7.25
4.2
( 4.1)
< 2.34>
2.75
6.4
( 7.0)
< 2.15>
3.60
7.3
( 15.0)
< 4.72>
3.30
3. 7
1 2.7)
< 0.99>
3.10
3.3
I 3.6)
< 3.14>
2.00
11.6
( 12.0)
< 1.58>
7.20
14.0
< 14.3)
< 1.56>
8.60
11.7
( 13.1)
< 1.26>
4.70
4.9
( 4.0)
< 1. 15>
4.10
Source*     DICHLOBOBETHIRE  2,4-Dicui.oBOpusHoi.  DIETHTLPHTHALITE   DIISOOCTYLPHTIUI.UE  DIOCTTLPHTHILATE  OODECANOIC icio
  it******************************************** •********'*********»*************•*•***«****•**»»**•**•****»»****•**•»*«***•**••*••*
  10000   »T        72.2                7.7                6.5                63.1                 7.3              0.0
         SD      (   0.0)             (   8.1)             (   9.3)             (111.8)              (  9.2)           (   0.0)
         S       <  0.0 )             <  1.23>             <  3.03>             < 2.78>             < 1.32>          <  0.0 >
         BO      *••***               4.1Q               2.50               18.40                2.00             0.0
1000*



90000



90001



ir
so
S
HD
IV
SD
S
ND
IT
SD
S
(ID
0.0
{ 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
5.5
( 0.0)
< 0.0 >
******
  11.7

< 2.78>
  7.45

   6.9
(  5.1)
< 0.88>
  4.80

   6.7
( 10.9)
< 2.65>
  3.00
                                                         39.1
                                                       (  69-3)
                                                       <  4.55>
                                                       28.40

                                                         16.2
                                                       (  10.5)
                                                       <  0.95>
                                                       15.35

                                                         15.9
                                                        13.00
  43.3
(144.2)
< 3.57>
  2.00
   2.0
   0.0)
  0.0 >
******

   2.0
(  0-0)
< 0.0 >
  2.00
  11.0
( 37.1)
< 3.75>
  2.00

   2.0
(  0.0)
< 0.0 >
******

   2.0
I  0.0)
< 0.0 >
  2.00
   0.0
(  0.0)
< 0.0 3
  0.0

   0.0
(  0.0)
< 0.0 )
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0

-------
Table C.1, continued
Source*    ETUTL BENZENE       HEPTADECANE         HEIADECANS     HEXAPECANOIC ACID  USTHYLHEPTADECANOATE  IETHH.HEXADECANOATK
****•*•
10000



10004



90000



90001



Source
4 444 44 1
10000



10004



90000



90001



!»•*>
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
RD

N44 4
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
BD
AT
SD
S
no
«»•**«»««»*««•»•»•* ***<
1.3
( 1-0)
< 3.30>
1.00
1.7
( 1.5)
< 4.37>
1.00
1.9
( 0.3)
<-2.67>
2.00
1.8
( 1-5)
< 3.35>
2.00
1-HETHYLRAPHTHALEHE
6.8
( 15.1)
< 3.64>
2.00
6.4
( 8.9)
< 3.79>
2.90
2.6
( 1-6)
< 0.92>
2.15
3.2
( 3.3)
< 2.86>
2.00
7.5
{ 7.7)
< 1.66>
3.90
14.3
( 14.8)
< 1.95>
10.95
6.9
( 4.0)
< 0.96>
5.85
3.6
( 3.5)
< 1.55>
2.00
2-flBTBTLPHENOL
6.1
( 6.3)
< 1.74>
2.25
5.3
( 5.4)
< 1.91>
3.30
2.6
( 1-8)
< 1.07>
2.20
1.9
( 1-5)
< 3. 21>
2.00
7.5
( 8.3)
< 1.46>
3.20
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< o.o •>
******
2.0
( 0.0)
< 0.0 >
2.00
4-1ETHTLPHE00L
8.7
{ 14.7)
< 3.90>
5.00
16.1
( 43.3)
< 4.71>
5.00
7.2
( 12.0)
< 2.38>
2.50
3.4
( 1-8)
< 0.71>
2.25
59. «
( 33.0)
< 0.69>
42.50
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
13.9
( 18.2)
< 0.0 >
13.90
NAPHTHALENE
3.1
( 1.9)
< 1.66>
2.00
14.2
( 22.2)
< 3.01>
7.85
20.5
( 32.9)
< 2.21>
8.75
5.3
< 5.5)
< 2.38>
2.50
8.4
( 11.D
< 1.66>
2.00
142.7
(690.0)
< 5. 19>
2.60
4.5
< 5.4)
< 2.35>
2.00
10.5
( 17.9)
< 2.44>
2.00
4-NONTL?HBNOL
0.0
( 0.0)
< 0. 0 >
0.0
12.1
{ 0.0)
< 0. 0 >
******
0.0
< 0.0)
< 0. 0 >
0.0
26.1
( 0.0)
< 0. 0 )
******
12.6
{ 24.2)
< 3. 18>
2.85
38.7
( 84.4)
< 3.65>
6.15
4.1
( 4.4)
< 2.30>
2. 15
16.9
( 22.1)
< 2.09>
7. 15
OCTADECANE
4.3
( 3.4)
< 1.24>
2.00
18.6
( 55.9)
< 4.95>
5.80
8.5
( 4.6)
< 0.71>
7.90
7.8
( 8.6)
< 1.67>
2.85

-------
Table C.1, continued
Source*
10000 IT
SO
S •
no
10004 IT
so
S •
BO
90000 AT
SO
S •
no
90001 IT
so
S «
no


10.5 20.0 8.1 4.8 1.9 6.8
( 8.4) ( 54.0) ( 16.2) ( 12.6) ( 2.4) ( 8.1)
< 1.71> < 4.03> < 3.10> < 3.24> < 2.66> < 4. 25>
10.00 5.10 2.00 1.00 1.00 5.00
9.7
( 11.5)
C 3.93>
8.20
8.4
( 7.3)
C 1.06>
6.75
8.3
( 7.2)
* 9^80


35.0
( 61.9)
< 2.71>
11.00
20.7
{ 24.1)
< 1.67>
10.00
11.7
( 13.9)
< 2.58>
10.00


16.8
( 27.4)
< 1.89>
2.00
18.8
( 30.2)
< 2. 10>
5.75
32.7
(113.3)
2.' 00
Source*
10000
10004
90000
90001
1.8
( 1-9)
< 3.59>
1.00
2.3
{ 1-4)
< 0.54>
2.00
2.1
( 1.8)
< 1.54>
1.00

1.6
( 2.1)
< 3.72>
1.00
1. 1
( 0.2)
< 1.67>
1.00
1. 1
( 0.5)
< 4. 13>
1.00

5. 1
( 1.D
< 1.75>
5.00
5.0
( 0.0)
< 0.0 >
******
4.9
( 0.3)
sloo

1.2
( 0.8)
< 4.01>
1.00
1. 1
( 0.3)
< 3.06>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.1
( 0.3)
< 2.39>
1.00

= Plant#2 Effluent June 1980 to February 1982
= Discharge From Force Main February 1982 to November 1983
= Effluent To Gray Farm June 1982 to November 1983
= Discharge From Hancock Reservoir//1 February 1982 to November 1983
                         ** AV = Arithmetic Average
                            SD = Standard Deviation
                             S = Skewness
                            MD = Median Value

-------
        TABLE  C.2.   RECOMMENDED MAXIMUM CONCENTRATIONS OF TRACE ELEMENTS
       	IN  IRRIGATION WATERS (Pettygrove & Asano 1984)
Element
Recommended
  maximum
Concentration3
   (mg/1)
                     Remarks
Al
(aluminum)
As
(arsenic)
Be
(beryllium)
Cd
(cadmium)
      5.0
Co
(chromium)
Cu
(copper)

F
(fluoride)

Fe
(iron)
      0.10
      0.10
      0.01
      0.1
      0.2


      1.0


      5.0
Can cause non-productivity in acid soils
(pH <5.5), but more alkaline soils at pH
<5.5 will precipitate the ion and elimi-
ate any toxicity.

Toxicity to plants varies widely, ranging
from 12 mg/1 for Sudan grass to <0.05 mg/1
for rice.

Toxicity to plants varies widely, ranging
from 5 mg/1 for kale to 0.5 mg/1 for bush
beans.

Toxic to beans, beets, and turnips at con-
centrations as low as 0.1 mg/1 in nutrient
solutions.  Conservative limits recommended
because of  its potential for accumulation
in plants and soils to concentrations that
may be harmful to humans.

Not generally recognized as an essential
growth element.  Conservative limits rec-
omended because of lack of knowledge on
toxicity to plants.

Toxic to a number of plants at 0.1 to 1.0
mg/1 in nutrient solutions.

Inactivated by neutral and alkaline soils.
Not toxic to plants in aerated soils, but
can contribute to soil acidification and
loss of reduced availability of essential
phosphorus and molybdenum.  Overhead sprink-
ling may result in unsightly deposits on
plants, equipment, and buildings.
                                                                     (continued)
                                    307

-------
Table C.2, continued
Element
Recommended
  maximum
Concentration^
   (mg/1)
                                                      Remarks
Li
(lithium)
Mn
(manganese)
Mo
(molybdenum)
Ni
(nickel)
Pb
(lead)

Se
(selenium)
Sn
(tin)

Ti
(titanium)

W
(tungsten)

V
(vanadium)
      2.5
      0.2
      0.01
      0.2
      5.0
      0.02
      0.1
Tolerated by most crops up to 5 mg/1;
mobile in soil.  Toxic to citrus  and  low
levels (>0.075 mg/1).  Acts similar to
boron.

Toxic to a number of crops at a few tenths
mg to a few mg/1, but usually only in acid
soils.

Not toxic to plants at normal concentra-
tions in soil and water.  Can be  toxic to
livestock if forage is grown in soils with
high levels of available molybdenum.

Toxic to a number of plants at 0.5 to 1.0
mg/1; reduced toxicity at neutral or  alka-
line pH.

Can inhibit plant cell growth at  very high
concentrations.

Toxic to plants at concentrations as  low as
0.025 mg/1 and toxic to livestock if  forage
is grown in soils with relatively high levels
of added selenium.  An essential  element for
animals but in very low concentrations.

Effectively excluded by plants; specific
tolerance unknown.

(See remark for tin)
                  (See remark for tin)
Toxic to many plants at relatively low con-
centrations.

    "(continued)
                                    308

-------
Table  C.2,  continued
Element
Recommended
  maximum
Concentration3
   (mg/1)
Remarks
Zn
(zinc)
2.0 Toxic to many plants at widely varying
centrations; reduced toxicity at pH >6
in fine textured or organic soils.
con-
.0 and
a The maximum concentration is based on a water application rate that is
    consistent with good agricultural practices 1.22 ha.m/ha.yr (4 ac-ft/
    ac.yr) the water application rate exceeds this, the maximum concentra-
    tion should be adjusted downward accordingly.  No adjustment should be
    made for application rates of less than 4 acre-ft per year per acre.
    The values given are for waters used on a continuous basis at one site
    for the irrigation supply water.
                                    309

-------
TABLE C.3.   RANGES  OF  CONCENTRATIONS  OF  ORGANIC  COMPOUNDS  IN
       MUNICIPAL  WASTEWATER  TREATMENT  PLANT  EFFLUENTS
      IN MICROGRAM5 PER  LITER  (Majeti  and  Clark  1981)

Compound
Chloroform
Trichloroethylene
Benzidine
Vinyl Chloride
Benzene
PCBs
End r in
Toxaphene
Methanol
Ethanol
Acetone
2,3-Dithiabutane
Carbon Disulfide
1 ,1 ,1-Trichloroethane
Tetrachloroethylene
Toluene
Xylene
Acrolein
Acetaldehyde
Carbon Tetrachloride
Chi o rod ibromome thane
Dichlorobromomethane
Bromoform
1 ,3-Dichloroethane
Methylene Chloride
Dayton, Ohio
Unchlo- Chlori-
nated nated
0.3-1.4 0.4-12
0.2-1.7 0.1-10
<01
<1
0.2-40
.1
.1
.1
150-510
150-3000
50_300
	 *
	 *
1-15
1-20
1-10
1 -1 5
20-200
90-1,350
3
0.1
0.1 0.1-0.4
* 0.1-4.6
1.4 0.1-4.6
2-50
Cincinnati, Ohio
Unchlo- Chlori-
nated nated
0.1-0.7 0.5-12
0.6-0.7
<01
<1
0.3-3.8
	 	
	 	
	 	
	 	
	 	
	 	
1
2-8
	 *
0.3-3
1
10
10-150
100-560
	 *
0,4-4.6
0.1-0.3 0.1-8
* 0.2-0.3
•* *•
1-10

 ^indicates none  detected;  	  indicates no data available
                            310

-------
TABLE C.4.   TRACE ORGANIC COMPOUNDS (ng/1) IN SECONDARY EFFLUENTS
    ORANGE  COUNTY WATER DISTRICT (Pettygrove and Asano 1984)

Compound
Trihalomethane
Chloroform
Bromod ichlorom ethane
Dibromochloromethane
Bromoform
Other volatile organics
Carbon tetrachloride
Methylene chloride
1 ,1 ,1-Trichloroethane
T rich lor oethylene
Tetrachloroethylene
Chlorobenzenes
Chlorobenzene
1 ,2-Dichlorobenzene
1 , 3-Dichlorobenzene
1 ,4-D.ichlorobenzene
1 ,3,4-Trichlorobenzene
Aromatic hydrocarbons
Ethylbenzene
m-Xylene
p-Xylene
Naphthalene
1 -Methylnaphthalene
2-Me thy 1 naphthalene

Jan.
No. of
Samples

52
42
35
24

	
41
50
46
39

14
15
15
15
15

13
—
—
16
11
10

1976

- Sept.
Range

0.2
<0.1
<0.1
<0.1

	
1.7
<0.3
<0.1
<0.1

0.2
0.3
0.2
0.8
<0.02

0.2
	
	
0.1
0.1
0.4

- 3.9
- 1.1
- 10
- 3


- 74
- 38
- 12
- 15

- 9.4
- 8.9
- 1.7
- 9.2
- 4.1

- 8.7


- 4.1
- 3.9
- 2.6

1976a
Geometric
mean

1.6
0.09
0.15
0.12

	
17.0
4.7
0.9
0.6

2.5
2.4
0.68
2.1
0.46

1.4
—
—
0.57
0.86
1.0

Mar .
No. of
Samples

28
27
28
23

28
--
28
—
28

27
27
26
26
27

25
24
24
27
27
27

1978 -
Range

0.8 -
0.2 -
0.2 -
0.1 -

<0.1 -
	
0.2 -
	
0.2 -

<0.02 -
0.07 -
<0.02 -
0.07 -
<0.02 -

<0.02 -
<0.02 -
<0.02 -
<0.02 -
<0.02 -
<0.02 -

Oct.


17
3.2
1.8
6.4

0.1

15

9.5

1.1
13
5.4
15
3.1

0.5
0.2
0.04
0.54
0.89
0.18

1978
Geometr ic
Mean

2.9
0.6
0.71
0.37

<0.1
—
2.9
—
1 .5

0.11
0.63
0.17
1.9
0.18

0.039
0.027
0.016
0.065
0.004
0.018
                                                                     (cont inuedT

-------
    Table C.4, continued


Compound
Solvent extractablesb
Dimethylph thai ate
Diethylphthalate
Oi-n-butylph thai ate
Di-isobutylph thai ate
Bis-[2-ethylhexyl]phthalate
PCB (as Aroclor 1242)
Lindane
Jan.
No. of
Samples

3
11
3
11
11
11
10
1976

- Sept .

Range

14.7
<2
0.5
<0.3
15
2
<0.1

- 18.7

- 0.5
- 16
- 65
- 7.6
- 0.6
1976a
Geometric
mean

0.6
<2.0
<0.5
2.9
28.0
3.3
0.19
Mar .
No. of
Samples

25
25
24
25
25
25
25
1978 -

Range

0.8 -
<0.3 -
<0.5 -
<1
<4
<0.3 -
0.09 -
Oct.



14
12
3.4
10
62
1.3
0.
. 1978
Geometric
Mean

5.4
<0.3
0.75
4.4
9.3
0.47
19 0.15

N3
    a.   Period  from Oct.  1976  to  Mar.  1978  trickling  filter  effluent,  period  from  Mar.  1978 to  Oct.  1978
        activated  sludge  treatment  with segregation of wastewaters  to  reduce  industrial inputs.

    b.   One  liter  of sample  extracted  with  2  x  15  ml  of hexane,  dried  with  sodium  sulfate, concentrated to
        2 ml, and  cleaned on a Florisil column  before analysis.

-------
TABLE C.5.   HANCOCK WELL WATER SAMPLES WHICH EQUALLED OR EXCEEDED DRINKING WATER STANDARDS

Parameter
N03-N
Baseline*
Well #
21234
10211
20112
21141
20842
10842
30312
i 40331
' 21323










Freq*
2/6
1/6
2/6
2/6
2/5
1/7
1/6
1/6
1/5











Se
Irrigationt Baseline* Irrigat
Well # Freq* Well #




20842 3/5 20842
10842
30312
40331
21323 1/4
21152 4/7
10112 1/5
10731 4/7
10931 2/5 10931
10821 1/5 10821
10932 1/11
40311
40421

20243 1/6
Freq* Well #


20112
21141
1/5
1/7
1/6
1/6 40331




2/5
2/6
10932
2/5 40311
2/5 40421
20721

Cd
iont Baseline* Irrigationt
Freq* Well # Freq* Code Freq*


1/5
2/4



1/5






2/11
2/4
1/5
2/4 20721 1/6

                                                                                      (cont inued)

-------
Table C.5,  continued
Parameter Pb Cl
Baseline* Irrigationt Baseline* Irrigationt Basel
Well # Frecf Well # Freq» Well // Freq» Well # Freq» Well #
21234 21234
10211
20112
21141
20842
10842
30312 2/5 30312
40331
21323
21152
10112
10731
10931
10821 1/6 10821
10932
40311
40421 1/5 40421
20721
10521 1/5 10521
10542
20243
10232
10721 2/5 10721
11032
20711
40231
10541
Fe
ine*
Freq*
1/6
1/6
2/6
2/6
2/5
2/7
2/6
2/6
2/5
1/1
1/6
1/1
2/5
2/6
1/1
2/5
2/5
3/6
3/5
2/5
3/6
2/5
2/5
1/5
2/5
3/6
2/5

Irr igat
Well #
21234
10211
20112
21141
20842
10842
30312
40331
21323
21152
10112
10731
10931
10821
10932
40311
40421
20721
10521
10542
20243
10232
10721
11032
20711
40231
10541

iont
Freq*
4/5
3/4
3/5
3/4
3/5
3/4
4/5
3/5
4/4
4/7
3/5
4/7
4/5
2/5
4/11
4/4
V5
2/4
3/5
3/4
3/4
3/5
3/5
4/5
4/4
3/4
4/4
                                                                                                       (continued)

-------
TABLE C.5, continued
Parameter


Mn S0{±
Baseline*
Well #
21234
10211
20112
21141

30312
40331
21323
21152
10112
10731
10931

10932

40421
20721
10521
10542
20243
10232
10721
11032
20711
40231
10541
Freq*
2/6
2/6
2/6
3/6

4/6
5/6
3/5
1/1
2/6
1/1
2/5

1/1

1/5
5/6
4/5
3/5
4/6
1/5
2/5
3/5
4/5
5/6
1/5

TDS
Irrigationt Baseline* Irrigation+ Baseline* Irrigation+
Well #
21234


21141
20842
30312
40331
21323
21152

10731
10931
10821
10932
40311


10521
10542
20243

10721
11032
20711
40231
10541
Freq* Well # Freq* Well # Freq» Well #
3/5


2/4
2/5
4/5 30312
1/5
3/4
2/7

2/7 10731 1/7
2/5 10931 2/5
2/5 10821 1/6 10821 1/5 10821
2/11
1/4


3/5
3/4
1/5

3/5 10721 2/5
1/5
4/4
4/4
3/4
Freq* Code Freq*





2/6 30312 2/5




10731 1/7

1/6 10821 1/5


40421 1/5











*Baseline Period = June 1980 to February 1982
tlrrigation Period = February 1982 through October 1983
^Frequency = Number of sampling periods the well water exceeded drinking water standards  for  a  specific  parameter/
             number of sampling periods for that well

-------
                          TABLE C.6.   HANCOCK FARM,
SIGNIFICANT DIFFERENCES BETWEEN BASELINE AND POST-BASELINE  WELL  WATER  QUALITY

Parameter Alk Cond IDS Ph Cl SO, TKN NO, NH, TP OP OKP COD TOC
Well No.
10112 *_
10211 *+ *_
10521 *+
10542 *-+
10931 * +
20112 * + *_ *_
20243 *_ *_
20743
20721 *--
21141 *_ *_
40331 * +
10232 ^._
10721 •*+ *+ * +
10821 *- *+ #- *-
10842
11032
20711
20842
21323
30312 ^+ #_ >+ ^_ ^+
40231 #_
40421
21234 ^_ ^_
40311
10541 _ ^-_
21152 * +
10731 *+ ^-i- -a--)- -X-J-

TC FC FS Al
* denotes stat ibtiual ly
significant Ui rfel'ciicuii
*+ *+ yreater than baseline
well water quality
parameter
- denotes post-baseline
less than baseline well
water quality parameter

-------
 Table   C.6  ,  continued




Parameter	As     Ba     B     Ca     Cd     Co     Cr    Cu     Fe     Pb     Mg     l-ln     Hg     Mo    Hi     K     Se     Ag

Well No.

10112

10211

10521                *-

10542                                                *+

10931                                                               * +                              *-

20112

20243                *-

20721                «_
                                                                                                           -*-
21141

40331                *-

10232

10721                             *+                               *+           *+    *+                              *+

10821                                                       -X—                  -X—

10842

11032

20711                                                               *+

20B42

21323

30312                                                               *+           *~    *+

40231

40421                                                       *+

21234                                                               *+

40311

10541

21152                *-          *-                       *-                  *-    *-

10731                -X--          *-                                            *+    *-

10932                                                *-    *-                                                        *~   *+

-------
        Table  c.6,      continued
                                                                                     Jcu  .-t   a,              -it   c   o   f*                             --»
                                                                                     .*j   CD  -iJ               u   a   c   £                             x
                                                                                     to  .c   CD               cc   u   a   .C  <-i  <-«                      .c



Well
Nuntier
£
1 £
.C O
U
c x

< .
4-*

J

O
(D
(H
41
»—
8
t;
(C

.H «
3 £
§ £
l< -ft
i-t U
O «-(
1 £


o
Ik
1*
t-\
j;

o
1
&

V

(C
*J
o
u

1

(D
•C
a
•4-1
•H
C
S
o
tH
i
O
•a


S t £
O N N
L. C C
*"^ ,
•1-1 -l-l -fcj
Q ° ^

u
0
o
j:
CD
t-
OJ


0>
fc
^-)
o

&
£
o
u
o
_c
(J
•H
1-4

>,
i
4-J
0
M
o
r
o
u.

 10112         *+        %+                                                         * +



 10211                                                                               * +



 10521                * +




 10542



 10931                   * +




 20112




 20243



 20721                                                                                                              * +



 21141




 40331



 10232




10721



10821



10842                                                                              * +




11032



11032                         *+ *~



20711




20842



21323                                                     *+                      * +




30312                                                *+  *+                      * +



40231                                                *~                                                            *~




40421



21234                                                                                                               *+                             * +



40311                                                    '^ +



10541         *+                                          *+                                                                                * +




i]j52                *-      *-- *-                *-  *~         *~                                     *-    *~             *~



 10731                                  .*+       *+                                                                * +


 10932

-------
                                                       Table C.7
    Simple Statistical Values of Groundwater Inorganics,  Physical and  Organic Parameters  Present  in Ground
      Water Beneath Hancock  Farm During the Baseline Monitoring  Period (June  1980  to February 1982)
VO
         •BLL      iLKllIBITY      COBDOCTIYITT
                  K CIC03/L
        •••»*••**••••••«»»•«**•*«***»»»*»•»•«»•«
        10112  IT'    295.            694.
              SO    ( 29.)           {  55.)
              S    <-0.75>           < 0.23>
              (ID    302.            690.
  769.
(  53.)
<-0.13>
  774.

  739.
( 189.)
<-1.07>
  819.

  969.
( 462.)
< 0.84>
  842.

 1067.
( 299.)
<-0.31>
 1080.

  872.
( 113.)
<-0.90>
  914.

  787.
                                     818.

                                     991.
                                   (  168.)
                                   <  0.55>
                                     962.

                                    1151.
                                   (  196.)
                                   <-0.85>
                                    1205.

                                    1021.
                                   (  172.)
                                   <-0.44>
                                    1060.
10211



10521



10542



10931



20112



20243



20721



21141



40331



IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
BD
IT
SD
S
HD
IT
SD
S
no
IT
SD
S
no
IT
SD
S
HD
IT
SD
S
HD
310.
( 6.)
< 0.05>
310.
260.
( 45.)
<-0.90>
296.
321.
( 16.)
< 1.09>
315.
297.
( 9.)
<-0.00>
296.
311.
( 18.)
<- 1.1 2>
319.
306.
( 11.)
< 0.31>
304.
299.
( 15.)
< 1.05>
293.
278.
( 10.)
< 0.98>
268.
278.
( 26.)
< 0.82>
271.
TDS
.10/1
465.
( 47.)
< 1. 11>
443.
503.
( 14.)
< 0.32>
501.
462.
( 115.)
<-1 . 01>
508.
628.
( 223.)
< 1.07>
534.
749.
( 169.)
<-0. 18>
785.
605.
( 32.)
< 0.27>
601.
501.
( 26.)
<-0.92>
510.
670.
( 106.)
< 1 . 01>
631.
765.
( 122.)
<- 1. 06>
816.
690.
( 80.)
<-0. 58>
713.
PR

7.68
(0.28)
< 0.84>
7.59
7.61
(0.31)
< 0.16>
7.59
7.61
(0.23)
< 0.70>
7.54
8.14
(0.10)
< 0.85>
8.11
7.69
(0.21)
< 0.62>
7.60
7.64
(0.33)
< 0.17>
7.62
7.61
(0.16)
< 0.48>
7.57
7.67
(0.27)
< 0.40>
7.63
7.64
(0.31)
< 0.57>
7.S6
7.82
(0.18)
<-0.07>
7.B3
CL
BG/L
17.
( 8.)
< 0.52>
16.
21.
( 2.)
<-0.69>
22.
28.
( 8.)
<-0.81>
31.
94.
( 89.)
< 0.94>
60.
27.
( 12.)
<-0.05>
29.
40.
( 35.)
< 1.15>
24.
34.
( 5.)
< 1.05>
33.
96.
( 57.)
< 1.06>
72.
119.
( 46.)
<- 1.01>
137.
86.
( 39.)
<-0.78>
97.
S04
HG/L
66.
( 33.)
< 0.08>
65.
67.
( 2.)
< 0.0 >
67.
76.
< 11.)
< 0.0 >
76.
72.
( 11.)
< 1.1 4>
67.
208.
(124.)
<-0.26>
230.
104.
( 18.)
<-1.03>
112.
78.
( 6.)
<-0.73>
79.
93.
( 7.)
< 0.1 8>
92.
147.
( 68.)
<-0. 12>
150.
158.
( 40.)
<-0.97>
174.
TOT1L 1
HG HA
0.49
( 0.42)
< 0. 12>
0.45
0.59
( 0.36)
<-0. 05 >
0.60
0.28
( 0. 14)
<-0. 17>
0. 28
0.49
( 0.40)
< 1. 14>
0.30
0. 3»
( 0.11)
< 0. 46 >
0.3)
0.38
( 0. 37)
< 0. 71 >
0.26
0.42
( 0.28)
< 0. 81>
0.33
0.29
( 0.25)
< 1.02>
0.20
0.4)
( 0.31)
< 0.27>
0.47
0.32
I 0.13)
< 0. 35 >
0. 30
»02/B03
BG «/l
5.57
( 3.89)
< 1.00>
4.86
2.62
( 1.99)
<-0.20>
2.89
0.52
( 0.55)
< 1.15>
0.39
1.54
( 1-47)
< 0.07>
1.48
9.25
< 2.35)
<-0. 11>
9.62
4.21
( 2.86)
<-0.30>
5.00
1.39
( 0.61)
< 0.26>
1.27
2.42
< 2.29)
< 0.52>
1.91
3.44
( 3.76)
< 0.44>
2.61
2.70
'( 2.18)
<-0.27>
3.59
NH3
HG M/L
0.03
( 0.02)
< 0.43>
0.02
0.03
( 0.03)
< 0.82>
0.02
0.07
( 0.07)
< 0.44>
0.06
0.06
( 0.03)
< 0.13>
0.06
0.03
< 0.03)
< 1. 43>
0.01
0.05
( 0.04)
< 0. 87>
0.03
0.04
( 0.03)
< 0. 37>
0.03
0.07
( 0.08)
< 0.57>
0.05
0.25
( 0.38)
< 1. 13>
0.08
0. 10
( 0.06)
< 0.00>
0.10

-------
     Table  C.7,  continued
N3
O
 10232  AV
        SD
        S
        (ID

 10721  AT
        SD
        S
        no

 10821  AT
        SD
        S
        ND

 10842  AT
        SD
        S
        no

 11032  AT
        SD
        S
        ND

20711   AT
        SD
        S
        HO

20842   AT
        SD
        S
        HO

21323   AT
        SD
        S
        (ID

30312   AT
        SO
        S
        no

40231   AT
        SD
       -S
        HO

40421   AT
        SD
        S
        (ID
         21234
                AT
                SD
                S
                HD
   280.
  (   9.)
 :  0.44>
   277.

   319.
  (  15.)

   315.

   258.
  (  12.)

   263.

   282.
  301.

  211.
  ( 18. )
  0.36>
  278.

  245.
  ( 35.)
  1.84>
  231.

  319.
  {  6.)
  0.75>
  319.

  268.
  269.

  231.
 (  6.)
< 0.54>
  231.

  283.
 ( 29.)
< 0.63>
  271.

  243.
 ( 12. »
<-0.27>
  247.

  272.
 ( 17.)
<-0.19>
  275.
                                           7flO.
                                           790.

                                           846.
                                         (   65.)
                                         <  0.35>
                                           R20.

                                          1225.
                                         t  213.)
                                         <  0.82>
                                          1180.

                                           732.
  760.

  796.
( 129.)
<-0.fiO>
  810.

 1038.
(  93.)
<-0.52>
 1090.

  630.
{  57.)
<-0.25>
  640.

 1130.
(  98.)
< 0.27>
 1990.

 1287.
( 115.)
<-0.72>
 1325.

 1022.
( 164.)
< 0.08>
 1030.

 1076.
( 166.)
<-1.01>
 1100.

  762.
< 128.1
< 0.60>
  750.
6J3.
( JO.)
< 0.31>
632.
604.
( 74.)
<-0.58>
651.
902.
f 96.)
< 0.57>
B64.
570.
( 25.)
< 0.67>
570.
6U1.
( 62.)
<-0.25>
661.
732.
( 18.)
<-0.4B>
736.
511.
( 23.)
<-1.32>
517.
843.
( 37.)
< 0.83>
830.
989.
( 42.)
< 0.49>
974.
774.
( 64.)
< 0.98>
761.
759.
( 98.)
< 0.12>
745.
601.
( 1«8.)
< 1.60>
547.
7.59
(0. 14)
< 0.57>
7.57
7. MO
(0.08)
<-1.04>
7.H2
7.48
(0.17)
< 0.51>
7.42
7.83
(0.18)
<-O.OU>
7.79
7.43
(O.OB)
< 0.37>
7.41
7.66
(0.13)
< 0.61>
7.62
7.52
(0.17)
< 0.09>
7.48
7.46
(0.09)
<-0.73>
7.49
7.48
(0.17)
< 1.36>
7.43
7.43
(0.08)
<-1. 17>
7.46
7.32
(0.15)
<-0.30>
7.40
7.63
<0.27)
< 1.
7.53
89.
(13.)
<• 0.77>
87.
125.
( 72.)
< 0.34>
116.
201.
(127.)
< 0.62>
161.
57.
( 11.)
< 0.22>
60.
123.
( 67.)
< 1.01>
1T6.
224.
( 27.)
< 0.48>
226.
41.
( 33.)
< 1.46>
27.
192.
( '•)
< 0.11>
194.
215.
( 85.)
<-1.65>
254.
147.
( 38.)
<-0.47>
150.
246.
(115.)
< 0.94>
192.
56.
( 15.)
< 0.32>
53.
   92.
 ( 10.)
<-0.59>
   94.

   83.
 ( 17.)
<-0.34>
   91.

  243.
 ( 57.)
< 0.50>
  227.

   71.
 (  7.)
< 1.17>
   70.

   87.
 ( 33.)
<-0.57>
  103.

   75.
 ( 31.)
<-0.36>
   77.

   69.
 ( 67.)
< 1.44>
   43.

  131.
 ( 22.)
< 0.42>
  129.

  175.
 ( 73.)
<-1.21>
  211.

  113.
 ( 39.)
<-0.09>
  111.

  108.
 ( 13.)
< 0.35>
  101.

   93.
 ( 15.J
<-0.86>
   98.
                                                                                                          0.9)
                                                                                                        (  0.96)
                                                                                                        <  1. 26>
                                                                                                          0. 60
  1. 19
( 1.79)

  0.35

  0.54
( 0.47)
< 1. 40>
  0.39

  0.79
( 1.14)

  0.32

  0.67
( 0.68)
< 0.93>'
  0.62
  4.21
( 5.011
< 0. 56 >
  2.85

  1.42
( 1.20)
<-0. 14>
  1.53

  0.41
( 0.34)
< 0.37>
  0.21

  0.85
( 0.62)
< 0. 83 >
  0.61

  3.66
( 4.501
< 1. 36>
  1.82

  0.39
( 0.61)
< 1.44>
  0. 15

  0.71
( 0.87)
< 0.77>
  0.21
  2.80
(  2.25)
<  0.30>
  2.10

  2.52
(  1.66)
<-0.55>
  3.05

  2.14
(  1.72)
<  0.99>
  1.67

  4.10
(  5.41)
<  1.46>
  2.01

  2.06
(  1.68)
< O.i27>
  1.74

  2.90
(  1-77)
<-0.05>
  3.21

  8.37
( 4.03)

  9^61

  7.92
( 5.15)
< 0.70>
  6.91

  5.94
( 3.22)
<-0.42>
  6.20

  2.52
( 1.87)
< 0.41>
  2.24

  4.57
( 2.30)
K-1.23>
  5.33

  6.54
(  5.50)
<  0.21>
  6.05
  0.08
( 0.06)
< 0.13>
  0.07

  0.20
( 0.35)
< 1. 41>
  0.01

  0.03
I 0.03)
< 0.73>
  0.01

  0.06
( 0.06)
< 0.32>
  0.04

  0.19
( 0.18)
< 0. 28>
  0.12

  0.37
( 0.60)
< 1.07>
  0.11

  0.05
( 0.07)
< 1.14>
  0.02

  0.08
( 0.05)
< 1.50>
  0.06

  0.08
 ( 0.06)
< 0. 21>
  0.08

  1.36
 ( 1.10)
< 0. 36>
  1.25

  0.03
 ( 0.02)
< 0.04>
  0.03

  0. 26
( 0.49)
< 1.74>
  0.07

-------
        Table C.7, continued
         0031 1
         10541
         21152
         10731
         10932
AT
SO
S
HD

AT
3D
S
HD
  257.
 (  17.)
< 0.81>
  248.

  290.
 (   6.)
<-0.05>
  290.
               AT     284.
               3D    (  0.)
               S    < 0.0 >
               no     ••*•
                      330.

                      0.0 >
AT
SO
S    <
no
                AT     349.
                SO    (  0.)
                S    < 0.0  >
                RD     ****
                                      1016.
                                     (  134.)
                                     <-1. 11>
                                      1050.
  660.
   49.)
  0.50>
  640.

  550.
    0.)
  0.0 >
 *****
  530.
(    0.)
<  0.0  >
 *****

  750.
(    0.)
<  0.0  >
 *****
791.
( 39.)
<-0. 3fl>
790.
541.
( 15.)
< 0.23>
536.
509.
( 0.)
< 0.0 >
*****
514.
( 0.)
< 0.0 5
*****
598.
( 0.)
< 0. 0 >
*****
7.M
(0.26)
< 1.27>
7.41
7.46
(0.13)
< 1.18>
7.40
7.59
(0.0 )
< 0.0 >
****
7.92
(0.0 (
< 0.0 >
**•*
7. '37
(0.0 )
< 0.0 >
****
175.
( 28.)
< 0.06>
176.
58.
( 12-)
< O.U1>
50.
63.
( 0-)
< 0.0 >
****
41.
( 0.)
< 0.0 >
****
88.
( 0.)
< 0.0 >
»***
147.
( 1«.)
< 0.00>
147.
72.
( 17.)
<-1.25>
77.
98.
( 0.)
< 0.0 >
****
32.
( o->
< 0.0 >
****
82.
( o.)
< 0.0 >
****
0. JO
( 0.11)
< 0.0} >
0.30
0.36
( 0.30)
< 0. 54>
0.23
1.80
( 0.0 )
< 0. 0 >
*****
0.49
( 0.0 )
< 0. 0 >
**»»>
0. 10
< 0. 0 )
< 0. 0 )
****•
4.44
( 2.44)
<-0.60>
5.70
1.03
( 0.92)
< 1.07>
0.50
1.57
( 0.0 )
< 0.0 >
*****
0.79
( 0.0 )
< 0.0 >
*****
0.83
( 0.0 )
< 0.0 >
*****
0.0 J
( O.J3)
< l.23>
0.01
0.04
( 0.05)
< 1.26>
0.03
0.16
( 0.0 )
< 0.0 >
*****
0.22
( 0.0 )
< 0.0 >
*****
0.05
( 0.0 )
< 0.0 3
*****
hO
           * AV  = Arithmetic Average
             SD  = Standard  Deviation
               S  = Skewness
             MD  = Median  Value

-------
                                                       Table  C.8

    Simple  Statistical  Values  of Groundwater  Inorganics, Physical  and  Organic  Parameters  Present in  the
Ground Water Beneath the Hancock  Farm After  the Baseline Monitoring Period  (February 1982 to  October 1983)
      •ILL      »LK»LI»ITT
                HG CtCOl/L
      ••••*»««•««•»••••«•*•*•••
      10112  »T'    295.
            SD    ( 29.)
            S    <-0.75>
            ND    302.
      10211
      10521
      105*2
      10931
     20112
AT
3D
S
no
            IT
            SD
            S
            HD

     202*3  IT
            SD
            S
            HD

     20721  IT
            SD
            S
            no

     211*1  AT
            SD
            S
            no

     10331  AT
            SD
            S
            no
                  310.
                  (  6.)
                  0.05>
                  310.
AT     280.
SO    ( 45.)
S    <-0.90>
HD     296.

AT     321.
SD    ( 16.)
S    <  1.09>
HD     315.

IT     297.
SD    ( 9.)
S    <-0.00>
HD     296.
      311.
      ( 18.)
     <-1.12>
      319.

      306.
      ( 11.)
     < 0.31>
      304.

      299.
      ( 15.)
     < 1.05>
      293.

      278.
      ( 30.)
     < 0.98>
      268.

      278.
      ( 26.)
     < 0.82>
      271.
COUDDCTITITT

694.
( 55.)
< 0.23>
690.
769.
( 53.)
<-0. 1 3>
774.
739.
( 189.)
<- 1.07>
819.
969.
( 462.)
< 0.84>
842.
1067.
( 299.)
<-0.31>
1080.
872.
( 113.)
<-0.90>
914.
787.
( 78.)

818.
991.
( 168.)
< 0.55>
962.
1151.
( 196.)
<-0.85>
1205.
1021.
( 172.)
<-0.44>
1060.
TDS
.1G/L
465.
( 47.)
< 1.1 1>
443.
503.
( 14.)
< 0.32>
501.
462.
( 115.)
<-1 . 01>
508.
628.
( 223.)
< 1 . 07>
534.
749.
( 169.)
<-0. 1B>
785.
605.
( 32.)
< 0.27>
603.
501.
( 26.)
<-0.92>
510.
670.
( 106.)
< 1 . 01>
631.
765.
( 122.)
<- 1 . 06>
816.
690.
( 80.)
<-0.58>
713.
PH

7.68,
(0.28)
< 0.84>
7.59
7.61
(0.31)
< 0.16>
7.59
7.61
(0.23)
< 0.70>
7.54
8.14
(0.10)
< 0.85>
8.11
7.69
(0.21)
< 0.62>
7.60
7.6*
(0.33)
< 0.17>
7.62
7.61
(0.16)
< 0.48>
7.57
7.67
(0.27)
< 0.40>
7.63
7.64
(0.31)
< 0.57>
7.56
7.82
(0.18)
<-0.07>
7.83
CL
HG/L
#**## $»*#$#<
17.
( 8.)
< 0.52>
16.
21.
( 2.)
<-0.69>
22.
28.
( 8.)
<-0.81>
31.
94.
( 89.)
< 0.94>
60.
27.
( 12.)
<-0.05>
29.
40.
( 35.)
< 1.15>
24.
34.
( 5-)
< 1.05>
33.
96.
( 57.)
< 1.06>
72.
119.
( 46.)
<-1.01>
137.
86.
( 39.)
<-0.78>
97.
S04
HG/L
'•••••4t+t#Vt
66.
( 33.)
< 0.08>
65.
67.
( 2.)
< 0.0 >
67.
76.
( ID
< 0.0 >
76.
72.
( 11.)
< 1.1 4>
67.
208.
(124.)
<-0.26>
230.
10*.
( 18.)
<-1.03>
112.
78.
( 6.)
<-0.73>
79.
93.
( 7.)
< 0.1 8>
92.
147.
( 68.)
<-0. 12>
150.
158.
( 40.)
<-0.97>
174.
TOTAL 1
(IG HA
0.49
( 0.42)
< 0. 12>
0.45
0.59
( 0-36)
<-0. 05 >
0.60
0.28
( 0. 14)
<-0. 17>
0.23
0.49
( 0.40)
< 1. 14>
0.30
0.34
( 0.11)
< 0. 46 >
0.31
0.38
( 0.37)
< 0. 71 >
0.26
0.42
( 0.23)
< 0. 81>
0.33
0.29
i 0.25)
< 1.02>
0.20
0.41
( 0.31)
< 0. 27>
0.47
0.32
( 0. 131
< 0. 35 >
0.30
H02/H03
HG i/L
5.57
( 3.89)
< 1.00>
4.86
2.62
( 1-99)
<-0.20>
2.89
0.52
( 0.55)
< 1.15>
0.39
1.54
{ 1.47)
< 0.07>
1.48
9.25
< 2.35)

9^62
4.21
( 2.86)
<-0.30>
5.00
1.39
( 0.61)
< 0.26>
1.27
2.42
( 2.29)
< 0.52>
1.91
3.44
( 3.76)
< 0.44>
2.61
2.70
( 2.18)
<-0.27>
3.59
                                                                                                       NB3
                                                                                                      HG  H/L
  0.03
( 0.02)
< 0. 43>
  0.02

  0.03
< 0.03)
< 0. 82>
  0.02

  0.07
( 0.07)
< 0.44>
  0.06

  0.06
( 0.03)
< 0. 13>
  0.06

  0.03
( 0.03)
< 1. 43>
  0.01

  0.05
 ( 0.04)
< 0. 87>
  0.03

  0.04
 ( 0.03)
< 0.37>
  0.03

  0.07
 I 0.08)
< 0.57>
  0.05

  0.25
 ( 0.38)
< 1.1 3>
  0.08

  0. 10
 ( 0.06)
<• o.oo>
  0. 10

-------
      Table  C.8,  continued
        10232
10721
CO
       AT
       SD
       S
       no

       if
       SD
       S
       HD
10821  if
       SD
       S
       no

10842  if
       SD
       S
       RD

11032  if
       SD
       S
       HD

20711  if
       SD
       S
       HD

20842  if
       SD
       S
       no

21323  if
       SD
       S
       no

30312  if
       SD
       S
       HD

40231  if
       SD
       S
       HD

40421  if
       SD
       S
       no

21234  if
       SD
       S
       HD
  276.
 ( 12.)

  281.

  282.
 ( 99.)
< 0.24>
  211.

  285.

<-0.80>
  309.

  319.
 (  3.)

  320.

  272.

< 1.10>
  270.

  289.
 ( 38.)
< 0.77>
  280.

  292.
 (  6.)

  293.

  273.

< 0.28>
  272.

  382.
 (116.)
< 0.41>
  357.

  284.
 ( 21.)
< 0.06>
  283.

  238.
 (  7.)
< 0.57>
  237.

  274.
  ( 15.)
< 0.55>
  270.
  920.
 (  56.)
<-0.32>
  930.

 1933.
 (1103.)
< 0.66>
 1550.

  951.
 ( 175.)
< 1.20>
  890.

  879.
 (  63.)
<-0.72>
  894.

  974.
 ( 162.)
<-0.01>
  975.

 1085.
 ( 281.)
<-0.67>
 1170.

  968.
 ( 119.)
 <-0.77>
 1000.

 1368.
 ( 127.)
 <-1.06>
 1416.

 1632.
 ( 194.)
 <-0.77>
 1690.

 1258.
 ( 364.)
 <-0.71>
 1346.

 1445.
 ( 179.)
 <-0.00>
 1445.

  763.
 (  76.)
 < 0.47>
  730.
716.
( 271.)
< 1.«8>
611.
1250.
( 6B2.)
< 0.56>
1021.
674.
( 256.)
< 1.146*
575.
592.
( 54.)
< 0-i»8>
584.
644.
( 17.)
<-1.03>
650.
663.
( 114.)
<-1.04>
706.
631.
( »7.J
<-0.38>
639.
867.
{ 44.)
<-0.64>
881.
975.
( 145.)
< 0.17>
964.
848.
( 107.)
< 0.06>
846.
953.
( 110.)
< O.W>
934.
<182.
( 71.)
< 0.38>
««2.
7.76
(0.38)
< 0.05>
7.76
7.56
(0.25)
<-0.11>
7.59
7.83
(0.24)
< 0.98>
7.78
7.96
(0.15)
< 0.30>
7.95
7.54
(0.07)
<-0.»7>
7.55
7.77
(0.15)
<-0.20>
7.79
7.46
(0.13)
<-0.26>
7.47
7.69
(0.25)
< 0.61>
7.61
7.73
(0.24)
< 0.00>
7.73
7.65
(0.25)
< 0.68>
7.58
7.33
(0.14)
< 0.01>
7.33
7.73
(0.28)
< 0.«3>
7.73
76.
( 23.)
<-1. 14>
87.
345.
(270.)
< 0.66>
277.
86.
(113.)
< 1.50>
37.
65.
( 18.)
<-0.07>
65.
129.
( 7.)
< 0.72>
127.
183.
( 62.)
<-1.01>
207.
55.
I 5.)
< 1.05>
53.
200.
( 22.)
< O.I2>
198.
295.
( 59.)
<-0.12>
298.
205.
( 73.)
< 0.06>
204.
269.
( 9.)
< 0.57>
267.
1)6.
( 15.)
<-0.40>
45.
                                                                                              98.
                                                                                             ( 38.)
                                                                                           <  1.10>
                                                                                              82.

                                                                                              271.
                                                                                             (250.)
                                                                                           <  0.77>
                                                                                              183.

                                                                                              147.
                                                                                             ( 98.)
                                                                                           <  1.47>
                                                                                              105.

                                                                                              68.
                                                                                             (  6.)
                                                                                           <  0.13>
                                                                                              68.
                                                                                    (  6.)
                                                                                   < 0.76>
                                                                                      86.

                                                                                      48.
                                                                                    ( 18.)
                                                                                   <-0.62>
                                                                                      53.

                                                                                      98.
                                                                                    ( 30.)
                                                                                   <-0.59>
                                                                                     104.

                                                                                     132.
                                                                                    ( 35.)
                                                                                   < 0.14>
                                                                                     130.

                                                                                      96.
                                                                                    ( 75.)
                                                                                   < 0.24>
                                                                                      87.

                                                                                     114.
                                                                                    ( 20.)
                                                                                   <-0.81>
                                                                                     121.

                                                                                     104.
                                                                                    < 23.)
                                                                                   < 0.00>
                                                                                     104.

                                                                                      83.
                                                                                    (  27.)
                                                                                   < 0.10>
                                                                                      84.
   0. 27
 (  0. 34)
 <  1. 15>
   0. 10

   2.97
 (  3.52)
 <  1.21>
   1.42

   0.27
 (  0.27)
 <  1. 31>
   0.12

   0.59
 {  0.31)
 <  0. 15>
   0.56

   0.74
 (  0.13)
 <  0. 76>
   0.73

   4.03
 <  3.55)
 <  0. 69>
   3.09

   0.82
 (  0.90)
 <  0. 62>
   0.56

   0.32
 (  0.12)
 <  0. 50 >
   0.30

 24.89
 (21.27)
<  0. 32>
 21.26

   2.37
 (  1.86)
<  0. 18>
   2.15

  0. 35
 ( 0.26)
< 0. 74>
  0.28

  0.54
 ( 0.451
< 0. 98 >
  0. U4
   3.IS
 ( 4-30)
 < 1.10>
   1.58

   2.59
 ( 2.50)
 < 0.21>
   2.73

   3.82
 ( 8.11)
 < 1.50>
   0.26

   2.21
 ( 1.61)
 < 0.37>
   1.94

   2.48
 ( 1-31)
 <-0.07>
   2.63

   0.30
 (  0.22)
 <-0.42>
   0.32

  10.07
 (  2.20)
 <-0.25>
  10.70

   8.39
 I  2.48)
 <-0.66>
   8.91

   0.10
 (  0.11)
<  0.97>
   0.06

   2.69
 (  1-77)
<-0.42>
  2.91

  4.47
 (  3.76)
< 0.30>
  5.00

  0.87
 ( 0.85)
< 0.53>
  0.68
   0. 16
 ( 0.29)
 < 1.«6>
   0.04

   2.54
 ( 3.65)
 < 1.29>
   0.92

   0.05
 ( 0.04)
 <-0. 26>
   0.06

   0.05
 ( 0.06)
 < 1.08>
   0.02

   0.15
 (  0.08)
 <-0.37>
   0. 16

   3.07
 (  2.49)
 <  0.63>
   2.41

   0.44
 (  0.64)
 <  1.15>
   0.12

   O.It
 (  0.08)
 <  0. 36>
   0.10

 15.15
 (  9.43)
 <-0.05>
 15.50

   0.58
 (  0.60)
<  0.56>
   0.46

   0.03
 (  0.02)
<-0. 12>
   0.03

   0. 18
 (  0.11)
<  0.99>
  0. 16

-------
Table  C.8,  continued
  40311
 21152
 10731
 10932
        SD
        S
        HD
»T
SD
S
ND
       2*7.
      (  5.)
       0.07>
       2«6.
IT     289.
SD    ( 18.)
S    <-0.70>
RD     293.

»T     285.
SD    ( 21.)
S    < 0.93>
HD     280.
               297.
              ( 43.)
               1.3H>
               277.
        »T     375.
        SD    ( 43.)
        S    < 0.04>
        HD     377.
 1353.
 ( 125.)
<-0.67>
 1380.

  874.
 (  91.)
<-0.50>
  887.

  875.
 ( 231.)
<-0.22>
  960.

 1276.
 ( «03.)
<-1.33>
 1390.

  809.
 ( 354.)
< 0.91>
  795.
904.
( 36.)
<-0.24>
906.
547.
( 23.)
<-0. 91>
554.
645.
( 215.)
< 0.78>
637.
804.
( 217.)
<-0. 74>
798.
478.
( 90.)
<-1 . 06>
500.
7.-51
(0.13)
< 0.67>
7.48
7.60
(0-1M
< 1.0<4>
7.56
7.65
(0.24)
< O.f)2>
7.55
7.89
(0.41)
<-0.38>
8.07
7.88
(0.41)
< 0.28>
7.82
194.
( 13.)
< 0.16>
193.
69.
( 17.)
< 0.22>
67.
93.
( 92.)
< 0.63>
88.
143.
( 66.)
<-1 . 28>
160.
98.
(236.)
< 2.04>
8.
 168.
( 27.)
-0.10>
 170.

  72.
(  a.)
 0.70>
  70.

  56.
( 14.)
 0.21>
  59.

 161.
(102.)
 0.65>
 128.

  44.
( 16.)
 0.37>
  44.
  0. 11
( 0.04)
<-0. 51>
  0. 11

  0.30
( 0.20)
< 0. 00>
  O.JO

  0. 3S
( 0.13)
<-0. 15>
  0.35

  0.53
( 0.25)
<-0.35>
  0.61

  0.73
( 0.79)
< 0.65>
  0.38
  6.65
I 1-65)
< 0.21>
  6.49

  0.84
( 0.46)
< 0.12>
  0.79

 14.99
( 9.87)
< 0.48>
 11.42

 11.70
( 7.50)
< 0.25>
 12.57

  6.33
( 3.31)
< 0.45>
  5.53
  0.04
( 0.06)
< 1.14>
  0.01

  0.04
( 0.04)
< 0.27>
  0.03

  0.06
( 0.04)
< 0.47>
  0.06

  0.04
( 0.03)
< 1.00>
  0.02
                                                                                                                0.05
                                                                                                                0.05)
                                                                                                                0.99>
                                                                                                                0.05
         AV  = Arithmetic Average
         SD  = Standard  Deviation
          S  = Skewness
         MD  = Median Value

-------
        Table  C.9
 Hancock Wells Baseline
Phosphorus and Organics
• ELL
10112



10211



10521



10542



10931



20112



20243



20721



211*1


40331


10232

10721
10821
10842

AT*
SD
S
no
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
BO
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
no
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
no
TOTAL P
«G P/l
0.3*
( 0.34|
< 0.96>
0.25
0.58
( 0.94)
< 1.70>
0.28
0.31
( 0.21)
< 1.0*>
0.27
0.55
( 0.29)
< 1.30>
0.45
0.25
( 0.22)
< 0. 15>
0.30
0.47
( 0. 38)
< 0.03>
0.44
0.29
( 0.25)
< 0.86>
0.20
0.29
( 0.23)
< 0.58>
0.29
0.38
( 0.21)
<-0.05>
0.39
0.44
( 0.40)
< 1.00>
0.37
0.26
( 0.19)
<-0.00>
0.30 s
0.23
( 0.17)
<-0.04>
0.18
0.19
( 0.16)
< 0.00>
0.18
0.27
( 0.27)
< 0.36>
0.12
OBTHO P
BG P/L
0.05
( 0.06)
< 1.05>
0.02
0.0*
( 0.04)
< 0.78>
0.03
0.14
( 0.13)
< 0.57>
0.15
0.05
( 0.04)
< 0.37>
0.04
0.01
( 0.00)
< 1.50>
0.01
0.22
( 0.34)
< 1.68>
0.09
0.11
( 0.14)
< 1.40>
0.07
0.15
( 0.11)
< 0.31>
0.17
0. 10
( 0.13)

olo5
O.OB
( 0.05)
< 0.38>
0.07
0.03
( 0.02)
< 0.35>
0.03
0.05
( 0.05)
< 0.15>
0.05
0.02
( 0.02)
< 0.97>
0.01
0.03
( 0.03)
< 1.07>
0.01
OK3. P
HG P/L
0.26
( 0.35)
< 1. 30>
0.13
0.50
( 0.92)
< 1.69>
0.15
0. 11
( 0.12)
< 0.85>
0. 11
0.43
( 0.32)
< 1.42>
0.32
0.22
( 0.21)
< 0.31>
0.25
0.24
( 0.31)
< 0.41>
0.01
0.13
( 0.14)
< 0.39>
0.10
0.13
( 0.19)
< 1.22>
0.07
0.24
( 0.11)
< 0.92>
0.20
0.34
( 0.39)
< 1.09>
0.28
0.22
( 0. 17)
< 0.07>
0.22
0. 16
( 0.12)
flllS
0.15
( 0.15)
< 0. 15>
0.12
0.24
( 0.24)
< 0.37>
0.10
COD
BG/L
73.4
( 62.5)
<-0. 12>
94.0
56.2
{ 79.8)
< 0.89>
5.0
12.3
( 4.4)
< 0.07>
12.0
11.3
( 16-5)
< 1. 13>
4. 1
17.3
( 10.9)
< 0.90>
14. 1
•)7.6
( 87.4)
< 1.42>
17.0
116.7
(135.2)
< 0.96>
67.6
47.4
( 59.7)
< 0.94>
12.0
63.5
( 83.4)
< 1.47>
30.0
40.5
{ 38.0)
< 1.34>
26.7
31.5
( 11-8)
36.0
25.1
( 19.2)
<-0.25>
27.0
57.9
( »3.2)
< 1.05>
35.0
38.7
( 25.2)
< 0.62>
37.4
TOC
HG/L
40.5
(32.2)
< 0.07>
36.8
31.2
(21.4)
< 0.42>
21.0
22.4
(14.7)
< 0.22>
20.8
19.8
( 8.8)
<-0.04>
20.2
18. 8
(15.2)
< 0.99>
13.0
30.0
(21.4)
< 0.61>
24.6
38.9
(37.8)
< 0.73>
22.9
33. 1
(23.0)
<— 0. 1 9>
43.0
29.1
(21.9)
<-0. 19>
38. 7
29.1
(19.1)
<*0. 17>
34.0
27.5
(18.6)
< 0.10>
26. S
22.9
(12.6)
< 0.87>
19.3
22.*
(19.5)
< 0.52>
18.9
29.8
(21.4)
< 0.79>
18.0
            325

-------
Table  C.9, continued


     11032  AT     0.26           0.03         0.20          21.5          21.7
            SO   (  0.19)        (  0.04)       (  0.21)        (  16.«)        (17.0)
            S    <  0.30>        <  1.50>       <  0.60>        <  0.0  >       <  0.56>
            SD     0.29           0.01         0.11          21.5          18.8

     20711  AT     0.25           0.10         0.1H          «5.7          21.5
            SD   (  0.21)        (  0.1«)       (  0.11)        (  21.7)        (  5.5)
            S    <  0.52>        <  1.09>       <  0.22>        <  0.12>       <  0.20>
            «D     0.23           0.01         0.11           «3.3           20.9

     208«2  AT     0.29           0.03         0.26           6.6           15.3
            SD   (0.20)        (0.02)       (0.191        (  6.7)       (10.0)
            S    <  1.25>        <  0.68>       <  1.1»>       <  0.37>      < 0 39>
            BD     0.21           0.01          0.20           5.3           12.0

     21323   AT     O.«1           0.02          0.37           «6.8           19.9
            SD   (  0.33)         (  0.01)       (  0.32)       ( U2.7)       (15.3)
            S     <  O.«1>       <  0.00>       <  0.5fl>       <  1.06>      < 0.89>
            (ID     O.M           0.02          0.39          30.5           15.3

     30312   AT      0.21           0.03         0.18          H1.5          27.8
           SD    <  0-2D        (  0.01)       ( 0.23)       ( 32.2)       (15.7)
           s    <  1-»0>       <  1.69>      <  1.52>       < 0.27>      < 0.22>
           "D     0.16          0.01         0.12          28.0          23.8


    «0231  AT     0.«5          0.1J         0.26         105.9          53.3
           SO   ( 0.»6)        ( 0.15)       ( O.»3|        ( 6H.S)        (  7.2)
           S    < 0.73>        < 0.7«>      < 1.59>       < 0.72>      < 0.28>
           no     0.27          0.01         0.06          91.7          51.2

    • 0»21  AT     0.22          0.03         0.19          36.6          17.6
           SD   ( 0.15)        ( 0.03)       ( 0.13)        ( 2H.7)        (11.7)
           S    < O.»0>        <  0.«9>      <-0.11>       < O.»1>      < 0.97>
           BO     0.20          0.02         0.19          31.5          11.7

    2123*  AT     0.30          0.05         0.25          30.9          28.7
           SD   ( O.»1)        (  O.Oaj       ( O.«0)        ( 37.0)        (18.7)
           S    < 1.33>        <  0.09>      < 1.52>       <  1.00>      < 0.67>
           (ID     0.15          0.05         0.09          1».0           17.2

    H0311  AT     0.23          0.01         0.22          16.2           20.0
           SD   ( 0.20)        (  0.01)       ( 0.21)        (  17.8)        (17.0)
           S    < 0.12>        <  1.50>      < 0.09>       < 0.79>       < 0.27>
           "0     0.25          0.01         0.25          11.0           18.0

    105«1  AT     0.29          0.01         0.22          13.«           26.6
           SD   ( 0.23)        (  0.01)       ( 0. t«|        (  16.0)        (2H.O)
           S    < 0.29>        <  1.50>      <-0.51>       <  O.B9>      < 0.72>
           BD     0.28          0.01         0.26          16.0           10.8

    21152  AT     0.3*          0.06         0.07           0.0            7.6
           SD   ( o.o  )        (  o.o  )       ( o.o  )        (   o.o)        (  o.o)
           S    < 0.0  >        <  0.0  >      < 0.0  >       < 0.0  >       < 0.0 >
           no    •••**          *•»••
                                            •*•••           o.o         •••••
    10731   IT     0.08           0.01          0.01           0.0           7  1
           1°    ( 0.0 )        (  0.0 )       (  0.0 |        {  0.0)        ( 0.0)
           s     < o-o >        <  o.o >       <  o.o >        < o.o >      < o.o  >
           80    «**••         ***••        *..,.           0>0         ••«»»

    10932   "    , 9-*1           0.29          0.06           0.0          16.0
           "    ' "'? I        (  °-° )       (  0-0 )        (  0.0)        ( 0.0)
           HO    .2:2.*        <  0.0 >       <  0.0 >        < 0.0 >      < 0.0  >
           ID    ••»..         .....        .....           0>8         .,„.


AV =  Arithmetic  Average
SD =  Standard  Deviation
 S -  Skewness
MD =  Median
                                   326

-------
     Table C.10

Hancock Wells After Baseline
   Phosphorus and Organics
IBtL
• ••• ••• 4
10112



10211



10521



105*2



10931



20112



202*3



20721



211*1



00331



10232



10721



10821



108*2




fc« • •'
IT*
SD
S
SD
IT
SD
S
NO
IT
SD
S
BD
IT
SO
S
SD
IT
SD
S
NO
IT
SD
S
no
AT
SD
S
no
»v
so
3
no
IT
SD
S
BD
IT
SD
3
BD
IT
SO
S
no
AT
SD
S
BD
IT
3D
S
BO
IT
3D
S
BD

TOTIL 9
HG PA
••*•••*• •^•••44
0.07
( 0.11)
< 1.15>
0.01
1.02
( 2.02)
< 1.15>
0.01
0.23
( 0.36)
< 1.1»>
0.06
0.15
( 0.11)
< 0.76>
0.12
0.10
< 0.16)
< 1.46>
0.0*
0.1*
< 0.19)
< 0.83>
0.07
0.06
( 0.09)
< 1.15>
0.01
0.13
( 0.19)
< 1.06>
0.0*
0.20
( 0.27)
< 1.13>
0.08
0.1*
( 0.25)
< 1.15>
0.01
0.08
( 0.10)
< 0.89>
0.02
0.13
( 0.1*)
< 0.6*>
0.06
0.05
( 0.07)
< 1.31>
0.01
0.10
{ 0.17)
< 1.15>
0.01

ORTHO P
BG PA
0.05
( 0.08)
< 1.15>
0.01
0.85
{ 1.68)
< 1.1 5>
0.01
0.05
( 0.07)
< 1.15>
0.01
0.01
( 0.00)
< 1.15>
0.01
0.05
( 0.07)
< 1.39>
0.02
0.05
( 0.08)
< 1.1";>
0.01
0.06
( O.OH)
< 1.11>
O.CP
O.Ofi
( 0.09)
< 1.1»>
0.01
0.07
( 0.08)
< 0."M>
0.0*
0.05
( 0.06)
< 1. 13>
0.02
0.0*
( 0.06)
< 1.»3>
0.01
0.06
( 0.07)
< 1.31>
0.03
0.03
{ 0.03)
< 1.39>
0.02
0.07
{ 0.11)
< 1.13>
0.02
327
OiG. P
NO PA
0.02
( 0.02)
< 1. 15>
0.01
0.01
( 0.0 )
< 0.0 >
0.01
0.03
( 0.03)
< 0. «9>
0.02
0.07
( 0.08)
< 1.02>
0.0*
0.05
( 0.09)
< 1.«9>
0.01
0.03
( 0.0»)
< 1.15>
0.01
0.01
( 0.0 )
< 0.0 >
0.01
0.02
( 0.01)
< 1.15>
0.01
0.06
( 0.11)
< 1.15>
0.01
0.01
( 0.0 )
< 0.0 >
0.01
0.01
( 0.00)
< 1.15>
0.01
0.02
( 0.03)
< 1.50>
0.01
0.02
( 0.02)
< 1.50>
0.01
0.01
( 0.0 |
< 0.0 >
0.01

COD
SG/L
7.7
( 5.8)
<-0.»9>
8.8
35.8
( »1.9)
< 0.80>
23.3
32.9
( 33.7)
< 0.86>
22.0
11.2
( 5.9)
< 1.1 2>
8.6
11.0
( 1.8)
<-0.«1>
11.3
17.0
{ 26.6)
< 1.01>
6.0
17. 1
( 21-3)
< 1.1 »>
6.6
1».9
( 13.1)
< 0.29>
13.8
15.3
( 17.8)
< 0.08>
13.5
16.2
( 15.*)
< 0.51>
13.8
6.0
( «-3)
< 0.68>
5.0
31.8
( 16.8)
< 0.08>
31.*
9.6
( 6.9)
<-0.62>
11.1
6.1
( 7.7)
< 0.82>
3.8

TOC
BOA
1.*
( 0.3)
< 1.08>
1.3
1.2
( 0.9)
<-0.33>
1.3
«.5
( 5.2)
< 1.1*>
2.1
3.2
( 2.5)
< 1.13>
2. 1
3.9
( 0.6)
< O.»1>
3.9
3.0
( 2.2)
<-0.»1>
3.3
1.7
( 0.7)
<-0.51>
1.9
2.*
{ 1-6)
< 0.37>
2.2
6.7
( 7.7)
< 1.06>
3.6
». 1
( 1-9)
< 0.33>
3.8
1.5
( 0.7)
<-0.58>
1.7
*.S
( 1-7)
<-0.72>
5.0
2.7
( 2.*|
< 0.51>
1.7
10.6
(18.0)
< 1.1»>
2.*


-------
 Table C.10,  continued
      11032
      20711
      20842
      21323
      30312
AT
SD
S
BO
                    0.06
                  (  0.02)
                  <  0.00>
                    0.06
IT     0.26
SO   ( 0.22)
S    < 0.89>
BO     0.19

IT     0.0*
SD   ( 0.05)
S    < 1. 15>
NO     0.01

IT     0.13
SD   ( 0.23)
S    < 1.15>
no     0.02

IT     0.41
SD   ( 0.10)
S    <-0.63>
80     0.43
                0.02
              ( 0.01)
              < 0.00>
                0.02

                0.08
              ( 0.06)
              < 0.25>
                0.07

                0.03
              < 0.03)
              < 1.09>
                0.01

                0.03
              ( 0.0«)
              < 1.15>
                0.01

                0.13
              ( 0.08)
              <-1.02>
                0.16
               0.01
             ( 0.0 )
             < 0.0 >
               0.01

               0.04
             < 0.05)
             < 0.92>
               0.02

               0.01
             ( 0.0 )
             < 0.0 >
               0.01

               0.08
             ( 0.13)
             < 1, 15>
               0.01

               0.04
             ( 0.06)
             < 1.07>
               0.02
                35.1
              ( 27.2)
              < 0.85>
                27.6

                26.3
              (  5.7)
              <-0.82>
                27.9

                 7.6
              (  4.9)
              <-0.52>
                 8.4

                18.2
              (  9.8)
              <-0.66>
                20.9

                33.4
              ( ".4)
              < 0.93>
                27.5
    C.4
  i  2-«)
< 0.06>
    6.3

    5.3
  (  2.5)
< 0.06>
    5.3

    9.7
  (12.7)
< 1.13>
    3.8

    5.7
  (  2.3)
<-0.39>
    6.0

    9.3
 <  3.9)
< 0.85>
    8.2
40231



40421



21234



40311



AT
SD
3
no
AT
SD
S
no
AT
SD
3
no
AT
SD
S
8D
0.18
( 0.15)
< 0.25>
0.16
0.04
( 0.03)
< 0.19>
0.03
0.12
< 0.18)
< 1.36>
0.04
0.04
( 0.07)
< t, 15>
0.01
      10541  AT
             SO
             S
             HD
      21152
      10731
AT
SO
S
(ID

AT
SD
S
no
      10932  AT
             SD
             S
             SD
  0.02
{ 0.02)
< 1.15>
  0.01

  0.10
( 0.11)
< 0.91>
  0.05

  0.10
{ 0.11)
< 1.20>
  O.OB

  0.19
< 0.22)
< o.ao>
  0.05
  0.09
( 0.12)
< 0.99>
  0.04

  0.03
( 0.03)
< 1.07>
  0.01

  0.06
( 0.07)
< 1.31>
  0.0]

  0.01
( 0.03)
< 1.1S>
  0.01

  0.03
( 0.04)
< 1.12>
  0.01

  0.04
( 0.08)
< 1.50>
  0.01

  0.05
(0.07)
< 1.38>
  0.03

  0.10
i 0.12)
< 0.81>
  0.03
  0.05
 { 0.05)
< 0.02>
  0.05

  0.01
 ( 0.0 )
< 0.0 >
  0.01

  0.05
 ( 0.09(
< 1.»9>
  0.01

  0.01
 ( 0.0 )
< 0.0 >
  0.01

  0.01
 ( 0.0 )
< 0.0 >
  0.01

  0.03
 ( 0.04)
< 1.50>
  0.01

  0.02
 ( 0.01|
< 0.91>
  0.02

  0.03
 ( 0.03)
< 0.97>
  0.01
                                                            84.3
                                                          ( 31.0)

                                                            88.0

                                                            19.0
                                                          (  9.5)
                                                          < 0.65>
                                                            16.6

                                                            29.0
  10.1

  22.5
( 25.0)
< 0.30>
  18.1

   5.8
(  4.6)

   6.1

  11.0
( 11-5)
< 1.02>
   7.0

  15.2

< 0.02>
  16.0

  27.3

< 0.43>
   4.1
   15.4
  M2.S)
< 0.53>
   13.3

    4.3
  ( 3.6)
< 0.93>
    3.2

    3.3
  ( 2.1)
< 1.11>
    2.7

    6.7
  ( B.9)
< 0.96>
    3.5

    0.9
  ( 0.5)
<-o.as>
    1.0

    3.2
  ( 1.6)
<-0.26>
    3.6

    3.4
  ( 1-3)
< 0.27>
    3.3

    6.3
  C 9-6)
< t.71>
    2.3
* AV =  Arithmetic  Average
  SD =  Standard Deviation
    S =  Skewness
  MD =  Median  Value
                                       328

-------
                                                Table  C.11
                        Hancock Wells Baseline  -  Ground  Water Metal  Concentrations
     Metals,  Dissolved (mg/1)
M3
HELL
10112



10211



10521



105*2



10931



20112



202*3



20721



211*1



40331



10232




AT*
SD
S
ID
AT
SD
S
RD
AT
SD
S
FID
AT
SD
3
BD
AT
SD
S
RD
AT
SD
S
RD
AT
SD
S
ID
AT
SD
S
FID
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD
AL
0.494
(0.484)
< 1.70>
0.284
1.420
(2.849)
< 1.78>
0.290
0.799
(1.350)
< 1.46>
0.169
1.216
(1. 194)
< 0.20>
0.929
0.616
(0.710)
< 0. B5>
0.555
1.100
(0.829)
< 0.69>
0.756
1.389
(1.988)
< 1.37>
0.726
2.629
(3.993)
< 1.45>
0.623
2.316
(2.096)
< 1.39>
1.881
2.808
(5.074)
< 1.72>
0.634
0.5*5
(0.410)
<-0.23>
0.650
AS
0.007
(0.003)
< 0.88>
0.005
0.007
(0.004)
< 1.30>
0.005
0.006
(0.001)
< 1.50>
0.005
0.007
(0.004)
< 1.36>
0.005
0.013
(0.013)
< 1.37>
0.007
0.006
(0.002)
< 1.57>
0.005
0.006
(0.002)
< 1.36>
0.005
0.007
(0.005)
< 1.50>
0.005
0.005
(0.001)
< 1.79>
0.005
0.006
(0.002)
< 1.57>
0.005
0.006
(0.002)
< 1.50>
0.005
BA
0.102
(0.057)
< 0.38>
0.089
0.108
(0.057)
< 0.45>
0. 101
0.207
(0.077)
< 0.42>
0.168
0. 103
(0.051)
< 0. 14>
0.096
0.093
(0.059)
< 1.00>
0.075
0.091
(0.048)
< 0.1 5>
0.086
0.179
(0.117)
< 0.69>
0. 164
0.168
(0.050)
< 0.33>
0.157
0.13*
(0.085)
< 0.53>
0.117
0.275
(0.242)
< 1.49>
0.201
0.068
(0.021)
<-0.57>
0.066
B
0.756
(0.670)
< 0.07>
0.729
0.565
(0.404)
<-0.70>
0.775
0.818
(1.055)
< 0.67>
0.325
0.717
(0.562)
<-0. 4 1>
0.850
0.241
(0.244)
< 0.71>
0.100
0.61*
(0.796)
< 0.69>
0.211
0.458
(0.334)
<-0.29>
0.511
1. 186
(1.605)
< 0.67>
0.429
1.108
(1.506)
< 0.68>
0.385
0.673
(0.810)
< 0.65>
0.319
0.347
(0.336)
< 0.62>
0.211
CA
40.0
( 1"»-7)
< 0.31>
39.
38.8
( 20.4)

33.
36.4
( 17.9)

29.
28.6
( 17.3)
< 1.02>
19.
24.0
( 9.4)

26.
51.3
( 24.7)
< 0.32>
44.
62.2
( 60.8)
< 1.49>
37.
46.2
( 40.9)
< 1.47>
33.
53.7
( 20.1)
< 0. 1 2>
54.
49.7
( 23.6)
< 1. 10>
4U.
33.0
( 1J.O)
< 0.0 >
33.
CD
0.001
(0.001)
< 1.79>
0.000
0.001
(0.002)
< 1 . 71>
0.001
0.000
(0.0 )
< 0.0 >
0.000
0.001
(0.001)
< 1. 15>
0.000
0.001
(0.001) •
< 1. 15>
0.000
0.001
(0.001)
< 1.43>
0.000
0.004
(0.009)
< 1.79>
0.001
0.00*
(0.006)
< 1.46>
0.001
0.001
(0.001)
< t.25>
0.000
0.001
(0.001)
< o.sa>
0.001
0.001
(0.002)
< 1.50>
0.000
CO
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.006~
(0.003)
< 1.50>
0.005
0.005
(0.0 )
< o.o •>
0.005
0.006
(0.002)
< 1.79>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.006
(0.002)
< 1.79>
0.005
0.016
(0.028)
< 1.79>
0.005
0.011
(0.015)
< 1.79>
0.005
0.005
(0.0 )
< 0.0 >
0.005
Cl
I* # *> t • ** •• #•
0.005
(0.0 •
< 0.0 >
0.005
0.007
(0.00» •
< 1.79>
0.005
0.005
(0.0 I
< 0.0 >
0.005
0.018
(0.017.-
< 1.08>
0.009
0.005
(0.000)
< 1.50>
0.005
0.005
(0.0 n
< 0.0 >
0.005
0.007
(0.003)
< 0.7>
0.005
0.008
(0.001.
< 0.1 6>
0.008
0.006
(0.001-
< 1.79>
0.005
0.009
(0.00% <
< 0.98>
0.007
0.005
(0.0 )
< 0.0 >
0.005
CO
0.007
(0.004)
< 1.79>
0.005
0.008
(0.004)
< 0.79>
0.006
0.011
(0.009)
< 0.57>
0.005
0.015
(0.014)
< 1. 15>
0.012
0.007
(0.003)
< 0.41>
0.005
0.014
(0.022)
< 1.79>
0.005
0.031
(0.043)
< 1 . 0 1>
0.006
0.010
(0.007)
< 0.66>
0.006
0.008
(0.005)
< 1.43>
0.006
0.012
(0.008)
< 0.96>
0.008
0.009
(0.003)
<-0.5 1>
0.011
re
0. 175
(0.116)
< 3.62>
0.140
0.170
(0.130)
<-o.oa>
0.183
0.444
(0.461)
< 1.38>
0.306
1.053
(1.385)
< 0.84>
0.243
1. 118
(1.924)
< 1.44>
0.257
0.42*
(0.448)
< 1.60>
0.282
1.108
(1.228)
< 0.65>
0.528
1.205
(1.778)
< 1.49>
0.308
0.422
(0.392)
< 1.52>
0.275
0.425
(0.522)
< l.66>
0.226
0.624
(0.669)
< 0.45>
0.189
PB
0.002
(0.001)
< 1. 12>
0.002
0.003
(0.001)
< 0. 23>
0.003
0.007
(0.007)
< 0.97>
0.003
0.006
(0.006)
< 0.84>
0.002
0.003
(0.001)
< 0.91>
0.003
0.005
(0.005)
< 1.04>
0.002
0.008
(0.009)
< 1. 53>
0.003
0.009
(0.010)
< 1.4 1>
0.006
0.006
(0.005)
< 0.88>
0.004
0.005
(0.004)
< 1. 16>
0.003
0.006
(0.009)
< 1.49>
0.002

-------
   Table C.11, continued
O
      10721
      10821
      10842
      11032
     20711
     20842
     21323
     30312
     40231
     40421
     2123*
AV
SO
S
no
AT
SD
S
(ID
A?
SD
S
HD
AT
SD
S
ND
AT
SD
S
HD
AT
SD
S
ND
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
no
AT
SD
S
HD
1.059
(1.746)
< 1.45>
0.340
0.190
(0. 199)
< 1.21>
0.129
0.124
(0.15fi|
< 1.29>
0.023
0.635
(0.743|
< 1.27>
0.380
2.208
(2.917)
< 0.44>
0.112
0.328
(0.302)
< 0. 58>
0.364
0.774
(0.956)
< 1.27>
0.450
0.611
(0.773)
< 0.95>
0.324
0.476
(0.486)
< 1.1 4>
0.392
0.172
(0.216)
< 1.07>
0.088
0.251
(0.213)
< 0.27>
0.226
0.006
(0.001)
< 1.50>
0.005
0.007
(0.004)
< 1.61>
0.005
0.009
(0.006)
< 0.97>
0.005
0.006
(0.003)
< 1.50>
0.005
0.008
(0.007)
< 1.49>
0.005
0.005
(0.0 )
< 0.0 3
0.005
0.006
(0.002)
< 1.50>
0.005
0.006
(0.002)
< 1.43>
0.005
0.013
(0.007)
<-0.04>
0.013
0.006
(0.002)
< 1.36>
0.005
0.018
(0.029)
< 1.50>
0.005
0.096
(0.057)
< 1.1 8>
0.081
0.092
(0.044)
<-0.46>
0.102
0.089
(0.028)
<-0.82>
0.09R
0.077
(0.037)
< 0.92>
0.072
0.165
(0.059)
< 0.22>
0.180
0.112
(0.054)
< 1.03>
0.099
0.095
(0.038)
< 0.58>
0.087
0.067
(0.011)
<-0.09>
0.066
0.114
(0.048)
<-0.51>
0.125
0.065
(0.016)
<-0.14>
0.068
0.096
(0.048)
< 1.04>
0.084
0.335
(0.396)
< 0.71>
0. 113
0.356
(0.199)
< 1.00>
0. 192
0.202
(0.138)
< 1.06>
0. 160
0. 188
(0.093)
( 0. 18>
0.179
0.433
(0.456)
< 0.63>
0.246
0.805
(0.493)
< 0.02>
0.800
1.099
(1.228)
< 0.50>
0.728
0.711
(0.770)
< 0.44>
0.523
0.440
(0.343)
< 0.04>
0.433
0.476
(0.493)
< 0.59>
0.294
0.217
(0.156)
< 0.63>
0.170
47. a
( If.O)
<-0.35>
57.
5S.8
( 21-9)
< 0.17>
S6.
27.7
( 11.1)
< 0.27>
29.
40.8
( 19.6)
<-0. 13>
44.
51.6
( 15.5)
< 0. 33>
«9.
34.7
( 13.2)
< 0.48>
29.
45.9
( 7.9)
<-0.40>
48.
66.8
( 24.8)
< 0.47>
66.
49.8
( 15.5)
<-0. 27>
54.
42.6
( 15.8)
<-0.08>
39.
41.4
( 25.3)
<-0.52>
47.
0.001
(0.001)
< 1.50>
0.000
0.001
(0.001)
< 1.64>
0.000
0.001
(0.001)
< 2.04>
0.000
0.001
(0.001)
< 1.50>
0.000
0.001
(0.002)
< 1.43>
0.000
0.001
(0.002)
< 1.50>
0.000
0.001
(0.001)
< 1.50>
0.000
0.001
(0.001)
< 0.88>
0.001
0.001
(0.000)
< 1.79>
0.000
0.000
(0.0 )
< 0.0 >
0.000
0.001
(0.000)
< 0.41>
0.000
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
' < 0.0 >
0.005
0.006
(0.002)
< 1.50>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< o.o •>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 )
0.005
0.005
(0.0 )
< 0.0 >
o.oos
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.001)
< 1.79>
0.005
0.005
(0.0 I
< 0.0 )
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.011
(0.013 •
< 1.50>
0.005
0.007
(0.005)
< 1.50>
0.005
0.005
(0.0 I
< 0.0 >
0.005
0.005
(0.0 I
< 0.0 )
0.005
0.005
(0.0 ••
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
o.ooa
(0.009)
< 1.79>
O.OOS
J.UU6
(0.003)
< 1.50>
0.005
0.029
(0.033)
< 0.70>
0.011
0.005
(0.001)
< 1.36>
0.005
0.007
(0.004)
< 1.50>
0.005
0.009
(0.007)
< 1.39>
0.005
0.008
(0.005)
< 1.25>
0.005
0.007
(0.004)
< 1.50>
0.005
0.012
(0.007)
< 0.59>
0.009
0.015
(0.026)
< 1.79>
0.005
0.031
(0.023)
<-0.23>
0.041
0.046
(0.075)
< 1.43>
0.005
o.ysi
(1.685)
< 1.40>
0.242
0.915
(1.658)
< 1.66>
0. 165
0. 179
(0.213)
< 0.85>
0.037
1.288
(2.652)
< 1.50>
0. 144
2.332
(3.047)
< 0.45>
0.245
0.397
(0.530)
< 1.19>
0.267
0.712
(1.1261
< 1.44>
0.289
0.626
(0.849)
< 0.75>
0.098
1.223
(1.742)
< 1.28>
0.318
0.64*
(0.738)
< 0.54>
0.261
0.319
(0.541)
< 1.69>
0. 1 10
0.0^12
(0.001)
< 0.41>
0.002
0.002
(O.OUO)
< 1.79>
0.002
0.002
(0.000)
< 1.00>
0.002
0.003
(0.001)
<-0.41>
0.003
0.006
(0.005)
< 0. 85>
0.003
0.002
(0.000)
< 1.00>
0.002
0.007
(0.010)
< 1.47>
0.003
0.003
(0.002)
< 0.67>
0.002
0.002
(0.000)
< 1.00>
0.002
0.004
(0.001)
<-0.87>
0.004
0.087
(0.209)
< 1.79>
0.002

-------
Table C.11, continued
20112 AT
SD
S
no
20243 AT
SD
S
(ID
20721 AT
SD
S
no
21141 AT
SD
S
NO
40331 AT
SD
S
no
10232 AT
SD
S
no
10721 AT
3D
S
no
10821 AT
SD
S
no
10842 AT
SD
S
no
11032 AT
SD
S
(ID
20711 AT
SD
S
no
46.8
( 2.8)
<-0.72>
47.0
34.5
( 9.0)
< 0.72>
33.0
28. S
( 3.8)
< 0.42>
27.5
45.8
( 8.9)
49.5
49.0
(6.1)
51.5
41. «
(10.4)
38.0
54.2
(14.7)
< 0. 84 >
51.0
66.2
( 9.2)
64. 1
35.9
( 5.0)
<-0.75>
36.0
52.4
(11.5)
50.0
65.8
(10.8)
< 0.35>
66.0
0.049
(0.070)
< 1.09>
0.010
0.093
(0.076)
< 0.54>
0.091
0.174
(0.209)
< 1.49>
0.107
0.053
(0.042)
< 0.17>
0.046
0.086
(0.053)
<-0.02>
0.083
0.045
(0.026)
0.035
0.124
(0.164)
< 0.41>
0.008
0.016
(0.016)
< 0.69>
0.012
0.006
(0.006)
< 0.99>
0.004
0.048
(0.021)
<-0.04>
0.052
0.341
(0.364)
< 0.38>
0.111
0.000
(0.0 )
< 0.0 >
*****
0.000
(0.0 )
< 0.0 >
*****
0.000
(0.000)
< 0.00>
0.000
0.000
(0.0 )
< 0. 0 >
0.000
0.000
(0.000)
< 0.00>
0.000
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.000
(0.0 )
< 0.0 >
*****
0.001
(0.0 )
< 0.0 >
0.001
0.000
(0.0 )
< 0.0 >
*****
0.000
(0.000)
< 0.00>
0.000
o.oos
(0.002)
< 0. 12>
0.005
0.014
(0.013)
< 1.40>
0.011
0.039
(0.015)
<-0.90>
0.042
0.011
(0.004)
<-0.05>
0.011
O.OIfl
(0.019)
< 1.49>
0.009
0.009
(0.004)
<-0.92>
0.010
0.013
(0.006)
<-0.49>
0.012
0.015
(0.004)
< 0.42>
0.014
0.013
(0.006)
< 0.73>
0.013
0.011
(0.007)
< 1.33>
0.008
0.009
(0.007)
< 0. 15>
0.008
0.006
(0.003)
< 1.79>
0.005
0.015
(0.024)
< 1.79>
0.005
0.010
(0.010)
< 1 . 7 0>
0.005
0.005
(0.001)
< 1.79>
0.005
0.006
(0.0021
< t.12>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.028
(0.036)
< 0.78>
0.005
0.044
(0.038)
<-0.07>
0.055
0.005
(0.0 )
< 0.0 >
0.005
0.006
(0.03 1)
< 0.41>
0.005
8.1
( 0.9)
8.2
8.7
( 1.6)
9.0
8.5
( 2.7)
< 1.58>
7.6
10.9
( 2.8)
< 1.29>
10.2
10.2
( 1.6)
< 1.22>
9.8
8.7
( 1-8)
<-0.74>
9.6
10.4
( 2.9)
< 0.40>
9.5
11.6
( 2.4)
< 0.61>
11.0
** **
(*..*)
< 2.04>
11.0
11.0
( 1-3)
< 0. 97>
11.0
12.2
( 1-0)
< 0.05>
12.0
O.OOS
(0.0 )
< 0.0 >
o.oos
0.005
(0.000)
< 1.79>
0.005
0.006
(0.001)
< 0.88>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.008
(0.008)
< 1.75>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
o.oos
0.009
(0.006)
< 0.74>
0.005
0.006
(0.002)
< 2.04>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 J
0.005
O.OOS
(0.0 )
< 0.0 >
o.oos
0.005
(0.0 1
< 0.0 >
o.oos
0.005
(0.0 )•
C 0.0 >
o.oos
o.oos
(0.0 )
< 0.0 >
o.oos
0.005
(0.0 1
< 0.0 >
0.005
0.005
(0.0 I
< 0.0 >
0.005
0.005
(0.0 1
< 0.0 >
o.oos
0.005
(0.0 ••
< 0.0 )
o.oos
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 »
< 0.0 >
0.005
0.005
(0.0 1
< 0.0 )
0.005
9*. 8
( 31.4)
< o.os>
93.5
138.2
( 96.3)
< 1.68>
103.0
99.0
( 12.6)
< 0. 18>
99.0
119.8
(101.3)
< 1.65>
86.5
148.3
( 64.6)
124.0
120.2
( 44.1)
< 0.36>
94.0
94.8
( 39.2)
< 0. 16>
87.0
147.0
( 74.6)
< 1.06>
131.5
124.3
( 70.3)
102."o
94.8
( 56.0)
< 1.28>
77.0
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( 9.0)
< 0.15>
68.0
0.007
(0.004)
< 1.79>
O.OOS
O.OOS
(0.0 )
< 0.0 >
o.oos
0.007
(0.005)
< 1.79>
0.005
0.007
(0.006)
< 1.79>
0.005
0.007
(0.005)
< 1.79>
0.005
O.OOS
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
o.oos
c.oos
(0.0 )
< O.D >
0.005
0.005
(0.0 |
< 0.0 >
o.oos
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
O.OS8
(0.059)
< 1. 57>
0.036
0.247
(0.348)
< 1.66>
0.095
0.111
(0.094)
< 0.61>
0.096
0.046
(0.035)
< 1. 20>
0.033
0.072
(0.050)
0.090
0.030
(0.012)
< 0.73>
0.025
0.097
(0.078)
< 0.74>
0.081
0.131
(0.145)
< 1.55>
0.075
0.034
(0.015)
< 0. 25>
0.028
0.028
(0.010)
< 0.75>
0.022
0.096
(0.081)
< 0. 41>
0.053

-------
      Table C.11, continued
40311


10541


i1152



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10932



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< 1.50>
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0.007
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0.043
0.067
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0.488
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0.005
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0.005
0.005
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0.031
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0.047
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0.006
0.009
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0.090
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0.032
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0. 141
0.775
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4.688
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< 0.0 >
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0.002
(0.001)
< 1.50>
0.002
0.002
(0.000)
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10211



10521



10542



10931




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0.162
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0.022
0.196
(0.130)
< 0. 08>
0. 193

-------
Table C.11, continued
20842



21323



30312



40231



40421



21234



40311



10S41



21152



10731



10932



AT
SD
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no
AT
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< 1.46>
39.0
63.5
(15.9)
< 0.27>
62.0
70.1
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< 0.20>
67.0
59.5
(12.8)
< 0.44>
56.0
55.0
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51.3
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< 1.20>
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50.8
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< 0.43>
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< 0. 55>
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0.059
(0.040)
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0.061
0.063
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< 0.47>
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0.190
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< O.R9>
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< 0.66>
0.019
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0.028
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0.231
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< 0.0 >
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< 0.0 >
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(0.0 )
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0.002
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< 0.0 >
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< 0.0 >
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< 0.42>
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< 1.50>
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< 1.36>
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0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 )
o.oos
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
0.037
(0.008)
<-0. 69>
0.037
0.036
(0.015)
<-0.32>
0.043
0.145
(0.161)
< 1.42>
0.076
0.14J
(0.242)
< 1.73>
0.051
0.078
(0.081)
< 1.35>
0.045
0.035
(0.019)
< 0.67>
0.026
0.070
(0.081)
< 1. 27>
0.027
0.037
(0.019)
< 0. 67>
0.038
0.109
(0.0 )
< 0. 0 >
*****
0.07 1
(0.0 )
< 0.0 >
*****
0.041
(0.0 )
< 0. 0 >
*****
 * AV = Arithmetic Average;  SD = Standard Deviation;  S = Skewness;  MD =  Median

-------
NET US.  DISSOLTED(RG/L)
    • ELL        IL
                                                 Table C.12
                            Wells  After Baseline  - Ground Water  Metal Concentrations
                        AS
                                                                                                 Tt
• •••**
10112
10211
10521
105*2
10931
Vj-J
VjJ
20112
202*3
20721
211*1
40331
10232

• •••'
IT*
SO
S
no
IT
SD
S
SD
IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
(ID
IT
SD
S
no
IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
no
IT
SD
S
no
IT
SD
a
no
0.570
(0.316)
0.707
1.006
(0.520)
1.023
2.702
(2.139)
< 0.05>
2.667
1.735
(1.328)
<-0. 30>
1.859
0.92*
( 0. * 0 * )

0.972
1.063
(1.269)
< 0.98>
0.635
1.73*
(2.280)
< 1.07>
0.823
0.81*
(0.626)
< 0.29>
0.73*
1.7*1
(1.858)
< 0. 87>
1.212
1.625
(2.067)
0.666
0.173
(0.124)
< 0.84>
0. 131
0.006
(0.001)
< 0.0 >
0.006
0.005
(0.0 )
< 0.0 >
0.005
0.007
(0.003)
< 0.55>
0.006
0.007
(0.003)
< 0.00>
0.007
0.008
(0.001)

0.008
0.006
(0.001)
< 0.71>
0.005
0.005
(0.001)
< 0.0 5
0.005
0.006
(0.003)
< 0.71>
O.OOS
0.006
(0.002)
< 0.71>
0.005
0.006
(0.002)
< 0.64>
0.006
0.006
(0.002)
< 0. 0 >
0.006
>••*•••**•*•
0.063
(0.016)
< 0.00>
0.063
0.064
(0.034)
< 0.00>
0.064
0.081
(0.112)
< 0.69>
0.024
0.078
(0.0*5)
< 0.00>
0.078
0.033
(0.005)
0.033
0.039
(0.003)
< 0.00>
0.039
0.0*3
(0.005)
< 0.00>
0.0*3
0.069
(0.036)
< 0.37>
0.061
0.080
(0.046)
< 0.43>
0.069
0.060
(0.039)
< 0.52>
0.047
0.038
(0.002)
< 0.00>
0.038
*••••»••*•*
1. 169
(0.059)
< 0.0 >
1. 168
1.088
(O.OR8)
< 0.0 •>
1.088
0.953
(0.089)
< 0.00>
0.953
0.0
(0.0 )
< 0.0 >
0.0
2.175
(0.106)
2/175
0.0
(0.0 )
< 0.0 >
0.0
1.0*2
(0.059)
< o.o •>
1.0*2
0.990
(0.0 )
< 0.0 >
• ••*•
0.510
(0.0 )
< 0.0 5
*****
0.760
(0.0 )
< 0.0 >
. *****
0.851
(0.0 )
• *•••
*«••*•»•**•»
37.6
( 4.0)
< 0.67>
37.
37.5
( 2. J)
37.
37.6
( 2.1)
<-0.80>
38.
39. 1
37.
41.0
( 12.9)
41.
«2.8
( 9.6)
,<-0.79>
•S.
38.0
( 8.0)
< 0.79>
35.
36.9
( 1.9)
38.
57.1
<-0.98>
6*.
44.9
( 15.8)
<-0.76>
49.
55.6
( 27.2)
< 1. 09>
• *.
*•»••••••**
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 )
< o.o •>
0.000
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 )

0.000
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 |
< 0.0 >
0.000
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 )
0.000
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.001)
< 0.0 >
0.005
0.005
(0.000)
< 0.71>
0.005
0.007
(0.003)
< 0.0 >
0.007
0.005
(0.000)
O.OOS
0.006
(0.001)
<-0.65>
0.007
0.005
(0.0 )
< 0.0 >
0.005
0.006
(0.001)
<-0.65>
0.007
0.007
(0.003)
< 0.70>
0.005
0.007
(0.002)
<-0.35>
0.007
0.005
(0.0 )
O.OOS
0.005
(0.0 1
< 0.0 >
0.005
0.005
(0.0 •<
< 0.0 >
0.005
0.005
(0.0 1
< 0.0 >
0.005
0.076
(O.ioa,
< 0.00>
0.076
O.OOS
(0.0 )
O.OOS
0.026
(0.037)
< 0.7 1>
O.OOS
O.OOS
(0.0 |
< 0.0 >
O.OOS
O.OOS
(0.0 i>
< 0.0 >
O.OOS
O.OOS
(0.0 I
< 0.0 >
0.005
O.OOS
(0.000)
< 0.71>
0.005
O.OOS
(0.0 |
0.005
>•*•••••••*<
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 J
< 0.0 >
0.005
0.007
(0.003)
< 0.71>
O.OOS
0.013
(0.012)
< 0.0 >
0.013
0.005
(0.0 )
0.005
O.OOS
(0.0 )
< 0.0 >
O.OOS
O.OOS
(0.0 |
< 0.0 >
O.OOS
0.007
(0.002)
< 0.31>
0.006
0.008
(0.005)
< 0.70>
O.OOS
0.033
(0.0*9)
< 0.71>
O.OOS
0.005
(0.0 )
0.005
0.337
(0. 1291
< 0.45>
0.320
0.497
(0.2731
< 1.00>
0.400
1.601
(1.467)
< 0.10>
1.532
1.727
< 0.09>
1.688
8.885
(*»•»•)
5.280
0.71*
(0.5391
< 0.02>
0.710
0.8S9
(0.958)
< 1. 12>
0.445
0.486
(0.370)
0.510
0.730
(0.562)
< 0.28>
0.68S
1.310
(1.285)
< 0.3S>
1.090
0.371
(0.235)
<— 0. 9*>
0.45«
»•••*••»
0.005
(0.0 )
< 0.0 >
O.OOS
0.012
(0.011)
< 0.0 >
0.012
0.021
(0.026)
< 0.70>
0.007
0.014
(0.012)
< 0. 00>
0.01*
0.00*
(0.001)
0.00*
0.011
(0.011)
< 0.71>
O.OOS
0.007
(0.001)
< 0.0 >
0.007
0.012
(0.012)
< 0. 71>
O.OOS
0.013
(0.008)
< 0.01>
0.013
0.011
(0.006)
0.012
0.006
(0.001)
< 0. 0 >
0.006

-------
Table C.12,  continued
10721

10821
10842
11032
20711
208*2
21323
30312
40231

40421
21234
40311
AT
SD
s
no
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
ND
AT
SD
S
HD
AT
SD
S
no
AT
SD
no
AT
SD
S
no
AT
SD
S
no
AT
SD
S
no
2.719
(2.198)
< 0. 15>
2.542
0.232
(0.118)
< 0.86>
0.196
0.15*
(0.291)
0.464
0.659
(0.378)
< 0.0t>
0.648
3.647
(2.141)
3.654
0.278
(0.128)
< 0. 1 2>
0.270
1.436
(0.837)
< 0. 32>
1.33*
1.000
(0.400)
1.091
1.658
(1.081)
<~1 1*>
2.142
0.915
(0.424)
<-0.24>
0.961
0.797
(0.407)
<-0. 83>
0.914
0.548
(0.479)
< 0.89>
0.401
0.005
(0.0 )
^0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.008
(0.005)
< 0.0 >
0.008
0.005
(0.0 )
< 0.0 >
0.005
0.006
(0.002)
< 0.00>
0.006
0.010
(0.008)
< 0.00>
0.010
0.005
(0.0 )

0.005
0.005
(0.0 )
< 0.0 >
0.005
0.009
(0.003)
< o.o •>
0.009
0. 151
(0.040)

0.022
0.045
(0.011)
< 0.0 >
0.045
0.236
(0.231)
< 0.00>
0.236
0.134
(0.022)
< 0.00>
0. 134
0.046
(0.019)
< 0.00>
0.0*6
0.068
(0.029)
< 0.00>
0.068
0. 1««
(0.023)
< 0.00>
0. 144
0.108
(0.036)

0.059
0.017
(0.009)
< 0.0 >
0.017
0.022
(0.010)
< 0.0 >
0.022
1.189
(0.438)
v 0* 00^
1.189
0.970
(0.0 |
< 0.0 >
*****
1.240
(0.0 )
< 0.0 >
*****
1.094
(0.334)
< 0.00>
1.094
1.026
(0.316)
< 0.00>
1.026
0.774
(0.175)
< 0.00>
0.774
0.520
(0.594)
< 0.0 >
0.520
1.008
(0.059)
< 0.00>
1.008
0.740
(0.453)
0.740
0.876
(0.235)
< 0.00>
0.876
0.81]
(0.011)
< 0.00>
0.812
0.956
(0.076)
< 0.00>
0.956
117.8
( 67.2)

37.
29.0
( 2.9)
< 0. 13>
29.
51.5
( 4.1)
< 0. 19>
51.
57.2
( 10.6)
59.
53.2
( 6.2)
< 0. 35>
53.
57.8
( 5.5)
< 0. 20>
57.
55.3
( 12.8)
<-0.56>
57.
63.5
( 10.4)
<~ n i c>
^ U* J D^
65.
71.6
( 12.5)
< 0. 98>
67.
42.8
( 7.7)
<-0.55>
4*.
62.6
( «.«)
<-0.7»>
6*.
0.000
(0.0 )

0.000
0.000
(0.0 )
< 0.0 >
0.000
0.003
(0.00*)
< 0.00>
0.003
0.001
(0.000)
< 0.00>
0.001
0.000
(0.0 )
< 0.0 >
0.000.
0.000
(0.0 )
< 0.0 )
0.000
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 |
< 0*0 >
0.000
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 )
< 0.0 >
0.000
0. DOS
(0.00*)

0.008
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.000)
< 0.00>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.006
(0.001)
< 0.00>
0.006
0.005
(0.000)
< 0 QQy
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 • <
0.005
0.005
(0.0 1
< 0.0 >
0.005
0.005
(0.0 1
< 0.0 >
0.005
0.005
(0.0 1
< 0.0 >
0.005
0.005
(0.0 1
< 0.0 >
0.005
0.005
(0.0 n
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 |
< 0.0 >
0.005
0.005
(0.0 I
0.005
0.005
(0.0 ••
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 I
< 0.0 >
0.005
0.005
(0.0 )
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 )
0.005
0.005
(0.0 |
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 )
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
0.005
0.126
(0.005)
< 0.00>
0.126
0.005
(0.0 )
< 0.0 >
0.005
0.007
(0.003)
< 0.00>
0.007
5.881
(6.319)
4.330
«.400
(5.269)
< 0.22>
3.510
0.872
(0.646)
<-0.52>
1.039
1.305
(1.048)
< 0.32>
1.095
6.268
(5.651)
< 0.78>
4.566
1.089
(0.960)
<-0.08>
1.130
1.821
(0.933)
< 0.85>
1.565
7.044
(2.8641
<-0.86>
7.838
3.358
(3.315)
2.667
2.998
(1-473)
2.421
4.370
(2.284)
<-0.77>

1. 152
0.010
(0.007)
< 0. 0 >
0.010
0.003
(0.00,»
< o.oo
0.003
0.003
(0.002)
< 0.00>
0.003
0.004
(0.001)
< 0.00>
0.004
0.005
(0.000)
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.012
(0.010)
< 0.00>
0.012
0.011
(0.008)

0.006
0.008
(0.004)
< 0.00>
0.008
0.005
(0.0 |
< 0.0 J
0.005

-------
Table C.12, continued
105*1 IT
SD
S
HD
21152 XT
SD
S
HD
10731 IT
SD
S
RD
10932 IT
SD
S
HD
0.430
(0.303)
0.307
1.593
(0.660)
<-0. 37>
1.688
1.656
(0.9*1)
< o.e*>
1.382
4.656
(5.947)
< 1.23>
1.714
0.005
(0.000)
< 0.00>
0.005
0.005
(0.001)
< 0.0 >
0.005
0.009
(0.004)
< 0.00>
0.009
0.005
(0.000)
< 0.0 >
0.005
0.025
(0.002)
< 0.0 )
0.025
0.202
(0.021)
< 0.0 >
0.202
0. 103
(0.059)
< 0.00>
0. 103
0.121
(0.020)
< 0.0 >
0. 121
0.981
(0.001)
< 0.00>
0.981
1.183
(0. 193)
< 0.00>
1.183
1.451
(0.016)
< 0.00>
1.225
(0.191)
< 0.0 >
1.225
34.9
( 3.9)
< 0. 70>
34.
65.5
( 19-5)
< 0.30>
63.
67.8
( 37.7)
< 0.98>
55.
52.1
( 31.7)
< 1.44>
41.
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 )
< 0.0 >
0.000
0.006
(0.001)
< 0.00>
0.006
O.OOS
(0.0 )
< 0.0 >
O.OOS
0.006
(0.002)
< 0.00>
0.006
0.005
(0.001)
< 0.0 >
O.OOS
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 n
< 0.0 >
0.005
0.005
(0.0 |
< 0.0 >
O.OOS
0.005
(0.0 1
< 0.0 >
0.005
0.011
(0.006)
< 0.0 >
0.011
0.005
(0.0 )
< 0.0 >
O.OOS
O.OOS
(0.0 )
< 0.0 >
O.OOS
O.OOS
(0.0 )
< 0.0 >
O.OOS
2. 114
< 0.1 3>
1.990
1.168
(0.806)
< 0.86>
0.916
1.240
(1.054)
< 0.63>
0.93*
3.721
(5.423)
< 1.40>
1.563
0.009
(0.006)
< 0. 00>
0.009
0.005
(0.0 )
< 0.0 >
0.005
0.008
(O.OOS)
< 0.0 >
0.008
0.006
(0.002)
< 0.0 >
0.006
• BLL HO M HG NO II K SB 1C 11 TL Zl
••••**• •»*••••••••••••«»••***»•*»•**••*•••*•«»•*•**••**••*»•*•»*•••*••*••»•••••••»»••»•*••• •»•«**»»» **••*•••••*•••*•»*»»•»•••*•••
10112 IT 33.9 0.009 0.0 0.0 0.005 5.5 O.OOS 0.001 63.3 O.OOS 0.0*2
SD ( 3.1) (0.010) (0.0 ) (0.0 ) (0.0 ) ( 2.5) (0.0 ) (0.0 I ( 16.9) (0.0 ) (0.015)
S < 1.00> < 1. 10> < 0.0 > < 0.0 > < 0.0 > <-0. 37> < 0.0 > < 0.0 > < 0.37> < 0.0 > <-1.15>
HD 32.7 O.OOS 0.0 0.0 0.005 5.9 O.OOS 0.001 61.0 **••• 0.050
10211 AT
SD
S
ON 10521 IT
SD
S
HD
105*2 IT
SD
S
BO
10931 IT
SD
S
RD
20112 IT
SD
S
RD
202*3 IT
SD
S
RD
20721 IT
SD
S
NO
33.9
( 1-1)
33.5
28.3
( 5.3)
30.3
36.*
( 9.7)
< 1.02>
33.0
43.9
(13.8)
< 0.36>
• 2.0
45.3
<-0.74>
30.0
( 1.D
< 0.39>
29.8
38.5
(10.0)
< 0.65>
0.013
(O.OOS)
< 1.05>
0.011
0.087
(0.07*)
0.092
0.121
(0.12*)
< 0.91>
0.08*
0.123
(0.151)
0.051
0.016
(0.017)
< 0. 81>
0.011
0.038
(0.059)
0.010
0.013
(0.014)
< 0.92>
0.008
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 3
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.005
(0.0 )
< 0.0 >
0.005
O.OOS
(0.0 )
< 0. 0 >
O.OOS
0.190
(0.262)
< 0.00>
0.190
O.OOS
(0.0 )
< 0.0 >
0.005
0.0*7
(0.072)
< 0.71>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.000)
< 0. 71>
0.005
6.*
I 2.2)
< 0. 14 >
6.1
8.8
( 3.6)
<-0.72>
9.7
9.9
( 2.5)
< 0.87>
9.2
10.2
( 2.8)
<-0.60>
10.9
8.2
( 2.6)
8.5
7.8
( 1-9)
<-0.56>
8.2
8.*
( 3.1)
<-0.05>
8.5
0.005
(0.0 )
< 0.0 >
O.OOS
0.006
(0.002)
< 0.71>
O.OOS
0.005
(0.0 )
< 0.0 >
O.OOS
0.006
(0.002)
< 0.0 >
0.006
0.010
(0.008)
< 0.71>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.012
(0.007)
0.013
0.001
40.0 |
< 0.0 >
0.001
0.002
(0.002)
< 0.7 t>
0.001
0.003
(0.003)
< 0.00>
0.003
O.OOS
(0.0 )
< 0.0 >
0.005
0.002
(0.002)
< 0.7 1>
0.001
0.001
(0.0 I
< 0.0 >
0.001
0.002
(0.0021
< 0.71>
0.001
68.8
( 23.9)
6olo
70.3
( 33.0)
<-0.24>
73.5
101.8
( 51.0)
< 0.86>
87.0
106.3
( 23.5)
< 1.0S>
97.0
73.8
( 25.2)
< 0.47>
69.5
86.5
( 18.8)
< 0.99>
80.0
110.0
( 30.0)
<-0.06>
111.0
O.OOS
(0.0 )
< 0.0 >
0.005
(0.0 )
< 0.0 >
••*••
O.OOS
(0.0 )
< 0.0 >
0.005
(0.0 |
< 0.0 >
••*»»
O.OOS
(0.0 )
< 0.0 >
• **••
O.OOS
(0.0 )
< 0.0 >
• *•••
O.OOS
(0.0 )
< 0.0 >
• *••*
0.0*3
(0.014)
0.050
0.067
(0.057)
< 0.30>
0.055
0.132
(0.061)
<-0.52>
0.1*2
0.044
(0.017)
0.051
0.105
(0.073)
< 0. 86>
0.081
0.037
(0.015)
0.040
0.529
(0.925)
0.076

-------
Table C.12, continued
211*1 IT
SD
S
RD
•0331 IT
SD
S
HD
10232 AT
SD
S
HD
10721 AT
SD
S
HD
10821 AT
SD
S
no
108*2 AT
SD
S
Vj-4 HD
^ 11032 AT
SD
S
HD
20711 AT
SD
S
HD
208*2 AT
SD
S
HD
21323 AT
SD
S
HD
30312 AT
SD
S
no
•0231 AT
SD
S
HO
5*. 1
( 9.*)
<-0.72>
56.3
• 8.5
( 9.9)
52.6
• 0.7
( 8.0)
< 1.07>
37.6
• *••
(64.5)
< 0.26>
100.0
(22l 8)
33.7
37.2
( 3.1)
<-0.07>
37.3
53.2
( 2.0)
< 0.00>
53.2
62.8
(11.5)
66.6
53.0
53.6
66.3
<-0.02>
66.5
• 5.*
(10.0)
<-0.59>
«7.2
65.8
(11.0)
< 0.»7>
6*. 2
0. 157
(0.2*3)
0.052
0.067
(0.096)
< t.09>
0.029
0.013
(0.013)
< 0. 96>
0.009
0.367
(0.264)
<-0.33>
O.»10
0.142
(0.190)
< 0.70>
0.081
0.022
(0.018)
<-0.06>
0.023
0.032
(0.013)
< 0. 72>
0.028
0.171
(0.059)
0.176
0.077
(0.093)
< 0.80
0.0*8
0.052
(0.021)
< 0. 10>
0.051
1.6*2
(0.781)
< 0. 04>
1.620
0.135
(0.075)
< 0. 10
0.130
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0. 0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 )
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.006
(0.002)
< 0.71>
0.005
0.005
(0.001)
< 0.71>
0.005
0.005
(0.0 )
< 0.0 )
0.005
0.005
(0.0 )
< 0.0 >
O.OOS
0.005
(0.0 )
< 0.0 >
0.005
O.OOS
(0.0 )
< 0.0 >
0.005
O.OOS
(0.0 |
< 0.0 >
O.OOS
O.OOS
(0.0 )
< 0.0 >
0.005
O.OOS
(0.0 )
< 0.0 >
0.005
O.OOS
(0.0 I
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
12.0
( 3.0)
< 0.13>
11.8
9.*
( 2.0)
<-0.68>
9.9
8.*
( 2.0)
9.1
16.9
( 6.8)
< 1.11>
13.9
9.6
< 1.1)
10.1
11.8
( 2.6)
< 0.9»>
10.9
10.*
( 2.7)
< o.oa>
10.3
13.3
13.9
10.0
( 2.6)
10.5
12.3
( 2.*)
13.3
( 2.6)
< o. «a>
14.3
13.3
( 3.5)
<-0.52>
13.9
0.012
(0.006)
<-0.22>
0.013
0.008
(0.006)
< 0.68>
0.005
0.005
(0.0 )
< 0.0 >
O.OOS
0.007
(0.003)
< 0.0 >
0.007
0.007
(0.003)
< 0.00>
0.007
O.OOS
(0.0 )
< 0.0 >
O.OOS
0.006
(0.001)
< 0.00>
0.006
O.OOS
(0.0 )
< 0.0 >
O.OOS
0.005
(0.0 )
< 0.0 >
0.005
O.OOS
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.007
(0.003)
< 0.00>
0.007
0.002
(0.002*
< 0.7 1>
0.001
0.002
(0.002)
< 0.7 1>
0.001
0.003
(0.003)
< 0.00>
0.003
0.003
(0.003)
< 0.00>
0.003
O.OOS
(0.0 )
< 0.0 )
*****
0.001
(0.0 )
< 0.0 >
• »*••
0.003
(0.003)
< 0.00>
0.003
0.001
(0.0 I
< 0.0 >
0.001
0.001
(0.0 1
< 0.0 >
0.001
0.003
(0.003)
< 0.00>
0.003
0.003
(0.003)
< 0.0 0>
0.003
0.003
(0.003)
< 0.00>
0.003
97.5
( 18.7)
< 1.00>
91.0
100.3
( 22.3)
< 0.02>
99.5
105.3
( 23.1)
< 0.98>
97.0
118.3
I 80.3)
< 0.22>
111.5
9«.0
( 23.2)
< 0.82>
87.5
101.8
( 12.8)
< 0.82>
98.0
70.8
( 22.2)
< 0.28>
68.0
67.0
( 21.0)
< 0.20
65.5
49.8
( 24.0)
< 1.00>
• 1.5
106.3
<-0.35>
108.0
180.8
( 65.5)
19*. 0
86.5
( 17.1)
< 0.0 >
86.5
0.005
(0.0 )
< 0.0 >
• •»*•
O.OOS
(0.0 1
< 0.0 >
• *•••
O.OOS
(0.0 |
< 0.0 >
*****
O.OOS
(0.0 )
< 0.0 >
*****
o.oos
(0.0 )
< 0.0 >
•••*•
O.OOS
(0.0 I
< 0.0 >
• »*••
O.OOS
(0.0 )
< 0.0 >
*»•••
0.007
(0.0 )
< 0.0 >
• •••*
O.OOS
(0.0 )
< 0.0 >
*••••
O.OOS
(0.0 |
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
O.OOS
(0.0 )
< 0.0 >
*****
0.061
(0.032)
< 0. 2*>
O.OS8
0.072
(0.056)
< 0.97>
0.053
0.48*
(0.5*3)
< 1.00
0.262
0.05S
(0.022)
< 0.77>
0.050
0.0*7
(0.021)
0.050
0.0*2
(0.015)
0.050
0.0*3
(0.01S)
0.050
0.061
(0.025)
< 1. 1«>
0.050
0.425
(0.770)
< 1. 1S>
0.050
0.04S
(0.010)
0.050
0.237
(0.393)
< 1. 15>
0.050
0.269
(0.432)
< 1. 15>
0.05*

-------
      Table  C.12,  continued
CD
40421



21234



40311



10541



21152



10731



10932



IT
SO
S
no
IT
SO
S
NO
IT
SO
S
no
IT
SO
S
no
IT
SO
S
80
»T
SO
S
RD
AT
SO
S
BO
69.4
( 7.1)
< 0.86>
67.4
48. 1
( 3.3)
<-0.05>
48. 1
63.5
( 4.4)
< 0. 16>
63.3
34.4
( 2.7)
<-0.01>
34.4
43.3
( 4. 1)
< 0.14>
42.9
62.5
(23.4)
< 0.63>
58.0
36.5
( 2.9)
<-0.20>
37.2
0.042
(0.005)
<-0. 22>
0.042
0.144
(0.137)
<-0. 01>
0.145
0.029
(0.021)
< 0. 34>
0.026
0.058
(0.020)
< 0. 31>
0.056
0.064
(0.049)
< 0.51>
0.053
0.085
(0.092)
< 0.39>
0.067
0.121
(0. 187)
< 1.45>
0.052
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0. 0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 »
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 |
< 0.0 >
0.005
0.005
(0.0 I
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 )
0.005
0.005
(0.0 |
< 0.0 >
0.005
13.1
( 4.4)
< 0.54>
12.4
9.3
( 2.6)
<-0.80>
10.1
11.0
I 1*9)
< 0. 17>
10.9
0.6
( 1-5)
<-0. 89>
9.1
10.0
( 3.8)
<-0.45>
10.5
13.5
( 5.3)
<-0.32>
14.0
12.3
( 5.8)
< 0. 26>
11.1
0.087
(0.117)
< 0.00>
0.087
0.005
(0.0 )
< 0.0 >
0.005
0.059
(0.067)
< 0.00>
0.059
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0. 134
(0.158)
< 0.00>
0.134
0.001
(0.0 )
< 0.0 >
0.001
0.001
(0.0 )
< 0.0 >
0.001
0.003
(0.003)
< 0.00>
0.00)
0.003
(0.00)1
< 0.0 0>
0.003
0.001
(0.0 |
< 0.0 >
0.001
0.005
(0.0 I
< 0.0 >
0.005
0.00)
(0.003)*
< 0.00>
0.00)
102.)
( 12.6)
< 0.80>
98.5
34.5
( 20.6)
< o.et>
28.0
120.0
( 17.2)
< 0.41>
117.0
86.0
( 14.3)
< 0.44>
84.0
60.0
( 31.5)
<-0.97>
71.0
75.0
( 47.0)
<-0.65>
89. 5
84.0
« 41.3)
< 0.64>
70.0
0.005
(0.0 )
< 0.0 >
•••••
0.005
(0.0 )
< 0.0 >
•••••
0.005
(0.0 )
< 0.0 >
*•»••
0.005
(0.0 )
< 0.0 >
• «*••
0.005
(0.0 )
< 0.0 >
•••••
0.005
(0.0 )
< 0.0 >
«•*••
0.007
(0.0 )
< 0.0 >
*•**•
O.C44
(0.012)
< - 1. 1 •>
0.050
0.042
(0.015)
<- 1. 15>
0.050
0.029
(0.014)
< 1.07>
0.022
0.075
(0.035)
< 0.96>
0.063
0.037
(0.015)
<-0.03>
0.038
0.128
(0.173)
< 1. 14>
0.050
0.053
(0.025)
< 0.1 7>
0.050
       *  AV  =  Arithmetic  Average
         SD  =  Standard  Deviation
          S  =  Skewness
         MD  =  Median

-------
        OIGUICS(PPB)
                                           Table  C.13
                                   Hancock  Wells  Baseline
                                 Priority Organic Pollutants
       I ELL      tCCmPRTRTLEHE  »*THR»CZHE/PHE»ITKS EWE    1T81ZTRE  BERZeNE/TRICHLOBOETHTLElE
       ••••*•••••••••••••••••«•»«!
       10 11 2  AT *
              SD
              S
              RD
       10211
       10521
       105*2
       10931
MD
AT
SD
S
BD

IT
SD
S
RD

IT
SD
S
no

»T
SD
S
no
       20112  IT
              SD
              S
              an
       202*3
       20721
       211*1
        «0331
        10232
IT
SD
S
no

IT
SD
S
HD

IT
SD
S
no

IT
SD
S
RD

IT
SD
S
RD
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
I 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.9
( 2.0)
< 1.50>
5.00
5.0
( 0.0)
< 0.0 )
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
».3
( 1*5)

5loO
2.0
( 0.0)
< 0.0 >
2.00
2.4
( 0.6)
< 0.71>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 5
2.00
2.2
( 0.5)
< 1.79>
2.00
1.0
( *«')
< 1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.3
( 0*6)
< 1.72>
2.00
2.0
( 0.0)
< 0.0 >
2.00
3.0
( 1.9)
< 1. 15>
2.00
2.2
( 0.6)
< 1.79>
2.00
2.3
( 0.3)
< 1.79>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 1.50>
2.00
2.0
( 0.0)
< 0.0 )
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
6.2
( 1.9)
< 0. 09>
5.65
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 1.50>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1. 1
( 0.2)
< 1.79>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
2.3
( 3.0)
< 1.50>
1.00
EHUcenc
0.0
( 0.0)
< 0.0 >
0.3
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.3
0.0
< 0.0)
< 0.0 >
0.3
0.0
( 0.0)
< 0.0 >
0.0
12.0
( 0.5)
< 0.00>
12.05
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.3
0.0
( 0.0)
< 0.9 >
0.3
0.0
( 0.0)
< 0.3 >
0.0
»CIO 4-T-BUTTLPHEHOL
2.3
( 0.71
< 1.79>
2.00
2. 1
( 0.2)
< 1.79>
2.00
2.5
( 1.1)
< 1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
< 0.0)
< 0.0 >
2.00
2.»
( 1.0)
< 1.50>
2.00
2.0
I 0.0)
< 0.0 >
2.00
2.0
( 0.01
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.2
( 0.»)
< 1.50>
2.00

-------
Table  C.13,  continued
lOSl 1



10821



10842



11032



20711



20842



21323



30312



40231



40421



21234



40311



AM
SO
S
NO
AT
SD
S
HD
AT
SO
S
HD
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
no
AT
SD
s
no
5.0
t 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< o.o •>
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 )
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
t 0.0)
< 0.0 >
5.00
                                      2.0
                                    (  0.0)
                                   < 0.0 >
                                     2.00
                                      2.0
                                      0.0)
                                     0.0 >
                                     2.00
                                      2.0
                                   (  0.0)
                                   < 0.0 >
                                     2.00

                                      2.4
                                   (  0.5)
                                   < 0.42>
                                     2.00

                                      2.0
                                   (  0.0)
                                   < 0.0 >
                                     2.00

                                      2.0
                                   (  0.0)
                                   < 0. 0 >
                                     2.00

                                      2.0
                                   (  0.0)
                                   < 0.0 >
                                     2.00
                                      2.0
                                      0.0)
                                     0.0 >
                                     2.00

                                      4.1
                                      2.6)
                                     0.03>
                                     4. 15
                                      2.2
                                   (  0.5)
                                   < 1. 50>
                                     2.00

                                      2.6
                                   (  1-t)
                                   < 1.79>
                                     2.00
                                      2.0
                                      0.0)
                                     o.o :>
                                     2.00
   2.0
(  0-0)
< 0.0  >
  2.00
 2.0
 0.0)
0.0 >
2.00

 2.0
 0.0)
0.0 >
2.00

 4.8
 4.1)
0.74>
2.00

 2.0
 0.0)
0.0 >
2.00

 2.0
 0.0)
0.0 >
2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.7
(  1-2)
< 0.88>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   2.4
   1.1)
  1.79>
  2.00

   2.0
   0.0)
  0.0 >
  2.00
    J. 0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 2.04>
  1.00
   1.0
   0.0)
  1.50>
  1.00

   1. 1
   0.1)
  1.50>
  1.00
   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
{  0.0)
< 0.0 >
  1.00

   1.0
t  0.1)
< 1.50>
  1.00
   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 1.50>
  1.00
(  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0
                                             0.0
                                             0.0)
                                            0.0 >
                                            0.0
                                             0.0
                                          (  0.0)
                                          < 0.3 >
                                            0.0
                                             0.0
                                          {  0.0)
                                          < 0.0 >
                                            0.0
   0.0
 (  0.0)
< 0.0 >
  0.0

   0.0
 {  0.0)
< 0.0 >
  0.0
   0.0
 (  0.0)
 < 0.3 >
  0.0
   0.0
 (  0.0)
< 0.0 >
  0.0

   0.0
 (  0.0)
< 0.0 >
  0.0
   0.0
 (  0.0)
 < 0.3  >
  0.0

   0.0
 (  0.01
 < 0.0 >
  0.0
(  0.81
< 1.50>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.9
(  2.3)
< 1.79>
  2.00

   2.0
(  O.D
< 1.50>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 •>
  2.00

   3.4
(  3.2)
< 1.50>
  2.00

   2.4
 (  1.11
< 1.79>
  2.00

   2.9
 (  2.1)
< 1.50>
  2.00

   2.0
 (  0.0)
< 0.0 >
  2.00
                                                              2.0
                                                           (   0.0)
                                                           < 0.0 >
                                                            2.00

                                                              2.0
                                                           (   0.0)
                                                           < 1. S0>
                                                            2.00

-------
  Table C.13,  continued
 10541
21152
10731
       AT
       SO
       S
       no

       IT
       SO
       S
       no

       IT
       SO
       S
       no
10932  »T
       SD
       S
       HO
                   5.0
                   0.0)
                  0.0 >
                  5.00
           5.0
        {   0.0)
        <  0.0 >
        ******

           5.0
        (   0.0)
        <  0.0 >
        ******
                  5.0
                  0.0)
                 0.0 >
»ELL   C1RBOI TETHiCBLORIDE
•A**************************
10112  »T        6.3
       SO     (  3. 1)
       S      < 1.79>
       NO       5.00
10211
10521
AT
SD
S
SD

AT
SD
S
(ID
105«2  »T
       SD
       S
       no

10931  AT
       SD
       S
       (ID
20112
202*3
AT
SD
S
no

AT
SD
S
ND
 5.0
 0.0)
0.0 >
5.00

 5.0
 0.0)
0.0 >
5.00

 5.0
 0.0)
0.0 >
5.00

 5.0
 0.0)
0.0 >
5.00

 5.0
 0.0)
0.0 >
5.00

 5.0
 0.0)
0.0 >
5.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< o.o >
******
2.0
( 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
******
HLOROASILIHE
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< o.o •>
10.00
10.0
( 0.0)
< 0.0 >
10.00
2.0
{ 0.0)
< 0.0 >
2.00
38.9
( 0-0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
******
CHLOBOBERZERB
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
{ 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< o.o •>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
******
1.0
( 0.0)
< 0.0 >
******
1.0
( 0.0)
< 0.0 >
• ******
CRLOBOFORH
1.0
( 0.0)
< 0.0 >
1.00
3.8
( 6.7)
< 1.79>
1.00
7.»
( 1«.2)
< 1.50>
1.00
1.8
( 1-7)
< 1.50>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0. 0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
0.0
( 0.0)
< 0.0 >
0.3
0.0
( 0.0)
< 0.0 >
0.0
0.0
{ 0.0)
< 0.0 >
0.0
0.0
{ 0.0)
.< 0.0 >
0.0
2-CHLOEUPBEIOI
2.0
( 0.0)
< 0. 0 >
2.00
2.0
( 0.01
< 0.0 >
2.00
2.0
I 0.0)
< 0. 0 >
2.00
,2.0
( 0.0)
< 0. 0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0. 0 )
2.00
2.0
( 0.0)
< 0. 0 >
2.00
                                                                                                    2.0
                                                                                                 (   0.0)
                                                                                                 <  0.0 >
                                                                                                   2.00

                                                                                                   75.9
                                                                                                 (   0.0)
                                                                                                 <  0.0 >
                                                                                                 ******

                                                                                                    2.0
                                                                                                 (   0.0)
                                                                                                 <  0.0 >
                                                                                                 ******

                                                                                                    2.0
                                                                                                 (   0.0)
                                                                                                 <  0.0 >
                                                                                                 •***••
                                                                                                         1-CBLOBOTETB4DECAIIE
                                                                                                    ****************************
                                                                                                                  2.0
                                                                                                               (  0.0)
                                                                                                               < 0.0 >
                                                                                                                 2.00

                                                                                                                  2.0
                                                                                                               (  0.0)
                                                                                                               < 0.0 >
                                                                                                                 2.00
                                                                                                                (  5.0)
                                                                                                                < 1.50>
                                                                                                                 2.00
                                                                                                                  2.0
                                                                                                               (  0.0)
                                                                                                               < 0.0 >
                                                                                                                 2.00
                                                                                                                  2.0
                                                                                                               (  0.0)
                                                                                                               < 0.0 >
                                                                                                                 2.00
                                                                                                                  2.0
                                                                                                                  0.0)
                                                                                                                 0.0 >
                                                                                                                 2.00

                                                                                                                  2.0
                                                                                                                  0.0)
                                                                                                                 0.0 >
                                                                                                                 2.00

-------
Table  C.13,  continued
20721



211*1



10331



10232



10721



10821
VjJ
-P-
K>
108*2



11032



20711



208*2



21323



»f
SD
S
no
AT
SD
S
BD
AT
SD
S
no
AT
SO
S
no
AT
SD
S
BD
AT
SD
S
no
AT
SD
S
no
AT
SO
S
no
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
no
5.5
( 1-3)
< 1.79>
5.00
5.0
{ 0.0)
< o.o •>
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
6.5
( 3-»)
< 1.50>
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
{ 0.0)
< 0.0 >
5.00
                                   10.0
                                 (   0.0)
                                 <  0.0 >
                                  10.00

                                   10.0
                                 (   0.0)
                                 <  0.0 >
                                  10.00
                                   11. 1
                                    2.7)
                                   1.79>
                                  10.00
                                   10.0
                                 (   0.0)
                                 <  0.0  >
                                  10.00

                                   10.0
                                 (   0-0)
                                 <  0.0  >
                                  10.00

                                   10.0
                                 (   0.0)
                                 <  0.0  >
                                  10.00

                                   10.0
                                 (   0.0)
                                 <  0.0  >
                                  10.00

                                   10.0
                                 (   0.0)
                                 <  0.0  >
                                  10.00

                                   10.0
                                 {   0.0)
                                 <  0.0  >
                                  10.00

                                   10.0
                                 {   0.0)
                                 <  0.0  >
                                  10.00

                                   10.0
                                 (   0.0)
                                 <  0.0  >
                                  10.00
   1.0
(  0.0)
< 0.0 5
  1.00
   1.0
   0.0)
  0.0 >
  1.00
    1.0
 (   0.0)
< 0.0 >
  1.00

    1.0
 {   0.0)
< 0.0 >
  1.00
   1.0
   0.0)
  0.0 >
  1.00

   1.0
   0.0)
  0.0 >
  1.00

   1.0
   0.0)
  0.0 >
  1.00
   1.0
(  0.0)
< 0.0 >
  1.00
   1.0
(  0.0)
< 0.0 >
  1.00
   1.0
   0.0)
  0.0 >
  1.00

   1.0
   0.0)
  0.0 )
  1.00
   1.0
   0.0)
  0.0 >
  1.00

   1.0
   0.0)
  0.0 >
  1.00
   1.0
(  0.0)
< 0.0 >
  1.00

   1.1
(  0.8)
< 1.50>
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00
   1.0
   0.0)
  0.0 >
  1.00

   1.7
   1.7)
  1.50>
  1.00
   1.0
(  0.0)
< 0.0 >
  1.00
 1.5
 1.2)
1.50>
1.00

 1.8
 1.8)
1.50>
1.00
   2.0
   0.01
  0.0 >
  2.00

   2.0
   0.01
  0.0 >
  2.00
   2.0
(  O.Ol
< 0.0 )
  2.00

   2.0
I  0.01
< 0. 0 >
  2.00

   2.0
(  0.0)
< 0. 0 >
  2.00

   2.0
(  0.01
< 0.0 >
  2.00
   2.0
   0.01
  0.0 >
  2.00

   2.0
   0.01
  0.0 >
  2.00
   2.0
 (  0.0)
< 0. 0 >
  2.00
                        2.0
                        0.0)
                       0.0 >
                       2.00
                        2.0
                     (   0.01
                     <  0.0  >
                       2.00
                                        2.0
                                     (   0.01
                                     <  0.0 >
                                       2.00
                                        3.0
                                     (   2.U)
                                     <  1.79>
                                       2.00


                                        2.2
                                     (  0.6)
                                     < 1.79>
                                       2.00

                                        2.0
                                     (  0.0)
                                     < 0.0 >
                                       2.00

                                        2.0
                                     (  0.0)
                                     < 0.0 >
                                       2.00

                                        2.0
                                     {  0.0)
                                     < 0.0 >
                                       2.00

                                        2.0
                                     (  0.0)
                                     < 0.0 >
                                       2.00

                                        3.0
                                     (  2.2)
                                     < 1.50>
                                       2.00

                                        2.0
                                     C  0.0)
                                     < 0.0 >
                                       2.00
                      2.0
                    I  0.01
                    < 0.0 >
                     2.00
                      2.0
                    (  0.0)
                   < 0.0 >
                     2.00

-------
Table C.13, continued
30312



11023 1


«0«21



21234



10311



105U1



21152



10731



10932



• ELL
10112



10211



AT
SD
S
HD
AT
SD
S
(ID
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
ND
AT
SD
S
no
AT
SD
S
(ID
AT
SD
S
no
AT
SD
S
HD
DIB
AT
SD
S
HO
AT
SD
S
no
5.0
( 0.0)
< 0.0 >
5.00
5.2
( 0.6)
< 1.79>
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 )
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
{ 0.0)
< 0.0 >
5.00
193.0
( 0.0)
< 0.0 >
******
5.0
( 0.0)
< 0.0 >
•*»**•
5.0
( 0.0)
< 0.0 >
******
OTTLPHATHALATE
5.1
( 5*. 6)
< 0.97>
2.00
«.9
( 4*1)
< 1. 13>
3.05
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< o.o •>
10.00
10.0
{ 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
{ 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
******
10.0
( 0.0)
< 0.0 >
******
10.0
( 0.0)
< 0.0 >
******
2.3-DICHLOHOAHILIRB
8.0
( 7.3)
< 1.79>
5.00
5.0
( 0.0)
< 0.0 >
5.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 ">
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
< 0-0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< o.o •>
******
1.0
( 0.0)
< 0.0 )
******
1.0
( 0.0)
< 0.0 5
******
3,ft-DICHLOROAHILrHE
2.0
( 0.0)
< 0.0 >
2.00
2.5
( 1-0)
< 1.64>
2.00
1.0
( 0.0)
< 0.0 )
1.00
1.0
{ 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 )
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0-0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
******
1.0
( 0.0)
< 0.0 >
******
1.0
( 0.0)
< 0.0 >
******
DICHLOBOEERZEJE fl
2.1
( 0.3)
< 1.79>
' 2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
{ 0.0)
< 0. 0 >
2.00
2.0
{ 3.01
< 0.0 >
2.00
2.0
I 0.0)
< 0.0 >
2.00
2.0
( 0.01
< 0. 0 >
2.00
2.0
( 0.01
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
** *•*•
2.0
( O.Ot
< 0.0 >
******
2.0
( 0.0)
< 0. 0 5
** ** **
DIcaLOHOBERZBRE P
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
5 4
{ 7.7)
< 1.77>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
{ 0-0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
{ 0.0)
< 0.0 >
2.00
52.2
( 0.0)
< 0.0 )
******
2.0
( 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
•••**•
DICULOBOBEIZERE 0
2.0
( 0.0)
< 0.0 >
2.00
2.6
( 1-5)
< 1.79>
2.00

-------
Table  C.13,  continued
10521



10542



10931



20112



20243



20721



21141



40331



10232



10721



10821



10842



IT
SO
s
no
AT
SD
S
no
AT
SO
s
no
IT
SO
s
HD
AT
SD
S
ND
AT
SD
S
ND
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
no
3.5
( 2.6)
< 1.23>
2.00
2.9
( 2.1)
< ^.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
7.6
( 9.3)
< 1.14>
2. 15
20.7
( 34.1)
< 1.43>
5.00
5.2
( 7.0)
< 1.76>
2.00
7.1
( 5.7)
< 0.26>
5.80
6,1
{ «-61
< 0. 14>
5.15
4.3
( ».5)
< 1. 15>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
   5.0
(  0.0)
< 0.0 >
  5.00

   5.5
(  1-1)
< 1.50>
  5.00

   5.0
(  0.0)
< 0.0 >
  5.00

   5.0
(  0.1)
                                   5.00

                                   5.0
                                {  0.0)
                                < 0.0 >
                                  5.00
                                   5.0
                                (  0.0)
                                < 0.0 >
                                  5.00
                                   5.0
                                   0. 1)
                                  1.79>
                                  5.00
                                   5.0
                                (  0.0)
                                < 0.0 >
                                  5.00

                                   7.5
                                (  5.0)
                                < 1.15>
                                  5.00

                                   5.0
                                (  0.0)
                                < 0.0 )
                                  5.00
                                   5.6
                                   1.4)
                                  1.79>
                                  5.00
                                   5.0
                                (  0.0)
                                < 0.0 >
                                  5.00
                                                         2.0
                                                      <   0.0)
                                                      <  0.0 >
                                                        2.00
                                                         2.0
                                                         0.0)
                                                        0.0 )
                                                        2.00
                                                         2.0
                                                      <  0.0)
                                                      < 0.0 >
                                                        2.00
    2.0
    0.0)
   0.0 >
   2.00

    2.8
    1.6)
   1.40>
   2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.3
(  0.7)
< 1.79>
  2.00

   2.0
(  0.0)
< 0.0 •>
  2.00

   4.4
(  3.9)
< 1.10>
  2.75

   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
t  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< o.o •>
  2.00
                        2.0
                        0.0)
                       0.0 >
                       2.00

                        2.1
                        0.2)
                       1.50>
                       2.00
                        2.0
                     (   0.0)
                     <  0.0 >
                       2.00
    2.0
    0.0)
   0.0 >
   2.00
    2.0
    0.0)
   0.0 >
   2.00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
   0.0)
  0.0 >
  2.00

   2.0
   0.0)
  0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
{  0.0)
< 0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
                       2.0
                    (   0.0)
                    < 0.0 >
                     2.00
                       2.0
                    I   0.0)
                    <  0.0 >
                      2.00

                       3.4
                    (   3.2)
                    <  1.50>
                      2.00
   2.0
 (  0.0)
 < 0.0 >
  2.00
   2.0
 (  0.0)
 < 0.0 >
  2.00
   2.0
 (  0.0)
< 0.0 >
  2.00

   2.0
 (  0.0)
< 0.0 >
  2.00

   2.0
 (  0.0)
< 0.0 >
  2.00

   2.0
 (  0.0)
< 0.0 >
  2.00

   2.0
 (  0.0)
< 0.0 >,
  2.00
   2.0
 I  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
(   0.8)
< 1.50>
  2.00

   2.8
(   1.7)
< 1.50>
  2.00

   3.2
(   2.7)
< 1.50>
  2.00

   2.9
(   2.2)
< 1.79>
  2.00
   2.6
(   1-3)
 < 1.50>
  2.00

   2.2
(   0.5)
 < 1.79>
  2.00

   3.2
(   2.9)
 < 1.79>
  2.00

   2. 1
(   0.3)
 < 1.79>
  2.00

   2.0
(   0.0)
 < 0.0  >
  2.00

   2.0
(   0.0)
 < 0.0  )
  2.00

   2.0
(   0.0)
 < 0.0  >
  2.00

   2.8
(   2.0)
< 1.79>
  2.0O

-------
Table C.
11032



20711



20842



21323



30312



40231



40421



21234



40311



10541



21152



10731



AT
SD
S
HD
AT
SD
S
no
AT
SD
S
ND
AT
SD
S
HD
AV
SD
S
ND
AT
SD
S
no
AT
SD
S
ND
AT
SD
S
P1D
AT
SD
S
no
AT
SD
S
ND
AT
SD
S
ND
AT
SD
S
ND
13, con
3.3
( 1-9)
< 0. 70>
2.00
2.8
( 1.6)
< 1. 15>
2.00
2.8
( 1.9)
< 1.50>
2.00
2.1
( 0.2)
< 1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
6.1
( 6.5)
< 0.83>
2.00
4.0
( «-5)
< 1.50>
2.00
2.4
( 0.6)
< 0.74>
2.00
2.9
( 2.D
< 1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
111.0
( 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
*•»**•
   5.4
(  0.6)
< 0.45>
  5.00
   5.6
(  1-3)
< 1.15>
  5.00
 5.0
 0.0)
o.o •>
5.00

 5.0
 0.0)
0.0 >
5.00

 5.0
 0.0)
0.0 >
5.00

 5.8
 U.O)
1.55>
5.00

 5.0
 0.0)
0.0 >
5.00

 6.5
 3.3)
1.74>
5.00
   5.0
 (  0.0)
< 0.0 >
  5.00
   5.0
 (  0.0)
< 0.0 >
  5.00
   9.2
   0.0)
  0.0 )
******

    5.0
(   0.0)
< 0.0 >
******
   4.0
<  1.9)
<-0.10>
  4.30

   2.0
(  0.0)
< 0.0 >
  2.00
                         2.0
                         0.0)
                        0.0 >
                        2.00

                         2.0
                         0.0)
                        0.0 >
                        2.00
                         2.0
                      (   0.0)
                      <  o.o  •>
                        2.00

                         7. 1
                      (  11.2)
                      <  1.74>
                        2.00
                         2.0
                         0.0)
                        0.0 >
                        2.00

                         2.0
                         0.0)
                        0.0 >
                        2.00
   2.0
 (  0.0)
< 0.0 >
  2.00
   2.0
 (  0.0)
< 0.0 >
  2.00
    2.0
 (   0.0)
 < 0.0 >
 ******

    2.0
 (   0-0)
 < 0.0 >
 ******
   3.1
(  2.5)
< 1.50>
  2.00

   3.9
{  3.8)
< 1.15>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   3.9
   4.3)
  1.50>
  2.00

   2.0
   0.0)
  0.0 >
  2.00

   2.4
   0.9)
  1.79>
  2.00

   2.0
   0.0)
  0.0 >
  2.00

   2.0
   0.0)
  0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
   0.0)
  0.0 )
  2.00

   2.0
   0.0)
  0.0 )
******

   2.0
(  0.0)
< 0.0 >
••**•*
                                                               2.0
                                                            (  0.0)
                                                            < 0.0 >
                                                              2.00

                                                               3.8
                                                            (  3.5)
                                                            < ,1.15>
                                                              2.00
                                            2.0
                                         i   0.0)
                                        < 0.0 >
                                          2.00
                                            2.0
                                         (   0.0)
                                         < 0.0 >
                                          2.00
                                            2.0
                                         1   0.0)
                                         < 0.0 )
                                          2.00

                                            2.0
                                         (   0.0)
                                         < 1.79>
                                          2.00

                                            2.0
                                         (   0.0)
                                         < 0.0 >
                                          2.00

                                            2. 1
                                         (   0.3)
                                         < 1.79>
                                          2.00
                                                               2.0
                                                            (   0.0)
                                                            <  0.0  >
                                                              2.00
                                                               2.0
                                                            (   0.0)
                                                            <  0.0 >
                                                              2.00
                                                               9.6
                                                            (   0.0)
                                                            <  0.0 >
                                                            ******

                                                               2.0
                                                            (   0.0)
                                                            <  0.0 >
                                                            ******
    2.9
 (   2.0)
 <  1.50>
  2.00

    2.3
 (   0.5)
 <  1.15>
  2.00

    2.0
 (   0.0)
 <  0.0  >
  2.00

    2.0
 (   0.0)
 <  0.0  >
  2.00

    2.0
 (   0.0)
 <  0.0  >
  2.00

    3.6
 (   3.5)
 <  1.74>
  2.00

    2.0
 (   0.0)
 <  0.0 >
  2.00

    2.0
 (   0.0)
 <  0.0 >
  2.00

    2.0
 (   0.0)
 < 0.3 >
  2.00

   2.0
 (  0.0)
 < 0.0 >
  2.00

   2.0
 (  0.0)
 < 0.0 >
******

   2.0
 (  0.0)
 < 0.0 >
*•*•»*

-------
Table C.13,  continued
 10932
        AT
        SD
        S
        RD
   2.0
(  0.0)
< 0.0 >
••**•*
                                    5.0
                                 (  0.0)
                                 < 0.0 >
                                 ******
                                                          2.0
                                                       (   0.0)
                                                       <  0.0 >
                                                       ******
    2.0
 (  0.0)
 < 0.0 >
 •*»•*•
   2.0
(  0.0)
< 0.0 >
f *****
                                                                                                             2.0
                                                                                                          C   0.0)
                                                                                                          < 0.0 >
                                                                                                          ******
• ELL         DICHLOBOdETHANE  2,4-DICHLOBOPHEROL  DIETRTLPHTHALATB   DIISOOCTTLPBTRALATE  DIOCTTLPHTHALATE  DODECAIOIC ACID
***»***••*•**«•*•»••********»*•**********•****••***»***•*»***•**•«*«•**•**•*********»**»****•******••**********•*•*»****•***•**•»
10112   AT          0.0                2.0                 2.0                12.2                 2.0              0.0
        SD       (   0.0)             (  0.0)             (   0.0)             (  15.2)              (  0.0)            (  0.0)
        S        <  0.0 >             < 0.0 >             < 0.0 >             <  1.20>             < 0.0 >          < 0.0 >
        HD         0.0                2.00               2.00                4.85                2.00             0.0
10211
10S21
AT
SD
s
HD

AT
SD
S
HD
                   0.0
                   0.0)
                  0.0 >
                  0.0

                   0.0
                   0.0)
                  0.0 >
                  0.0
                         2.0
                         0.1)
                        1.79>
                        2.00

                         3.2
                         2.6)
                        1.50>
                        2.00
                                                          2.0
                                                       (   0.0)
                                                      < 0.0 >
                                                        2.00
                                                          4.7
                                                          fi. 1)
                                                         1.50>
                                                         2.00
                                                                           122.6
                                                                          (263.5)
                                                                          < 1.78>
                                                                           19.15

                                                                           206.4
                                                                          (336.7)
                                                                          < 1.33>
                                                                           51.20
                      11.4
                     ( 17.4)
                     < 1.46>
                      2.00

                        4.8
                     (   6.4)
                     < 1.50>
                      2.00
                    0.0
                  (  0.0)
                 < 0.0 >
                   0.0

                    0.0
                  (  0.0)
                 < 0.0 >
                   0.0
       AV
       SD
       S
       no

10931  AT
       SD
       S
       no

20112  AT
       SD
       S
       HD

20243  AT
       SD
       S
       HD
20721
       AT
       SD
       S
       HD
21141  AT
       SD
       S
       RD

40331  AT
       SD
       S
       HD
     0.0
     0.0)
    0.0 >
    0.0

     0.0
     0.0)
    0.0 >
    0.0

     0.0
     0.0)
    0.0 •>
    0.0

     0.0
     0.0)
    0.0 >
    0.0

     0.0
     0.0)
    0.0 >
    0.0

     0.0
     0.0)
    0.0 >
    0.0

     0.0
     0.0)
    0.0  >
    0.0
                                      2.0
                                   {   0.0)
                                   <  0.0 >
                                     2.00
                                      2.0
                                      0.0)
                                     0.0 >
                                     2.00

                                      2.3
                                      0.7)
                                     1.50>
                                     2.00

                                      2.9
                                      2.0)
                                     1.50>
                                     2.00
                                      2.0
                                   (  0.0)
                                   < 0.0 >
                                     2.00
                                      2.0
                                      0.0)
                                     0.0 )
                                     2.00
                                      2.0
                                   (  0.0)
                                   < 0.0 >
                                     2.00
 3.7
 3.8)
1.50>
2.00

 3.8
 4.0)
1.50>
2.00

 2.0
 0.0)
o.o •>
2.00

 2.0
 0.0)
0.0 >
2.00
                                                          2.0
                                                       (   0.0)
                                                       <  0.0 >
                                                         2.00

                                                          4.5
                                                       (   4.0)
                                                       <  0.84>
                                                         2.00

                                                          2.0
                                                       (   0.0)
                                                       <  0.0 >
                                                         2.00
  51.6
I 70.3)
< 1.22>
 21.80

  24.8
( 29.3)
< o.ai>
 13.00

   9.9
( 10.7)
< 0.82>
  4.90

 179. 1
(256.3)
< 0.97>
 30.80

  23. 1
( 49.0)
< 1.79>
  3.00

  40.1
( 85.7)
< 1.78>
  5.65

  72.6
(160.7)
< 1.78>
  3.00
                                                                                                 2.0
                                                                                               (  0.0)
                                                                                              < 0.0 >
                                                                                                2.00
   8.4
 ( 14.3)
< 1.50>
  2.00

   2.0
 (  0.0)
< 0.0 >
  2.00

  62.2
 (134.6)
< 1.50>
  2.00

   2.0
 (  0.0)
< 0.0 >
  2.00

   2.8
 (  1.8)
< 1.79>
  2.00

  43.7
 ( 64.6)
< 0.71>
  2.OO
                                                                                                           0.0
                                                                                                           0.0)
                                                                                                          0.0 >
                                                                                                          0.0

                                                                                                           0.0
                                                                                                           0.0)
                                                                                                          0.0 >
                                                                                                          0.0

                                                                                                           0.0
                                                                                                           0.0)
                                                                                                          0.0 >
                                                                                                          0.0
                                                                                                                   0.0
                                                                                                                (   0.0)
                                                                                                                <  0.0  >
                                                                                                                  0.0
                                                                                                           0.0
                                                                                                         (  0.0)
                                                                                                         < 0.0 )
                                                                                                          0.0

                                                                                                           0.0
                                                                                                         (  0.0)
                                                                                                         < 0.0 >
                                                                                                          0.0

                                                                                                           0.0
                                                                                                         I  0.0)
                                                                                                        < 0.0 >
                                                                                                          0.0

-------
Table  C.13,  continued
10232



10721



10821



10842



11032



20711



20842



21323



30312



40231



40421



AT
SD
S
RD
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
no
AT
SD
S
ND
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
ND
AT
SD
S
HD

(
<


(
<


(
<


(
<


(
<


0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
84.3
(107.1)
<


(
<


(
<


(
<


(
<


(
<

0. 0 >
84.25
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 )
0.0
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0. 0 >
0.0
0.0
0.0)
0.0 >
0.0
                                       2.6
                                       1.4)
                                       1.50>
                                       2.00

                                       2.0
                                       0.0)
                                       0.0 >
                                       2.00

                                       2.0
                                       0.0)
                                       0.0 >
                                       2.00
                                       2.0
                                    (  0-0)
                                    < 0.0 >
                                      2.00
                                       2.0
                                     (  0.0)
                                    < 0.0 >
                                      2.00
 3.4
 2.8)
1.1 5>
2.00

 2.0
 0.0)
0.0 >
2.00

 2.0
 0.0)
0.0 >
2.00

 2.0
 0.0)
0.0 •)
2.00

 4.3
 2.8)
0.41>
2.90
                                       2.0
                                     (  0.0)
                                    < 0.0 )
                                      2.00
 4.5
 5.0)
1.15>
2.00

 2.9
 2.0)
1.50>
2.00

 3.4
 3.4)
1.79>
2.00

 2.7
 1.7)
1.79>
2.00

 2.0
 0.0)
0.0 >
2.00

 4.2
 4.4)
1.15>
2.00

 4.4
 5.3)
1.50>
2.00

 2.0
 0.0)
0.0 >
2.00

 4.2
 5.3)
1.79>
2.00

 3.4
 2.4)
1.28>
2.00

 4.6
 5.9)
1.50>
2.00
  17. 1
 ( 26.2)
< 1.11>
  5.10

  17.8
 ( 11-9)
< 0.04>
 17.80

  23.6
 ( 33.0)
< 1.18>
  6.40

  35.8
 ( 60.4)
( 1.72>
 15.35

  65.7
( 85.9)
< 1.22>
 30. 10

  29.7
 ( 31.9)
< 0.45>
 23.00

 223.8
(470.5)
< 1.50>
  8.30

  44.7
( 92.4)
< 1.50>
  2.60

  10.8
( 12.2)
< 0.96>
  5.20

  48.2
{ 78.9)
< 1.44>
  8.85

  19. 1
( 21.7)
< 0.96>
 15.00
  16.5
( 29.0)
< 1.15>
  2.00
(  6.4)
< 1.50>
  2.00
   2.0
I  0.0)
< 0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.Op

   5.4
(  7.6)
< 1.50>
  2.00

  11.6
I 15.2)
< 1.0 3>
  5.15

  18. 1
( 22.2)
< 0.44>
  2.00

   7.4
( 12.0)
< 1.50>
  2.00
   2.0
   0.0)
  0.0 >
  2.00

   4.5
   4.7)
  1.51>
  2.00

   5.7
   8.4)
  1.50>
  2.00
                                                                              0.0
                                                                           (   0.01
                                                                           <  0.0 )
                                                                             0.0

                                                                              0.0
                                                                           (   0.0)
                                                                           <  0.0 >
                                                                             0.0

                                                                              0.0
                                                                           (   0.0)
                                                                           <  0.0 >
                                                                             0.0

                                                                              0.0
                                                                           (   0.0)
                                                                           <  0.0 >
                                                                             0.0
                    0.0
                    0.0)
                   0.0 >
                   0.0

                    0.0
                    0.0)
                   0.0 >
                   0.0
                                                                                                                    0.0
                                                                                                                 (   0.0)
                                                                                                                 <  0.0 >
                                                                                                                   0.0

                                                                                                                    0.0
                                                                                                                 (   0.0)
                                                                                                                 <  0.0 )
                                                                                                                   0.0
                                                                                                                    0.0
                                                                                                                    0.0)
                                                                                                                  0.0  >
                                                                                                                  0.0

                                                                                                                    0.0
                                                                                                                    0.0)
                                                                                                                  0.0  >
                                                                                                                  0.0
                    0.0
                 (  0.0)
                 < 0.0 )
                   0.0

-------
Table C.13,  continued
-P-
CO
21234



40311



10541



21152



10731



10932



AT
SO
S
HD
AT
SO
S
HD
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD
0.0
( 0.0)
< 0.0 >
0.0
0.0
{ 0.0)
< 0.0 5
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
                                       2.0
                                    <   0.0)
                                    <  0.0  >
                                      2.00

                                       2.0
                                    (   0.0)
                                    <  0.0  >
                                      2.00
                                       2.0
                                    (   0.0)
                                    <  0.0 >
                                      2.00
                                      5.8
                                      0.0)
                                     0.0 >
                                   ******

                                      2.0
                                   {  0.0)
                                   < 0.0 >
                                   ******

                                      2.0
                                   (  0.0)
                                   < 0.0 >
                                   ******
                        2.7
                        1.7)
                       1.79>
                       2.00

                        3.3
                        3.0)
                       1.50>
                       2.00
                        2.0
                     (  0.0)
                     < 0.0 >
                       2.00
                       16.7
                        0.0)
                       0.0 >
                     ******

                        2.0
                     (   0.0)
                     <  0.0 >
                     ******

                        6.4
                     (   0-0)
                     <  0.0 >
                     ******
                      41.5
                    (  62.8)
                    <  1.62>
                    20.50

                      75.2
                    (  81.0)
                    <  0.88>
                    59.00

                      30.9
                    (  56.6)
                    <  1.49>
                      6. 10
                      19.4
                    (   0.0)
                    <  0.0 >
                    ******
                      10.5
                    (   0.0)
                    <  0.0 >
                    •••**•

                      HO. 1
                    (   0.0)
                    <  0.0 >
                    ******
                                                                                                         3.3
                                                                                                      (   XI)
                                                                                                      <  1.79>
                                                                                                        2.00

                                                                                                         5.3
                                                                                                      (   7.3)
                                                                                                      <  1.50>
                                                                                                        2.00

                                                                                                         X5
                                                                                                      I   3.4)
                                                                                                      <  1.50>
                                                                                                        2.00

                                                                                                        20.7
                                                                                                      (   0.0)
                                                                                                      <  0.0 >
                                                                                                      ******
                        2.0
                      <  0.0)
                      < 0.0 >
                      *•*•*•

                       15.9
                      (  0.0)
                      < 0.3 >
                      »•*•*•
                                         0.0
                                       (  0.0)
                                       < 0.0  >
                                        0.0

                                         0.0
                                       (  0.0)
                                       < 0.0  >
                                        0.0

                                         0.0
                                       (  0.0)
                                       < 0.0  >
                                        0.0
                  0.0
                  0.0)
                 0.0 )
                 0.0

                  0.0
                  0.0)
                 0.0 >
                 0.0
                  0.0
               I  0.0)
               < 0.0 )
                 0.0
»ELL       ETHTL  BEHZEKE         HEPTADECAHE         HEIADECAHE      HEX AD BCAHOIC ACID  BEtHrt HEPTA DB: ANOATE
•••••A*****************************************************************************************************
10112  IT        1.0                  2.1                  2.0                0.0                  2.0
       SD     (   0.0)              (  0.2)               (   0.0)            (   0.0)               <  0.0)
       S      < 0.0 >              < 1.79>             < 0.0 >            <  0.0 >              < 0.0 >
       HD      1.00                 2.00                2.00               0.0                  2.10
10211
10521
10542
10931
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD

(
<


(
<


(
<


{
<

1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
2.6
3.7)
1.50>
1.00
1.1
0.3)
1.50>
1.00
   2.8
   1.5)
  1.46>
  2.00

   2.2
   0.4)
  1.50>
  2.00
   2.0
(  0.0)
< o.o •>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   2.3
(  0.7)
< 1.50>
  2.00

   2.0
1  0.0)
< 0.0 >
  2.00
                                                          2.0
                                                          0.0)
                                                        0.0 >
                                                        2.00
   2.0
(  0.0)
< 0.0 >
  2.00
 115.0
(  0.0)
< 0.0 >
******

   0.0
(  0.0)
< 0.0 >
  0.0
                      0.0
                   (   0.0)
                   < 0.0  5
                    0.0
   0.0
(  0.0)
< 0.0 >
  0.0
 2.0
 0.0)
0.0 >
2.00

 X 1
 2.5)
1.50>
2.00
                                                                                                         2.0
                                                                                                      <  0.0)
                                                                                                      < 0.0 >
                                                                                                        2.00

                                                                                                         2.9
                                                                                                      (  2.1)
                                                                                                      < 1.50>
                                                                                                        2.00
                                                                                                                      HETUILUEXADECAROATE
                                                                                                                      >*»•• «****»•»•*•***•**
                                                                                                                              2.0
                                                                                                                            (  0.0)
                                                                                                                            < 0.0 >
                                                                                                                             2.00

                                                                                                                              2.0
                                                                                                                            (  0.0)
                                                                                                                            < 0.0 >
                                                                                                                             2.00

                                                                                                                              2.0
                                                                                                                            (  0.0)
                                                                                                                            < 0.0 >
                                                                                                                             2.00
                       2.0
                    (   0.0)
                    < 0.0 >
                     2.00

                       2.0
                    (   0.0)
                   < 0.0 >
                     2.00

-------
Table  C.13,  continued
20112



202*3



20721



21141



40331



10232



10721



(0821



10842



11032



2071 1



208*2



AT
SD
S
HD
AT
SD
S
HD
IT
SD
S
no
AT
SD
S
no
IT
SD
S
RD
AT
SD
S
HD
AT
SD
S
(ID
AT
SD
S
RD
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
RD
1.0
( 0.0)
< 0. 0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
2.3
( 2-9)
< 1.50>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0-0)
< 0.0 )
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.2
{ 0.3)
< 1. 15>
1.00
1.0
( 0.0)
< 0.0 >
1.00
                                       2.0
                                    (  0.0)
                                    < 0.0 >
                                      2.00

                                       3.7
                                    (  3.9)
                                    < 1.50>
                                      2.00

                                       2.0
                                    (  0.0)
                                    < 0.0 >
                                      2.00

                                       2.1
                                    (  0.2)
                                    < 1.79>
                                      2.00

                                       2.0
                                    (  0.0)
                                    < 0.0 >
                                      2.00

                                       1.0
                                    (  2.1)
                                    < 1.15>
                                      2.00
                                       2.0
                                       0.0)
                                      0.0 >
                                      2.00

                                       2.0
                                       0.0)
                                      0.0 >
                                      2.00

                                       2.0
                                       0.0)
                                      0.0 ~>
                                      2.00

                                       3.0
                                       1.3)
                                      O.»1>
                                      2. 10

                                       2.2
                                       0.3)
                                      1.15>
                                      2.00
                                       2.0
                                    (   0.0)
                                    <  0.0 >
                                      2.00
   2.5
 {  1-1)
<  1.50>
   2.00

   2. 1
 (  0.3)
<  1.15>
   2.00

   2.0
 (  0.0)
< 0.0 5
  2.00
   2.2
   0.5)
  1.50>
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 )
  2.00
   2.0
(  0.0)
< 0.0 )
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   2.3
(  0.7)
< 1.50>
  2.00

   2.3
{  0.7)
< 1.15>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
I  0.0)
< 0.0 >
  2.00
    0.0
 (   0.0)
 <  0.0 >
   0.0

   28.«
 (   0.0)
 <  0.0 >
 •***•*

    0.0
 (   0.0)
 <  0.0 >
   0.0

    0.0
 (   0.0)
 <  0.0 >
   0.0

    0.0
 (   0.0)
 <  0.0 >
   0.0

    0.0
 (   0.0)
<  0.0  >
   0.0
   0.0
(  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0  >
  0.0
                     0.0
                   (  0.0)
                  < 0.0  >
                    0.0

                    17.6
                   (  0.0)
                  < 0.0  >
                  ******

                    23.7
                   {  0.0)
                  < 0.0  >
   0.0
(  0.0)
< 0.0 >
  0.0
    2.0
 (   0.0)
 <  0.0  >
   2.00

    2.0
 (   0.0)
 <  0.0  >
   2.00

    2.0
 (   0.0)
 <  0.0  >
   2.00

    2.7
 (   1.6)
 <  1.50>
   2.00

    3.5
 (   3-8)
 <  1.79>
   2.00

    2.6
 (   1-3)
<  1.50>
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00
                         2.8
                         1.6)
                        1.53>
                        2.00

                         2.0
                         0.0)
                        0.0 >
                        2.00
                         2.0
                      <   0.0)
                      < 0.0 >
                       2.00
   3.9
   H.2)
  1.50>
  2.00
                                                                 2.0
                                                              (   0.0)
                                                              <  0.0 >
                                                                2.00

                                                                 2.4
                                                              (   0.8)
                                                              <  1.50>
                                                                2.00
                                                                 2.0
                                                              (   0.0)
                                                              < 0.0 >
                                                               2.00
                                                                2.0
                                                              (  0.0)
                                                             < 0.0 >
                                                               2.00

                                                                2.0
                                                             (  0.0)
                                                             < 0.0 )
                                                               2.00

                                                                2.0
                                                             (  0.0)
                                                             < 0.0 >
                                                               2.00
                                                                2.0
                                                             (  0.0)
                                                             < 0.0 >
                                                               2.00

                                                                2.0
                                                             (  0.0)
                                                             < 0.0 >
                                                               2.00
                        2.0
                      (  0.0)
                     < 0.0 >
                       2.00

                        2.0
                      (  0.0)
                     < 0.0 >
                       2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.9
(  2.1)
< 1.50>
  2.00

-------
Table  C.13,  continued
21323



30312



40231



«0421



2123*



40311



10541



21152



10731



10932



IT
SO
s
no
AT
SD
S
no
AT
SD
S
no
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
RD
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
{ 0.0)
< 0.0 >
1.00
1.0
{ 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
******
1.0
( 0.0)
< 0.0 >
******
1.0
( 0.0)
< 0.0 >
******
                                    2.0
                                 (   0.0)
                                 <  0.0  t
                                   2.00

                                    2.0
                                 (   0.0)
                                 <  0.0  >
                                   2.00

                                    2.0
                                 (   0.0)
                                 <  0.0  >
                                   2.00

                                    2.9
                                 (   2.0)
                                 <  1.50>
                                   2.00

                                    2.0
                                 (   0.0)
                                 <  0.0  >
                                   2.00

                                    2.5
                                 (   1.2)
                                 <  1.50>
                                   2.00
                                    2.0
                                    0.0)
                                   0.0 >
                                   2.00
                                   2.0
                                (  0.0)
                                < 0.0 >
                                ******
                                   2.0
                                (  0.0)
                                < 0.0 >
                                ******
                                   2.0
                                   0.0)
                                  0.0 >
    2.0
 (   0.0)
< 0.0 >
  2.00

    2.0
 (   0.0)
< 0.0 >
  2.00
    2.0
    0.0)
   1.79>
   2.00

    2.0
    0.0)
   0.0 >
   2.00
   2.0
 (  0.0)
< 0.0 >
  2.00

   2.0
 (  0.0)
< 0.0 >
  2.00
    2.0
    0.0)
  0.0 >
  2.00

   2.0
   0.0)
  0.0 >
******

   2.0
(  0.0)
< 0.0 >
******
   2.0
(  0.0)
< 0.0 >
******
  25.7
 (  0.0)
< 0.0 >
******
   0.0
 (  0.0)
 < 0.0 >
  0.0
  106.0
 {  0.0)
 < 0.0 >
 ******
    0.0
 (   0.0)
 < 0.0 >
  0.0
  37.0
 (  0.0)
 < 0.0  >
 ******
    0.0
 (   0.0)
< 0.0 >
  0.0

    0.0
 (   0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0
   0.0
<  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0
   2.0
(  0.0)
< o.o •>
  2.00
   2.0
{  0.0)
< 0.0 >
  2.00
   1.1
 (  4.6)
< 1.50>
  2.00
   2.0
 (  0.0)
< 0.0 >
  2.00
   2.0
 (  0.0)
 < 0.3 >
  2.00
   2.0
 «  0.0)
 < 0.) >
  2.00

   2.0
 (  0.0)
 < 0.0 >
  2.00

  36.0
 (  0.0)
< 0.0 >
******

   2.0
 (  0.0)
< 0.0 >
******

   2.0
 (  0.0)
< 0.0 >
******
   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
   0.0)
  0. 0 >
  2.00
(  3.8)
< 0.85>
  2.00
   2.0
 (  0.0)
< 0.0 >
  2.00
   2.0
 (  0.0)
 < 0. 0 >
  2.00
   2.0
 (  0.0)
 < 0.0 >
  2.00

   2.0
 (  0.0)
 < 0.0 >
  2.00
 560.0
 (  0.0)
< 0.0 >
******

   2.0
 (  0.0)
< 0.0 >
• •••»*

   2.0
 (  0.0)
< 0.0 >
******

-------
   Table  C.13, continued
• E1L        l-HErHTLBAPHTRALEBE   2-HETHTI.PHBHOI.   «-«THILPHESOL     BAPHTHALEBB
******•*••••*•*•»***••***»**•***»
10112  AT
       SD
       S
       no

10211  AT
       SD
       S
       no

10521  AT
       SD
       S
       HD

105*2  AT
       SD
       S
       HD

10931  AT
       SD
       S
       HD

20112  AT
       SD
       S
       HD

202*3  AT
       SD
       S
       no

20721  AT
       SD
       S
       no
211*1
«»0331
10232
AT
SD
S
ND

AV
SD
S
no

AT
SD
S
no
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.1
( 0.1)
< 1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.1)
< 1.79>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0. 0 >
2.00
2.1
( 0.1)
< 0.8
2.00
5.0
( 0.0)
< 0.0 >
5.00
5.1
( 0.2)
< 1.79>
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
6.8
( 2.S)
< 1.08>
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0-0)
< 0.0 >
5.00
5.0
( 0.0)
< 0. 0 >
5.00
5.0
( 0.0)
< 0.0 )
5.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
0.0
{ 0.0)
< 0. 0 >
0.0
0.9
( 0.3)
< 0. 0 >
0.0
0.0
( 0.0)
< 0. 0 >
0.0 ,
0.)
( 0.0)
< 0. 0 >
0.0
0.3
( 0.0)
< 0-0 >
0.0
0.0
{ 0.0)
< 0. 0 >
0.0
0.0
( 0.0)
< 0. 0 >
0.0
0.3
( 0.0)
< 0. 0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0. 0 >
0.0
0.0
( 0.0)
< 0. 0 >
0.0
                                                                                  a-IOHILPBESOL        OCTADECABE
                                                                                                      i***********
                                                                                                          2.0
                                                                                                        <  0.0)
                                                                                                        < 0.0 >
                                                                                                         2.00

                                                                                                          2.8

                                                                                                        < 1.76>
                                                                                                         2.00

                                                                                                          3.8
                                                                                                        (  2.7)
                                                                                                        < 0.77>
                                                                                                         2.00

                                                                                                          2.0
                                                                                                        (  0.0)
                                                                                                       < 0.0 >
                                                                                                         2.00

                                                                                                          ». 1
                                                                                                        (  «.8)
                                                                                                       < 1.50>
                                                                                                         2.00
                                                                                                       (  6.1)
                                                                                                       < 1.79>
                                                                                                         2.00

                                                                                                          2.0
                                                                                                       (  0.0)
                                                                                                       < 0.0  >
                                                                                                         2.00

                                                                                                          2.0
                                                                                                       (  0.0)
                                                                                                       < 0.0  >
                                                                                                         2.00
 3.6
 3.9)
1.79>
2.00

 2.0
 0.0)
0. 0 >
2.00

 3.2
 1.2)
0.69>
2.90

-------
Table  C.13,  continued
     10721   AT
            SD
            S
            ND

     10821   AT
            SD
            S
            ND

     10842   IV
            SD
            S
            (ID

     11032   JIT
            SD
            S
            HD

    20711   IT
            SD
            S
            (ID

    20842   AT
            SD
            S
            no

    21323   IT
            SD
            S
            no

    30312   IT
            SD
            S
            HO

    40231   IT
            SD
            S
            (ID

    40421   IT
            SD
            S
            no

    21234   AT
            SD
            S
            no
   2.0
   0.0)
  o.o  •>
  2.00

   2.0
   0.0)
  0.0  >
  2.00

   2.0
   0.0)
  0.0 >
  2.00

   2.0
   0.0)
  0.0 >
  2.00
   2.0
(  0-0)
< 0.0  >
  2.00

   2.0
(  0.0)
< 0.0  >
  2.00
   2.0
   0.0)
  0.0 >
  2.00

   2.0
   0.0)
  0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
   0.0)
  0.0 5
  2.00

   2.0
   0.0)
  0.0 >
  2.no
   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
   0.0)
  0.0 >
  2.00

   2.0
   0.0)
  0.0 >
  2.00
   2.8
(  1-5)
< 1. 15>
  2.00
   2.0
   0.0)
  0.0 >
  2.00

   2.0
   0.0)
  0.0 5
  2.00
   2.0
(  0.0,
< 0.0 3
  2.00

   2.0
(  0.0)
< 0.0 5
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
   0.0)
  0.0 >
  7.00
   5.0
   0.0)
  0.0 >
  5.00

   5.0
   0.0)
  0.0 >
  5.00

   5.0
   0.0)
  0.0 >
  5.00

   5.1
   0.2)
  1.50>
  5.00
   5.0
{  0.0)
< 0.0 >
  5.00

   5.0
(  0.0)
< 0.0 >
  5.00

   5.0
(  0.0)
< 0.0 >
  5.00

   5.0
(  0.0)
< 0.0 >
  5.00

   5.4
(  0.7)
< 1.07>
  5.00
   5.0
   0.0,
  0.0 >
  5.00
   5.0
(  0.0)
< 0.0 >
  s.oo
   2.0
   0.0,
  0.0 >
  2.00

   2.0
   0.0)
  0.0 >
  2.00
   2.0
(  0.0)
< 0.0  >
  2.00
   2.0
(  0.0,
< 0.0 >
  2.00
   2.0
(  0-0,
< 0.0 >
  2.00
   2.0
(  0.0,
< 0.0  >
  2.00

   2.0
(  0.0,
< 0.0  )
  2.00
   2.0
(  0.0,
< 0.0 >
  2.00

   2.4
(  1.1)
< 1.79>
  2.00
   2.0
   0.0,
  0.0 >
  2.00

   2.0
   0.0)
  0.0 >
  7.00
   0.)
   0.0)
  0. 0 >
  0.0

   0.9
   0.0,
  0.0)
  0.0

   0.3
   0.0,
  0. 0 >
  0.0
   0.0
(  o.o,
< 0. 0 >
  0.0
   0.)
(  o.o,
< 0. 0 >
  0.0

   0.)
(  o.o,
< 0. 0 >
  0.0

   0.3
(  0.3,
< 0.0 >
  0.0

   0.3
(  o.o,
< 0. 0 >
  0.0
                        0.0
                        0.0)
                       0. 0 >
                       0.0
   0.0
(  o.o,
< 0. 0  >
  0.0
   0.3
(  0.0)
< 0.0 >
  1. n
   2.0
   0.0,
  0.0 >
  2.00

   2.0
   0.0,
  0.0 >
  2.00
   2.0
(  0.0,
< 0.0 >
  2.00
   2.2
(  0.4,
< 1.50>
  2.00

   6.7
(  4.9,
< 0.30>
  6.05

   4.6
(  2-6)
< 0.10>
  5.20
   2.4
 (  0.8)
 < 1. 50>
  2.00

   2.0
 (  0.0,
 < 0.0 >
  2.00

   3.0
 (  1-9,
 < 1.56>
  2.00
   2.0
 (  0.0)
< 0. 0 >
  2.00

   2.2
(  0.4)
< 1.79>
  -* nn

-------
Table C.13, continued
4031 1



10541



21152



10731



10932



VEIL
• ##> +t
10112



10211



10521



10542



10931



20112



AV
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD
• ••4
AT
SD
S
HD
AT
SD
S
RD
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD




















PREIOL
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< o.o •>
******
2.0
( 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
******
PBOPAZIHB
2.9
( 2.2)
< 1.79>
2.00
4.0
{ 3.4)
< 1.03>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.1)
< 0.0 > < 1.79>
10.00
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
******
2.0
{ 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
******
A-TEBPIHEOL
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0. 0 )
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
5.0
( 0.0)
< 0.0 )
5.00
5.0
( 0.0)
< 0.0 >
5.00
4.6
( 0.0)
< 0. 0 )
******
5.0
( 0.0)
< 0.0 >
******
5.0
( 0.0)
< 0.0 >
******
TETBACHLOBOETHTLEIE
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
< 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
( 0.0 >
2.00
7.0
( 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
******

(
<


(
<


(
<


(
<


(
<

rOLDEHB TBICHLOBOETHAIE
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0. 0 >
1.00
1.3
( 0.7)
< 1.50>
1.00
1.0
( 0.0)
< 0.0 )
1.00
• »»»»»»»»p»»*^
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0. 0 >
5.00
5.0
( 0.0)
< 0. 0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0. 0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0. 0 >
0.0
0.0
0.0)
0.0)
d.o
0.]
0.0)
0. 0 >
0.0
0.0
0.0)
0. 0 >
0.0




















2.2
( 0.4)
< 1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0. 0 >
******
2.0
( 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
••••**
TBICILOBOBTBTLEIB
























vvwwvww
4.7
( 6.8)
< 1.39>
1.00
2.7
( 2.5)
< 0.59>
1.00
1.8
« 1.5)
< 1 . 1 5>
1.00
2.4
( 1.9)
< 0.56>
1.00
2.4
( 1.8)
< 0.4
2.00
1.7
( 1-5)
< 1.50>
1.00
wwvw v^v
























-------
Table C.13, continued
3.3
2.9)
1.50>
2.00
2.0
0.0)
0.0 >
2.00
3.4
3.1)
1.77>
2.00
2.0
0.0)
0.0 >
2.00
4.1
4.3)
1.1 5>
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
4.5
5.1)
1.66>
2.00
4.5
5.7)
1.50>
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.4
0.8)
1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
3.9
( «-7)
< 1.7<)>
2.00
1.4
( 5-5)
< 1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0. 0 >
2.00
2.0
1 0.0)
< 0.0 )
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 3
2.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
« 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.2
( O.U)
< 1.79>
1.00
2. 6
< 3.8)
< 1.79>
1.00
1.0
( 0.0)
< 0.0 >
1.00
2.4
( 3.1)
< 1.76>
1.00
1.0
( 0.0)
< 0.0 5
1.00
1.0
( 0.0)
< 0.0 )
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.2
( 0.5)
< 2. 04>
1.00
1.2
( 0.4)
< 1.50>
1.00
12.3
{ 15.5)
< 0.42>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 )
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0. 0 >
5.00
11.5
( 1».»)
< 1.50>
5.00
5.0
( 0.0)
< 0.0 5
5.00
5.0
( 0.0)
< 0.0 >
s.oo
1.6
( 1-6)
< 1.79>
1.00
2.0
( 2.3)
< 1.50>
1.00
1.5
( 1.2)
< 1.50>
1.00
1.6
( 1-0)
< 1.79>
1.00
1.9
( 1.6)
< 0.71>
1.00
6.4
( <».5)
< 0.00>
6.40
2.1
( 1.5)
< 0.42>
1.00
1.5
( 1.2)
< 1.79>
1.00
1.8
( 1.5)
< 1.12>
1.15
7.5
( 11.2)
< 1.42>
3.30
3.9
( 3.9)
< 0.66>
2.70
2.0
( 1.2)
< 0.03>
1.95

-------
Table C.13,  continued
30312
40231

40*21
21230

40311

10541

21152


10731


10932


AT 10.0
SD ( 0.0)
S < 0.0 >
(ID 10.00
AT 10.2
SD ( 0.4)
S < 1.50>
ND 10.00
AT 10.0
SD ( 0.0)
S < 0.0 >
no 10.00
AT 10.0
SD { 0.0)
S < 0.0 >
no 10.00
AT 10.0
SD ( 0.0)
S < 0.0 >
no 10.00
AT 10.0
SD ( 0.0)
S < 0.0 >
no to.oo
AT 24.9
SD ( 0.0)
S < 0.0 >
•n * ** * A •
flD * w »»p
AT 10.0
SD ( 0.0)
S < 0.0 >
DO »•«**•
AT 10.0
SD ( 0.0)
S < 0.0 >
flD ******
2.0
( 0.0)
< 0.0 >
2.00
3. 1
( 2.7)
< 1.79>
2.00
2.1
( 0.1)
< 0.59>
2.00
2.3
( 0.8)
< 1.79>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 )
******
2.0
( 0.0)
< 0.0 >
******

2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 5
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
******

1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
J.O
( 0.0)
< 0.0 >
1.00
1.3
( 0.6)
< 1.79>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
{ 0.0)
< 0.0 :>
1.00
1.0
{ 0.0)
< 0.0 >
******
1.0
( 0.0)
< 0.0 >
******
1.0
( 0.0)
< o.o •>
******

1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 5
1.00
1.0
( 0.0)
< 0.0 >
1.00
1. 3
( 0.8)
< 1.79>
1.00
1. 0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
******
1.0
( 0.0)
< 0.0 >
**••*•
1.5
( 0.0)
< 0.0 >
******

5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
s .00
5.0
( 0.0)
< 0.0 >
5.00
5. 0
{ 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0. 0 >
5.00
5. 0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
******
5.0
( 0.0)
< 0.0 >
******
5.0
( 0.0)
< 0.0 >
******

2.5
( 1.9)
< 0.61>
1.85
1.8
( 1-3)
< 0.86>
1 00
1.0
( 0.0)
< 0.0 >
1.00
27
• /
( 2.4)
< 0.69>
1.00
30
. y
( 6.5)
< 1.50>
1.00
2-t
• I
( 2.0)
< 0.14>
2.45
8 a
. 7
( 0.0)
< 0.0 >
******
5.0
( 0.0)
< 0* 0 >
******
1.0
( 0.0)
< 0. 0 >
******
   AV = Arithmetic Average
   SD = Standard Deviation
    S = Skewness
   MD = Median

-------
ON
           ORGMICS(PPB)
fELL
*•*••••••••*•••
10112  »T *
       SO
       3
       no

10211  »T
       SO
       S
       no

10521  »T
       SO
       S
       HD

105*2  IT
       SD
       S
       NO

10931  »T
       SD
       S
       no

20112  »T
       50
       S
       HD

202*3  »T
       SD
       S
       no

20721  IT
       SD
       S
       HO
                                                Table  C.14
                                      Hancock  Wells After  Baseline
                                      Priority Organic Pollutants
         211*1
         •0331
                IT
                SD
                S
                BD
                SD
                S
                no

         10232  IT
                SD
                S
                HD
(IPBTBTLENE ARTHBICEIE/PRENAT Bl E1E UTRKZINE 8ENZENE/TIICBL010BTHYLE1E BEIZElU^iriC »CIO »-T-BUTTLPH CTOL
(

(
<


(
<


(
3.0
1.7)
0.71>
2.00
3.0
1.7)
0.71>
2.00
3.5
1.7)
0.0 >
3.50
3.5
1.7)
<-0.00>


«



(
<


(



(
<


(
<


(
<


(


3.55
2.8
1.5)

2loO
3.5
1.7)
0.0 >
3.50
3.0
1-7)
0.71>
2.00
3.5
1.7)
0.0 >
3.50
3.5
1.7)
0.0 >
3.50
3.5
1.7)
0.0 >
3.50
3.0
1.7)
0.71>
2.00
7.2
<-0,66>
9.20

(
5.*
3.1)
< 0.71>
2.00
3. 1
< 0.56>
2.40
7.3
( "
.6)
<-0.36> <-0.71>


(
<


(
<


(
<


(
<


<



(
<


(
<


(
<


«
<

6.00
2.0
0.0)
0. 0 >
2.00
2.0
0.0)
0.0 >
2.00
2.*
0.9)
1. 15>
2.00
2.0
0.0)
0.0 >
2.00
*.1
3.6)
0.71>
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
10.00
13
( 18
< 1.
6.
6
( *
< 0.
6.
.9
.8)
02>
00
.0
.6)
0 >
00
«
< 0
1

(

1

(
< 1
1
12.5
( H
.0)
< 0.73>
10.
6
( *
< 0.
6.
7
( *
<-0.
10.
6
( 1
< 0.
6.
6
( *
< 0.
6.
6
( 1
< 0.
S.
00
.0
• 6)
0 >
00
.3
.6)
71>
00
.0
.6)
0 >
00
.0
.6)
0 >
00
.0
.6)
0 >
00
(
< 1
1

(
1.7
0.5)
.»5>
.60
1.1
0.1)
. 15>
.00
1.0
0.0)
. 15>
.00
3.7
*.3)
. 11>
.80
1.5
0.6)
< 0.3«>
1

(
< 0
2

(
< 1
.35
2.9
1-3)
.2»>
.70
1.8
1.1)
.08>
10.0
( 0.0)
< 0.0 >
*«••»•

(
<


(
<


(
<


(
<


(
<


(
<


(
<
1.35

(
< 0
1

(
< 1
1
7.3
( 1-6)
(
1.0
0.0)
.0 5
.00
1. 1
0.3)
. 15>
.00
1.5
0.9)
<-0.71> < 0.71>
10.
00
1
.00

(
<


(
<


(
<

0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
(

(
<


(
<


(
<


(



(
<


1



(
<


(
<


{
<


(


1.8
0.7)
2.00
1.3
0.61
0.71>
1.00
1.5
0.6)
0.0 >
1.50
1.5
0.6)
0.0 >
1.50
2.5
2.*)
1.03>
1.50
1.5
0.6)
0.0 >
1.50
1.3
0.6)
0.71>
1.00
1.5
0.6)
0.0 >
1.50
1.5
0.6)
0.0 >
1.50
1.5
0.6)
0.0 >
1.50
1.3
0.6)
0.71>
1.00

-------
Table  C.14,  continued
  10721   »f         2.8
         SD      (   1.5)
         S        <  1.15>
         HD        2.00
  10821   If
         SD
         S
         no

  109*2   If
         SD
Ui
   3.2
(  1.6)
< O.»1>
  2.00

   3.0


11032



20711



208«2



21323



30312



«0231



• 0*21



2123*



«0311



S
RD
If
SD
S
RD
If
SD
S
no
if
SD
S
RD
If
SD
S
RD
If
SD
S
RD
If
3D
S
RD
If
SD
S
HD
If
SD
S
HD
If
SD
S
HD
< 0.71>
2.00
3.0
( 1.7)
< 0.71>
2.00
3.0
( 1-7)
< 0.71>
2.00
3.0
( 1-7)
< 0.71>
2.00
3.0
( 1-7)
< 0.71>
2.00
3.0
( 1.7)
< 0.71>
2.00
3.0
( 1.7)
< 0.71>
2.00
3.0
( 1-7)
< 0.71>
2.00
2.8
( 1.5)
< 1.15>
2.00
3.0
I 1-7)
< 0.71>
2.00
                                                 2.0
                                              (  0.0)
                                              < 0. 0 >
                                                2.00

                                                 2.0
                                              (  0.0)
                                              < 0.0 )
                                                2.00

                                                 2.0
                                              (  0.0)
                                              < 0.0 >
                                                2.00
                                                 2.0
                                              (   0.0)
                                              <  0. 0 >
                                                2.00
                                        2.0
                                        0.0)
                                       0.0 >
                                       2.00

                                        3.7
                                        3.0)
                                       0.71>
                                       2.00
                                        3.9
                                      (  3.3)
                                      < 0.71>
                                       2.00

                                        3.2
                                      (  2.1)
                                      < 0.71>
                                       2.00
 3.8
 3.1)
0.71>
2.00

 2.8
 1.3)
0.71>
2.00

 2.0
 0.0)
0.0 >
2.00

 3.5
 2.7)
0.71>
2.00
   11.9
 ( 10.0)
 < 0.6U)
  10.00

    7.1
 (  7.5)
 < 0.90>
   2.60

    7.3
  10.00

    7.3
 (  ».6)
 <-0.71>
  10.00

    7.3
 (  »-6)
 <-0.71>
  10.00

    7.3
 (  »•«>
 <-0.71>
  10.00

    7.3
 (  »-6)
 <-0.71>
  10.00

   10.8
 {  9-3)
 < 0. 16>
  10.00

    7.3
 (  «-6)
 <-0.7!>
  10.00

    7.3
1 (  »-«)
 <-0.71>
  10.00

    8.0
 (  «.0)
 <-1. 15>
  10.00

    7.3
 (  «-6)
 <-0.71>
  10.00
    1.*
 (   0.5)
< 0.17>
  1.35

    1.3
 (   0.6)
< 1.»2>
  1.00

    1.6
 (   0.9)
< 0.70>
  1.10

    1.5
 I   0.5)
<-0. 1«>
  1.50

    1.8
 (   0.»)
< 0.71>
  1.60

    1.2
 {   0.3)
< 0.71>
  1.00

    1.3
 (   0.6)
< 0.71>
  1.00

    1.5
 (   0.9)
< 0.71>
  1.00

    1.9
 (   1.5)
< 0.71>
  1.00

    2.2
 (   1-0)
<-0. 19>
  2.30

    1.8
 (   1.0)
< 0.88>
  1.55

    1.5
 (   0.8)
< 0.71>
  1.00
                                                              0.0
                                                           (   0.0)
                                                           < 0.3  >
                                                            0.0
                                                              0.0
                                                           (   0.0)
                                                           < 0.0 >
                                                            0.0
                                                             0.0
                                                           (  0.0)
                                                           < 0.0 >
                                                            0.0

                                                             0.0
                                                           (  0.0)
                                                           < 0.0 >
                                                            0.0

                                                             0.0
                                                           (  0.0)
                                                           < O.D >
                                                            0.0

                                                             0.0
                                                           (  0.0)
                                                           < 0.0 >
                                                            0.0

                                                             0.0
                                                           I  0.0)
                                                           < 0.0 >
                                                            0.0
                                                                                                             0.0
                                                                                                           (  0.0)
                                                                                                           < 0.0 >
                                                                                                            0.0
                                                                                                             0.0
                                                                                                           (  0.0)
                                                                                                           < 0.0  >
                                                                                                            0.0
                                                                                                             0.0
                                                                                                           (  0.0)
                                                                                                          < 0.0 >
                                                                                                            0.0

                                                                                                             0.0
                                                                                                           (  0.0)
                                                                                                          < 0.0 >
                                                                                                            0.0

                                                                                                             0.0
                                                                                                           <  0.0)
                                                                                                          < 0.9 >
                                                                                                            0.0
    2.1
 (   1.7)
 <  0.90>
   1.50

    1.8
 (   0.9)
 <  O.SO>
   2.00

    1.3
 (   0.6)
 <  0.71>
   1.00

    3.9
 (   »-D
 <  0.66>
   2.00

    1.3
 (   0.6)
 <  0.71>
   1.00

    1.3
 (   0.6)
 <  0.71>
   1.00

    1.3
 (   0.6)
 < 0.71>
   1.00

    1.3
 (   0.6)
 < 0.71>
   1.00

    1.3
 <   0.6)
 < 0.71>
  1.00

    1.3
 (  0.6)
< 0.71>
   1.00

    1.3
 (  0.5)
< 1.15>
  1.00

    1.3
 (  0.6)
< 0.71>
  1.00

-------
       Table C.14, continued
Ui
oo
105*1 »T 1.0 6.3 7. i
SD ( 1.7) ( 7.1) ( *.6)
S < 0.71> < 0.71> <-0.71>
(ID 2.00 2.00 10.00
21152 AT 2.8 2.0 fl.O
SD ( 1.5) ( 0.0) ( «. 0)
S < 1. 15> < 0.0 > <-1. 1S>
HD 2.00 2.00 10.00
10731 AT 3.9 3.2 12.6
SO ( 2.3) ( 2.») ( 11.2)
S < 0.25> < 1. !5> < 0.75>
HO 3.50 2.00 10.00
10932 AT 3.2 2.0 8.8
SD ( 1.6) ( 0.0) ( 7.0)
S < O.»1> < 0.0 ) < 0.52>
no 2.00 2.00 10.00
VEIL CARBOR TETIACBLORIDE t-CHLOROAIHLIHE CRLOROBEMZENE
10112 AT 5.* 7.0



10211



10521



10542



10931



20112



202*3



20721



SO
S
ID
AT
SD
S
RD
AT
3D
S
HD
AT
SD
S
HO
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
SO
AT
SD
S
no
( 3.6)
< 0.20>
5.00
3.5
( 1.5)
< 0.08>
3.HO
5.0
( 0.0)
< 0.0 >
5.00
3.5
t 1-7)
< 0.0 >
3.50
3.7
( 2.0)
< 0. 10>
3.50
3.5
( 1-7)
< 0.0 >
3.50
».1
< ll9)
<-0.67>
5.00
*.o
( 1.*)
<-0.82>
• .•50
« 5.2)
<-0.71>
10.00
10.0
{ 0.0)
< 0.0 )
10.00
10.0
< 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 )
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
{ 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< o.o •>
10.00
10.0
( 0.0)
< 0.0 >
10.00
(
<


(
<


(
<


{
<

I
{
<


(
<


(
<


(
<

1.0
0.0)
o.o •>
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.7
( 0.6)
< 0.6B>
1.10
1.5
( 0.8)
< 1. 10>
1.20
1.4
( 0.6)
< 0.82>
1.20
1.5
( 1.0)
1.00
CHlOROrOIH

(
<


(
<


(
<


(
<


(
<


(
<


{
<


(
<

12.2
12.*)
0.31>
10.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.3
0.6)
1. 15>
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
0.0
« 0.0)
< O.J >
0.0
0.0
< 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 )
0.0
2-CBLORt PHENOL

(
<


J
<


1
<


(
<


(
<


(
<


(
<


f
<

1.3
).6|
0.71>
1.00
1.3
0.6|
0.71>
1.00
1.5
0.61
0.0 >
1.50
1.5
0.6)
0. 0 >
1.50
1.3
0.5)
1. 15>
1.00
1.5
0.6)
0.0 >
1.50
1.3
0.61
0. 71>
1.00
1.5
3.6)
0. 0 >
1.50
1.1
( 0.6)
< 0.71>
1.00
2.2
< 1.7)
< 0.93>
1.50
2.0
< O.B2>
1.50
1.9
( 1.1)
< 0. 74>
2.00
1-CHLOROTBT 1ADECAIE

I
<


(
<


<



(
<


(
<


(
<


(
<


(
<

2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
3.*
1-9)
0.76>
2.75
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
3.3
2.2)
0.71>
2.00
2.0
0.0)
0.0 >
2.00

-------
          Table  C.14,  continued
MD
21 1« 1



40331



10232



10721



10021



108*2



11032



20711



206*2



21323



30312



40231



40421



»T
3D
S
no
»T
3D
S
8D
IT
SO
S
no
»T
SO
S
no
IT
SD
S
no
IT
SO
S
no
IT
SD
S
BO
IT
SO
S
HD
IT
SD
S
no
AT
3D
S
HO
IT
SD
S
no
IT
3D
3
no
IT
SD
S
ND
3.6
I 1-6)
<-0.07>
3.90
3.6
r 1.6)
<-0.02>
3.65
3.4
( LSI
< 0.31>
3.10
3.4
1 1.6)
< 0.05>
3.25
4.6
( 1.5)
<-1.2B>
5.00
3.1
( 1.6)
< 0.66>
2.40
3.0
( 1-7)
< 0.71>
2.00
3.1
( 1-7)
< 0.68>
2.30
3.0
( 1.7)
< 0.71>
2.00
3.0
( 1-7)
< 0.71>
2.00
3.0
( 1.8)
< 0.70>
2.00
3.2
( 1-6)
< 0.63>
2.50
3.3
( 1.5)
< 0.38>
1.00
   10. 0
 (   0.0)
<  0.0 >
 10.00

   10.0
 (   0.0)
<  0.0 >
 10.00

   10.0
(   0.0)
<  0.0 >
 10.00

   10.0
(   0.0)
<  0.0 >
 10.00

   10.0
(   0.0)
<  0.0 >
 10.00

   10.0
(   0.0)
<  0.0 >
 10.00

   10.0
(   0.0)
< 0.0 >
 10.00

   10.0
(   0.0)
< 0.0 >
 10.00

   10.0
(   0.0)
<  0.0 >
 10.00

   10.0
(   0.0)
< 0.0 >
 10.00

   10.0
t   0.0)
< 0.0 >
 10.00

   10.0
f   0.0)
< 0.0 >
 10.00

   10.0
(   0-0)
< 0.0 >
 10-09
    1.0
(  o-o>
< 0.0 >
  1.00

   i.o
(  0.0)
< 0.0 >
  1.00
                                                                    1.0
                                                                    0.0)
                                                                   0.0 >
                                                                   1.00
    1.0
 (   0.0)
< 0.0 >
  1.00

    1.1
 (   0.2)
< 1.50>
  1.00
   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00
                                                                    1.0
                                                                 t   0.0)
                                                                 <  0.0  >
                                                                   1.00
                                                                    1.0
                                                                    0.0)
                                                                   0.0  >
                                                                   1.00

                                                                    1.0
                                                                    0.0)
                                                                   0.0  >
                                                                   1.00
                                                                    1.0
                                                                 (   0.0)
                                                                 <  0.0  )
                                                                   1.00
                                                                    1.0
                                                                 (   0.0)
                                                                 <  0.0 >
                                                                   1 .00
                                                                                         1.0
                                                                                      (   0.0)
                                                                                      <  0.0  >
                                                                                        1.00
                                                                                         1.0
                                                                                      (   0.0)
                                                                                      <  0.0 >
                                                                                        1.00
                        1.0
                        0.0)
                       0.0 >
                       1.00

                        1.7
                                                                                        1.00

                                                                                         1.4
                                                                                     (   1-0)
                                                                                     <  1.50>
                                                                                        1.00

                                                                                         1.0
                                                                                     I  0.0)
                                                                                     < 0.0 >
                                                                                       1.00
                       1.0
                    {  0.0)
                    < 0.0 >
                      1.00

                       1.0
                    {  0.0)
                    < 0.0 >
                      1.00

                       6.1
                    (  8.8)
                    < 0.71>
                      1.00

                       1.0
                    (  0.0)
                    < 0.0 >
                      1.00

                       1.0
                    (  0.0)
                    < 0.0 >
                      1.00
                       1.0
                       0.0)
                      0.0 >
                      1.00

                       1.2
                       0.«)
                      0.71>
                      t 09
                                            1.5
                                          (  0.61
                                         < 0. 0 >
                                           1. SO
                                            1.5
                                          (  0.6)
                                         < 0.0 >
                                           1. SO
                                            1.3
                                         (   0.6)
                                         <  0.7 1>
                                           1.00
                                                                                                             1.5
                                                                                                          (  0.6)
                                                                                                          < 0. 0 >
                                                                                                            USD
    1.4
 I   3.5)
 <  0.41>
   1.00

    1.3
 (   0.6)
 <  0.71>
   1.00

    1.3
 (   0.6)
 <  0.71>
   1.00

    1.3
 (  9.61
 <  0.71>
   1.00

    1.3
 I  0.61
 <  0.71>
   1.00

   1.3
 (  0.6)
< 0.71>
   1.00

   1.3
 (  0.6)
< 0.71>
   1.00
                                           1.3
                                        (  0.6)
                                        < 0. 71>
                                          1.00
                                           1.3
                                        (  J-6)
                                        < 0. 7t>
                                          1.00
    2.0
 I  0.01
 < 0.0 >
   2.00

    3.2
 (  2.1}
 < 1.15>
   2.00

    2.0
 (  0.0)
 < 0.0 >
   2.00

    2.0
 (  0.1)
 <-1.15>
   2.00

    2.0
 (   0.0)
 <  0.0 >
   2.00
    2.0
 (  0.0)
 < 0.0 >
   2.00

    2.4
 (  0.6)
 < 0.71>
   2.00
                                                                                                                               2.0
                                                                                                                             (  0.0)
                                                                                                                             < 0.0 >
                                                                                                                              2.00
                                                               2.0
                                                            I   0.0)
                                                            <  0.0 >
                                                              2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   8.9
I 11.9)
< 0.71>
  2.00

   1.7
(  0.5)
<-0.71>
  2.00

   2.0
<  0.0)
< 0.0 >
  t/00

-------
Table  C.14,  continued
*0421



2123*



40311



105*1



21152



10731



10932



IT
SD
S
no
IT
SD
S
(ID
IT
SD
S
*D
IT
SD
S
HO
IT
SD
S
no
IT
SD
S
no
IT
SD
S
no
3.3
{ 1-5)
< 0.38>
3.00
2.6
( 1.«)
< 1.10>
2.20
3.0
( 1.7)
< 0.71>
2.00
3.3
( 1-6)
< 0.50>
2. SO
3.5
( 1.8)
<-0.00>
3.50
2.8
{ 1.5)
< 1.15>
2.00
3.0
( 2.0)
< 0.00
2.90
                                      10.0
                                    (   0.0)
                                    <  0.0  >
                                     10.00

                                      10.0
                                    (   0.0)
                                    <  0.0  >
                                     10.00

                                      10.0
                                    (   0.0)
                                    <  0.0  >
                                     10.00

                                      10.0
                                    (   0.0)
                                    <  0.0  >
                                     10.00

                                      10.0
                                    (   0.0)
                                    <  0.0  >
                                     10.00

                                      10.0
                                    (   0.0)
                                    <  0.0  >
                                     10.00

                                      10.0
                                    {   0.0)
                                    <  0.0  >
                                     10.00
   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< o.o •>
  1.00

   1.0
I  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00

   1.6
(  1.3)

  1.00
   1.0
   0.0)
  0.0 )
  1.00
                        1.2
                     {   0.«)
                    < 0.71>
                      1.00

                        1.3
                     (   0.5)
                    < 1.15>
                      1.00
    1.0
(  0.0)
< 0.0 >
  1.00

    1.0
(  0.0)
< 0.0 >
  1.00

    1.1
(  0.3)

  KOO

    1.0
(  0.0)
< 0.0 >
  1.00
   1.0
(  0.0)
< 0.0 >
  1.00
                       1.3
                     (  3.6)
                    < 0.71>
                      •i.oo

                       1.3
                     I  0.51
                    < 1.  15>
                      1.00
   1.3
I  0.6)
< 0. 71>
  1.00

   1.3
I  0.6)
< 0.71>
  1.00

   1.3
«  0.5)
< 1. 15>
  1.00

   1.7
I  0.9)
< O.M>
  1.50
   1.*
(  0.51
< 0. M>
  1.00
                      2.0
                   (  0.0)
                   < 0.0 >
                     2.00

                      3.0
                   (  1.9)
                   < 1.15>
                     2.00
                                                               2.0
                                                            I   0.0)
                                                            < 0.0 >
                                                             2.00
                                                              2.0
                                                            (  0.0)
                                                            < 0.0  >
                                                             2.00

                                                              3.1
                                                            (  2.2)

                                                             2*00
                                                               3.0
                                                               1.9)
                                                              1.tS>
                                                              2.00
                                                               2.0
                                                            (   0.0)
                                                            < 0.0 >
                                                             2.00
 IBIL    DIBOTTLPHATRAUTE  2.3-DICHT.OBOimillB   3, «-DICBLOB01IILIBS   DICBIOROBBIZEIE B  DICHIOBOBEMBIE P  OICHLOIOBBIIB*B O
 ••••••••••••••••••••••••ft********************************************************************************************************
 10112  IT      1«.9                 3.1                   8.3                  1.7                1.7                1.3
        SD    (  5.5)             (   1.7)               (  11.0)              |  0.6)             |  0.6)             (  0.6)
        S     < 0.«6>            < 0.70>               <  0.71>              <-0.63>             <-0.71>              < 0.71>
        (ID     13.«0               2.20                  2.00                 2.00               2.00               1.00
10211



10521



105«2



10931



IT
SD
S
no
IT
SD
S
no
IT
SD
S
(ID
»T
SD
S
no
9.7
( 7.6)
< 0.71>
5.40
' «.5
( 3.7)
< 0.91>
3.10
3.8
( 3.7)
< 1.15>
2.00
8.3
( 5.2)
<-O. 2B>
9.00
                                     3.0
                                  (   1.7)
                                 < 0.71>
                                   2.00

                                     3.5
                                  (   1-7)
                                 < 0.0 J
                                   3.50
                                     1.5
                                  (   1-7)
                                  < 0.0 >
                                   3.50

                                     2.8
                                  (   1-5)
                                  <  1 . 1 5>
                                   2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
i  0.0)
< 0.0 >
  2.00
   2.0
   0.0)
  0.0 >
  2.00

   3.9
   3-B)
                       1.6
                    <  0.5)

                      1.70

                       1.6
                    I  0.5)

                      1.70

                       2.1
                    (  1.0)

                      2! oo

                       1.3
                    (  0.5)
                    < 1. 15>
                      1.00
                       1.3
                    I   0.6)
                    < 0.71>
                     1.00

                       1.5
                    <   0.6)
                    < 0.0 >
                     1.50

                       1.5
                    (   0.6)
                    < 0.0 >
                     1.50
                       1.3
                      0.5)
                     1.3
                  I  0.6)
                   < 0.71>
                    1.00

                     1.8
                  I  0.5)
                   <-1. 15>
                    2.00

                     1.5
                  (  0.6)
                   < 0.0 )
                    1.50

                     1.3
                  (   0.5)
                   < 1.15>
                    t.oo

-------
Table  C.14,  continued
  20112  »T       «.«
         SD     (  3. 1)
         S     < 0.58>
         HD      3.50
202*3



20721



211*1



*0331



10232



10721



10821



108*2



11032



20711



208*2



IT
SD
S
RD
IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
RD
IT
SD
S
RD
IT
SD
S
RD
IT
SD
S
RD
IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
HD
IT
3D
S
RD
t*.6
( 1«. 9)
< 0.61>
7.90
3.1
i 2.3)
< 1.15>
2.00
2. ft
( 1-1)
< 1.15>
2.00
2.9
I 1.9)
< 1. 15>
2.00
8.3
( 2.0)
<-0.52>
8.90
8.0
( «-7)
<-0. 18>
8.30
5.3
( *.9)
< 0.*5>
2.00
7.3
{ 5.0)
<-o. m
7.80
12.9
( 2.3)
<-0.70>
1*. 10
7.7
( 7.*)
< 0.58>
5.00
8.5
i 11-3)
< 0.71>
2.00
   3.5
(  1-7)
< 0.0 >
  3.50

   8.2
(  8.2)
< 0.60>
  5.10
                                      J.5
                                      1.7)
                                    0.0 >
                                    3.50

                                      3.5
                                      1.7)
                                    0.0 >
                                    3.50
   3.5
(  1.7)
< 0.0 >
  3.50

   3.0
(  1.7)
< 0.71>
  2.00

   3.3
(  1.5)
< 0.13>
  3.10

   3. 1
(  1.8)
< 0.33>
  2.00

   3.0
(  1.7)
< 0.71>
  2.00

   3.0
(  1-7)
< 0.71>
  2.00

   3.0
(  1-7)
< 0.71>
  2.00

   3.0
(  1.7)
< 0.71>
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
• 2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
                                                           2.0
                                                           0.0)
                                                          0.0 >
                                                          2.00

                                                           2.2
                                                           0.3)
                                                          1.15>
                                                          2.00
                                                           2.0
                                                        (   0.0)
                                                        < 0.0 >
                                                         2.00

                                                           2.0
                                                        (   0.0)
                                                        < 0.0 >
                                                         2.00
                                                          2.0
                                                          0.0)
                                                         0.0 >
                                                         2.00

                                                          2.0
                                                          0.0)
                                                         0.0 >
                                                         2.00
                                             1.6
                                             0.5)
                                           -0.31>
                                            1.70

                                             3.2
                                             3.0)
                                            0.62>
                                            2.00

                                             2.0
                                             0.8)
                                           -0.11>
                                            2.00

                                             1.5
                                             0.6)
                                            0.0 >
                                            1.50
                                             1.5
                                          (   0.6)
                                         < 0.0 >
                                           1.50

                                             1.3
                                          (   0.6)
                                         < 0.71>
                                           1.00
                                             1.5
                                         <   0.6)
                                         < 0.05>
                                           1.50
                                            1.*
                                         (  0.5)
                                         < O.*1>
                                           1.00

                                            1.3
                                         (  0.6)
                                         < 0.71>
                                           1.00
                                            1.3
                                            0.6)
                                           0.71>
                                           1.00

                                            1.3
                                            0.6)
                                           0.71>
                                           1.00
                                                          2.0
                                                        (  0.0)
                                                        < 0.0 >
                                                         2.00
                                            1.3
                                         (  0.6)
                                         < 0.71>
                                           1.00
    1.5
 I  0.6)
 < 0.0 >
   1.50

    1.3
 I  0.6)
 < 0.71>
   1.00

    1.5
 (  0.6)
 < 0.0 >
   1.50

    1.5
 <  0.6)
 < 0.0 >
   1.50

    1.5
 I  0.6)
 < 0.0 >
   1.50

    1.3
 (   0.6)
 <  0.71>
   1.00

    1.3
 {   0.5)
 <  1.15>
   1.00

    1.*
 I   0.5)
 < 0.41>
   1.00

    1.3
 I   0.6)
 < 0.71>
  1.00

    1.3
 I   0.6)
 < 0.71>
  1.00

    1.3
 (   0.6)
 < 0.7  1>
  1.00

    1.3
 I  0.6)
< 0.71>
  1.00
    1.9
 (  0.7)
  <-0.23>
   2.00

    1.3
 (  0.6|
  < 0.71>
   1.00

    1.8
 (  0.6)
  <-0.93>
   2.00

    1.7
 (  0.5)
  <-0.95>
   1.90

    i.a
 (   0.6)
  <-0.93>
   2.00

    1.3
 (   0.6)
 <  0.71>
   1.00

    1.3
 (  0.5)
 <  1.15>
  1.00

   1.*
 (  0.5)
 < O.«t>
  1.00

   1.3
 (  0.6)
 < 0.71>
  1.00

   1.3
 I  0.6)
 < 0.71>
  1.00

   1.3
(  0-6)
 < 0.71>
  1.00

   1.*
(  0.8)
 < 0.7I>
  1.00

-------
          Table C.14,  continued
ON
ho
21323



30312



•0231


• 0*21



2123*



H0311



105*1



21152



10731



10932



WELL
10112



10211



AT
SD
S
HD
AT
SD
S
no
AT
SD
S
no
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
RD
AT
3D
3
RD
AT
SD
S
HD
AT
SD
S
HD

AT
SD
3
HD
AT
SD
S
no
12.5
( 5.0)
< 0.5«>
10.90
13.7
( 3.*)
<-0.0<>
13.80
».7
« 3.1)
< 0.39>
• .00
10.0
( 2.0)
<-0.52>
10.60
10.*
( 7.7)
< 0.38>
9.50
16.*
( 6.9)
<-0. 12>
16.90
6.6
( 6.9)
< 0.68>
3.30
6.3
( 3.2)
<-0.57>
6.90
8.2
( 5.5)
<-0. 1 1>
8.55
5.6
{ 3.6)
< 0.22>
6.40
DICHLOBORETHANE
1.0
( 0.0)
< 0.0 >
•••*•*
0.0
( 0.0)
< 0.0 >
0.0
3.0
( '-7)
< 0.71>
2.00
3.0
( '.7)
< 0.71>
2.00
3.2
( 1.6)
< 0.63>
2.50
3.2
{ 1.6)
< 0.63>
2.50
2.8
( 1.5)
< 1. 15>
2.00
3.0
( 1-7)
< 0.71>
2.00
3.0
{ 1.7)
< 0.71>
2.00
2.8
( 1-5)
< 1.1 5>
2.00
2.8
( 1.5)
< 1 . 1 5>
2.00
• .3
( 1^9)
<-0.0*>
5.00
2,«-DICRLOROPREN3L
2.0
( 1-0)
< 0.0 >
2.00
2.7
{ 0.6)
<— 0. 7 t>
3.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 )
2.00
2.0
( 0.1)
< 0.71>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
DIETRTLPRTHALATE
23.6
C 21.D
< 0.21>
21.10
25.8
( 23.6)
< 0.56>
17.. 70
    1.3
(   0.6)
< 0.71>
  1.00

    1.3
(   0.6)
< 0.71>
  1.00

    1.3
(   0.6)
< 0.71>
  1.00

    1.3
(   0.6)
< 0.71>
  1.00

    1.3

< 0.60>
  1.20

    1.3
(   0.6)
< 0.71>
  1.00

    1.3
(   0.6)
< 0.71>
  1.00
                                                                                       1.3
                                                                                       0.5)
                                                                                      1. 15>
                                                                                      1.00

                                                                                       1.3
                                                                                       0.5)

                                                                                      KOO
                                                                                    (  0.5)
                                                                                    < O.«1>
                                                                                      1.00
   1.3
<  0.6)
< 0.71>
  1.00

   1. 3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
I  0.6)
< 0.71>
  1.00

   1.3
<  0.5)

  iloo

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
C  0.6)
< 0.71>
  1.00

   1.3
I  0.5)

  1.00

   1.3
«  0.5)
< 1.15>
  1.00
                    I  0.5)
                   < O.*1>
                     1.00
     1.3
  (  0.6)
   < 0.71>
    1.00

     1.5
  (  0.8)
   < 0.71>
    1.00

     1.4
  I  O.S)
   < 0.«5>
    1.30

     1.3
  I  0.6)
   < 0.71>
    1.00

     1.3
  <  0.5)
   < 1.15>
    1.00

     1.3
  I  0.6)
   < 0.71>
    1.00

     1.3
  I  0.6)
   < 0.71>
    1.00

     1.3
  I  0.5)
   < 1. 15>
    1.00

     1.3
  I  0.5)
   < 1.15>
    1.00

     1.6
  I  0.6)
   <-0.39>
    2.00
                                                                              DIISOOCTTLPBTHiLITI  0IOCTTLWTH»LiT»  DODBC1IOIC »CID
                                                            • ••••••ft************************************************************************
                                                                                     15.3                 2.9              0.0
                                                                                   (17.5)              (1.3)           (  0.0)
                                                                                   < 0.0 >             < 0.0 >          < 0.0 >
                                                                                    15.35                2.95             0.0
                                                                                     • 0.6
                                                                                   <  0.0)
                                                                                   < 0.0 >
                      2.0
                    I  0.0)
                   < 0.0 >
   0.0
(  0.01
< 0.0 >
  0.0

-------
        Table C.14,  continued
         10521  IV         0.0
                SD       (  0.0)
                S        < 0.0 >
                no        o.o
105*2  IT
       3D
       S
       HD
         10931
20112
ON
       IT
       SD
       S
       no

       IT
       SD
       S
       no
20 2* 3  IT
       SD
       S
       no

20721  IT
       SD
       S
       HD

211*1  IT
       SD
       S
       HD

•0331  IT
       SD
       S
       HD

10232  IT
       SO
       S
       HD

10721  IT
       3D
       S
       BD

10821  IT
       SD
       S
       no

108*2  IT
       SD
       S
       no
 o.o
 0.0)
o.o >
o.o

 o.o
 0.0)
o.o >
o.o

 o.o
 0.0)
0.0 >
0.0

 0.0
 0.0)
0.0 >
0.0

 0.0
 0.0)
0.0 >
0.0

 0.0
 0.0)
0.0 >
0.0

 0.0
 0.0)
0.0 >
0.0

 0.0
 0.0)
0.0 >
0.0

 0.0
 0.0)
0.0 >
0.0

 0.0
 0.0)
0.0 >
0.0

 0.0
 0.0)
o.o •>
0.0
   2.5
(  0.6)
< 0.0 >
  2.50
                                      2.5
                                   (   0.6)
                                   <  0.0 >
                                     2.50
                                               5.8
                                            (   6.3)
                                            <  1.1 »>
                                              3.00

                                               2.5
                                            (   0.6)
                                            <  0.0  >
                                              2.50

                                               2.7
                                            {   0.6)
                                            <-0.71>
                                              3.00
                                               2.5
                                            (  0.6)
                                            < 0.0 >
                                              2.50
                                               2.5
                                            (  0.6)
                                            < 0.0 >
                                              2.50
   2.5
(  0.6)
< 0.0 >
  2.50

   2.7
(  0.6)
<-0.71>
  3.00

   5.6
                                   < 1.13>
                                     3.00
(  *.«)
< 1.50>
  2.00

   2.7
(  0.6)
<-0.71>
  3.00
                                                        12.5
                                                       ( 12.1)
                                                      < 0.00>
                                                       12.20

                                                         3.0
                                                       {  2-0)
                                                      < 1.15>
                                                        2.00
                    ( 16.6)
                   < 0.57>
                    10.35

                     11.9
                    ( 18.6)
                   < 1.15>
                     2.95

                     12.8
                    ( 18.7)
                   < 0.71>
                     2.00

                      7.3
                    <  9.8)
                   < 1.15>
                     2.55

                     10.0
                    ( 16.1)
                   < 1.15>
                     2.00

                      9.*
                                                                 2.00

                                                                 16.9
                                                               ( 13.2)
                                                               <-0.55>
                                                                21.«0

                                                                 17.*
                                                               ( 1«.3)
                                                               < 0.70>
                                                                13.25

                                                                 15. 1
                                                               ( 12.8)
                                                               < 0.01>
                                                                19.60

                                                                 2*.9
                                                               ( 23-0)
                                                               < 0.01>
                                                                2*.80
                                         33.8
                                       {  »5.0)
                                       <  0.00>
                                       33.80

                                          2.0
                                       <   0.0)
                                       <  0.0 >
                                         2.00
                                        216.0
                                       (  0.0)
                                       < 0.0  >
                                       •••*••

                                        14.8
                                       < 18.1)
                                       < 0.0  >
                                        i«.eo

                                        *0.9
                                       (  0.0)
                                       < 0.0  >
                                       •••••*

                                        27.5
                                       ( 36.1)
                                       < 0.0  >
                                        27.50

                                        11.0
                                       ( 12.8)
                                       < 0.0  >
                                        11.05

                                        18.8
                                       { 23.7)
                                       < 0.0  >
                                        18.75

                                        10.1
                                       (  0.0)
                                       < 0.0  >
                                        11.7
                                      (  0.0)
                                      < 0.0 >
                                      ****••

                                         6.6
                                      (  6-5)
                                      < 0.00>
                                        6.60

                                       161.0
                                      (  0.0)
                                      < 0.0 >
                                      ••***•
                                                                                                 2.0
                                                                                              I   0.0)
                                                                                              < 0.0 >
                                                                                               2.00
                                                                                                          2.0
                                                                                                       (  0.0)
                                                                                                       < 0.0  >
                                                                                                         2.00
                                                                                                 2.0
                                                                                              (  0.0)
                                                                                              < 0.0  >
                                                                                              *•••**
                                                                                                 2.0
                                                                                              I   0.0)
                                                                                              <  0.0 >
                                                                                                2.1)0
                                                                                                 2.0
                                                                                              <   0.0)
                                                                                              < 0.0 >
                                                                                              • *••*•
                                                                                                 2.0
                                                                                              I   0.0)
                                                                                              < 0.0 >
                                                                                               2.00

                                                                                                 2.0
                                                                                              I   0.0)
                                                                                              < 0.0 >
                                                                                               2.00
                                                                                                2.0
                                                                                              I  0.0)
                                                                                             < 0.0 >
                                                                                               2.00

                                                                                                2.0
                                                                                              (  0.0)
                                                                                             < 0.0 >
                                                                                             ••••**

                                                                                                2.0
                                                                                              I  0.0)
                                                                                             < 0.0 >
                                                                                                2.0
                                                                                             (  0.0)
                                                                                             < 0.0 >
                                                                                               2.00
                                                                                                2.0
                                                                                             <  0.0)
                                                                                             < 0.0 >
                                                                                             *•«•*•
                                                                                                                  0.0
                                                                                                               (  0.01
                                                                                                               < 0.0 >
                                                                                                                 0.0
                                                                               0.0
                                                                             I  0.0)
                                                                            < 0.0 >
                                                                              0.0
                                                                                                                  0.0
                                                                                                               (   0.0)
                                                                                                               <  0.0 >
                                                                                                                 0.0

                                                                                                                  0.0
                                                                                                               (   0.01
                                                                                                               <  0.0 >
                                                                                                                 0.0

                                                                                                                  0.0
                                                                                                               (   o.oi
                                                                                                               <  0.0 >
                                                                                                                 0.0

                                                                                                                  0.0
                                                                                                               (   o.oi
                                                                                                               <  0.0 >
                                                                                                                 0.0

                                                                                                                  0.0
                                                                                                               (   0.0)
                                                                                                              < 0.0 >
                                                                                                                0.0
                                                                                                                          0.0
                                                                                                                          O.OI
                                                                                                                         0.0 >
                                                                                                                         0.0
                                                                                                                 0.0
                                                                                                              (  O.OI
                                                                                                              < 0.0 >
                                                                                                                0.0

                                                                                                                 0.0
                                                                                                              <  o.oi
                                                                                                              < 0.0 >
                                                                                                                0.0

                                                                                                                 0.0
                                                                                                              (  0.0)
                                                                                                              < 0.0 >
                                                                                                                0.0
                                                                                                                 0.0
                                                                                                                 0.0)
                                                                                                                0.0 >
                                                                                                                0.0

-------
Table  C.14,  continued
ON
11032



20711



20842



21323



30312



40231



40421



2173*



40311



10541



21152



10731



IT
SD
S
.ID
IT
SD
S
RD
IT
SD
S
no
IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
RD
IT
SD
S
RD
IT
SD
S
RD
IT
SD
S
HD
IT
SD
S
RD
IT
SD
S
RD
IT
SD
S
HD
0.0
( 0.0)
< 0.0 >
0.0
0.0
( o.oj
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
   2.7
(  0.6)
<-0.71>
  3.00

   2.7
(  0.6)
<-0.71>
  3.00

   2.7
(  0.6)
<-0.71>
  3.00

   2.7
(  0.6)
<-0.71>
  3.00

   2.7
(  0.6)
<-0.71>
  3.00

   2.7
(  0.6)
<-0.71>
  3.00

   2.7
{  0.6)
<-0.71>
  3.00

   2.8
(  0.5)
<-1.15>
  3.00

   2.7
<  0.6)
<-0.71>
  3.00

   2.7
(  0.6)
<-0.71>
  3.00

   5.1
(  5.0)
< 1.12>
  3.00

   4.9
(  4.4)
< 1.11>
  3.00
  16.5
( 11.9)
<-0.68>
 22.20

  18.9
( 1».9)
<-0.60>
 24.60

  18.5
( 17.9)
< 0.25>
 16.00

  21.5
( 20.6)
< 0.38>
 17.00

  62.3
( 40.8)
< 0.65>
 44.40

  11.6
( 16.6)
< 0.71>
  2.00

  18.4
( 15.3)
<-0.40>
 21.90

  13.1
( 22.3)
< 1.15>
  2.00

  16.3
{ 18.3)
< 0.58>
  9.70

  23.1
( 11-7)
< 0.64>
 18.10

  12.4
( 12.8)
< 0.30>
  9.90

  19.0
( 16.3)
< 0.25>
 17.«0
                                                                             20.0
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                             23.5
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                           ******

                                                                             33.6
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                           *••*•«

                                                                             83.6
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                             99.4
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                           ******

                                                                             31.3
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                           •••*••

                                                                             31.8
                                                                           (  0.0)
                                                                           < 0.0 1
                                                                           •*••••

                                                                             11.*
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                           *••»••

                                                                             45.2
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                           *•**••

                                                                            378.0
                                                                           <  0.0)
                                                                           < 0.0 >
                                                                           ••*»•*

                                                                             16.9
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                           **»«•«

                                                                            *••••
                                                                           (  0.0)
                                                                           < 0.0 >
   2.0
(  0.0|
< 0.0 >
******

   2.0
(  0.0)
< 0.0 >
»•••**

   2.0
<  0.0)
< 0.0 >
******

   2.0
(  0.0)
< 0.0 >
*»*•••

   2.0
(  0.0)
< 0.0 >
   2.0
 C  0.0t
< 0.0  >
******

   2.Q
 t  0.0)
< 0.0  >
•*•»••

   2.0
 I  0.0)
< 0.0 >
*«••*•

   2.0
 I  0.0)
< 0.0 >
*•••*•

   2.0
 C  0.0)
< 0.0 >
******

   2.0
 I  0.0)
< 0.0  >
• ••**•

   2.0
I  0.0)
< 0.0 >
                                                                                                                           0.0
                                                                                                                        (   0.01
                                                                                                                        <  0.0  >
                                                                                                                          0.0
                                                                                                                           0.0
                                                                                                                           0.01
                                                                                                                          0.0  >
                                                                                                                          0.0

                                                                                                                           0.0
                                                                                                                           0.0)
                                                                                                                          0.0  >
                                                                                                                          0.0
                                                                                                                           0.0
                                                                                                                        (  0.0)
                                                                                                                        < 0.0 >
                                                                                                                          0.0

                                                                                                                           0.0
                                                                                                                        (  0.0|
                                                                                                                        < 0.0 >
                                                                                                                          0.0
                                                                                                                           0.0
                                                                                                                        (  0.0)
                                                                                                                        < 0.0 )
                                                                                                                          0.0
                                                                                                                           0.0
                                                                                                                        (  0.0)
                                                                                                                        < 0.0 >
                                                                                                                          0.0
                                                                                                                           0.0
                                                                                                                           0.0)
                                                                                                                          0.0 >
                                                                                                                          0.0

                                                                                                                           0.0
                                                                                                                           0.0)
                                                                                                                          0.0 >
                                                                                                                          0.0
                                                                                                                           0.0
                                                                                                                        (  0.0)
                                                                                                                        < 0.0 >
                                                                                                                          0.0
                                                                                                                           0.0
                                                                                                                        I  0.0)
                                                                                                                        < 0.0 >
                                                                                                                          0.0
                                                                                                                           0.0
                                                                                                                           0.0)
                                                                                                                          0.0 >
                                                                                                                          0.0

-------
Table  C.14,  continued
 10932  *f         0.0
        SD      (   0.0)
        S        <  0.0 >
       no
                 0.0
                                      3.U
                                      2.0)
                                     1.27>
                                     3.00
                               12. 3
                             (  13.8)
                            <  0.«2>
                               3.00
                                                                           J1.3
                                                                           0.00>
                                                                          31.30
                         2.0
                      I   0.01
                      < 0.0 >
                       2.00
                                                                                                                 0.0
                                                                                                              I  0.0)
                                                                                                              < 0.0 >
                                                                                                                0.0
• ELt       ETRTL BERZERE
••••*•••••••*•••«••*••••«
10112  AT       1.5
       SD    (  0.7)
       S     < 0.0 >
       HD      1.50
10211  AT
       SD
       S
       BD

10521  AT
       SD
       S
       RD

105*2  AT
       SD
       S
       RO
10931
       AT
       SD
       S
       RD
20112  AT
       SD
       S
       RD

202*3  AT
       SD
       S
       RD

20721  AT
       3D
       S
       RD

211*1  AT
       SD
       S
       RD

40331  AT
       SD
       S
       RD

10232  AT
       SD
       S
       no
       REPTADBCARE         BEIADECAHB     REIADECANOIC  ACID   BBTHTLBEPTi DE» ROATE  RETHTLHEIADECAROATE
•••••••••••••••••••ft************************************************************************************
           1.5                 2.0                1.0                   3.3                   2.0
        (  0.7)              (  0.0)            (   0.0)               (   1.8)               (   0.0)
        < 0.0 >             < 0.0 1            < 0.0 >               <  0.00>               <  0.0 >
          1.50              ••••»«             •••••»                  3.30                  2.00
                 1.0
              (   0.0)
              < 0.0 >
               1.00
                 1.0
              (   0.0)
              <  0.0 >
                1.00
   1.5
(  0.6)
< 0.0 >
  1.50

   1.8
(  0.5)

  2^00

   1.5
(  0.6)
< 0.0 >
  1.50

   1.7
(  0.6)

  2 ".00

   1.5
(  0.6)
< 0.0 >
  1.50

   1.5
(  0.6)
< 0.0 >
  1.50

   1.5
(  0.6)
< 0.0 >
  1.50

   1.7
(  0.6)

  2.00
           1.3
        <  0.6)
        < 0.71>
          1.00

           1.5
        (  0.6)
        < 0.0 >
          1.50

           1.5
        (  0.6)
        < 0.0 >
          1.50

           1.3
        (  0.5)
        < 1.15>
          1.00
 1.5
 0.6)
0.0 >
1.50

 2.8
 2.*)
0.57>
2.00

 1.5
 0.6)
0.0 >
1.50

 1.5
 0.6)
0.0 >
1.50

 1.5
 0.6)
0.0 >
1.50

 1.3
 0.6)
0.71>
1.00
                                                         2.0
                                                      (   0.0)
                                                      <  0.0  >
                                                      »••**•

                                                         2.0
                                                      {   0.0)
                                                      <  0.0  •>
                                                        2.00
                                                         2.0
                                                         0.0)
                                                        0.0 >
                                                        2.00

                                                         2.0
                                                         0.0)
                                                        0.0 5
                                                         2.0
                                                         0.0)
                                                        0.0  >
                                                        2.00

                                                         2.0
                                                         0.0)
                                                        0.0  >
                                                         2.0
                                                      (   0.0)
                                                      <  0.0 >
                                                        2.00
                                                         2.0
                                                      (   0.0)
                                                      <  0.0  >
                                                        2.00
                                                         2.0
                                                         0.0)
                                                        0.0 >
                                                        2.00
                                                         2.0
                                                      (   0.0)
                                                      <  0.0 >
                                                      «•*»••
   0.0
 (  0.0)
 < 0.0 >
  0.0

   0.0
 (  0.0)
< 0.0 >
  0.0

   0.0
 {  0.0)
< o.o •>
  0.0

   0.0
 (  0.0)
< 0.0 >
  0.0

   0.0
 (  0.0)
< 0.0 >
  0.0

   0.0
 (  0.0)
< 0.0 >
  0.0

   0.0
 (  0.0)
< 0.0 >
  0.0

   0.0
 (  0.0)
< 0.0 >
  0.0
                                                 0.0
                                              (  0.0)
                                              < 0.0 >
                                                0.0
                                                 0.0
                                              <  0.0)
                                              < 0.0  >
                                                0.0
   2.0
 {  0.0)
< 0.0 >
  2.00

   2.0
 (  0.0)
< 0.0 >
  2.00

   2.1
 {  0.3)

  2.00

   3.3
 (  2.6)

  2.00

   2.6
 I  1.1)
< 1.15>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
C  0.0)
< 0.0 >
  2.00

   X2
«  2.*)

  z!oo

   2.0
(  0.0)
< 0.0 >
  2.00
    2.0
 (   0.0)
 < 0.0 >
  2.00

    2.0
 (   0.0)
 < 0.0 >
  2.00

    2.0
 I   0.0)
 < 0.0 >
  2.00

    2.0
 (   0.0)
 < 0.0 >
  2.00

    3.3
 (   2.6)

  2.00

    2.0
 (   0.0)
< 0.0 >
  2.00
                                                                                        < 1. !5>
                                                                                          2.00
                                                                                           2.0
                                                                                        (  0.0)
                                                                                        < 0.0 >
                                                                                          2.00
                                                                                                                     2.0
                                                                                                                  (   0.0)
                                                                                                                  <  0.0 >
                                                                                                                    2.00
                                                                                                                     2.0
                                                                                                                  (   0.0)
                                                                                                                  <  0.0 >
                                                                                                                    2.00

-------
ON
Table
10721



10821



10842



11032



20711



20842



21323



30312



40231



40421



21234



40311



c.
AT
SD
S
no
AT
SO
S
HD
AT
SD
S
NO
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
RD
AT
SD
S
RD
AT
SD
S
RD
AT
SD
S
RD
AT
SD
S
RD
AT
SD
S
HD
14, continued
1.0
( 0.0)
< 0.0 >
1.00
1.8
( 1.7)
< 1.50>
1.00
1.7
( 0.6)
<-0.71>
2.00
1.7
( 0.6)
<-0.71>
2.00
1.7
( 0.6)
<-0.71>
2.00
1.7
( 0.6)
<-0.71>
2.00
1.7
1 0.6)
<-0.71>
2.00
1.7
( 0.6)
<-0.71>
2.00
1.7
( 0.6)
<-0.71>
2.00
1.7
( 0.6)
<-0. 71>
2.00
1.0
( 0.0)
< 0.0 >
1.00
1.7
( 0.6)
<-0.71>
2.00
   1.3
(  0.5)
< 1.15>
  1.00

   1.4
(  0.5)
< 0.41>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
i  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.5)
< 1.15>
  1.00

   1.3
{  0.6)
< 0.71>
  1.00
                                                                 2.0
                                                              (   0.0)
                                                              <  0.0 >
                                                              •*•*••
                                                                 2.0
                                                              (   0.0)
                                                              <  0.0 >
                                                                2.00
                                                                 2.0
                                                                 0.0)
                                                                0.0  >
                                                                 2.0
                                                              (   0.0)
                                                              <  0.0 >
   2.0
(  0.0)
< 0.0 >
******

   2.0
(  0.0)
< 0.0 >
******

   2.0
(  0.0)
< 0.0 >
••**••

   2.0
(  0.0)
< 0.0 >
******
 2.0
 0.0)
0.0 >
2.00

 2.0
 0.0)
0.0 >
                                                              ******

                                                                 2.0
                                                              (   0.0)
                                                              <  0.0 >
                                                              *•*•»•
                                                                 2.0
                                                                 0.0)
                                                                0.0 >
                                                                2.00
   0.0
<  0.0)
< 0.0  >
  0.0

   0.0
(  0.0)
< 0.0  >
  0.0

   0.0
(  0.0)
< 0.0  >
  0.0

   0.0
(  0.0)
< 0.0  >
  0.0

   0.0
(  0.0)
< 0.0  >
  0.0

   0.0
(  0.0)
< 0.0  >
  0.0

   0.0
<  0.0)
< 0.0  >
  0.0

   0.0
(  0.0)
< 0.0  >
  0.0

   0.0
<  0.0)
< 0.0  >
  0.0

   0.0
«  0.0)
< o.o  •>
  0.0

   0.0
I  0.0)
< 0.0  >
  0.0

   0.0
I  0.0)
< 0.0  >
  0.0
                                         2.0
                                      (   0.0)
                                      < 0.0  >
                                       2.00

                                         2.0
                                      I   0.0)
                                      < 0.0  >
                                       2.00
                                         2.0
                                      I   0.0)
                                      <  0.0 >
                                        2.00
                                         2.0
                                      (   0.0)
                                      <  0.0 >
                                        2.00
                                                                                                        2.0
                                                                                                      (  0.0)
                                                                                                      < 0.0 >
                                                                                                       2.00
                                                                                                        2.0
                                                                                                      <  0.0)
                                                                                                     < 0.0 )
                                                                                                       2.00
                                         2.0
                                      <  0.0)
                                      < 0.0 >
                                        2.00
                                                                                                        2.0
                                                                                                      (  0.0)
                                                                                                      < 0.0 >
                                                                                                       2.10

                                                                                                        2.5
                                                                                                      <  0.9)
                                                                                                      < 0.71>
                                                                                                       2.00
                                                                                                         2.0
                                                                                                      I   0.0)
                                                                                                      < 0.0 >
                                                                                                       2.00
                                         2.0
                                      (  0.0)
                                      < 0.0 >
                                        2.00

                                         2.0
                                      I  0.0)
                                      < 0.0  >
                                        2.00
                                                                2.9
                                                             I  1.8)
                                                             < 1. I5>
                                                               2.00

                                                                2.0
                                                             I  0.0)
                                                             < 0.0 >
                                                               2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2. 1
I  0.1)
< 0.71>
  2.00

   2.0
(  0.0)
< 0. 0 >
  2.00
                                                              2.0
                                                              0.0)
                                                             0.0 >
                                                             2.00
                                                                                                                              2.0
                                                                                                                           I   0.0)
                                                                                                                           <  0.0 >
                                                                                                                             2.00
   3.2
(  2.1)
< 0.71>
  2.00

   2.0
I  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   3.9
(  3-9)
< 1.15>
  2.00

   2.0
(  0,01
< 0.0 >
  2.00

-------
       Table  C.14,  continued
ON
105* 1



21152



10731



10932



tHtt
0 00 0 00 I
10112



10211



10521



105*2



10931



20112



202*3



20721



»»
SO
s
HD
IT
SD
S
80
»T
SD
S
no
IT
SD
S
HD

AT
SD
S
BO
IT
SD
S
no
»T
SD
S
no
IT
SD
S
BD
IT
SD
S
RD
IT
SD
S
no
IT
SD
S
no
IT
SD
S
no
1.0
( 0.0)
< 0.0 >
1.00
1.5
( 0.6)
< 0.0 >
1.50
1.8
( 0.5)
<-1.15>
2.00
1.6
( 0.5)
<-0. »1>
2.00
1-NETBTtlllPBTBItLEIZ
1.7
( 0.6)
<-0.71>
2.00
1.3
( 0.6)
< 0.71>
1.00
1.6
( 0.5)
<-0.31>
1.70
1.5
( 0.6)
< 0.0 >
1.50
1-3
( 0.5)
< 1.15>
1.00
1.5
( 0.6)
< 0.0 >
1.50
1.5
( 0.5)
< 0.0 >
1.50
1.8
( 0.5)
<-1.05>
2.00
1. J
( 0.6)
< 0.71>
1.00
3.1
( »-2)
< 1.15>
1.00
1.3
( 0.5)
< 1.15>
1.00
1.»
( 0.5)
< O.»1>
1.00
2-NETHTLPBEirOL
1.7
( 0.6)
<-0.71>
2.00
1.3
( 0.6)
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1.00
1.5
( 0.6)
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1.50
1.5
( 0.6)
< 0.0 >
1.50
1.3
( 0.5)
< 1.15>
1.00
1.6
( 0.5)
<-0.69>
1.80
1.3
( 0.6)
< 0.71>
t.OO
1.5
( 0.5)
<-0.07>
1.60
2.O
C 0.0)
< 0.0 >
•••*•*
2.0
( 0.0)
< 0.0 >
•«•••«
2.0
( 0.0)
< 0.0 >
••••••
2.0
( 0.0)
< 0.0 >
2.00
t-NETBTLPBEIOL
2.7
• 2.1)
< 0.53>
2.00
3.0
( 1-7)
< 0.71>
2.00
3.5
{ 1-7)
< 0.0 >
3.50
3.5
( 1.7)
< 0. 0 >
3.50
2.9
( 1-«)
< 0.98>
2.35
3.5
( 1.7)
< 0.0 >
3.50
3.0
< 1.7)
< 0.71>
2.00
3.5
< 1.7)
< 0.0 >
3.50
u.u
( 0.0)
< 0.0 >
0.0
0.0
{ 0.0)
< 0.0 )
0.0
0.0
( 0.0)
< 0.0 J
0.0
0.0
( 0.0)
< 0.0 >
0.0
I1PBTH1LEIE
2.6
( 0.5)
<-0.67>
2.80
2.2
( 0.3)
< 0.2«>
2.20
2.5
C 0.6)
< 0.21>
2.*0
1.9
( 0.7)
<-0.51>
2.00
2.3
« 1-1) '
<-0.33>
2.50
1.8
1 0.5)
<-1.05>
2.00
2.0
( 1-0)
< 0.0 >
2.00
2.1
( 0.9)
< 0.27>
2.00
4.U
C 0.0)
< 0.0 >
2.00
3.«
( 2-9)
< 1.15>
2.00
2.0
1 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
«-IOIYLFBHOL
0000 00 0 000 00 40V 0 0'
2.0
< 0.0)
< 0.0 >
• »•••*
0.0
( 0.0)
< 0.0 >
0.0
0.)
( 0.0|
< 0. 0 >
0.0
0.0
( 0.0)
< 0. 0 >
0.0
0.0
1 0.0)
< 0. 0 >
0.0
0.)
« 0.0)
< 0. 0 >
0.0
0.0
< 0.0|
< 0.0 >
0.0
0.0
( 0.0)
< 0. 0 >
0.0
                                                                                                                      (   O.Ot
                                                                                                                      <  0.0  >
                                                                                                                        2.00
                                                                                                                         2.0
                                                                                                                      (  0.01
                                                                                                                      < 0.0 >
                                                                                                                        2.00
                                                                                                                         2.0
                                                                                                                      I   0.0)
                                                                                                                      <  0.0 >
                                                                                                                        2.00
                                                                                                                         2.0
                                                                                                                      (   0.0)
                                                                                                                      < 0.0 >
                                                                                                                       2.00
       OCT1DBC1II
• ••••••••••*••»••••*••••••
          5.5
        <  3.3)

         5*90

          3.9
        (  1-9)
        < 0.0 >
         3.90

          «.*
        (  3.1)
        < 0. 58>
         3.50
                                                                                                                    C  0.8)
                                                                                                                   < 1. 15>
                                                                                                                     2.00

                                                                                                                      3.3
                                                                                                                    (  2.6)

                                                                                                                     2.00

                                                                                                                      2.0
                                                                                                                    (  0.0)
                                                                                                                   < 0.0 >
                                                                                                                     2.00

                                                                                                                      6. 1

                                                                                                                   < 0.31>
                                                                                                                     5.30

                                                                                                                      3.0
                                                                                                                    (  2.1)
                                                                                                                   < 1. 15>
                                                                                                                     2.00

-------
        Table C.14,  continued
           211*1  IT
                  SO
                  s
                  no

           «0331  IT
                  3D
                  S
                  no

           10232  IT
                  SD
                  S
                  no
ON
CD
           10721
           10821
           108*2
           11032
          20711
          208*2
          21323
          30312
          • 0231
If
SD
S
HD

IT
SD
S
HD

IT
SO
s
HD

IT
SD
S
HD

IT
SD
S
HO

IT
SD
S
RD

IT
SD
S
HD

IT
SD
S
RD

IT
SD
S
no
    1.5
 i   0.6)
 < 0.0 >
  1.50

    1.7
 <   0.5)
 <-1.03>
  1.90

    1.3
 (   0.6)
 < 0.71>
  1.00

    1.6
 (  0.8)
< 0.27>
  1.50

    1.*
 (  0.5)
< O.*1>
  1.00

    1.3
 (  0.6)
< 0.71>
  1.00
                               1.8
                            (   0.8)
                            <-0.38>
                              2.00
   1.5
(  0.5)
< 0.0 >
  1.50

   1.*
(  0.6)
< 0.6B>
  1.10

   1.3
(  0.6)
< 0.71>
  1.00

   1.6
(  0.5)
<-0.«5>
  1.70

   1.5
(  0.5)
< 0.0 >
  1.50
    1.5
 (  0.6)
< 0.0 >
  1.50

   1.7
 (  0.5)
<-0.88>
  1.85

   1.3
 (  0.6)
< 0.71>
  1.00

   1.3
 (  0.5)
< 1.15>
  1.00

   1.*
 (  0.5)
< 0.01>
  1.00

   1.3
 «  0.6)
< 0.71>
  1.00

   1.3
{  0,6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
 (  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00
                        1.3
                        0.6)
                      0.71>
                      1.00

                        1.*
                        0.6)
                      0.68>
                      1.10
   3.1
(  1.7)
< 0.0 )
  3.50

   3.5
<  1.7)
< 0.0 3
  3.50

   3.0
(  1-7)
< 0.71>
  2.00

   2.8
(  1-5)
< 1. 15>
  2.00

   3.2
(  1.6)
< 0.11>
  2.00

   3.0
(  1.7)
< 0.71>
  2.00

   3.3
(  1-5)
< 0.«5>
  2.90

   5.9
(  6,8)
< 0.71>
  2.00

   3.0
(  1.7)
< 0.71>
  2.00

   3.0
(  1.7)
< 0.71>
  2.00
 3.0
 1.7)
0.71>
2.00

 3.0
 1-7)
0.71>
2.00
                   1.6
                (   0.5)
               <-0.»9>
                 1.75

                   2.0
                (   0.8)
               <-0.11>
                 2.00

                   2.5
                (   O.«|
               <-0.53>
                 2.60

                   2.6
                (   0.5)
               <-0.09>
                 2.60

                   2.3
                (   1-2)
               < 0.95>
                 2.00

                   2.5
                (   1.5)
               < 0.0 >
                 2.50

                   2.8
                (   2.3)
               < 0.55>
                 2.00

                   1.9
                (   0.9)
               <-0.1«>
                 2.00

                   2.0
                (   1-0)
               <-0.06>
                 2.00

                   2.3
                I   1-«)
               < 0.33>
                 2.00
                                     2.8
                                   (  0.8)
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                                    2.70

                                     2.5
                                   (  1-7)
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                                    2.00
                                                                              0.)
                                                                              0.0)
                                                                             0.0 >
                                                                             0.0

                                                                              0.0
                                                                              0.0)
                                                                             0.0 >
                                                                             0.0

                                                                              0.)
                                                                              0.01
                                                                             0. 0 >
                                                                             0.0

                                                                              0.0
                                                                              0.0)
                                                                             0.0 )
                                                                             0.0
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                                                                           I  0.0)
                                                                           < 0.0 >
                                                                             0.0

                                                                              0.)
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                             0.0
                                                                              0.3
                                                                           I  0.0)
                                                                           < 0. 0 >
                                                                             0.0

                                                                              0.0
                                                                           (  o.oi
                                                                           < 0. 0 >
                                                                             0.0

                                                                              0.3
                                                                           I  0.0)
                                                                          , < 0.0 >
                                                                             0.0

                                                                              0.3
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                             0.0
                                        0.0
                                      I  0.0)
                                      <  0. 0 >
                                        0.0

                                        0.3
                                      (  0.0)
                                      <  0.0 >
                                        0.0
                                                                                                            2.0
                                                                                                         (  0.0)
                                                                                                         < 0.0 >
                                                                                                           2.00

                                                                                                            3.6
                                                                                                         I  3.3)
                                                                                                         < 1. 15>
                                                                                                           2.00

                                                                                                            5.5
                                                                                                         (  3.1)
                                                                                                         <-0. 65>
                                                                                                           6.90
                                                                                                                             2.1
                                                                                                                           (  0.3)
                                                                                                                           <  1. 15>
                                                                                                                             2.00
                                                                                                                              2.0
                                                                                                                           (   0.0)
                                                                                                                           <  0.0  >
                                                                                                                             2.00
  0.71>
  2.00

   5.2
   5.5)
  0.71>
  2.00

   3.*
   2.5)
  0:71>
  2.00
   3.3
<  2.3)
< 0.71>
  2.00

   2.7
(  1.3)
< 0.71>
  2.00

   3.6
I  2.8)
< 0. 71>
  2.00

   2.1
(  0.1)
< 0.71>
  2.00

-------
Table C.14, continued
lent i



2123*



«0311



10541



21152



10731



VJ 10932
ON
MD

tELL
10112



10211



10521



105*2



10931



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SO
5
no
IT
SD
S
RD
IT
SD
S
HD
IT
SD
S
HD
IT
SO
S
no
IT
SD
S
(ID
IT
SD
S
no

IT
SD
S
HD
IT
SD
S
no
IT
SD
S
HD
IT
SD
S
no
IT
SD
S
no

(
<


(
<


(
<


(
<


(
<


(
<


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PBEIOt
5.5
( 6.4)
< 0.0 >
5.50
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< 0.71>
1.00
5.5
( 5.1)
<-0.00>
5.60
5.5
( 5.2)
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5.50
«.7
( 4.5)
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3.85
1.5
0.5)
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1.60
1.7
0.8)
0.33>
1.50
1.3
0.6)
0.71>
1.00
1.3
0.6)
0.71>
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1.3
0-5)
1. 15>
1.00
3.2
3.7)
1. 10>
1.50
1.*
0.5)
0.41>
1.00
PBOPIZIHB
6.8
( *• 3)
<-0.61>
8.50
7.3
( 4.6)
<-0.7 1>
10.00
6.0
( 4. 6)
< 0.0 >
6.00
6.0
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6.00
8.0
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10.00
1.3
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1.00
1.3
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1.00
1.3
( 0.6)
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1.3
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1,00
1.3
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1.00
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1.00
1.*
( 0.*5)

t'.OO
I-TBHPIBBOL
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
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1.00
1.5
( 0.6)
< 0.0 >
1.50
1.5
( 0.6)
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1.50
1.3
( 0.5)
< 1.15>
1.00
3.0
( 1.7)
< 0.71>
2.00
2.8
( 1.5)
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2.00
3.0
( 1-7)
< 0.71>
2.00
3.0
( 1-7)
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2.00
2.8
{ 1.5)
< 1. 15>
2.00
2.8
( 1.5)
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2.00
3.2
( 1.6)

2^00
TETRICSLOBOETBTLEIIE
1.5
( 0.5)
<-0.71>
1.80
2.4
{ 2-2)
< 0.70>
1.20
1.7
I 0.8)
< 0.07>
1.60
1.0
( 0.0)
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1.00
2.9
( 3.2)
< 1. 10>
1.»5

«



(
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TOLOEVB
1.0
( 0.0)
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1.00
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1.00
1.0
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0.0)
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0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.9
0.0)
0. 0 >
0.0
0.0
0.0)
0. 0 >
0.0
TtlCI





















(
<


<
<


(
<


I
<


(
<


(
<


(
<

1LOIOBTBTLEIB
1.0
( 0.0)
< 0.0 >
1.00
1.0
1 0.0)
< 0.0 >
1.00
1.5
( 0.9)
< 0.71>
1.00
1.1
I 0.1)
< 1. 15>
1.00
1.0
( 0.0)
< 0.0 >
1.00
». 5
2.3J
-0. 42>
5. 10
3.*
2.8)
1. 15>
2.00
2.9
1.6)
0.7I>
2.00
2.0
0.0)
0. 0 >
2.00
«.5
2^9)
0. 13>
4.10
4.0
2.6)
0.«6>
3. «0
2.5
1.1)
1.50>
2.00






















-------
o
Table
20112



20243



20721



21141



40331



10232



10721



10821



108*2


11032

20711



208*2



21323


C.14, continued
IT
SD
S
ND
IT
3D
S
no
IT
SD
S
no
IT
SD
S
HD
IT
SD
S
no
IT
3D
3
HD
IT
SD
S
RD
IT
SD
a
RD
IT
SD
s
HD
IT
SD
S
HD
IT
SD
S
RD
IT
SD
S
RD
IT
SD
S
5.5
( 5.2)
< 0.0 >
5.50
4.7
( 4.7)
< 0.54>
3.20
6.1
( *-5)
<-0.03>
6.40
5.5
( 5.2)
< 0.0 >
5.50
5.5
( 5.1)
<-0.00>
5.60
4.0
( 5.2)
< 0.71>
1.00
7.*
( 8.0)
< O.»1>
5.50
4.6
( *-9)
< 0.41>
1.00
4.0
( 5.2)
< 0.71>
1.00
7.0
( 5.2)
<-0.71>
9.90
5.0
( 4.6)
< 0.36>
4.10
4.0
( 5.2)
< 0.71>
1.00
4.0
( 5.2)
< 0.71>
5.6
( 4.2)
< 0.06>
5.25
7.3
( 1-6)
<-0.71>
10.00
6.0
( 4.6)
< 0.0 5
6.00
5.6
( «-2)
< 0.07>
5.20
6.0
( 4.6)
< 0.0 >
6.00
7.3
< »-6)
<-0.71>
10.00
8.0
( 4.0)
<-1.15>
10.00
6.8
( •*•)
<-0.*1>
10.00
7.3
t «.6)
<-0.71>
10.00
7.3
i 4.6)
<-0.71>
10.00
7.3
( »-6)
<-0.71>
10.00
7.3
( ».6)
<-0.71>
10.00
7.3
( 4.6)
<-0.71>
1.5
( 0.6)
< 0.0 >
1.50
1.3
{ 0.6)
< 0.71>
1.00
1.5
( 0.6)
< 0.0 >
1.50
1.5
( 0.6)
< 0.0 >
1.50
1.5
( 0.6)
< 0.0 >
1.50
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.5)
< 1.15>
1.00
1.4
( 0.5)
< 0.41>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.3
t 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0.71>

I
<


(
1.5
0.7)
0.18>
1.45
1.8
0.7)
<-0.69>


(
<


(
<


(
<


(
<


(
<


i
<


(
<

(
<


(
2.10
2.5
2.9)
1.15>
1.05
1.9
1.8)
1.15>
1.00
1.7
0.9)
0.35>
1.55
2.2
2.0)
0.71>
1.00
2.4
2.0)
0.73>
1.80
2.9
2.7)
0.61>
1.00
2.1
2.0)
0.71>
1.00
1.0
0.0)
0.0 >
1.00
2.4
1.2)
<-0.70>


(
<


(
<
3.10
1.4
0.5)
0.38>
1.30
1.6
0.7)
0. 31>

{
<


(
<


(
<


(
<


(
<


(
<


(
<


(
<


(
<

(
<


(
<


(
<


(
<
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0. 0 >
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0. 0 >
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
o.o •>
1.00
1.0
0.0)
0.0 >
1.00
1.4
0.9)
1.49>
1.00
1.1
0.1)
0.71>
1.00
1.0
0.0)
0.0 )
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
o.o >
5.0
( 0.0)
< 0. 0 >
5.00
5.0
< 0.0)
< 0.0 )
•**•*•
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0. 0 >
5.00
5.0
( 0.0)
< 0.0 >
******
5.0
C 0.0)
< 0.0 >
******
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
«•••**
5.0
( 0.0)
< 0.0 >
••*•*•
5.0
I 0.0)
< 0.0 >
******
5.0
( 0.0)
< 0. 0 >
•»*•*•
5.0
( o.oj
< 0 0 >

(
<


(
<


(
<


(
<


(
<


(
<


(
<


(
<


(
<

(
<


(
<


(
<


(
C
2.6
2.1)
0.59>
1.80
1.0
0.0)
0.0 >
1.00
1.5
0.8)
0.71>
1.00
4.1
4.3)
0.77>
2.65
2.7
2.0)
0. 12>
2.45
1. 1
0.2)
0.0 >
1.15
2.8
3.2)
0.71>
1.00
1.6
1.3)
1. 15>
1.00
5.8
6.8)
0.00>
5.80
1.0
0.0)
0.0 >
1.00
t.O
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0- 9 >

-------
Table
21323


30312



40231



40421



21234



40311



10541


21152


10731



10932

* AV
SD
S
Md
C.14, continued
JIT 4.0
SD { 5.2)
S < 0.71>
no i.oo
IT 5.6
3D ( 4.5)
S <-0.05>
HD 5.70
IT 7.2
SD ( 5.4)
S <-0.69>
BO 10.00
IT 4.0
SD ( 5.2)
S < 0.71>
RD 1.00
IT 9.3
SD ( 11.3)
S < 0.7O
no 5.50
IT 4.0
SD ( 5.2)
S < 0.71>
no i.oo
IT 4.0
SD ( 5.2)
S < 0.71>
90 1.00
IT 3.3
SD ( 4.5)
S < 1.15>
80 1.00
IT 3.3
SD ( 4.5)
S < 1.15>
no i.oo
IT 3.2
SD { 3.9)
S < 1.35>
no i.oo
7.3
( «-6)
<-0.71> •
10.00
7.3
(4.6) i
<-0.71> <
10.00
7.3
( «-6)
<-0.71>
10.00
7.3
( 4.6)
<-0.71>
10.00
9.6
( 0.8)
<-1.15>
10.00
7.3
( »-S)
<-0.71>
10.00
9.8
( 7.7)
<-0.06>
10.00
8.0
( »-0)
<-1.15>
10.00
8.0
( *,0)
<-1.15>
10.00
6.8
( «-»)
<-0.41>
10.00
1.3
{ 0.6)
C 0.71>
1.00
1.3
( 0.6)
C 0. 71>
1.00
1.3
( 0.6)
C 0.71>
1.00
1.3
( 0.6)
C 0.71>
1.00
1.3
( 0.5)
< 1.15>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.5)
< 1.15>
1.00
1.3
( 0.5)
< 1.15>
1.00
1.4
( 0.5)
< 0.41>
1.00
1.6
{ 0.7)
< 0,33>
1,50
2.2
( 2.0)
< 0.71>
1.00
1.5
( 0.9)
< 0.71>
1.00
3.3
{ 2.0)
<-0.67>
4.20
4.9
{ 5.0)
< 0.99>
3.25
1.0
( 0.0)
< 0.0 >
1.00
2.4
( 2.4)
< 0.71>
1.00
2.9
1 3.1)
< 1.13>
1.50
1.8
( 1.0)
< 0.19>
1.65
2.1
< 0.8)
<-0.31>
2.10
1.0
( 0.0)
< 0.0 >
1.00
1.0
{ 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.1
( 0.1)
< 1. 15>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 )
1.00
5.0
( 0.0)
< 0.0 >
••*•*•
5.0
( 0-0)
< 0.0 >
*•»**•
5.0
( 0.0)
< 0.0 >
******
s.o
( 0.0)
< 0.0 >
*•••»*
5.0
( 0.0)
< 0.0 >
******
5.0
( 0.0)
< 0.0 >
*•«*••
5.0
( 0.0)
< 0. 0 >
«•»***
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0. 0 >
*•••*•
3.7
< 2.3)
<-0.71>
5.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
I 0.0)
< 0.0 >
1.00
1.0
1 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0,0 >
1.00
1.0
I 0.0)
< 0.0 >
1.00
1.0
I 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
< 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
2. 1
( 2-3)
< 1.15>
1.00
= Arithmetic Average
= Standard
= Skewness
= Median
Deviation


















-------
TABLE C.15.   BASELINE  HANCOCK  WELL   INDICATOR  BACTERIA (per 100 ml)
Well No.
10212


10211


10232


10413


10521


10541


10542



Av*
SD*
F*
Av
SD
F
.Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Total
Coliforms
2724
4088
4/6
835
982
4/6
3960
3913
5/5
4190
3608
5/5
4840
4328
4/5
2000
4000
1/5
3212
4371
3/5
Fecal
Coliforms (FC)
6
1590
2/6
91
220
2/6
1655
2605
4/5
1635
2581
5/5
3462
3169
4/5
0
0
0/4
1220
2672
2/5
Fecal
Streptococcus (FS)
1723
4057
3/6
14
32
3/6
451
923
4/5
897
1875
5/5
275
519 '
4/5
42
91
2/5
115
105
4/5
£c '
FS Salmonel
0.0 	
— — — _
0/6
6.5
	
1/6
3.7
-: 	
1/5 •
3.7 	
	
2/5
12.6 	
	
1/5
0 	
	
0/5
10.6 	
	
0/5
(Continued)
                               372

-------
Table VI.32, continued
Well No.
10721


10731


10821


10842


10931

10932

11032

20112



Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F

Total
Coliforms
3305
4286
5/5
2000
	
1/1
0
0
0/6
1440-
2986
5/7
1567
2013
5/5
0
0/1
6800
2683
5/5
3161
3813
5/6

Fecal
Coliforms (FC)
2080
3067
4/5
90
	
1/1
0
0
0/6
88
160
3/7
934
1779
2/4
0
0/1
3740
2068
5/5
1250
2343
4/6

Fecal
Streptococcus (FS)
1202
2412
3/5
38
	
1/1
0
0
0/6
920
2205
2/7
57
83
3/5
0
0/1
2503
4231
5/5
2302
4066
3/6

£C
FS Salmonella
1.7 	
	
0/5
2.4 	
	
0/1
0 	
	
0/6
0.1 	
	
0/7
16.4 	
1/5
0 	
0/1
1.5 	
0/5
0.5 	
1/6
(Continued)
                                        373

-------
Table C.15,  continued
Well No.
20243


20711


20721


20842


21141


21152


21234


21323



Av-
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Total
Coliforms
2671
4128
3/6
3610
4088
5/5
3925
3352
5/6
2775
3031
5/5
2356
2911
5/6
2000
	
1/1
2158
2992
5/6
2370
2256
4/5
Fecal
Coliforms (FC)
550
1299
2/6
1423
2602
4/5
613
617
4/6
488
853
4/5
400
587
2/5
150
	
1/1
74
76
4/6
730
1255
2/5
Fecal FC ~— '
Streptococcus (FS) "FS Salmonella
52 10.6 	
122 	
2/6 2/6
2868 0.5 	
4351
4/5 1/5
458 1 .3 	
916 	
3/6 1/6
62 7.2
92 	
5/5 0/5
1951 0.2 	
4001 	
4/6 0/6
60 2.5 	
	 	
1/1 0/1
76 1.0 	
106 	
4/6 0/6
2578 0.3 	
4283 	
4/5 0/5
(Continued!
                                      374

-------
Table C.13, continued
Well No.
30312


40231


40311


40331


40421



Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Total
Coliforms
1980
3043
6/6
5800
3429
6/6
400
894
1/5
1475
3204
3/6
401
894
2/5
Fecal
Coliforms (FC)
517
765
4/6
1558
2068
3/5
220
492
1/5
367
804
2/6
300
671
1/5
Fecal FC
Streptococcus (FS) TS Salmonella
49 10.6 	
83 	
4/6 1/6
368 0.4 	
4916 	
5/6 0/6
0 » 	
	 	
0/5 0/5
148 2.5 	
212 	
4/6 2/6
0 °° 	
	 	
0/5 0/5

*Av =  Arithmetic  average
 SD =  Standard  Deviation
 F  =  Frequency of Detection
                                      375

-------
TABLE C.I6.   HANCOCK  WELLS AFTER  BASELINE INDICATOR BACTERIA (per 100 ml)
	 _____ — _ 	 ;______
Well No.
10112


1021.1


10232


10521


10541


10542


10721


10731



Av*
SD*
F*
Av
SD
F-
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Total
Coliforms
3128
2836
4/4
34653
5193
3/4
936
1576
5/5
25215
49858
4/4
573
836
3/4
1385
24312
4/4
19180
34144
5/5
568
811
4/5
Fecal
Coliforms (FC)
1006
1406
4/4
308
595
2/4
422
883
3/5
22502
44999
2/4
146
175
3/4
1038
1975
4/4
233
431
4/5
360
805
2/5
Fecal
Streptococcus
8
5
4/4
12
19
4/4"
21
23
3/5
68
57
4/4
810
1397
3/4
1699
2578
4/4
1644
2591
5/5
507
789
5/5
i£
(FS) FS Salmonell
125.8 	
	
0/4
25.7
	
0/4
20.1 	
	
0/5
330.9
	
0/4
0.2 	
	
1/4
0.6 	
	
0/4
__„
	
1/5
0.7
	
0/5
(Continued]
                                376

-------
Table C.16, continued
Well No.
10821


10842


10931


10932


11032


20112


20243


20711



Total Fecal
Coliforms Coliforms (PC)
Av
5D
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F

488
850
4/5
218
210
3/4
16032
35759
4/5
590
1187
5/6
8250
6131
4/4
13668
26889
4/4
825
1452
3/4
43275
49578
4/4

160
358
1/5
43
53
3/4
420
939
1/5
13
23
3/6
923
739
4/4
667
1219
3/4
560
1029
2/4
8700
15559
4/4

Fecal FC
Streptococcus (FS) FS Salmonella
85
176
3/5
69
89
3/4
883
1747
5/5
29
36
6/6
10110
14245
4/4
11863
22766
4/4
26
38
3/4
4705
4218
4/4

1.9 	
	
0/5
0.6 	
	
0/4
0.5 	
	
0/5
0.4 	
	
0/6
0.1 	
	
0/4
0.1
	
0/4
21.5 	
	
0/4
1.8 	
	
0/4
( Continued)
                                        377

-------
Table C.16,  continued
Well No.
20721


10842


21141


21152.


21234


21323


30312


49231



Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F
Total
Coliforms
953
1112
4/4
1430
2071
4/4
68
47
3/4
360
391
4/5
4142
7289
5/5
550
640
2/4
13675
6710
4/4
29150
35966
4/4
Fecal
Coliforms
5
10
1/4
903
1426
3/4
5
6
2/4
5
7
2/5
69
119
5/5
276
550
2/4
2025
2356
4/4
15170
29887
4/4
Fecal
Streptococcus Salmonella
68 0.1 	
83
4/4 0/4
1200 0.8 	
1225 	
3/4 0/4
1085 0.0 	
2143 	
4/4 Q/4
665 0.0 	
1261 	
5/5 1/5
19200 0.0 	
32940 	
5/5 0/5
358 0.8 	
449 	
4/4 1/4
4543 0.4 	
6431 	
4/4 0/4
11353 1.3 	
9367 	
4/4 0/4
(Continued,
                                      378

-------
Table C.16, continued
Well No.
40311


40331


40421



Av
SD
F
Av
SD
F
Av
SD
F
Total
Coliforms
828
1648
2/4
33
47
2/4
4065
7957
4/4
Fecal
Coliforms
0
0
0/4
1
2
1/4
751
1433
3/4
Fecal
Streptococcus
19
32
2/4
805
1597
3/4
1129
1928
4/4
Salmonella
0.0 	
	
0/4
0.0 	

0/4
0.7 	
	
0/4
Av- = Arithmetic Average
SD = Standard Deviation
 F = Frequency of Detection
                                        379

-------
TABLE C.17.   GRAY WELL WATER SAMPLES WHICH EQUALLED  OR  EXCEEDED  DRINKING  WATER  STANDARDS

Parameter
NO
Baseline*
Code
6880
6881
6882
6883
6884
6885
6886
6887
6888
6889

6891
6892
co 6893
6894
6896
6848
6849
6852
6854
6855
6856
6857
6864
6870
Freq*
4/6
4/6
6/6
6/6
1/6
3/6
5/6
5/7
5/6
4/4

5/5
3/6
3/5
5/5
4/5
6/6
6/6
6/6
5/5
5/5
6/6
5/5
6/6
6/6
3-N
Mercury
Chloride
Irrigation Baseline Irrigation Baseline*
Code
6880
6881
6882
6883

6885
6886
6887
6888
6889

6891


6894
6896
6848
6849
6852
6854
6855
6856
6857
6864
6870
Freq* Code Freq* Code
1/4 6880 1/6
2/4
2/4
4/4 6883 1/6

4/4 6885 1/6
4/4
3/4
1/4
1/4

3/4


4/4
2/4
3/4
4/4
4/4
4/4
4/4 6855 1/6
3/4
1/4
4/4
1/3
Freq* Code
6880
6881
6882


6885
6886
6887
6888
6889
6890
6891
6892
6893
6894
6896
6848
6849
6852
6854
6855
6856
6856
6864
6870
Freq*
4/6
4/6
2/6


5/6
3/6
5/7
4/6
3/4
1/6
4/5
5/6
5/5
5/5
5/5
6/6
6/6
6/6
5/5
4/5
6/6
5/5
6/6
6/6
Irr igat ion
Code
6880

6882
6883
6884
6885

6887
6888
6889
6890
6891
6892
6893
6894
6896
6848
6849
6852
6854
6855
6856
6857
6864
6870
Freq*
1/4

3/4
1/4
1/4
4/4

4/4
1/4
3/4
2/4
3/4
3/3
4/4
4/4
4/4
4/4
4/4
4/4
4/4
4/4
4/4
4/4
4/4
3/3
                                                                                        (continued)

-------
Parameter
Iron
Baseline*
Code
6880
6881
6882



6886
6887



6891
£ 6892
-> 6893
6894
6896





5856

6864
6870
Freq*
1/6
2/6
1/6-



1/6
1/7



1/5
4/6
1/5
4/5
1/5





1/6

2/6
2/3
Irrigationt
Code
6880
6881
6882
6883
6884

6886
6887
6888
6889
6890

6892
6893
6894
6896
6848
6849
6852

6855
6856

6864

Freq"
2/4
3/4
2/4
2/4
2/4

1/4
1/4
2/4
3/4
3/4

1/3
1/4
2/4
2/4
1/4
2/4
1/4

3/4
2/4

1/4

Manganese
IDS
Baseline* Irrigationt Baseline*
Code
6880
6881
6882
6883

6885
6886
6887
6888
6889
6890

6892
6893
6894






6856

6864

Freq* Code
2/6
2/6
1/6 6882
1/6
6884
3/6
2/6
1/7
1/6
2/6 6889
2/6

3/6 6892
3/5 6893
3/5 6894






1/6

1/6

Freq* Code
6880
6881
1/4 6882
6883
1/4 6884
6885
6886
6887
6888
3/4 6889
6890
6891
2/3 6892
3/4 6893
4/4 6894
6896
6848
6849
6852
6854
6855
6856
6857
6864
6870
Freq*
4/6
6/6
5/6
6/6
4/6
6/6
5/6
6/7
5/6
4/4
3/6
5/5
5/6
5/5
5/5
5/5
6/6
6/6
6/6
5/5
5/5
6/6
5/5
6/6
6/6
Irrigat lont
Code
6880
6881
6882
6883
6884
6885
6886
6887
6888
6889
6890
6891
6892
6893
6894
6896
6848
6849
6852
6854
6855
6856
6857
6864
6870
Freq«
1/4
4/4
3/4
4/4
1/4
4/4
2/4
4/6
1/4
4/4
4/4
4/4
3/3
4/4
4/4
4/4
4/4
4/4
4/4
4/4
4/4
4/4
4/4
4/4
3/3
(continued)

-------
    Table  C.17, continued
CD
Parameter


6880
6881
6882
6885
6886
6887
6888
6889
6891
6892
6893
6896
6848
6849
6852
6855
6856
6857
6864
Basel
Code
3/6
2/6
3/6
4/6
4/6
1/7
2/6
3/4
5/5
5/6
5/5
5/5
4/6
6/6
6/6
5/5
5/6
4/5
6/6
Sulfate Chromium " Lead
ine*
Freq*
6880
6881
6882
6885

6887
6888
6889

6892
6893
6896
6848
6849
6852
6855
6856
6857
6864
Irrigationt Baseline*
Code Freq* Code Freq*
3/4
2/4
1/4
2/4

1/4
1/4
1/4

1/4
2/4
3/4
4/4
3/4
4/4
4/4 6855 1/5
4/4
4/4
4/4
Irrigationt Baseline* Irrigationt
Code Freq* Code Freq* Code Freq*
6880 1/4














6855 1/5



                                                                                                        (continued)

-------
      Table  C.17, continued	
      Parameter	Selenium	Cadmium	     Arsenic	
               Baseline*         Irrigationt       Baseline*          Irrigationt       Baseline*          Irrigationt
              Code     Freq*    Code     Freq*    Code     Freq*    Code     Freq*    Code      Freq*    Code      Freq*


                                                  6886      1/6
     6888     1/6

                                                                                      6889      1/4
     6893     1/5

     6896     1/5       6896    2/4


     *Baseline Period = June  1980 to February 1982
     tlrrigation Period = February 1982  through October 1983
     *rrequency = Number  of sampling periodsthe well water exceeded drinking water standards for  a specific parameter/
^                 number  of sampling periods  for that well
CD

-------
                                                            Table  C.18
         Simple  Statistical  Values of Inorganic,  Physical,  and Organic Constituents Present in Ground  Water
              Beneath  Gray Farm During the Baseline Monitoring  Period  (June 1980 to February 1982)
             BELL
                      ALK1LIIITT
                      8G CAC03/L
                                      COBDOCTITITT
00
• •••••
06848



06849



06852



06854



06855



06856



06857



0686*



06870



06880



IT*
SO
s
HD
IT
SO
S
HD
IT
SD
S
ao
IT
SO
s
HD
IT
SD
3
HD
IT
SO
S
RD
IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
HD
402.
( 12.)
<-1.53>
406.
380.
( 5.)
< 1.40>
378.
380.
( 21.)
< 0. 72>
378.
398.
( 24.)
< 1.01>
389.
349.
1 »7.)
<-1.41>
366.
384.
( 20.)
<-1.40>
389.
365.
( 9.) .
< 0.42>
365.
321.
( 46.)
<-0.88>
330.
351.
( «-»
<-0.83>
353.
224.
(137.)
< 1.25>
204.
2388.
( 130.)
<-0.92>
2405.
2333.
« 125.)
< 0.01>
2345.
2368.
( 120.)
<-0.71>
2375.
2526.
( 163.)
<-0.29>
2530.
2290.
( 195.)
<-0.36>
2270.
2343.
( 299.)
<-0.38>
2375.
2254.
( 212.)
<-0.55>
2310.
2373.
( 1«3.)
<-0.50>
2415.
1982.
( 105.)
<-0.05>
1985.
1503.
{ 721.)
<-0.69>
1915.
TDS       PB          CL           S04      TOTAL «       I02/IO3         IB3
HG/L                HG/L          HG/L     HC S/t         HG  «/L         HG »/l
                ••»•••«••»•»•»»•••••»»«•••••*••••••••••••••»•»••«•••«•••«»•••••••
                                  318.       0.62          19.54          0.05
                                 (  26.)    ( 0.47)        (  5.16)       ( 0.06)
                                <  0.04>    < 0.71>       <  0.23>       < 0.91>
                                  317.       0.48          18.33          0.02
1628.
( 80.)
< 0.49>
1823.
1822.
( 51.)
<-0. 04>
1824.
1880.
( 120.)
< 0.27>
1868.
1992.
( 68.)
<-0.20>
1974.
1923.
( 71.)
<-0.44>
1917.
1962.
( 90.)
<-0.34>
1988.
1755.
( 70.)
<-0.84>
1767.
1823.
( 96.)
<-0. 19>
1836.
1536.
( 42.)
<-0.68>
1539.
1240.
( 598.)
<-0.59>
1528.
7.14
(0.16)
< 0.75>
7.14
7.20
(0.19)
< 1.54>
7.14
7.16
(0.13)
< 0.61>
7.12
7.32
(0.21)
< 0.61>
7.28
7.18
(0.09)
< 0.08>
7.17
7.35
(0.36)
< 1.38>
7.22
7.15
(0.08)
< 0.73>
7.14
7.36
(0.35)
< 1.58>
7.22
7.19
(0.16)
< 1.27>
7.15
7.32
(0.32)
< 1.70>
7. 19
487.
( 23.)
< 0.61>
477.
490.
( 32.)
< 0.80>
475.
506.
( 50.)
< 0.04>
503.
535.
( 42.)
< 0.90>
513.
380.
(190.)
<-0.88>
491.
523.
( 60.)
< 0.50>
501.
473.
( 12.)
< 0.02>
471.
466.
( 47.)
< 0.84>
459.
418.
( 16.)
< 0.39>
419.
336.
(183.)
<-0.68>
443.
                                  312.
                                 (  11.)
                                <-0.81>
                                  347.

                                  343.
                                 (  27.)
                                <  0.6S>
                                  338.

                                  357.
                                 (   8.)
                                <-0.08>
                                  358.

                                  394.
                                 I  26.)
                                <-0.49>
                                  393.

                                  354.
                                 I  33.)
                                <-0.68>
                                  361.

                                  329.
                                 (  50.J
                                <  1.35>
                                  310.

                                  354.
                                 (  24.)
                                <  0.40>
                                  346.

                                  261.
                                 (  11- >
                                <  1.04>
                                  258.

                                  231.
                                 ('07.)
                                <-0.62>
                                  28*.
  0.66
( 0.66)
< 1. 07 >
  0.37

  1.26
( 1-63)
< 0. %>
  0. "»3

  0.41
{ 0.30)
< 0. 65>
  0.33

  0.26
( 0.21)
< 0.07>
  0.30

  0.76
( 0.59)
< 0.09>
  0.70

  0.61
( 0.41)
< 0. 6S>
  0.39

  0.42
( 0.26)
< 0.67>
  0.34

  0.59
( 0.34)
<-0. 04>
  0.56

  0.57
I 0. 32)
< 0. 15 >
  0.47
 20.63
( 5.67)
<-0.04>
 21.03

 23.48
( 3.03)
< 0.28>
 22.60

 25.14
( 4.63)
<-0.84>
 27.24

 27.32
( 5.63)
< 0. 14>
 25.29

 24.91
( 9.55)
< 0.28>
 23.56

 28.66
O1.23)
< 1.2«>
 25.46

 24.35
( 3.10)
<-O.S2>
 24.76

 14.22
( 4.33)
< 0.72>
 11.79

 11.24
( 5.57)
<-0.30>
 12.62
  0.03
( 0.03)
< 1.55>
  0.02

  0.06
( 0.09)
< 1.68>
  0.02

  0.02
( 0.01)
< 0. 59>
  0.01

  0.02
( 0.02)
< 0. 84>
  0.01

  0.03
I 0.03)
< 0. 83>
  0.01

  0.02
I 0.01)
< 0.59>
  0.01

  0.05
< 0.08)
< t.67>
  0.03

  0.08
I 0.11)
< 1. 35>
  0.03

  0.13
• 0. 15)
< l.36>
  0.08

-------
          Table  C.18,  continued
CD
06881   IT
        SD
        3
        BD

06882   IT
        SD
        S
        BD

06883   IT
        SD
        S
        BD

06884   IT
        SD
        S
        HO

06885   IT
        SD
        S
        BD

06886   IT
        SD
        S
        BD

06887   IT
        SD
        S
        BD

06888   »T
        SD
        S
        BD

06889   IT
        SD
        S
        BD

06890   IT
        SD
        S
        BD

06891   IT
        SD
        S
        BD

06892   IT
        SD
        S
        BD
  257.
  ( 43.)
< 0.72>
  235.

  241.
  ( 26.)
< 1.50>
  229.

  278.
  ( 12.)
< 0.85>
  273.

  361.
  (101.)
< 1.53>
  327.

  357.
  ( «5.)
<-0.56>
  364.

  255.
  ( 75.)
<-0.63>
  275.

  293.
  ( 24.)
< 1.00>
  292.

  299.
  ( 74.)
<-1.27>
  325.

  260.
  ( 12.)
<-0.01>
  260.

  392.
                          <  1.69>
                            338.

                            2*1.
                           ( 15.)
                          <  0.67>
                            240.

                            399.
                           (100.)
                          <-0.58>
                            M2.
 1752.
( 330.)
<-0.60>
 1815.

 1603.
( 177.)
< 0.09>
 1565.

 1405.
(  84.)
< 0.49>
 1385.

 1487.
( 301.)
<• o.04>
 1530.

 2122.
( 252.)
<-1.0»>
 2160.

 1713.
( 285.)
<-0.30>
 1765.

 1531.
( 193.)
<-0.99>
 1580.

 1685.
( 397.)
<-0.17>
 1675.

 1663.
( 254.)
<-0.»5>
 1705.

 1244.
( 216.)
< 0.06>
 1250.

 1726.
( 126.)
<-1.20>
 1780.

 2165.
( 715.)
<-l.31>
 2335.
1035.
( 156.)
<-0.70>
1459.
1375.
( 38S.)
< 0.55>
1254.
1137.
( »6.)
< 0.60>
1124.
1078.
( 138.)
<-0.82>
1120.
1683.
( 1«7.)
<-0.92>
1741.
1410.
( 500.)
<-O.B6>
1599.
1467.
( 197.)
< 1.02>
1363.
1427.
( 404.)
<-0.53>
1U74.
1483.
( 63.)
< 0.28>
1477.
1010.
( 101.)
<-0.30>
1008.
1460.
( 71.)
<-0.13>
1460.
1787.
( 599.)
<-1.43>
2044.
7.59
(0.34)
< o.ua>
7.49
7.21
(0.12)
<-0.64>
7.22
7.46
(0.36)
< 1.53>
7.34
7.38
(0.35)
< 0.91>
7.25
7.47
(0.39)
< 1.39>
7.38
7.40
(0.17)
< 1.23>
7.37
7.44
(0.32)
< 1.37>
7.31
7.47
(0.23)
< 1.07>
7.46
7.28
(0.09)
< 0. 18>
7.27
7.43
(0.25)
<-0.06>
7.38
7.65
(0.41)
< 0.30>
7.18
7.23
(0.26)
< 0.77>
7.09
348.
( 84.)
<-0.04>
350.
302.
( 84.)
< 0.44>
289.
242.
( 24.)
< 0.03>
245.
226.
( 20.)
< 0.01>
225.
417.
( 79.)
<-0.42>
436.
255.
( 98.)
<-0.53>
274.
339.
( 57.)
<-1.01>
344.
343.
(102.)
<-0.39>
373.
321.
I 62.)
<-1.09>
346.
208.
( 77.)
< 0.17>
202.
316.
( 15-)
<-0.38>
315.
443.
(163.)
<-1.05>
504.
   299.
  (  16.)
 <  0.58>
   295.

   310.
  (  79.)
 <  0. 33>
   291.

   254.
  {  22.)
 <  1.06>
   251.

   180.
  (  2«-l
 <-0.66>
   184.

   306.
  I  18.)
 <-0.17>
  309.

  341.
 (H9.)
 <-0.88>
  396.

  261.
 (  6».)
 < 0.71>
  241.

  278.
 (  46.)
 <-1.15>
  288.

  356.
 (  81.)
 <-1.15>
  395.

  198.
 (  31.)
 <-0.42>
  206.

  365.
 (  34.)
<-0.99>
  3B3.

  329.
 (1".)
<-1.51>
  376.
   1. 14
 ( 1. 10)
 < 0.99>
   0.86

   1.43
 ( 2.13)
 < 1.44>
   0.64

   0.99
 ( 1.25)
 < 1.68>
   0.47

   0.90
 (  0.92)
 < 1. 11>
   0.71

   2.52
 ( 4.00)
 <  1. 48>
   0.56

   1. 11
 (  1.35)
 <  1. 30>
   0.61

   1.32
 (  1-67)
 <  1.52>
   0.74

   0.88
 (  0.66)
 <  0. 16>
   0.83

   1. 13
 <  1.56)
<  1. 10>
   0.48

   0.95
 (  1.43)
<  1. 60>
   0.37

   0. 41
 (  0. 35)
<  0. 66 >
   0.27

   6.97
 ( 10. 99)
<  1. 39>
   1.78
  12.25
 ( 5.57)
 < 1.22>
  11.15

  16.58
 ( 3.48)
 < 0.97>
  16.11

  15.71
 ( 3.99)
 < 0.32>
  15.21

   7.11
 ( 3.06)
 <-0. 19>
   8.01

  13.19
 I 9.40)
 <  0.46>
  10.96

  35.89
 (14.17)
 <-1.55>
  39.92

  25.78
 (10.91)
 <-0.28>
  26.11

  17.80
 ( 7.35)
 <-0.51>
  18.75

  18.62
 ( 4.60)
<-0.74>
  19.83

  5.05
 ( 3.36)
< 0.46>
  4.18

 35.82
 (13.11)
< 0.52>
 33.35

  9.19
 ( 7.69)
< 0.26>
  8.07
   0.09
 ( 0. 18)
 < 1.74>
   0.01

   0.09
 ( O.OS)
 < 1.27>
   0.08

   0.08
 ( 0.07)
 < 1.06>
   0.05

   0.07
 I  0.04)
 <-0.07>
   0.06

   0.93
 (  1.14)
 <  0.83>
   0.40

   0. 08
 (  0.10)
 <  0. 71>
   0.02

   0.04
 (  0.04)
 <  0. 85>
   0.01

   0.13
 (  0. 18)
 <  1. 22>
   0.05

   0.02
 (  0.02)
 <  1. I5>
   0.01

   0.06
 (  0.05)
 <  0.63>
   0.03

   0.03
 (  0.02)
<  0. 38>
   0.02

   2.05
 (  3-47)
<  1. 40>
   0.22

-------
        Table  C.18,  continued
06893



06894



06896



AT
SO
S
MD
AT
SD
S
no
AT
SD
S
HO
360.
( 55.)
<- 1. 02>
371.
301.
( 5.)
< 0.50>
299.
243.
( 55.)
< 0.93>
226.
                                2556.
                                ( 387.)
                               <-0.71>
                                2650.

                                1566.
                                ( 489.)
                               <-1.35>
                                1720.

                                2882.
                                ( 236.)
                               <-0.15>
                                2890.
2271,
( 503.)
<-0.09>
2300.
1559.
( 352.)
< 1. 16>
1492.
2261.
( 254.)
<-0.35>
2265.
7.72
(0.08)
<-0.6 1>
7.75
7.20
(0.12)
< 0.33>
7. 18
7.10
(0.12)
< 0.26>
7.09
421.
( 42.)
<-1. 48>
440.
358.
( 9.)
<-0.40>
360.
680.
(131.)
<-0.27>
710.
795.
(307.)
< 0.52>
753.
149.
( ".I
<-0.70>
148.
424.
( 43.)
<-0.23>
422.
0.73
( 0. 36)
< 0. 29>
0.68
0.57
( 0.19)
<-0.78>
0.60
0.28
( 0.26|
< 0. 24 >
0. 19
                                                                                             11.89
                                                                                             ( 4.70)
                                                                                             < 0.73>
                                                                                             11.43

                                                                                             31.92
                                                                                             ( 8.91)
                                                                                             < 0.14>
                                                                                             32.40

                                                                                             18.09
                                                                                             (10.75)
                                                                                             <-0.42>
                                                                                             20.82
                                                                                                   0.31
                                                                                                 (  0. IB)
                                                                                                 <-0.13>
                                                                                                   0.36

                                                                                                   0.20
                                                                                                 (  0.28)
                                                                                                 <  0.77>
                                                                                                   0.01

                                                                                                   0. 12
                                                                                                 (  0.08)
                                                                                                 <  0.01>
                                                                                                   0.12
CD
* AV
  SD
   S
  MD
Arithmetic Average
Standard  Deviation
Skewness
Median

-------
                                                Table C.19
       Simple Statistical Values of Inorganic,  Physical,  and Organic Constituents Present in Ground Water
           Beneath Gray Farm After the Baseline Monitoring. Period (February 1982 through October 1983)
00
WELL
• •••••
06848



06849



06852



06854



06855



06856



06857



0686*



06870



06880




' *•• •#
AT *
SD
S
BD
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
no
AT
SD
S
BD
AT
SD
S
HD
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
BO
ALKALIIIITT
BG CAC03/L
391.
( 24.)
<-0.49>
395.
325.
( 64.)
< 1.09>
299.
384.
( 3.)
< 0.90>
383.
384.
( 35.)
< 0.1 0>
381.
386.
( 5.)
< 0.69>
384.
386.
( 21.)
<-1. 13>
395.
361.
i 25.)
< 0. 76>
357.
292.
( 21.)
< 0.26>
290.
162.
( 7.)
< 0.13>
361.
140.
( 24.)

129.
CORDtlCTITtTr

2549.
( 166.)

2723.
2480.
( 274.)
< 0.97>
2390.
2919.
( 253.)
<- 1. 14>
3035.
2750.
( 164.)
< 0.23V
2735.
2899.
( 214.)
<-0.0 1>
2900.
2616.
( 384.)
<-0.67>
2726.
2704.
( 178.)
< 0. 16>
2685.
2678.,
( 167.)
< 0.04>
2675.
2440.
( 10.)
<-0.06>
2440.
1451.
( 613.)
< 1. 15>
11S7.
TDS
NG/L
1767.
( 70.)
<-0.47>
1777.
1724.
( 239.)
< 1 . 11>
1625.
1942.
( 33.)
< 0.04>
1941.
1804.
( 228.)
<-0. 99>
1896.
1971.
( 37.)

1986.
1864.
( 62.)
<-0.48>
1874.
1898.
( 97.)
< 0.58>
1880.
1815.
( 4?.)
< 0.76>
1802.
1495.
( 107.)
<-0.69>
154 A.
1066.
t 590.)
< 1. 15>
790.
PR

7.44
(0.49)
< 0.89>
7.26
7.50
(0.53)
< O.^fO
7.29
7.50
(0.40)
< 0.99>
7.36
7.43
(0.45)
< 1. 11>
7.23
7.28
(0.20)
< 0.39>
7.25
7.47
(0.55)
< 1. 11>
7.23
7.66
(0.53)
<-0.2>2>
7.71
7.52
(0.33)
< 0.90>
7.42
7.90
(0.44)
<-0.69>
B.12
7.69
(0.38)
<-0.74>
7.81
CL
IG/L
482.
( 14.)
< 0.06>
482.
425.
( inn.)
< 1. 13>
377.
535.
( 7.)
< 0.77>
533.
492.
( 19.)
<-0.03>
493.
535.
( 12.)
< 0.33>
533.
485.
( 59.)
<-1. 12>
510.
494.
{ 24.)
< 0.45>
491.
475.
( 14.)
<-0.65>
478.
440.
( 2.)
<-0.38>
440.
298.
(181.)
< 1. 15>
209.
S04
(IG/L
••••••••• ••••••4
323.
( 12.)
< 0.0 >
323.
352.
( 50.)
<-0.49>
362.
356.
( 9.)
< 0.05>
356.
362.
( 32.)
< 0.08>
361.
399.
( in.)
< 0.01>
399.
336.
( 5.)
< 0.0 >
336.
331.
( 6.)
<-0.92>
333.
387.
( 23.)
< 1. 10>
377.
271.
( 2.)
< 0.3B>
271.
277.
(111.)
<- 1. 15>
129.
TCTAL 1
1C H/l.
>•• • ••• •# 646 •••!
0.34
( 0.21)
< 0.21>
0.32
1.99
( 3.67)
< 1. 15>
0.18
0.30
( 0.16)

0.24
0.28
( 0.18)
< 0. 40>
0.26
0.37
I 0.07)
< 0. 74 >
0.35
0.40
( 0. 13)
< 0. 28>
0.38
0.25
( 0.11)
<-0.45>
0.26
0.43
( 0.30)
<-0. 03>
0.43
0.68
( 0. 35)
< 0. 70>
0.49
0.44
( 0.48)
< 0. 83>
0.26
K02/I03
NG H/L
16.89
( 9.04)
<-1.07>
20.44
23.85
( 1.20)
<-0.06>
23.90
26.42
( 5.95)
< 0.05>
26.32
20.18
( 6.14)
<-0.81>
22.05
29.92
( 5.77)
< 0.97>
28.03
14.45
( 8.79)
<-0.44>
15.58
10.70
( 8.96)
< 0.57>
9.17
27.93
( 3.95)
< 0.06>
27.82
9.52
( 5.47)
< d.69>
6.75
11.28
115.43)
< 1. 15>
1.70
«U3
BG I/I
0.02
( 0.01)
< 0. 00>
0.02
0.01
1 0. 0 )
< 0. 0 >
0.01
0.02
( 0.02)
< 0. 96 >
0.01
0.01
( 0.00)
< 1. 15>
0. 01
0.02
( 0.02)
< 1. 15>
0. 01
0. 19
( 0.31)
< 1. 13>
0.04
0.01
( 0. 0 |
< 0. 0 >
0.01
0.02
( 0.03)
< 1. 15>
0. 01
0.01
( 0.01)
< 0. 71>
0. 01
0.03
( 0.01)
<-0. 21>
0.03

-------
         Table C.19,  continued
          06681
                 »T     2*2.
                 SD    ( 14.)
                 S     < 0.16>
                 MO     241.
00
O3
 06882  »T
        SD
        S
        RD

 06883  »T
        SD
        S
        no

 0688*  IT
        SD
        S
        no

 06B8S  IT
        SD
        S
        HD

 06886  IT
        SD
        S
        no

 06887  IT
        SD
        S
        HD

06888   AT
        SD
        S
        HD

06889   AT
        SD
        S
        HD

06890   IT
        SD
        S
        HD

06891   »T
        SD
        S
        HD

06892  IT
        SD
        S
        HD
   261.
  (  71.)
 <-0. 37>
   270.

   294.
  (  22.)
 <-0. 32>
   296.

  295.
  (  37.)
 <-0.»2>
  302.

  313.
  (  35.)
 < 1.06>
  300.

  200.
  <  21.)
 < 0.96>
  m.

  28«.
  (  6.)
< 0.99>
  282.

  198.
  ( "9.)
< 1.10
  171.

  359.
  (176.)
< 0.59>
  31*.

  365.
  ( 29.)
<-0.59>
  371.

  283.
                       28*.

                       • 25.
                       ( 6».)
                       -0.0»
                       • 26.
  1710.
 (  H5.)
 <-0.48>
  1755.

  1996.
 (  120.)
 <-0.77>
  2123.

  1652.
 (  233.)
 <  0.23>
  1635.

  1335.
 (  773.)
 <  0.90>
  1099.

 2424.
 (  330.)
 <-0. 10>
 2447.

 1530.
 <  122.)
< 0.21>
 1521.

 2017.
 ( 219-1
<-0.36>
 2050.

 1098.
 ( »67.)
< 1.07>
  917.

 203p.
 ( 278.)
< 0.25>
 1980.

 1771.
 ( 302.)
<-0.6«i>
 1860.

 1965.
 ( 208.)
<-0.84>
 2035.

 213».
 ( "2.)
< 0.54>
 2082.
1221.
( 46.)
< 0. S5>
1206.
1320.
( 31H1.)
<-O.S3>
1375.
1243.
( 22.)
<-0. 1»>
1245.
928.
( 525.)
< 0.71>
775.
1650.
( 221.)
<-0.87>
1719.
1032.
( 184.)
< 0. 88>
975.
1316.
( 137.)
<-0.6B>
1348.
723.
( 395.)
< 1.1S>
538.
1324.
( 108.)
<-0.62>
1346.
1217.
( 146.)
<-0. 19>
1228.
1327.
( 44.)
< l.S6>
1312.
1502.
( 462.)
< 0.69>
1265.
7.79
(0.36)
<-O.OJ>
7. BO
7.37
(0.17|
< 1.14>
7.29
7. SB
(0.50)
< O.B5>
7.43
7.30
(0.08)
<-0.41>
7. 11
7.62
(0.22)
< 0.04>
7.61
a. 02
(0.22)
<-1.15>
8.13
8.02
(0.34)
<-0.88>
8.12
7.69
(0.26)
< 0.72>
7.61
7.77
(0.37)
<-0.01>
7.77
7.69
(0.30)
< 0.52>
7.63
7.R9
(0.35)
< 1.14>
7.52
7.82
(0.26)
<-0.51>
7.90
256.
( 6.)
< 0.09>
256.
336.
1 95.)
<-1.00>
369.
267.
( 51.)
<-1.0S>
287.
193.
(176.)
< 0.82>
139.
424.
( «2.)
<-0.20>
437.
223.
( 44.)
< 0. 18>
219.
362.
( 38.)
<-0.77>
372.
154.
(101.)
< 1.15>
106.
326.
( 54.)
<-0.30>
335,
318.
( 49.)
< 0.32>
313.
306.
( 11.)
< 0.54>
305.
422.
(155.)
< 0.60>
162
    296.
  (183.)
 <-0.08>
    101.

    245.
  (100.)
 <  0.50>
    224.

    250.
  (  18.)
 <  0.05>
    248.

    152.
  (103.)
 <  0.85>
    117.

    315,
  (  17.)
 <-0.5J>
    320.

    223.
  (  50.)
 <  1.02>
    205.

    256.
  I  99.)
 <  0.97>
    224.

    232,
  (109.)
 <-1.09>
    277.

    228.
  (110.)
 <-0.06>
    232,

    210.
  (  2B.)
 <-0.53>
    217.

    276.
  (  20.)
< 0.00>
    275.

    231,
 (125.)
< 0.10>
   22U.
   0.41
 ( 0.57)
< 1. 10>
   0.1B

   0.64
 ( 3.581
< 0.00>
   0.64

   0.20
 ( 0.12)
< 0. 18>
   0.18

   2.77
 ( 4.37)
< 1. 13>
   O.flt

   0.45
 ( 0.3t>)
< 0. 30>
   0.38

   0.46
 ( 0.43)
< 0. 13>
   0.41

   1.18
( 0.56)

   1.25

   0.47
C 0.48)
< 0.61>
   0.32

   7.65
( 9.32)
< 0.63>
   5.09

   2.46
( 1-62)
< 0.22>
   2.25

   0.42
( 0.41)
< 0. 52 >
   0.31

   1.48
( 1.26)
< 0. 63 >
  0.96
   11.11
 (  3.02)

   10.75

   13.54
 (12.75)
 <  o.ao>
   10.29

   18.26
 (  2.82)
 <-0.03>
   18.36

   2.79
 (  3.93)
 <  0.98>
   1.23

   23.52
 (  6.61)

   23.89

   21.01
 (  6.32)

   23.25

   23.53
 (14.41)

   24.30

   8.98
 (  6.49)

   5.98

   3.66
 (  5.75)

   1.19

   0.77
 (  0.61)
 <-0.09>
   0.78

   25.05
 (12.07)
 <-0.26>
   25.95

   2.87
 ( 2.97)
< 0.29>
   2. no
   0.02
( 0.0 1)
< 0.00>
   3.02

   0.02
( 0.021
< 1. 15>
   0.01

   0.04
( 0.03)
< 0. 13>
   0.04

   2. 32
( 4.52)
< 1. 15>
   3.08

   0.04
( 0.03)
< 0. 36>
   0.03

   0.04
( 0.04)
< 0.00>
   0.04

   0. 15
( 0.26)
< 1. 15>
   O.OJ

   0.06
( 0.08)
< 1. 11>
   0.02

   6.96
( 9. 29)
< 0.68>
   4.04

   0.57
I 0.78)
< 1.06)
   0.25

   0. 28
( 0-41)
< 1.09>
   0.11

   0. 80
(  1.02)
< 0. 71>
  0. 22

-------
         Table  C.19,  continued
           06893
           06894
           06896
                 If    419.
                 SO    ( 30.)
                 S    <-0.09>
                 HD    440.
       11
       3D
       S
       HD
                       299.
                       (  6.)
                       -0. 10>
                       299.
                 if    234.
                 SD    ( 33.|
                 S    < 1.15>
                 (ID    218.
 3846.
( 422.)
< o.on>
 3H32.

 2060.
( 1".)
<-1.08>
 2219.

 2975.
( 666.)
<-0.67>
 3121.
2812.
( 66.)
<-0.35>
2826.
1322.
( 28.)
< 0.24>
1320.
1953.
( 502.)
<-O.S9>
2122.
8.13
(0.16)
< 0. 10>
8.12
7.72
(0.16)
< 0.05>
7.72
7.37
(0.07)
< 0.26>
7.36
433.
( 6.)
<-0.05>
433.
357.
( 1«.)
< 0.63>
354.
686.
(255.)
<-1.09>
788.
1067.
(137.)
< 0.0 >
1067.
148.
( s.l
< 0.10>
147.
388.
( 79.)
<- 1.09>
423.
6.02
( 2.38)
<-0.03>
6.09
0.61
( 0.45)
< 0.09>
0.59
0.32
(0-13)
< 1.00>
0.27
3.45
( 3.83)
< 0.92>
2.05
33. 4J
( 6.69)
<-0.57>
34.86
1J.32
(11.34)
< 0.08>
12.97
 4.95
 1.46)
0. 19>
 4.82

 0.07
0.05)
0. 91>
 0.06

 0.06
0.08)
0. 89>
 0.03
CD
MD
AV  = Arithmetic Average
SD  = Standard  Deviation
 S  = Skewness
MD  = Median

-------
Parameter
Well #
6892
6885
6882
6887
6852
6881
6889
6886
6883
6890
u 6884
MD
0 6888
6856
6893
6849
6848
6857
6870
6880
6R94
U(J J H
6864
6891
6854
6896
6855
Table C.20
Gray Farm
Significant Differences Between Baseline and Post Baseline Well Water Quality Tot Fee Fee
Alk TDC Cond TDS pH Cl~ TKN NO3 NH3 TOTP ORTOP ORGP COD SOj2 Col Col Strep

"^"-4- °^~_ "fr_ "" —
*+

*+ *+ *+ *+
*+ *+

*+ *+ *+ *_ *+ *_
*_ *+

*+ *+
*+
*_ *_ *_ *_
*-
-)(• L '^•J™ ^"+ ^+ ^ +
*+

•Jt"_ ^(-J_ ^"+ "^" —
*+ * +
*-
^"+ ~^"+ » Uenutus aliitiiiLicul ly
siyiii ficant differences
+ deriuLuu post-baseline
yreater than buseldnc
"**"— wellwdter quality
*— - dertuLes post-baseline
less than baseline well
water qual i ty parameter
*_ *+ *+

-------
           Table  C.20 >  continued
  Parameter   Al   As   Ba    B   Ca
Cd   Co   Cr   Cu   Fe   Pb   Mg   Mn   Hg   Mo   Mi
Se   Ag   Na
Tl
                                                                                 Zn
  Hell #
  6892
  6885
  6882
  6887
  6852
  6881
  6889
  6886
  6883
^6890
MD
"^6884
  6888
  6856
  6893
  6849
  6848
  6857
  6870
  6880
  6894
  6864
  6891
  6854
  6896
  6855
                                                                 *+
                              *_

-------
Table  C.20>  continued







Well
Number


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C
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£ &
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a

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D O
O U


OJ
£
-u
O
I*
--1
U
£

 6692
 6885
 £882
 £887
 £652
 £881
 6889
 6866
 6883
 £890
 6884
 6888
 6856
 £89]
 6849
 6648
 6657
 £870
 6880
 6894
£864
6891
6654
6896
6855
                                                        -Sf-
                                                        •jf-

-------
                                Table C.21

              Baseline  Ground-Water  Quality,  Gray  Farm
                          Phosphorus and Organics
IBLL
06848



06849



06852



06854



06855



06856



06857



06864



06870



AT
SD
S
80
AT
SD
S
RD
AT
SD
S
RD
AT
SD
S
RD
AT
SD
S
HD
AT
SD
S
RD
AT
SD
S
HD
AT
SD
S
RD
AT
SD
S
ID
TOTAl t
HG P/L
0.74
( 1-01)
< 1.38>
0.43
0.12
( 0.11)
< 0.35>
0.11
0. 10
( 0.03)
< 0.57>
0.09
0.17
( 0.14)
< 0.70>
0.18
0.11
( 0.10)
< 0. 96>
0.07
0.28
( 0.36)
< 1.58>
0.14
0.17
( 0.15)
< 0.31>
0.18
0.25
( 0.18)
< 0.33>
0.22
0. 16
( 0.13)
< 0.60>
0.11
01THO P
BG P/L
0.01
( 0.01)
< 1.79>
0.01
0.01
( 0.01)
< 1.12>
0.01
0.01
( 0.01)
< 1 . 1 2>
0.01
0.02
( 0.01)
< 1. 15>
0.01
0.03
( 0.02)
< 0.38>
0.02
0.01
( 0.00)
< 1.79>
0.01
0.02
( 0.01)
< 0.84>
0.01
0.02
( 0.02)
< 0.97>
0.01
0.01
( 0.01)
< 1.1 2>
0.01
OBG. P
BG P/L
0.68
( 1.02)
< 1.53>
0.35
0.11
( 0.11)
< 0.54>
0.09
0.08
( 0.05)
< 0.33>
0.06
0.16
( 0.14)
< 0.89>
0. 14
0.08
( 0.10)
< 1. 31>
0.05
0.26
( 0.36)
< 1.61>
0.14
0. 15
( 0.15)
< 0.44>
0.17
0.22
( 0.19)
< 0.34>
0.20
0.15
( 0. 13)
< 0.62>
0.11
COD
BG/L
86.8
( 82.3)
< 0.49>
58.2
68.6
( 77.7)
< 1.47>
38.4
54.8
( 64.1)
< 1.28>
34.0
84.3
( 56.7)
< 0.80>
69.8
94.9
( 91.0)
< 0.72>
71. 1
86.8
(123.5)
< 1.4 1>
41.3
52.1
( 2"». 1)
<-0.24>
54.8
63.3
( 66.5)
< 0.57>
26.7
47.7
( 33.3)
< 0.20>
38.0
TOC
SG/L
32.2
(27.5)
< 1.26>
24.4
32.0
(31.5)
< 0.87>
26. 1
31.8
(24.4)
< O.S8>
31.5
34.1
(30.4)
< 0.99>
22.4
38.5
(32.6)
< 0.54>
33.0
32.8
(33.1)
< 0.56>
36.0
38.6
(31.9)
< 0.33>
35.5
29.2
(26.7)
< 0.71>
27.5
32.8
(27.6)
< 0.8S>
27.4
06892  AT
       SD
       S
       RD

06893  AT
       SD
       S
       RD
06894
06896
AT
SD
S
• D

AT
SD
S
BD
  3.49
( ».51)
< 1.47>
  2.04

  0.28
i 0.20)
< 0.49>
  0.26

  0.30
( 0.19)
<-0.38>
  0.40

  0.28
( 0.28)
< 0. 28>
  0.29
  O.R4
( 1-07)
< 1.17>
  0.43

  0.09
( 0.08)
<-0.23>
  0.13

  0.05
( 0.08)
< 1.48>
  0.02

  0.10
C 0.17)
< 1.44>
  0.01
  2.31
( 3.98)
< 1.40>
  0.33

  0.13
( 0.17)
< 1.43>
  0.06

  0.23
( 0.19)
< 0.07>
  0.21

  0.18
( 0.16)
<-0.21>
  0.25
 124.S
(115.0)
< 1.38>
  79.0

  48.8
( 28,1)
< 0.76>
  40.0

 117.5
(158.2)
< 1.13>
  46.5

  48.4
( 34.3)
< 0.74>
  40.5
   34.4
 (21.3)
<-0.18>
   38.0

   26.0
 (12.6)
<-0.10>
   26.4

   17.7
 (13.8)
< 0.21>
   13.0

   15.8
 ( 9.6)
<-0.05>
   16.6
                                       393

-------
Table  C.21,  continued
 36880  AT
        SD
        S
        no

 06881  AT
        SD
        S
        BD

 06882  IT
        SD
        S
        SD

 06883  IT
        SD
        5
        ID

 0688*  IT
        SD
        S
        BD

 06885  IT
        SD
        S
        SD

 06886  IT
        50
        S
        an

 06887  IT
        SD
        S
        so

 06888  IT
        SD
        S
        BD

 06889  IT
        SD
        S
        BD

 06890  IT
        SD
        S
        BD

 06891  AT
        SD
        S
        BO

 06892  IT
        SD
        S
  0.40
 ( 0.38)
 < 1.10>
  0.33

  0.26
 ( 0.25)
 < 1.23>
  0.21

  0.38
 ( 0.27)
 < 0.41>
  0.29

  0.20
 ( 0.14)
 < 1.39>
  0.17

  0.40
 ( 0.24)
 < 0. 10>
  0.34

  0.25
 ( 0.14)
 <-0.61>
  0.25

  0.52
 ( 0.43)
 < 0.20>
  0.54

  0.28
 ( 0.29)
 < 1.35>
  0.17

  0.54
 ( 0.60)
< 0.63>
  0.24

  0.22
 ( 0.26)
< 0.60>
  0.15

  0.24
 ( 0.13)
<-0. 16>
  0.26

  0.19
 ( 0.22)
< 1.12>
  0.16

  3.49
   0.24
 (  0.20)
 <  0.51>
   0.16

   0.11
 (  0.13)
 <  1.21>
   0.06

   0.15
 (  0.11)
 <  0.19>
   0.15

   0.03
 (  0.02)
 <  0.64>
   0.02

   0.17
 (  0.16)
 <  0.7»>
   0.18

   0.06
 (  0.06)
 <  0.37>
   0.05

   0.35
 (  0.41)
 <  0.85>
   0.22

   0.15
 (  0.23)
 <  1.62>
   0.07

   0.08
 (  0.07)
<  0.32>
  0.06

  0.05
 ( 0.04)
< 0.00>
  0.05

  0.04
 ( 0.03)
 < 0.26>
  0.03

  0.02
 ( 0.02)
<  1.36>
  0.01

  O.R4
 (  1-07)
   0. 10
 (  0.11)
 <  0.81>
   0.06

   0.11
 (  0.13)
 <  0.63>
   0.04

   0.18
 (  0.20)
 <  0.59>
   0.09

   0. 14
 {  0.16)
 <  1.69>
   0.08

   0.21
 (  0.26)
 <  0.73>
   0.14

   0.13
 (  0.12)
 <  0.41>
   0.11

   0. 17
 (  0.21)
 <  0.56>
   0.04

  0.09
 ( 0.05)
 <-0.15>
  0.09

  0.31
 ( 0.53)
<  1.43>
  0.08

  0. 18
 ( 0.2tt)
< 0.9»>
  0.08

  0.17
 ( 0.15)
< 0.49>
  0.15

  0.14
 ( 0.23)
< 1.4U>
  0.04

  2.31
 { 3.98)
   40.9
 (  15.3)
 <  0.93>
   40.0

   68. 1
 {  69. 1)
 <  0.94>
   35.5

   39.7
 (  15.4)
 <-0.28>
   44.2

   27.2
 (  36.4)
 <  1.35>
   12.1

   74.8
 (114.0)
 <  1.36>
   17.9

   87.2
 (  66.9)
 <  0.14>
   81.8

   61.2
 (  51.6)
 <  1.24>
   40.0

 125.4
 (  79.0)
<-0.57>
 159.1

   71.3
 (  »7. 1)
< 0.36>
   76.0

  30.7
 (  17.5)
< 0.46>
   26.0

  69.0
 ( 85.0)
<  1.30>
  48.0

  83.1
 ( 81.7)
< 0.70>
  59.8

 124.5
 (115.0)
<  1.38>
    24.3
  (20.1)
 < 0.14>
    26.3

    25.0
  ( 9.9)
 <-0.73>
    27.5

    15.8
  (12.4)
 < 0.22>
    13.9

    20.9
  (14.5)
 < 0.88>
    15.0

    25.5
  (27.4)
 <  0.82>
    17.9

    34.1
  (30.8)
 <-0.03>
    42.4

    26.8
  (16.6)
 < 0.1S>
    24.6

    25.2
  (17.0)
 < 0.92>
   23.2

   29.6
  (26.1)
 < 0.60>
   22.0

   20.9
  (13.6)
<-0.50>
   25.0

   34.1
  (37.1)
< 1.18>
   29.0

   12.2
 < 7.0)
<-0.06>
   12.3

   34.4
 (21.3)
 *  AV  =  Arithmetic Average
    SD  =  Standard  Deviation
     S  =  Skewness
    MD  =  Median
                                  394

-------
      Table C.22

Gray Wells After Baseline
 Phosphorus and Organics
• ELL
06848



068*9



06852



0685*.



06855



068S6



06857



06864



06891



06892

06893

06890

06896


AT*
30
S
no
AT
SO
5
no
AT
SD
S
SO
IT
SO
S
DO
IT
SD
S
10
IT
SD
S
no
AT
SD
S
no
IT
SD
S
NO
AT
SD
S
NO
AT
SD
S
no
AT
SD
s
no
AT
SD
s
no
AT
SD
5
(ID
TOTAL P
«G P/L
0.08
( 0.08)
< 0.50>
0.07
0.03
( 0.03)
< 1.09>
0.01
0.01
( 0.00)
< 1.15>
0.01
0.02
{ 0.02)
< 1.15>
0.01
0.02
( 0.01)
< 1. 15>
0.01
0.0*
( 0.06)
< 1.13>
0.01
0.05
( 0.07)
< 1.15>
0.01
0.01
( 0.01)
< 1.1 5>
0.01
0.09
( 0.10)
< 0.46>
0.07
1.42
( 1-69)
< 0.5U>
0.87
0.79
( 0.19)
< 0.69>
0.70
0.20
( 0.18)
< 0. 16>
0.18
0.08
( 0.14)
< 1.15>
0.01
OBTHO P
HG P/L
0.02
( 0.01)
< 0.21>
0.02
0.01
( 0,0 )
< 0.0 >
0.01
0.01
< 0.0 )
< 0.0 >
0.01
0.02
( 0.01)
< 1.15>
0.01
0.01
( 0.00)
< 1.1 5>
0.01
0.01
( 0.00)
< 1.15>
0.01
0.01
( 0.01)
< 0.00>
0.01
0.01
( 0.00)
< 1.1 5>
0.01
0.03
( 0.01)
< 0.90>
0.02
1.20
( 1.«7)
< 0.57>
0.6fl
0.41
( 0.35)
<-0.68>
0.58
0.03
{ 0.04)
< 1.10>
0.02
0.02
( 0.02)
< 1.03>
0.01
DIG. P
.10 P/L
0.06
{ 0.08)
< 0. 35>
0.03
0.03
( 0.03)
< 1.15>
0.01
0.01
( 0.0 )
< 0.0 >
0.01
0.01
( 0.0 )
< 0.0 >
0.01
0.01
( 0.00)
< 1.15>
0.01
0.03
( 0.05)
< 1. 15>
0.01
0.05
( 0.07)
< 1.1 5>
0.01
0.01
( 0.0 )
< 0.0 >
0.01
0.02
( 0.02)
< 1.15>
0.01
0.16
( 0.26)
< 0.71>
0.01
0.02
( 0.02)
< 0.38>
0.02
0.08
( 0.11)
< 1.07>
0.03
0.03
( 0.04)
< 1.15>
0.01
COD
(IG/L
11. «
( 3.2)
< 0.88>
10.3
40.9
( 52.1)
< 1.14>
16.8
61.3
( 70.7)
< 1.06>
34.4
22.7
( 18.0)
< 0.72>
18.5
74.0
( 75.9)
< O.fl5>
46.9
19.8
( 1«-9)
< 0.55>
15.8
69. 1
(102.5)
< 1.00>
2fl.6
30.0
( 27.8)
< 0.29>
25.9
16.4
t 9.7)
< 0.32>
15.4
34.9
( 25.3)
< 0. 14>
33.0
29.9
( 21.0)
< 0.85>
23.8
32.*
( 30.5)
< 1.07>
21. 1
100.3
(175.4)
< 1.12>
19.5
TOC
HG/L
3.6
( 0.9)
<-0.99>
H. 1
2.2
( 0.9)
< 0.51>
2.0
3.2
( 0.6)
< 0.37>
3. 1
3.6
( 0.6)
< 1.02>
3. 3
1. 1
( 0.3)
<-o. n>
3. 1
3.6
( 1.1)
< 0.47>
3.3
2.3
( 0.4)
< 0. 12>
2.3
2.9
( 0-2)
< 0.43>
2.8
4.6
( 3.3)
< 0.4»>
3.9
5.7
( 4.1)
<-0.33>
6.5
8.4
( 6.4)
< 0.93>
6.2
4.3
( 3.0)
<-0.76>
5.0
4.6
( 2.0)
< 0.71>
4. 1
           395

-------
   Table  C.22,  continued
06870



06880



06881



06882



06883



06884



06885



06886



06887



06888



06889



06890



AT
SD
S
no
AT
SD
S
(ID
AT
SD
S
flD
AT
SD
S
3D
AT
SD
S
SD
AT
SD
S
HD
AT
SD
S
RD
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
(ID

(



(



(



(



(



(
<


(
<


{
0.03
0.03)
0.60>
0.02
0.55
0.07)
1. 06>
0.58
0. 15
0.21)
0.68>
0.05
0.12
0.22)
1. 15>
0.01
0.08
0. 12)
1.09>
0.03
0.91
0.75)
0.07>
0.89
0.04
0.05)
1. 13>
0.01
0.70
0. 19)

(



(



(
<-


(



(



(
<


(
<


t
0.02
0.01)
0.71>
0.03
0.51
0.07)
1.04>
0.51
0.02
0.01)
0.71>
0.02
0.01
0.01)
0.00>
0.01
0.01
0.01)
0.00>
0.01
0.57
0.76)
0.71>
0.32
0.01
0.00)
1. 15>
0.01
0.68
0.16)
<-1.10> <-0.88>


(
<


(
0.78
1.94
1.53)
0.55>
1.67
0.22
0.02)
<-0.69>


(
<


(
0.23
0.57
0.54)
1. 10>
0.35
0.33
0.18)


(
<


(
0.72
1.68
1.54)
0.41>
1.49
0.19
0.05)
<-0.92>


<
<


«
<-0.59> <

0.40

0.20
0.47
0.48)
1.08>
0.26
0.13
0.15)
0.68>
0.06

{
<


(
<


(
<


(
<


(



(
<


(
<


(
<


(
<-


(
<


(
<-


(
<-

0.02
0.01)
0.71>
0.01
0.01
0.01)
1. 15>
0.01
0.02
0.01)
0.71>
0.01
0.01
0.0 )
0.0 >
0.01
0.06
0.09)
1. 14>
0.01
0.23
0.32)
0. 95>
0. 10
0.02
0.02)
1. 15>
0.01
0.01
0.0 )
0.0 >
0.01
0.14
0. 10)
0.39>
0.16
0.03
0.04)
1. 15>
0.01
0.09
0.09)
0.01>
0.09
0.06
0.02)
0. 38>
0.06

(
<


(
<


(
<


(
<


(



(
<


(
<


(
27.2
24.2)
0.10>
25.9
67.9
94. 5)
1. 12>
26.6
29.2
18.4)
0.26>
27.8
30.0
20.2)
1.08>
21.6
24.6
10.9)
0.67>
21.5
43. 1
47.4)
1 . 1 3>
22.4
51.3
51.5)
1. 1 1>
28.5
21.2
9.8)
<-0.40>


(
22.6
18.4
13.8)
<-0.60>


(



(



(


42.0
29.3
9.7)
0.41>
27.9
35.8
24. 1)
0.52>
11.8
35.3
13.5)
0.88>
30.9

(
< 0


(
< 0


{
< 1


(
<-0


(
< 0


(
< 0


(
< 0


(
<-0


(
< 0


(
< 0


1
<-0


{
<-0

4.0
0.7)
.41>
3.8
4.2
1.5)
.41>
3. 9
4. 1
2.1)
. 15>
3. 1
3.3
2.5)
.36>
3.6
4.8
3.5)
-72>
3.7
9.9
8.0)
.66>
8.3
5.0
4. 8)
.60>
4.1
4.7
0.9)
.54>
4.9
8.4
2.6)
.37>
fl.O
3.8
1. 4)
.71>
3.4
4.4
1.0)
.50>
4.5
7.0
4.9)
.55>
8.2
AV = Arithmetic Average
SD = Standard Deviation
 S = Skewness
MD = Median
                            396

-------
                                                       Table  C.23
                                      Baseline  Ground-water Quality,  Gray  Farm
                                                          Metals
 firms, DISSOLTED(BC/L)
 nil          il         IS         Bl           B         Cl         CD         CO          CI          CO          PE         PB
• •»•*»•••»•••»*•»••*»••••«••«•••••••*»•»••«••«•«»•«»»••«••«•*•*«*«••••**•«•••••«••*•••»••«»•*••«••«• ••••••••«•••••»••»»••••••••••
06848  if*   0.207      0.006      0.118      0.929       96.7       0.001     < 0.005     <0.005       0.007       0.034     <0.002
       SO   ( 0.201)    (0.002)     (0.100)     (0.599)     ( 29.81      (0.000)     (0.0  )     (0.0  I     (0.003)     (0.028)     (0.001)
       S    < 0.70>    < 1.79>    < O.*1>    < 0.1«>      < 0.01>    < 1.79>     < 0.0  >     <  0.0  >     < 0.83>    < 1.3S>     < 1.79>
       BD    0.169     <0.005       0.085       0.880        93.        0.000      <0.005      <0.005    
      0.145
IT     0.116
SD   ( 0.120)
S    < 0.66>
HD    0.066

IT     0.149
SD   ( 0.180)
S    < 0.82>
BD    0.042
  0.006
  (0.002)
< 1.79>
<0.005

  0.006
  (0.002)
< 1.79>

<0.005
AT     0.261     <0.005
SD   ( 0.158)    (0.000)
S    <-0.37>    < 1.15>
RD    0.308     <0.005
       IT
       SD
       S
       no
       0.280
     ( 0.429)
     < 1.58>
      0.095
 < 0.005
  (0.000)
 <  1.79>
<0.005
  0.074
 (0.085)
< 1.43>
 0.034

  0.063
 (0.069)
< 1.65>
 0.041

  0.089
 (0.090)
< 0.82>
 0.054

  0.068
 (0.046)

 0.046

  0.125
 (0.144)

 0.045
  0.943
 (1.110)
< 0.97>
 0.555

  0.866
 (1.100)
< 1.08>
 0.433

  1.995
 (1.928)
< 0.70>
 0.950

  0.653
 (0.958)
< 0.71>
 0.100

  1.192
 (1.934)
< 1.15>
 0.288
  88.8
( 29.7)
< 0.45>
  79.

  88.2
( 23.8)
<-0. 01>
  84.

  91.0
( 30.9)
<-0.01>
  83.

  96.2
( 27.7)
< 0.26>
  88.

  87.8
( 35.2)
<-0.62>
  89.
  0.001
  (0.000)
< 0.71>
 0.000

  0.001
  (0.001)
< 1.43>
 0.000

  0.001
  (0.000)
< 0.41>
 0.000

  0.000
  (0.0  )
< 0.0 >
 0.000

  0.001
  (0.000)
< 0.71>
 0.000
 <0.005
  (0.0  )
< 0.0 >

<0.005

 <0.005
  (0.0  )
< 0.0 >
<0.005

  0.005
 (0.0  )
< 0.0 >
<0.005

< 0.005
 (0.001)
< 1.79>
<0.005
 < 0.005
  (0.0  )
<  0.0 >
<0.005

 <0.005
  (0.0  I
<  0.0 >
<0.005

<  0.005
  (0.0  I
<  0.0 >
<0.005

   0.025
 (0.04>|
<  1.50>
<0.005

   0.006
 (0.003)
<  1.79>
<0.005
  0.007
  (O.OOS)
< 1.76>
<0.005

 <0.005
  (0.0  )
< 0.0 >
<0.005

< 0.005
  (0.001)
< 1.50>

 0.01U

  0.013
  (0.007)
< 0. J7>
 0.011
   0.048
  (0.033)
< 0.46>
 0.046

   0.030
  (0.027)
< 1.6S>
 0.021

   0.021
  (0.007)

 0.020

   0.051
 (0.054)
< 1.43>
 0.026

   0.339
 (0.56«|
< 1.6 1>
 0.136
    0.003
  (0.002)
<  0.71>

<0.002

    0.003
  (0.1)01)
<  1.50>
<0.002

   0.060
  (0.116)
<  1. 47>
O.002

   0.003
  (0.001)
< 0. 24>
 0.003

-------
00
Table C.
06857



06864



06870



06880



06881



06882



06BB3



0688*



06885



06886



06887



06888



AT
SD
S
NO
If
3D
S
no
if
SD
S
SD
IT
SD
S
BD
IT
SD
S
BD
IT
SD
S
BD
IT
SD
S
BD
IT
SD
S
BD
IT
SD
S
BD
IT
SD
S
BD
AT
SD
S
BD
IT
SD
S
BD
23, continued
0.314
( 0.317)
< 0.64>
0.274
0.080
( 0.086)
< 1.00>
0.040
0.277
( 0.237)
< 1.09>
0.230
3.530
( 6.574)
< 1.71>
0.492
1.662
( 3.411)
< 1.76>
0.275
0.516
( 0.275)
< 0.22>
0.541
0.383
| 0.284)
< 0. 17>
0.372
0.399
( 0.183)
<-0.04>
0.389
0.317
( 0.339)
< 1.22>
0.183
0.779
( 0.876)
< 1.63>
0.380
0.997
( 0.883)
< 0.39>
O.S30
0.436
( 0.311)
< 0.77>
0.286
<0.005
(0.001)
< 1.50>
<0.005
0.006
(0.002)
< 1.79>
<0.005
0.006
(0.002)
< 1.79>
<0.005
0.006
(0.002)
< 0.97>
<0.005
0.007
(0.003)
< 0.71>
<0.005
0.006
(0.002)
< 0.76>
< 0.005
0.006
(0.002)
< 1.50>
<0.005
0.006
(0.002)
< 0.76>
<0.005
0.006
(0.002)
< 1.79>
<0.005
0.007
(0.003)
< 0.83>
<0.005
0.007
(0.003)
< 0.71>
< O.OOS
0.007
(0.003)
< 0.71>
<0.005
o.oae
(0.090)
< 0.83>
0.035
0.073
(0.066)
< 1.24>
0.053
0.083
(0.102)
< 0.92>
0.030
0.243
(0.198)
< 1.1 3>
0.199
0.116
(0.116)
< O.B2>
0.051
0.210
(0.127)
< 0.06>
0.213
0.114
(0.086)
< 0.59>
0.073
0.216
(0.107)
< 0.52>
0.176
0.124
(0.115)
< 0.88>
0.074
0.094
(0.083)
< 0.44>
0.071
0.144
(0.102)
< 0.«7>
0.090
0.125
(0.144)
< 1. 0 1>
0.068
0.829
(0.905)
< 0.97>
0.533
0.876
(0.897)
( 0.87>
0.619
0.705
(0.629)
< 0.62>
0.576
3.243
(5.035)
< 0.70>
0.579
1.311
(1.837)
< 0.67>
0.493
3.671
(5.738)
< 0. 70>
0.622
1.332
(1.653)
< 0.61>
0.686
1.443
(1.983)
< 0.67>
0.509
0.521
(0.384)
<-0.41>
0.611
0.949
(1.201)
< 0.00>
0.949
0.999
(1-272)
< 0.00>
0.999
2.640
(3.592)
< 0. 00>
2.640
103.4
( 27.5)
< 0. 22>
97.
100.2
( 42.2)
< 0.86>
83.
98.5
( 35.3)
< 0.1 6>
95.
161.7
(106.6)
< 0.69>
160.
81.0
( 27.8)
< 0.87>
72.
110.0
( 35.5)
<-0.69>
115.
81.8
( 27.6)
< 0.44>
82.
111.5
( 55.8)
< 0.78>
109.
79.0
( 53.8)
< 0.56>
58.
75.9
( 36.8)
< 0.09>
70.
111.0
( 30.6)
<-0.37>
114.
56.0
{ 21.6)
<-0.03>
56.
0.001
(0.000)
< 0. 41>
0.000
0.001
(0.000)
< 1.79>
0.000
0.001
(0.000)
< 1.79>
0.000
0.002
(0.002)
< 0.75>
0.001
0.004
(0.007)
< 1.78>
0.001
0.001
(0.002)
< 1.71>
0.001
0.002
(0.002)
< 0.58>
0.002
0.001
(0.002)
< 1.74>
0.000
0.001
(0.002)
< 1. 71>
0.001
0.003
(0.004)
< 1.22>
0.001
0.003
(0.002)
< 0.07>
0.002
0.001
(0.002)
< 1 . 71>
0.001
<0.005
(0.0 )
< 0.0 >
<0.005
<0.005
(0.0 )
< 0.0 >
<0.005
< 0.005
(0.0 |
< 0.0 >
< 0.005
0.012
(0.018)
< 1.79>
<0.005
0.006
(0.002)
< 1.79>
O.OOS
0.006
(0.002)
< 1.79>
< 0.005
0.006
(0.002)
< 1.79>
<0.005
0.006
(0.002)
< 1.79>
<0.005
0.006
(0.002)
< 1.79>
< 0.005
0.006
(0.002)
< 1.79>
< 0.005
0.006
(0.002)
< 0.95>
< O.OOS
0.006
(0.002)
< 1.79>
<0.005
< 0.005
(0.0 )
< 0.0 >
<0.005
<0.005
(0.0 )
< 0.0 >
<0.005
< O.OOS
(0.0 )
< 0.0 >
<0.005
0.008
(0.008)
< 1.79>
<0.005
0.009
(0.010)
< 1.79>

<0.005
< O.OOS
(0.002)
< 1.79>

<0.005
0.006
(0.002)
< 1.79>

<0.005
0.005
(0.004)
< 2.04>
< 0.005
< O.OOi
(0.0 )
< 0.0 >
< 0.00 5
0.009
(0.006)
< 0.84>
<0.005
0.010
(0.007)
< 1.06>
0.008
0.006
(0.002)
< 1.30>
<0.005
0.039
(0.040)
< 1.05>
0.024
0.106
(0.183)
< 1.48>
0.010
0.016
(0.017)
< 1.26>
0.007
0.012
(0.014)
< 1.74>

<0.005
0.009
(0.005)
< 0.88>
0.008
0.024
(0.032)
< 1.66>
0.010
0.049
(0.076)
< 1. 15>
<0.005
0.014
(0.007)
< 0.84>
0.012
0.128
(0. 133)
< 0.35>
0.065
0.211
(0.245)
< 0.70
0. 104
0.068
(0.076)
< l.44>
0.042
0.556
(1.003)
< 1.78>
0.135
0.467
(0.748)
< l.62>
0.164
0. 156
(0.176)

0.068
0. 107
(0.085)
< 1 . 1 0>
0.085
0.123
(0.056)
<-0.34>
0.131
0.094
(0.080)
< 0.88>
0.084
0.221
(0.068)
<-0.31>
0.234
0.320
(0.332)
< 1.79>
0.257
0. 174
(0.065)
< 0.76>
0. 161
O.OOJ
(0.001)
< 1.50>
<0.002
0.004
(0.003)
< 0.63>
0.003
< 0.002
(0.001)
< 1.79>
<0.002
0.010
(0.018)
< 1.77>
<0.002
0.010
(0.012)
< 1. 17>
0.003
0.007
(0.009)
< 1.54>
0.004
0.007
(0.010)
< 1. S3>
<0.002
0.007
(0.009)
< 1. 53>
0.003
0.011
(0.009)
< 0. 45>
0.009
0.009
(0.012)
< U66>
0.004
0.011
(0.013)
< 1.03>
O.OOS
0.007
(0.010)
< 1.73>
<0.002

-------
Table C.
06889 JIT
SD
S
HD
06890
06891
06892
06893
0689*
Vg 06896
vo
I ILL
••••*•
068*8
068*9
06852
0685*
06655
IT
SD
3
HD
»T
SD
S
RD
»T
SD
S
RD
IT
SD
S
no
IT
SD
S
HD
AT
SD
S
RD
• •••<
IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
no
IT
SD
S
HD
•23, continued
0.332 < O.OOS
( 0.202) (0.000)
< 0. 9B> < 1. 15>
0.260 <0.005
0.555
( 0.729)
< 1.78>
0.271
0.182
( 0.123)
< 0.01>
0.180
0.828
( 0.928)
0.598
0.269
( 0.188)
<-0.23>
0.220
0.157
( 0.092)
0.126
1.806
( 2.719)
0.5M
BG
>•••**•••••
89.8
(15.5)
95.5
84.7
(15.*)
<-0.72>
91.0
83.2
(17.8)
<-0.63>
82.5
85.8
(18.0)
<-0.83>
91.0
88.8
(19.2)
<-0.37>
9«.0
0.006
(0.002)
< 1.30>
<0.005
0.006
(0.002)
< 1.50>
<0.005
0.007
(0.003)
< 0.83>
<0.005
0.009
(0.006)
< 0.56>
<0.005
0.006
(0.003)
< 1.50>
<0.005
0.006
(0.002)
< 1.50>
<0.005
•*••*•••••••
0.002
(0.001)
< 1. 16>
<0.001
0.00*
(0.001)
< 1.00>
0.00*
0.002
(0.002)
< 1.69>
< 0.001
0.003
(0.003)
< 0.81>
0.002
0.003
(0.003)
< 1.23>
<0.001
0.058
(0.066)
0.029
0.106
(0.132)
< 1.22>
0.049
0.062
(0.086)
< 1.«3>
0.023
0.226
(0.153)
< 0.33>
0.175
0.060
(0.076)
0.032
0.06*
(0.070)
< 1.23>
0.0*3
0.12*
(0.108)
< 0.65>
0.072
BG
•••••••*«••
0.000
(0.000)
< 0. 00>
0.000
0.001
(0.001)
< 0.00>
0.001
0.000
(0.0 )
< 0.0 >
• •*••
0.0
(0.0 )
< 0.0 >
0.0
0.003
(0.004)
< 0.00>
0.003
1.0«3
(1.33*)
< 0.00>
1.0*3
0.671
(0.808)
< 0.00>
0.671
1.401
(1.773)
< 0.62>
0.682
1.715
(2.286)
< 0.6S>
0.714
0.795
(0.718)
0.752
1.130
(1.540)
< 0.68>
0.390
1. 130
(1.455)
< 0.65>
0.496
HO
!»»••«•••»••
0.010
(0.012)
< 1.56>
0.004
0.01*
(0.018)
< 1.28>
0.005
0.008
(0.010)
< 1.76>
< 0.003
0.015
(0.015)
< 0.6B>
0.005
0.019
(0.023)
< 1.07>
0.010
110.5
( 33.0)
< 0.09>
108.
65.8
( »5.7)
< 0. 9<>
57.
91.*
( 20.0)
<-0.39>
93.
105.6
( 58.7)
< 0.29>
115.
«7.7
( 21.1)
< O.SO>
40.
69.4
( 28.8)
< 0.80>
67.
122.2
( 94.7)
< 0.52>
94.
n
••**•*•••••
0.03*
(0.071)
< 1.79>
<0.005
0.025
(0.0*5)
< 1.50>

<0.005
0.029
(0.051)
< 1.50>
O.OOS
<0.005
(0.0 )
< 0.0 >
<0.005
0.003
(0.002)
< 0.21>
0.002
0.001
(0.002)
< 1.7«>
0.000
0.001
(0.000)
< 1.50>
0.000
0.002
(0.003)
< 0.75>
0.000
0.003
(0.004)
< 0.43>
0.001
0.001
(0.000)
< O.*1>
0.000
0.002
(0.003)
< 1.48>
0.001
K
••«»•*•*•*•
20.2
( 3.9)
< 0.79>
19.0
19.4
( 7.4)
< 0.29>
20.0
15.1
( «-«)
< 0.64>
13.0
21.5
( 5.2)
< 0. 89>
21.0
21.9
( 9.6)
< 0.21>
24.0
< O.OOS
(0.0 )
< 0.0 >
< 0.005
0.006
(0.002)
< 1.79>
< 0.005
0.005
(0.0 )
< 0.0 >
< 0.005
0.006
(0.002)
< 1.79>
< 0.005
0.005
(0.0 |
< 0.0 >
< O.OOS
< O.OOS
(0.0 )
< 0.0 >
< 0.005
< O.OOS
(0.0 )
< 0.0 >
< 0.005




<0.005
0.009
(0.004)
<-0.09>
0.009
< O.OOS
(0.0 )
< 0.0 >
<0.005
0.011
10.005)
< 0.60>
0.010
0.010
(0.007)
< 1.20
0.007
0.007
(0.003)
< 0.4S>
<0.005
0.009
(0.004)
< 0.47>
0.007
0.011
(0.013)
< 1.50>

0.008
0.008
(O.OOS)
< 1.00>
O.OOS
0.193
(0.067)
0.168
0.102
(0. tOO)
< 1.38>
0.060
0. 137
(0. 174)
< 1.22>
0.058
0.439
(0.452)
< 0.76>
0.389
0.179
(0. 184)
< 0.59>
0.113
0.445
(0.394)
< 0.52>
0.491
0.220
(0.243)
< 1.2S>
0.128
O.OOS
(0.004)
< 1.00>
0.003
0.009
(0.010)
< 1.48>
0.005
0.003
(0.001)
< 1.50>
<0.002
0.008
(0.009)
< 1.37>
0.004
0.003
(0.001)
< 1. 50>
< 0.002
0.004
(0.003)
< 1.23>
< 0.002
0.00*
(0.003)
< 0.81>
0.003
SI 10 It TL U
«•••••••»•••»•*•****«**•••*•••••*«••«••••*»•••«••«••
 < 0.0 > < 0.82> < 0.0 > < 0. 60>
< 0.005 
< 0.005
< 0.005
(0.0 )
< 0.0 )
< 0.005
<0.005
(0.0 )
< 0.0 >
< 0.005
< 0.005
(0.001)
< 0.005
< 0.00V
(0.0 )
< 0.0 >
< 0.00 5
< O.OOS
(0.0 )
< 0.0 >
<0.005
< 0.005
(0.0 )
< 0.0 >
< O.OOS
< O.OOS
(0.0 )
< 0.0 >
< 0.005
315.5
( 96.7)
<-0.25>
328.5
331.5
(1*7.3)
<-0.20>
338.5
401.6
( 87.9)
< 0.32>
387.0
345.2
(192.6)
< 1.06>
314.0



< O.OOS
0.0*6
(O.OS4)
0.02*
0.039
(0.044)
< 1.78>
0.021
0.027
(0.011)
< 1.03>
0.020
0.280
(0.543)
< 1.50>
0.040

-------
o
Table C.
06856
06857
06864
06870
06880
06881
06882
06883
06884
06885
06886
06887
IT
SD
S
RD
SD
S
flD
IT
SD
S
•D
IT
3D
S
HD
IT
SD
S
BD
IT
SD
3
HD
IT
3D
S
BD
IT
SD
3
flD
IT
SD
S
BD
IT
SD
3
BD
IT
SD
S
BD
IT
SD
S
HD
23, continued
88.2
(17.6)
92.0
89.1
( 9.6)
< 0.36>
90.0
' 84.5
(17.1)
87.0
68.8
(15.2)
<-0.95>
73.5
74.5
(43.0)
<-0.69>
98.0
80.0
(31.1)
68.0
69.7
(22.5)
<-0.30>
72.0
79.7
(17.0)
86.5
21.8
( 8.0)
<-0.40>
22.5
86.2
(16.8)
<-0.38>
89.0
69.7
(32.6)
<-0.83>
80.5
84.4
(17.3)
91.0
0.014
(0.020)
< 1.48>
0.007
0.003
(0.002)
< 0.61>
0.002
0.016
(0.027)
< 1.56>
0.003
0.007
(0.010)
< 1.37>
0.003
0.260
(0.578)
< 1.79>
0.026
0.075
(0.099)
< 0.70>
0.017
0.041
(0.057)
< 1.5S>
0.019
0.032
(0.023)
< 0.23>
0.033
0.015
(0.016)
< 1. 40>
0.011
0.056
(0.063)
< 0.74>
0.040
0.049
(0.057)
< 1.48>
0.022
0.113
(0.173)
< 1.54>
0.024
0.000
(0.0 )
< 0. 0 >
• •*••
0.0
(0.0 )
< 0.0 >
0.0
0.000
(0.0 )
< 0.0 >
0.000
(0.0 )
< 0.0 >
*****
0.002
(0.0 )
< 0.0 >
••**•
0.000
(0.0 )
< 0.0 >
0.000
(0.0 )
< 0.0 >
*****
0.003
(0.0 )
< 0.0 >
0.000
(0.0 )
< 0.0 >
0.000
0.001
(0.001)
< 0.0 >
0.001
0.000
(0.000)
< 0.00>
0.000
0.000
(0.000)
< 0.71>
0.000
0.013
(0.016)
< 1.30>
0.005
0.008
(0.010)
< 1.47>
<0.003
0.015
(0.012)
< 1.00
0.013
0.008
(0.008)
< 1.28>
0.004
0.016
(0.024)
< 1.65>
0.004
0.036
(0.052)
0.007
0.006
(0.006)
< 1.64>
< 0.003
0.008
(0.012)
< 1.78>
<0.003
0.007
(0.003)
< 0.03>
0.007
0.009
(0.006)
< 0.71>
0.007
0.016
(0.018)
< 1.67>
0.008
0.011
(0.015)
< 1.97>
0.005
0.036
(0.074)
< 1.79>
< 0.005
0.031
(0.057)
< 1.50>
< 0.005
0.070
(0.158)
< 1.79>
<0.005
0.036
(0.075)
< 1.79>
<0.005
0.023
(0.044)
< 1.79>
<0.005
0.069
(0.153)
< 1.79>
< 0.005
0.013
(0.021)
< 1.79>

< 0.005
< 0.005
(0.001)
< 1.79>
<0.005
0.007
(0.003)
< 0.73>
<0.005
0.006
(0.003)
< 1.79>
<0.005
< 0.005
(0.0 )
< 0.0 >

12.5
15.0
( 3.7)
< 0. 87>
14.0
12.8
( 5.0)
<-0. 30>
12.5
15.1
( 2.9)
< 0. 55>
15.0
12.3
( 1.9)
<-0.37>
12.0
10.9
( 3.5)
<-0.53>
12.0
10.2
( 0.9)
<-0.26>
10.4
13.2
( 1.9)
< 0. 10>
13.5
10.0
( 1-3)
<-0.54>
10.5
32.2
(10.8)
<-0.52>
33.4
19.5
( 8.5)
<-0.35>
22.0
23.0
< 0.91>
22.4
< 0.005
(0.000)
< 1.79>
< 0.005

< 0.005
<0.005
(0.001)
< 1.79>
< 0.005
< 0.005
(0.0 )
< 0.0 >
<0.005
< 0.005
(0.0 )
< 0.0 >
<0.005
< 0.005
(0.000)
< 1.79>
< 0.005
< 0.005
(0.0 )
< 0.0 >
< 0.005
< 0.005
(0.0 )
< 0.0 >
< 0.005
< 0.005
(0.0 )
< 0.0 >

< 0.005
< 0.005
(0.0 )
< 0.0 >
< 0.005
< 0.005
(0.0 )
< 0.0 >
<0.005
< 0.005
(0.0 )
< 0.0 >
< 0.005
<0.005
(0.0 )
< 0.0 >
<0.005
< 0.005
(0.0 |
< 0.0 >
<0.005

< 0.005
< 0.005
(0.0 )
< 0.0 >
< 0.005
< 0.005
(0.0 )
< 0.0 >
< 0.005
<0.005
(0.0 )
< 0.0 >
< 0.005
<0.005
(0.0 )
< 0.0 >
< 0.005
< 0.005
(0.0 |
< 0.0 >
< 0.005
< 0.0 05
(0.0 )
< 0.0 >
<0.005

< 0.005
297.5
(138.2)
<-0.07>
308.5
349.0
(169.1)
< 0.22>
313.0
288.2
(120.5)
< o.sa>
270.0
306.6
(111.9)
< 0.74>
256.5
72.8
( 50.9)
<-0.00>
78.0
179.3
< o.to>
135.0
109.5
( 35.5)
< t.00>
101.0
129.2
( 68.8)
< 1.76>
102.0
159.8
( 31.0)
< O.S5>
W7.5
252.3
( 60.6)
270.5
162.5
( 60.9)
<-0.66>
171.5
135.4
( 11.8)
< 0.47>
133.0
< 0.005
(0.0 )
< 0.0 >

< 0.005
< 0.005
(0.0 )
< 0.0 >



< 0.005
0.007
(0.004)
< 1.79>
<0.005
0.007
(0.005)
< 1.50>

<0.005

< 0.005
< 0.005
(0.0 )
< 0.0 3

< 0.005
O.OJO
(0.014)
< 0,77>
0.022
0.077
(0.114)
< 1.47>
0.020
0.176
(0.374)
< 1.79>
0.025
0.163
(0.331)
< 1.79>
0.027
0. 185
(0.219)
< 1. 44>
0.101
0.490
(0.709)
< t.02>
O.M3
0. 137
(0.087)
0.145
0.184
(0.185)
< 0. 85>
0.144
0.098
(0.070)
< 0. 19>
0.099
0.089
(0.068)
< 0.26>
0.080
0.591
(1-233)
< 1.78>
0.090
0.260
(0.517)
< 2.00>
0.056

-------
Table C.
06888 AT
SD
S
HD
06889 IT
SD
S
HD
06890 IT
SO
S
HD
06891 IT
SD
3
RD
06892 IT
SD
3
HD
06893 IT
SD
j;. S
o BD
0689* IT
SD
S
HD
06896 IT
3D
S
RD
23, continued
94.5
(35. 3)
<-0.88>
99.0
102.8
< 3.9)
< 0. 10>
102.5
62.7
(18.1)
< 0.48>
60.0
106.2
(2*. 2)
<-0.57>
106.0
76.3
(M.O)
<-0.62>
90.5
94.0
(23.9)
<-0.38>
102.0
62.8
(15.0)
65.0
137.6
(75.8)
<-0.35>
123.0
0.038
(0.053)
< 1.56>
0.016
0.010
(0.005)
< 0.60>
0.009
0.132
(0.289)
< 1.76>
0.003
0.013
(0.006)
< 0. 15>
0.013
0.2*7
(0.316)
< 0.79>
0.089
0.081
(0.07*)
< 1.*5>
0.051
0.086
(0.066)
< 1.29>
0.050
0.020
(0.018)
< 0.89>
0.015
0.000
(0.0 )
< 0.0 >
• •*••
0.000
(0.0 )
< 0.0 >
0.000
(0.000)
< 0.00>
0.000
0.0
(0.0 )
< 0.0 >
0.0
0.000
(0.000)
< 0.0 >
0.000
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.011
(0.017)
< 1.76>
< 0.003
0.016
(0.019)
< 1. 15>
0.007
0.012
(0.014)
< 1.70>
0.007
0.022
(0.029)
< 1.07>
0.005
0.008
(0.005)
< 0.47>
0.007
O.OSS
(0.070)
< 1.39>
0.022
<0.003
(0.001)
<0.003
0.005
(0.002)
< 0.97>
0.004
< 0.005
(0.0 )
< 0.0 >
< 0.005
0.010
(0.009)
0.005
0.006
(0.002)
< 1.79>

<0.005
0.010
(0.006)
< 0.27>
0.009
0.068
(0.142)
< 1.50>
< 0.005
0.077
(0.067)
0.107
0.007
(0.004)
< 1.50>
< 0.005
24.3
( 9.6)
< 0.20
23.1
17.2
( 3.7)
< 0.26>
16.9
18.4
( 3.9)
< 0.06>
18.3
17.7
( 5.0)
19.0
17.0
( 6.7)
< 0.30>
15.8
40.2
(16.1)
<-0.68>
39.0
7.8
( 1.2)
7.6
16.9
<-0. 26>
16.5
0.007
(0.005)
< 1.79>
<0.005
<0.005
(0.0 )
< 0.0 >
< 0.005

<0.005
<0.005
(0.0 )
< 0.0 >
< 0.005
0.006
(0.002)
< 1.79>
<0.005
0.006
(0.003)
< 1.50>
< 0.005

< 0.005
0.009
(0.009)
< 1.50>
< 0.005
< 0.005
(0.0 )
< 0.0 >
< 0.005
< 0.005
(0.0 I
< 0.0 >
<0.005
0.005
(0.0 )
< 0.0 >
<0.005
< 0.005
(0.0 )
< 0.0 >
< 0.005
< 0.005
(0.0 )
< 0.0 >

< 0.005
< 0.005
(0.0 |
< 0.0 >

<0.005
180.3
( 54.3)
183.5
190.5
( 30.3)
< 0. 10>
188.5
139.3
( 10.6)
i«Io
154.2
(116.5)
< t.29>
95.0
266.7
(115.2)
<-0.35>
293.5
475.6
(230.6)
436.0
249.8
( *3.7)
< 0.67>
221.0
1*1.6
( 56.9)
< 0.68>
108.0
0.007
(0.005)
< 1.50>

<0.005

< 0.005
•C0.005
(0.0 )
< 0.0 >

< 0.005
< 0.005
10.0 )
< 0.0 >

< 0.005
<0.005
(0.0 )
< 0.0 >

0.114
0.186
(0.174)
< 0. 90>
0.127
0.221
(0.380)
< 1.68>
0.053
0.084
(0.077)
< 0.77>
0.038
0.113
(0.137)
< 0.88>
0.033
0.206
(0.135)
< 0.05>
0.188
0.078
(0.074)
< 0.96>
0.065
0.104
(0.090)
< 0.26>
0.088
M = Arithmetic Average
SD = Standard Deviation
 S = Skewness
MD = Median

-------
                                               Table  C.24

                                       Gray  Wells  After Baseline
                                                 Metals
 HBT4LS. DISSOLTED(1G/L)
068*8
068*9
06852
0685*
06855
»••!
»T *
SD
S
no
IT
SD
S
no
IT
SD
S
no
IT
SO
S
HD
»T
SD
• ••••••••••i
'- 0.248
( 0. 1W)
,< 0.96>
0.187
0.296
{ 0.293)
< 0.58>
0.23*
0.393
( 0.55*)
< 1.08>
0.169
0.22*
( 0.3*7)
< 1.1«>
0.066
0.356
( 0.387)
«»«••*•»«•»
0.01*
(0.013)
< 0.00>
0.01*
0.006
K>. 002)
^ Oh 00^
0.006
0.005
inn \
(0.0 )
< 0.0 >
0.005
0.005
(0.000)
< 0.00>
0.005
O.OOS
(0.0 )
«••»•••»•»»
0.0*2
(0.013)
< 0.00>
0.0*2
0.02*
(0.00*)

0.037
D.OJ-;
(o.ood)
< o.oo>
0.035
0.031
(0.00*)
•»•**»»*••*•
0.0
(0.0 )
< 0.0 >
0.0
0. 100
(0.0 )
f n rt %
*. U • U S
*#**•
0.100
inn \
(U.U )
< 0.0 >
• •»*•
0.0
(0.0 )
< 0.0 >
0.0
o.rao
(0.0 |
••••**««•••
115.6
( 29. B)
<-0.52>
120.
112.9
( H.7)

113.
10*. 5
( 3B.«|
< 0.»5>
99.
110.7
( 17.7)
•••****••••
0.002
(0.002)
< 0.00>
0.002
0.000
(0.0 )

0.00*
0.002
(0.002)
< 0.0 >
0.002
0.002
(0.002)
»•**•«•••••<
0.010
(0.002)
< 0.0 >
0.010
0.007
(0.003)

0.010
0.01 1
(0.001)
< 0.00>
0.011
0.01*
(0.005)
»•*•••**• *»(
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.000)

0.005
0.005
(0.0 I
< 0.0 >
0.005
0.005
(0.0 )
»••****••*•<
0.005
(0.000)
< 0.00>
0.005
0.005
(0.000)
X rt AA'i
V U • \J\JS
0.005
0.005
i n ft i
(U. U J
< 0.0 >
0.005
0.006
(0.001)
< 0.00>
0.006
0.020
(0.021)
»••••••*•••!
0.223
(0.258)
< 1.15>
0. 100
0.207
(0. 172)
<"— rt i a •*
N U • 11^
0.220
0. 191
/ n n QII
|U • U 7 * |
< 0. 29>
0. 177
0.066
(0.0681
< 0.93>
0.0*5
0.298
(0.202)
»••»»*••
0.010
(0.005)
< 0.00>
0.010
0.018
(0.016)

0.018
0.012
t n /tint
\ U* U I U|
< o. oo>
0.012
0.013
(0.01«|
< 0.00>
0.013
0.012
(0.015)

-------
Table C.24, continued
06856
06857
0686*
06870
06880
06881
06882
06883
0688*
06885
06886
06887
AT
SD
S
BO
IT
SD
S
no
IT
SD
S
no
IT
SD
S
no
IT
SD
S
no
IT
3D
S
no
IT
3D
3
8D
IT
SD
S
ID
IT
SD
S
no
IT
SD
S
80
IT
SD
S
.10
IT
SD
S
NO
0.549
( 0.811)
< 1.00>
0.221
0.276
( 0.290)
< 0.62>
0.203
0.159
( 0.121)
0.227
0.25*
( 0.2«9)
< 0.20>
0.226
0.297
( 0.282)
< 0.0 1>
0.289
0.500
( 0.«97)
< 0.96>
0.340
1.«77
( 2.262)
< 1. 12>
0.518
0.167
( 0.125)
0.167
1.182
( 1-713)
< 1. 10>
0.165
0.309
< o!so>
0.229
0.287
{ 0.196)
<-0.44>
0.317
0. 153
( 0.111)
0.167
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.000)
< o.o •>
0.005
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.055
(0.017)
< 0.00>
0.055
0.028
(0.007)
< 0.00>
0.028
0.036
(0.0 )
< 0.0 >
*****
0.034
(0.003)
< 0.00>
0.014
0.11*
(0.030)
< 0.00>
0.114
0.047
(0.011)
< 0.00>
0.047
0.055
(0.007)
< 0.00>
0.055
0.035
(0.006)
< 0.00>
0.035
3.099
(0.068)
< 0.00>
0.099
0.050
(0.014)
< 0.00>
0.050
3.054
(0.008)
< 0.00>
0.054
0.084
(0.029)
< 0.0 >
0.084
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
C 0.0 >
0.0
0.616
(0.0 )
< 0.0 >
*****
0.100
(0.0 )
< 0.0 >
*****
0. 100
(0.0 )
< 0.0 >
*****
0. 100
(0.0 )
< 0.0 >
*****
0.0
(0.0 )
< 0.0 >
0.0
0.100
(0.0 )
< 0.0 >
*****
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.100
<• o.o >
*****
0.100
(0.0 )
< 0.0 >
*****
1 JJ.9
( 25.7)
< 0.66>
126.
115. 7
( 25.7)
117.
120.9
i 9.1)
<-0.52>
124.
114.3
( 16.1)
< 0.42>
110.
150.6
( 80.8)
< 1.03>
117.
109.8
( 12.9)
< 0.72>
107.
120.2
( 42.6)
< 0.22>
117.
117.8
( 20.2)
< 0.01>
118.
102.8
<-0.27>
104.
97.7
( 26.8)
98.
66.3
( tO. 3)
< 1.06>
62.
103.6
I 22. 1|
<-0.24>
105.
0.003
(0.003)
< 0.00>
0.003
0.004
(0.003)
< 0. 00>
0.004
0.000
(0.0 )
< 0.0 >
*****
0.001
(0.001)
< 0.00>
0.001
0.030
(0.0 )
< 0.0 >
0.000
0.001
(0.001)
< 0.00>
0.001
0.002
(0.003)
< 0.00>
0.002
0.001
(0.001)
< 0.0 >
0.001
0.000
(0.0 )
< 0.0 >
0.000
0.003
(0.004)
< 0.00>
0.003
0.001
(0.000)
< 0.00>
0.001
0.002
(0.002)
< J.O >
0.002
0.006
(0.002)
< 0.0 >
0.006
0.006
(0.001)
< 0.0 >
0.006
0.011
(0.0 )
< 0.0 >
*****
0.008
(0.002)
< 0.00>
0.008
0.005
(0.0 )
< 0.0 >
0.005
0.006
(0.002)
< 0.0 >
0.006
0.008
(0.004)
< 0.0 >
0.008
0.006
(0.001)
< 0.00>
0.006
0.006
(0.002)
< 0.0 >
0.006
0.005
(0.000)
< 0.00>
0.005
0.008
(0.004)
< 0.0 >
0.008
0.006
(0.002)
< 0.00>
0.006
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
o.oos
(0.0 |
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.021
(0.026)
< 0.0 >
0.023
0.005
(0.0 |
< 0.0 >
0.005
0.005
(0.001)
< 0.0 >
0.005
0.022
(0.024)
< 0.00>
0.022
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.008
(0.002)
< 0.00>
o.ooa
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
• *• *•
0.005
(0-0 )
< 0.0 >
0.005
0.006
(0.001)
< 0.00>
0.006
o.oos
(0.0 )
< 0.0 >
0.005
0.007
(0.002)
< 0.0 >
0.007
0.005
(0.0 )
< 0.0 >
0.005
0.035
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.006
(0.002)
< 0.00>
0.006
O.OJ7
(0.003)
< 0.0 >
0.007
3.587
(0.818)
< 1.07>
0.265
0.021
(0.010)
< 0. 35>
0.020
0. 142
(0. 155)
< 0. 36>
0. 1 10
1. 105
(1.643)
< 0. 68>
0.300
0.300
(0.133)
<-0.07>
0.305
0.423
(0.284)
< 1.00>
0. J2S
0.706
(0.661)
< 0.36>
0.565
0.292
(0.115)
< 0.22>
0.285
1.071
(1.404)
< 0.93>
0.557
0. 155
(0.041)
< 0. 12>
0. 150
3.260
(0.101)
<-0. 35>
0. 280
0.224
(O.OflO)
< 0. 51>
0.208
0.010
(0.007)
< 0.0 >
0.010
0.003
(0.002)
< 0.00>
0.003
0.011
(0.0 )
< 0.0 >
*»•••
0.010
(0.007)
< 0.0 >
0.010
0.0*1
(0.012)
< 0.00>
0.041
0.010
(0.006)
< 0.0 >
0.010
0.009
(0.006)
< 0.0 >
0.009
0.010
(0.007)
< 0.0 >
0.010
0.008
(0.005)
< 0.0 >
0.008
0.013
(0.0121
< 0. 0 >
0.013
0.003
(0.002)
< 0.00>
0.003
0.009
(0.005)
< 0.00>
0.009

-------
Table C.24, continued
06888 IT
SD
S
HD
06889 IT
SD
S
no
06890 IT
SD
S
no
06891 IT
SD
S
HD
06892 IT
SD
S
HD
06893 IT
SD
S
HD
06894 IT
SD
S
BD
06896 IT
SD
S
HD
0.324
( 0.341)
< 0.86>
0.206
0.392
( 0.376)
< 0.58>
0.321
0.581
( 0.517)
< 0.42>
0.514
0.265
( 0.314)
< 0.66>
0.170
0.551
( 0.207)
< 0.61>
0.471
0.277
( 0.209)
<-0.03>
0.279
1.446
( 1.440)
< 0. 83>
1.006
0.831
( 0.843)
0.530
0.005
(0.0 )
< 0.0 >
0.005
0.038
(0.023)
< 0.00>
0.038
0.006
(0.001)
< 0.00>
0.006
0.005
(0.0 )
< 0.0 >
0.005
0.010
(0.009)
< 0.71>
0.005
0.009
(0.006)
< 0.0 >
0.009
0.010
(0.007)
< 0.0 >
0.010
0.005
10. 0 )
< 0.0 >
0.005
0.180
(0.192)
< 0.00>
0.180
0.250
(0.040)
< 0.0 >
0.250
0.044
(0.002)
< 0.00>
0.044
0.020
(0.021)
< 0.0 >
0.020
0.190
(0.134)
<-0.68>
0.254
0.019
(0.013)
< 0.00>
0.019
0.012
(0.008)
< 0.00>
0.042
0.068
(0.030)
<-0.67>
0.082
0. 100
(0.0 )
< 0.0 >
*****
0. 100
(0.0 )
< 0.0 >
0.100
(0.0 )
< 0.0 >
• •••*
0.603
(0.0 )
< 0.0 >
*****
0.0
(0.0 )
< 0.0 >
0.0
1. 174
(0.0 )
< 0.0 >
*****
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
UO. 1
I 14.0)
< 0.73>
40.
103.7
( 1^.6)
97.
83.3
( 18.7)
< 0. 10>
fl2.
11H.3
( 7.U)
< 0.37>
117.
104. 1
( 52.0)
< 0.40>
12.
58.2
( 9.4)
< 0.97>
55.
99.7
1 19. 4)
<-0.57>
104.
175.1
( 57.5)
202.
0.000
(0.0 )
< 0.0 >
0.000
0.002
(0.003)
< 0.00>
0.002
0.002
(0.001)
< 0.00>
0.002
0.001
(0.001)
< 0.0 >
9.001
0.003
(0.004)
< 0.71>
0.000
0.002
(0.003)
< 0.00>
0.002
0.000
(0.0 )
< 0.0 >
0.000
0.001
(0.001)
< 0.71>
0.000
0.005
(0.0 )
< 0.0 >
0.005
0.008
(0.005)
< 0.0 >
0.008
0.008
(0.005)
< 0.00>
0.008
0.006
(0.001)
< 0.00>
0.006
0.006
(0.001)
< 0.71>
0.005
0.030
(0.019)
< 0.0 >
0.030
0.008
(O.OOS)
< 0.0 >
0.008
0.008
(0.003)
0.008
0.005
(0.0 )
< 0.0 >
0.005
0.005
to.o i
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.021
(0.008)
< 0.00>
0.021
0.009
(0.007)
< 0.71>
0.005
0. JJ6
(0.001)
< o.u >
O.OOb
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.006
(0.001)
< 0.71>
0.005
0.009
(0.006)
< 0.00>
0.009
0.005
(0.0 )
< 0.0 >
0.005
O.OOS
(0.000)
< 0.71>
0.005
0. J25
(J. 16B)
< 0.95>
C.265
0.417
(0. 156)
0.419
0.517
(0.422)
< 1.05>
0.360
0. 179
(0.087)
< 0. 17>
0. 175
0.823
(0.908)
< 0.69>
0.360
0.270
(0. 129)
< 1.03>
0.220
0.921
(0.710)
<-0.09>
0.963
0.450
(0.517)
< 1.03>
0.240
0.013
(0.0111
< 0. 0 >
0.013
0.009
(0.005)
< 0.00>
0.009
0.012
(0.010)
< 0.00>
0.012
0.017
(0.017)
< 0.0 >
0.017
0.008
(0.006)
< 0.71>
0.005
0.006
(0.001)
< 0.00>
0.006
0.003
(0.002)
< 0.00>
0.003
0.010
(0.008)
< 0.7 1>
O.OOS
• ELI HG XI HG HO HI K SB IG II TL Zl
• I********************************* ****•*•*****•*••*****•*******•******•••***•******•****•****•*********••*******•**********•»•*•
06848 IT 99. S 0.003 0.0 0.0 0.005 18.6 0.005 O.OOS 286.3 0.005 0.04S
SD ( 6.2) (0.002) (0.0 ) (0.0 ) (0.0 ) ( 3.7) (0.0 ) (0.0 ) ( 51.5) (0.0 ) (0.008)
S <-1.00> < 0.35> < 0.0 ) < 0.0 > < 0.0 > < 0.31> < 0.0 > < 0.0 > <-0.37> < 0.0 > <-1.11>
HD 101.8 0.003 0.0 0.0 0.005 18.3 0.005 0.005 294.5 ***** 0.049
06849 IT
SD
S
no
06852 IT
SD
S
HD
0685* IT
SD
S
fID
103.8
< 0.54>
102.0
97.7
< 0.40>
97.1
94.2
( 6.8)
< o.ia>
93.3
0.002
(0.002)
< 1. 15>
0.001
0.001
(0.001)
0.001
0.003
(0.004)
< 1.03>
0.002
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 )
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.006
(0.002)
< 0.00>
0.006
0.005
(0.0 (
< 0.0 >
0.005
0.005
(0.0 )
< o.o •>
O.OOS
21.1
( 4.5)
<-0.44>
21.8
12.4
( 1.8)
< 0.26>
. 12.1
18.S
( 4..1)
< 0.62>
17.7
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 )
0.005
0.005
(0.0 )
< 0.0 >
O.OOS
0.003
(0.003)
< 0.00>
0.00]
C.005
(0.0 I
< 0.0 >
0.005
0.001
(0.003)
< 0.00>
O.OOJ
220.8
1 45.8)
< 1. 11>
201.5
338.3
( 10.5)
< 0. 19>
337.5
, 367.5
( 21-9)
<-0. 89>
375. S
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
0.005
to.o i
< 0.0 >
• » *• •
0.085
(0.079)
< 0.92>
0.060
0.129
(0.1151
< 1.0S>
0.083
0.036
(0.0211
o.o«s

-------
      Table C.24,  continued
o
06855



06856



06857



06864



06870



06880



06881



06882



06883



0688*



06885



06886



AT
SD
S
(ID
AT
SD
S
no
AT
SD
S
no
AT
SD
S
no
AT
SD
S
(ID
AT
SD
S
(ID
AT
SD
S
flD
AT
SD
S
(ID
AT
SD
S
no
AT
SD
S
(ID
AT
SD
3
(ID
AT
SD
S
(ID
106.6
( 5-3)
<-0. 82>
107.9
102.1
( "• J)
<-1. 12>
104. 1
93.7
( 7-3)
<-0.55>
95.2
101.2
( 9.1)
<-0.64>
105. 1
74.6
( 1* 8)
< 0.60>
72.8
64.2
(40.5)
< 1. 15>
44.5
85.9
( 2.8)
<-0.76>
86.6
68.8
(14.6)
<-0.44>
70.8
97.8
< 6.9)
< 0.53>
96. 1
38.5
(43.5)
< 1. 15>
17.1
98.0
(15.3)
<-0.35>
99.6
56.3
(11.7)
< 0.23>
55.5
0.003
(0.005)
< 1. 15>
0.001
0.006
(0.010)
< 1. 1^>
0.001
0.002
(0.001)
< 1. 1*>>
0.001
0.008
(0.012)
< 0.71>
0.001
0.020
(0.026)
< 0.63>
0.010
0.008
(0.010)
< 1.09>
0.004
0.011
(0.014)
< 1.03>
0.006
0.028
(0.025)
< 0.30>
0.024
0.003
(0.001)
< 0.75>
0.002
0.293
(0.532)
< 1. 15>
0.040
0.006
(0.004)
<-0. 10>
0.006
0.008
(O.OOfl)
< 0.39>
0.007
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )

0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 )
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 1
0.0
0.0
(0.0 )
< o.o •>
0.0
0.0
(0.0 )
< o.o •>
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< o.o •>
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.005
(0.000)
< 0.00>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.006
(0.001)
< 0.00>
0.006
0.005
(0.0 |
< 0.0 >
*****
0.005
(0.000)
< 0.0 >
0.0,05
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 )
0.005
0.228
(0.294)
< 0.00>
0.228
0.005
(0.001)
< 0.0 >
0.005
0.019
(0.020)
< 0.0 >
0.019
0.049
(0.062)
< 0.00>
0.049
0.006
(0.002)
< 0.0 >
0.006
24.0
( 7.5)
< 0.63>
22.5
13.9
( 2.1)
<-0.04>
13.9
13. 1
( 3.1)
< 0.07>
12.8
11.6
( 2.6)
< 0.71>
10.1
14.9
( 3.9)
< 0.37>
14.1
8.8
( 3.0)
<-0.96>
9.8
12.6
( 2.4)
<-0. 38>
12.9
8.3
( 3.0)
<-0.55>
8.8
14.6
( 3.3)
< 0.26>
14.1
11.6
( 5.2)
<-0.30>
12.3
17.4
I 9.0)
< 1.00>
14.2
19. t
( 2.2)
< 1. 13>
18.0
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 (
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.006
(0.001)
< 0.00>
0.006
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.001 .
(0.0 |
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
0.003
(0.003)
< 0.00>
0.003
0.003
(0.003)
< 0.00>
0.003
0.003
(0.003)
< 0.00>
0.003
0.007
(0.004)
< 0.00>
0.007
0.003
(O.OOJj
< 0.00>
0.003
0.003
(0.003)
< 0.00>
0.003
0.005
(0.0 I
< 0.0 >
0.005
0.003
(0.003)
< 0.00)
0.003
356.S
( 20.2)
< 1 . 1 *>>
347.0
283.3
( 32.3)
<-0.99>
292.5
338.5
( 28.3)
< 0.60>
332.5
291.7
( 29.4)
<-0.32>
297.3
263.3
( "• 7)
<-0.57>
262.0
36.3
( 16.5)
< 0.62>
33.0
98.8
( 10.9)
< 1. 11>
94.0
172.0
( 82.6)
<-0.67>
196.0
93.8
( 23.0)
< C.04>
93.5
118.3
( 78.8)
< 0.55>
104.0
246.0
( 44.7)
<-0.03>
2Mb. 5
125.0
( 13.4)
< 0.26>
123.0
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 )
• «»•*
0.0
(0.0 )
< 0.0 >
0.0
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
• •*• •
0.005
(0.0 )
< 0.0 >
«•*••
0.005
(0.0 )
< 0.0 >
*****
0.234
10.388)
< 1. 1 5>
0.050
0.046
(0.008)
<- 1. 15>
0.050
0.044
(0.016)
<- 1. 11>
0.050
0.101
(0.115)
< 0.65>
0.050
0.571
(0.916)
< 0. 71>
0.050
0.044
(0.011)
<-1. 15>
0.049
0.064
(0.051)
< 0.88>
0.050
0.062
(0.033»
<-0.34>
0.067
0.064
(0.037)
<-0.06>
0.064
0.050
(0.018)
<-0. 10>
0.050
0.051
(0.027)
< 0. 16>
0.050
0.092
(0.080)
< 1. 15>
0.053

-------
Table C.24, continued
06887
06888
06889
06890
06891
06892
J>
0
ON
06893
0689*
06896
* AV
5D
S
MD
»T 87.0
SD (30.3)
S <-Q.T>>
no 94.9
»T 53.5
SO (29.0)
S < 1.15>
(ID 39.1
AT 99.0
SO (11.6)
S < 0. 15>
no 97.4
IT 87.2
SD (14.6)
S <-0.13>
HD 87.8
If 111.9
SD ( 7.0)
S <-0.42>
RD 113.2
»T 69. «
SD (23.0)
S <-0.71>
HD 82.3
*T 128.6
SD ( 7.8)
S < 1.08>
DO 125.5
IT 68.1
SD ( 4.5)
S <-0.6»>
HO 69. 1
IT 148.7
SD (98.3)
S <-0.»5>
HD 173.0
3.010
(0.010)
< 1.10>
o.oou
0.009
(0.011)
< 0.95*
0.005
0.078
(0.062)
< 0.05>
0.074
0.016
(0.016)
< 1.06>
0.010
0.003
(0.002)
<-0. 32>
0.00*
1.077
(0.939)
<-0.54>
1.390
1.464
(2.704)
< 1. 15>
0.135
0.058
(0.008)
< 0.62>
0.056
0.016
(0.021)
< 0.91>
0.008
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< o.o •>
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 )
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.007
(0.002)
< 0.0 >
0.007
0.005
(0-0 )
< 0.0 >
0.005
0.005
(0.0 |
< 0.0 >
0.005
0.005
(0.0 )
< O.Q >
0.005
0.009
(0.005)
< 0.0 >
0.009
0.009
(0.006)
< 0.71>
0.005
0.056
(0.073)
< 0.01>
0.056
0.271
(0.372)
< 0.00>
0.271
0.006
(0.002)
< 0.71>
0.005
23.2
( J.2)
<-0.21>
23.4
19. 3
( 5.9)
< 1.00>
16.9
16.7
I 3.4)
< 0.89>
15.6
21.4
( 5.2)
< 0.02>
21. a
20.3
( 6.6)
< 0.77>
18.6
28.5
( 5.0)
<-0.68>
30.9
64.9
( 0.8)
<-1.00>
65.2
7.4
( 1-0)
<-0.64>
7.6
17.8
( 3.3)
< 0.61>
17.1
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.006
(0.001)
< 0.71>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 |
< 0.0 >
0.005
0.015
(0.009)
<-0.45>
0.018
0.001
(0.0 )
< 0.0 >
0.001
0.001
(0.0 )
< 0.0 >
0.001
0.003
(0.003)
< 0.0 0>
0.003
0.003
(0.003)
< C.00>
0.003
0.009
(0.006)
< 0.00>
0.009
0.00)
(0.002)
<-0.71>
0.005
O.OOt
(0.004)
< 0.00>
0.004
0.001
(0.0 1
< 0.0 >
*****
0.002
(0.002)
< 0.71>
0.001
165.0
( 41.7)
<-0.45>
170.5
74.0
( 62. 4)
< 0.97>
52.5
151.8
( 21-9)
<-0.80>
159.0
144.8
( 32.7)
< 0.22>
139.5
93.0
( 5.4)
<-1.05>
95.0
256.3
( 46.0)
<-0.30>
264.0
637.5
( 20.5)
<-0.26>
639.5
206.8
I 24.7)
< 0.68>
201.0
122.5
( 7.3)
< 0.85>
120.5
0.005
(0.0 )
< 0.1) )
• •»••
0.005
(0.0 )
< 0.0 >
»•»•»
0.005
(0.0 )
< o.o •>
*****
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
0.006
(0.0 )
< 0.0 >
»*»••
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
•••*»
0.039
(0.012)
<-0.00>
0.039
0.061
(0.039)
< 0.86>
0.050
0.043
(0.015)
<- 1. 15>
0.050
0.054
(0.021)
<-0.50>
0.058
0.041
(0.014)
<-1.07>
0.047
0.052
(0.033)
< 0.11>
0.050
0.179
(0.131)
<-0.02>
0.181
0.060
(0.041)
< 0.68>
0.051
0.04S
(0.010)
<-0.76>
0.047
= Arithmetic Average
= Standard Deviation
= Skewness
= Median

-------
TABLE C.25.  GRAY WELLS AFTER BASELINE INDICATOR BACTERIA (per 100 ml,'
Well No.
6848


6849


6852


6854


6855


6856


6857


6864



Total Fecal Fecal FC
Coliforms Coliforms (FC) Streptococcus (FS) Fs Salmonella
Av*
SD*
F*
Av
SD
F
Av
SD
F
Av
SD
Av
Av
SD
F
Av
SD
F
Av
SD
F
Av
SD
F

1
1
1/9
340
813
2/6
343
812
2/6
1
3
2/5
3
7
1/5
342
8120
3/6
0
0
0/8
0
0
0/9

0
0
0/9
336
815
1/6
0
0
1/6
0
0
0/5
1
2
1/5
0
0
0/6
0
0
0/8
0
0
0/9

0
0
0/9
0
0
0/6
2
5
1/6
0
0
0/5
2
4
1/5
0
0
0/6
0
0
0/8
0
0
0/9

0 	
	
079
Q 	
	
0/6
0 	
	
0/6
0 	
	
0/5
0.5 	
	
0/5
Q 	
	
0/6
-0 0
0
0/8
0 	
	
0/9
(Continued)
                                 407

-------
Table C.25,  continued
Well No.
6870 Av
SD
F
6880 Av
SD
F
6881 Av
SD
F
6882 Av
SD
F
6883 Av
SD
F
6884 Av
SD
F
6885 Av
SD
F
6886 Av
SD
F
Total
Coliforms
1
2
2/6
3090
3870
5/6
691
1014
5/6
4227
3615
5/5
2285
3067
6/6
2183
2961
6/6
5669
3665
6/6
2049
3062
5/6
Fecal
Coliforms (FC)
0
0
0/6
2121
3009
6/6
40
79
3/6
1398
2381
6/6
411
888
4/5
1377
2398
4/6
3002
3284
5/6
80
173
2/5
Fecal FC 	 -;
Streptococcus (FS) FS Salmonella
10 0 	
24 	
1/6 Q/6
151 14.0 	
273
6/6 Q/6
16 2.5
35 	
4/6 0/6
2143 0.7 	
4007 	
4/6 0/6
5 82.2 	
7 	
3/6 1/6
1898 0.7 	
4002 	
4/6 0/6
869 3.5
1451 	
4/6 1/6
93 0.9 	
200 	
6/6 0/6
(Continued) ,
                                       408

-------
Table C.25,  continued
Well No.
6887 Av
SD
F
6888 Av
SD
F
6889 Av
SD
F
6890 Av
SD
F
6891 Av
SD
F
6892 Av
SD
F
6893 Av
SD
F
6894 Av
SD
F

Total
Coliforms
3086
3442
7/7
1718
3173
5/6
43
40
4/4
1364
3252
4/6
1062
1006
4/5
2067
3004
5/6
2002
3463
4/5
4730
3008
5/5

Fecal
Coliforms (FC)
1757
2899
4/7
406
894
2/5
1
2
2/4
0
0
0/6
180
349
2/5
1042
2429
4/6
1204
2681
2/5
1300
920
3/4

Fecal R:
Streptococcus (FS) FS
209 8.4
356
5/7
16 25.4
31
3/6
10 0.1
9
3/4
0 0
0
0/6
260 0.7
581
1/5
1824 0.6
4009
5/6
2 602.0
2
3/5
3601 0.4
4099
4/5

Salmonella
	
	
0/7
	
	
2/6
	
	
0/4
	
	
0/6
	
	
0/5
	
	
1/6

	
0/5
	
	
0.5
(Continued)
                                        409

-------
Table C.23, continued
Well No.
6896



Av*
SD
F
Total
Coliforms
2450
3242
4/5
Fecal
Coliforms (FC)
1556
2469
4/5
Fecal
Streptococcus (FS)
31
66
2/5
FC
FS
50.2


Salmonella
— — -._
	
0/5
~~
*Av = Arithmetic Average
 SD = Standard Deviation
  F = Frequency of Detection
                                      410

-------
TABLE C.26.  GRAY WELLS AFTER BASELINE INDICATOR BACTERIA (per 100 ml)
Well No.
6848 Av*
SD*
F*
6849 Av
SD
F
6852 Av
SD
F
6854 Av
SD
F
6855 Av
SD
F
6856 Av
SD
F
6857 Av
SD
F
6864 Av
SD
F

Total Fecal
Coliforms Coliforms (FC)
0
0
0/4
360
628
3/4
0
0
1/4
50
100
1/4
15
30
1/4
0
0
0/4
2
5
1/4
0
0
1/4

0
0
0/4
0
0
0/4
0
0
0/4
0
0
0/4
5
10
1/4
0
0
0/4
0
0
0/4
0
0
0/4

Fecal FC
Streptococcus (FS) FS Salmonella
30
59
1/4
0
0
0/4
0
0
0/4
78
155
1/4
5
10
2/4
1
2
1/4
0
1
1/3
0
1
1/4

0 	
	
0/4
0 	
	
0/4
0 	
	
0/4
Q 	
	
0/4
1.0 	
	
0/4
0 	
0/4
0 	
0/4
0 	
0/4
(Continued)
                               411

-------
Table C.26,  continued
Well No.
6870 Av
SD
F
6880 Av
SD
F
6881 Av
SD
F
6882 Av
SD
F
6883 Av
Sd
F
6884 Av
SD
F
6885 Av
SD
F
6886 Av
SD
F
Total
Co li forms
333
577
1/4
756
1496
3/4
20100
40000
3/4
227
204
4/4
130
137
4/4
20300
40000
3/4
1850
2271
3/4
5280
10500
3/4
Fecal
Coliforms (FC)
33
58
0/4
8
10
2/4
7500
15000
1/4
175
171
3/4
1
1
3/4
1025
1733
2/4
26
50
2/4
30
54
2/4
Fecal
Streptococcus
54
92
1/4
11
9
4/4
18
19
4/4
347
506
4/4
19
15
4/4
1385
2743
3/4
49
53
4/4
51
40
4/4
(FS) FS Salmonpl^
0.6
	
0/4
0.7 	
	
0/4
417.0 	
	
0/4
0.5
	
0/4
0.1 	
	
0/4
0.7
	
1/4
0.5
	
0/4
0.6 	
	
0/4
(Continued)
                                       412

-------
Table C.26, continued
Well No.
6887 Av
SD
F
6888 Av
SD
F
6889 Av
SD
F
6890 Av
SD
F
6891 Av
SD
F
6892 Av
SD
F
6893 Av
SD
F
6894 Av
SD
F

Total Fecal Fecal FC
Coliforms Coliform(FC)s Streptococcus (FS) "FS" Salmonella
10600
21000
4/4
930
1404
4/4
3610
6929
3/4
21000
39400
3/4
23300
38300
4/4
7067
11200
3/3
1093
752
4/4
31700
38000
4/4

2004
3998
3/4
30
48
2/4
178
355
1/4
375
450
3/4
304
597
3/4
2
3
1/3
523
558
4/4
13600
26900
4/4

116
197
4/4
78
93
3/4
20
40
2/4
263000
492000
4/4
6795
13470
4/4
3257
5580
2/3
227
163
4/4
898
885
4/4

17.3 	
	
0/4
0.4 	
	
0/4
8.9 	
	
0/4
0.0 	
	
0/4
0.0- 	
	
0/4
0.0 	
0/3
2.3 	
0/4
1.5 	
0/4
(ContinuedT
                                      413

-------
Table C.26, continued	
                       Total          Fecal             Fecal           FC
                                                                             ^Salmonella
                                                                                0/4
Well No.
6896 Av
SD
F
Total Fecal
Coliforms Coliforms (FC)
1350
2434
4/4
25
30
2/4
Fecal FC
Streptococcus (FS) FS
24
25
4/4
1 .0



*Av = Arithmetic Average
 SO = Standard Deviation
  F = Frequency Detection
                                      414

-------
 OBGUICS(PPB)
                   Table C.27
Baseline  Ground-water Quality,  Gray Farm
        Priority  Organic  Pollutants
• ELL       ACEBAPBTHrLEBE  ABTRRACENE/PBEBATHB EIE    ATIAZI1IE   BEIZERE/TBICULOBOETUILUB   BEBZSBBiCITIC 1CID  4-T-BOt TLPB EBOl
• ••»•••••••*»••••••••••»•»••»••«••••••*••••••••••• •••••»••*•*•**»••»•*••**•••••*•••••»•»•*•««**••»•*••••*••••••••*•••••••••••••••
068*6  if*        5.0               < 2.0                2.0              <1.0                    0.0               3.0
       3D      (  0.0)              (  0.0)             (   0.0)            (   0.0)                 (  0.0)            (  2.2)
       S       < 0.0 >              < 0.0 >             <  0.0 )            <  1.79>                 < O.J >           < 1.50>
       8D        5.00               <2.00               2.00             <1.00                   0.0               2.00
06849



06852



06854



06855
•O

Ul
06856



06857



06864



06870



06880



06881



AT
SD
S
BO
AT
SD
S
BD
AT
3D
S
BD
AT
SD
S
BD
AT
3D
S
BD
AT
SD
S
BD
AT
3D
S
HD
AT
3D
S
HD
AT
SD
S
HD
AT
SD
S
HD
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
                                    <2.0
                                   (   0.0)
                                   <  0.0 >
                                   <2.00

                                   < 2.0
                                   (   0.0)
                                   <  0.0 >
                                   <2.00

                                   < 2.0
                                   (   0.0)
                                   <  0. 0 >
                                     2.00

                                    <2.0
                                   (   0.0)
                                   <  0.0 >
                                   <2.00

                                   < 2.0
                                   (   0.0)
                                   <  0.0 >
                                   <2.00

                                   < 2.0
                                   (   0.0)
                                   <  0.0 >
                                   <2.00

                                    <2.0
                                   <   0.0)
                                   <  0.0 >
                                   <2. 00

                                    <2.0
                                   (   0.0)
                                  > <  0.0 >
                                   <2.00
                                      2.1
                                      0.2)
                                     1.64>
                                    <2.00
   2.5
 (  t.1)
< 1.79>
  2.00

   2.0
 (  0.0)
< 0.0 >
  2.00

   2.0
 (  0.0)
< 0.0 >
  2.00

   2.0
 {  0.0)
< 0.0 )
  2.00

   2.0
 (  0.0)
< 0.0 >
  2.00

   2.1
 (  0.1)
< 1.50>
  2.00

   2.6
 (  1.5)
< 1.79>
  2.00
                                    <2.0
                                   (   0.0)
                                   <  0.0 >
                                   <  2.00
 2.0
 0.0)
0.0 >
2.00

 2.0
 0.0)
0.0 >
2.00

 3.7
 3.6)
1.68>
2.00
                                    8.2
                                 < 17.6)
                                 < 1.79>
                                 < 1.00
                                 <  0.0)
                                 < 0.0 >
                                  <1.00

                                    1.0
                                 (  0-0)
                                 < 0.0 >
                                <  1.00

                                  < 1.0
                                 (  0.0)
                                 < 0.0 >
                                  <1.00
                                 (  0.0)
                                 < 0.0  >
                                 < 1.00
                                 {  0.0)
                                 < 0.0  >
                                 <1.00

                                    3.1
                                 (  3.6)
                                 < 1.20>
                                 < 1.00
                                 (   0.0)
                                 <  0.0  >
                                 < 1.00

                                 <  1.0
                                 (   0.0)
                                 <  0.0  >
                                 <1.00

                                 <  1.0
                                 (   0.0)
                                 <  0.0  >
                                 <1.00
    0.0
 (  0.0)
 < 0.3 >
   0.0

    0.0
 (  0.0)
 < 0.0 >
   0.0

    0.0
 (  0.0)
 < 0.0 >
   0.0

    0.0
 <  0.0)
 <  0.0 >
   0.0

    0.0
 (   0.0)
 < o.a >
   0.0

    0.0
 (   0.0)
 <  0.0 >
  0.0
   2.0
 (  o.o)
< 0.0 >
*»•**•

   0.0
(  0.0)
< 0.0 >
  0.0
   0.0
(  0.0)
< 0.0 >
  0.0
                                                            2.0
                                                         (  0.0)
                                                         < 0.0 >
                                                           2.00

                                                            2.0
                                                         (  0.0)
                                                         < 0.0 >
                                                           2.00

                                                            2.7
                                                         I  1.7)
                                                         < 1.50>
                                                           2.00

                                                            2.0
                                                         (  0.0)
                                                         <  0.0 >
                                                           2.00

                                                            2.0

                                                         <  0.0 >
                                                           2.00
                                                           2.0
                                                        (  0.01
                                                        < 0.0 >
                                                          2.00

                                                           2.2
                                                        (  0.4)
                                                        < 1.79>
                                                          2.00
                                                             2.0
                                                          (  0.0)
                                                          < 0.0  >
                                                            2.00

                                                             2.1
                                                          (  0.2)
                                                          < 1.79>
                                                            2.00
   0.0
(  0.0)
< 0.0 >
  0.0
                                                             2.0
                                                          (   0.0)
                                                          <  O.U >
                                                            2.00

-------
Table  C.27,  continued
06882



06883



0688*



06885



06886



06887



06888



06889



06890



06891



06892



06893



if
SD
S
BD
»T
SD
S
BD
IT
SD
S
BD
IT
SD
S
BD
AT
SD
S
BD
AT
SD
S
BD
IT
3D
S
BD
AT
SD
S
BD
AT
SD
S
HD
IT
SD
S
BD
IT
SD
S
BD
IT
SD
S
no

(
<


(
<


(
<


(
<


(
<


(
<


(
<


(
<


(
<


«
<


(
<


(
<

5.0
0.0)
0.0 >
S.OO
5.0
0.0)
0.0 >
S.OO
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
S.OO
5.0
0.0)
0.0 >
S.OO
5.0
0.0)
0.0 >
5.00
                                     <2.0
                                    (   0.0)
                                    <  0.0 >
                                    < 2.00

                                    < 2.0
                                    (   0.0)
                                    <  0.0 >
                                    < 2.00

                                    < 2.0
                                    (   0.0)
                                    <  0.0 >
                                    < 2.00
(
                                       2.9
                                       2.U
                                    < 2.00

                                     <2.0
                                    (   0.0)
                                    <  0.0 )
                                    <2.00
                                       2.5
                                       1-2)
                                      1.79>
                                    <2.00
                                    <  2.0
                                    (   0.0)
                                    < 0.0 >
                                    <2.00

                                    <  2.0
                                    (   0.0)
                                    < 0.0 >
                                    <2.00
                                    <  2.0
                                       0.0)
                                      1.79>
                                    <2.00
                                    <  2.0
                                    I   0.0)
                                    < 0.0 >
                                    < 2.00

                                    <  2.0
                                    (   0.0)
                                    < 0.0 >
                                    < 2.00

                                     <2.0
                                    (   0.0)
                                    < 0.0 3
                                    <2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   3.9
(  «-8|
< 1.79>
  2.00

   2.8
(  2.1)
< 1.79>
  2.00

   3.8
(  3.2)
< 1.27>
  2.00

   2.9
(  2.2)
< 1.79>
  2.00

   5.7
i  5.8)
< 0.81>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.8
(  1.7)
< 1.15>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.4
(  0.9)
< 1.79>
  2.00

   2.0
C  0.0)
< 0.0 >
  2.00
   1.6
i  1.5)
< 1.79>
< 1.00

<  1.0
(  0.0)
< 0.0 >
<1.00

   1.3
(  0.7)
< 1.79>
<1.00

   1.J
(  0.8)
< 1.79>
<1.00

<  1.0
(  0.0)
< 0.0 >
<1.00

 < 1-0
(  0.0)
< 0.0 >
<1.00

  11.9
( 26.7)
< 1.79>
<1.00

<  1.0
<  0.0)
< 0.0 >
< 1.00

 < 1.0
(  0.0)
< 0.0 >
<1.00

 < 1.0
I  0.0)
< 0.0 )
< 1.00

   3.9
(  7.2)
< 1.79>
< 1.00

 < 1.0
(  0.0|
< o.o >
< 1.00
                                                               0.0
                                                            (  0.0)
                                                            < 0.0 >
                                                              0.0
                                                               0.0
                                                            (  0.0)
                                                            < 0.3  >
                                                              0.0
   0.0
(  0.0)
< 0.3 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0
                                                               0.0
                                                               0.0)
                                                              0.0 >
                                                              0.0
                                                               0.0
                                                            (  0.0)
                                                            < 0.0 )
                                                              0.0
                                                               0.0
                                                            (  0.0)
                                                            <  0.0 >
                                                              0.0
                                                               0.0
                                                            (   0.0)
                                                            <  0.0 >
                                                              o.o
                     2.0
                  <  0.0)
                  < 0. 0 >
                    2.00
   2.2
(  0.«)
< 1.79>
  2.00

   3.3
(  3.1)
< 1.79>
  2.00

   2.0
(  0.0)
< 0. 0 >
  2.00
                                                                                 2.0
                                                                              C  0.01
                                                                              < 0.0 >
                                                                                2.00
                                                                              (  3.7)
                                                                              < 2.00
                                                                                2.00

                                                                                 2.0
                                                                              (  0.0)
                                                                              < 0.0 >
                                                                                2.00
                                                                                 2.0
                                                                              (  0.0)
                                                                              < 0.0 >
                                                                                2.00
                     2.0
                  (  0.0)
                  < 0.0 >
                    2.00
                     2.$
                  (  1.2)
                  < 1.SO>
                    2.00

                     2.0
                  (  0.0)
                  < 0.0 >
                    2.00

                     2.0
                  I   0.0)
                  <  O.O >
                    2. OO

-------
Table C.27,  continued
06894 »T
SO
s
BD
06896 If
SD
S
BD
S.O
( 0.0)
< 0.0 >
5.00
S.O
( 0.0)
< 0.0 >
5.00
                                     <2.0
                                    (   O.OJ
                                    <  0.0 >
                                    < 2.00

                                     <2.0
                                    (   0.0)
                                    <  0.0 >
                                    < 2.00
    2.0
    0.0)
   0.0 >
   2.00

    2.3
    0.6)
   1.50>
   2.00
(  0.0)
< 0.0 >
< 1.00

   1.1
(  0.3)
< 1.SO>
< 1.00
      0.0
   (  0.0)
   < 0.0 >
     0.0
   (
      0.0
      0.0)
   < 0.0 >
     2.0
  (  0.0)
  < 0.0 >
    2.00
     2.0
  (  0.0)
  < 0.0 >
    2.00
• ILL   CIIBOI TBTIICBIOIIDE    4-CHLOI01IILIIE     CBLOIOBBIZZIE        CBLOROFOBH        2-CILOB) PUEIOL   1-CHLOiOttT 11DBC1If
•••••••*••••••••••••••»••«•••••••••••••»•••«••••••»**•*»••*•»•*»**•«»•••«***••*»•»•••••••**••»**•*•••••••»•»•»*»»*•••**«*««*•••••
06848  IT        S.O                <10.0              <1.0                <1.0                  2.0               < 2.6
       SD      (  0.0)              (  0.0)             (0.0)              (  0.0)              (0.0)             (  0.0)
       3      < 0.0 >              < 0.0 >             < 0.0 >             < 0.0 >              <  0.0 >             < 0.0 >
       BD       5.00                10.00             < 1.00               <1.00                 2.00              <2.00
06849



06852



06854



06855



06856



06857



06864



06870



06880



IT
SO
S
BD
IT
SD
S
BD
IT
SD
S
BD
IT
SD
3
BD
IT
SO
S
BD
IT
SD
S
RD
AT
SO
S
BD
IT
SD
S
BD
IT
SD
S
BD
5.0
( 0.0)
< 0.0 >
s.oo
5.0
I 0.0)
< 0.0 >
s.oo
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
S.O
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
s.oo
4.3
( 1.6)
<-1.79>
S.OO
5.0
( 0.0)
< 0.0 >
S.OO
S.O
( 0.0)
< 0.0 >
s.oo
                                    <10.0
                                   (  0.0)
                                   < 0.0 >
                                  <10.00

                                   < 10.0
                                   (  0.0)
                                   < 0.0 >
                                  <10.00

                                    <10.0
                                   (  0.0)
                                   < 0.0 >
                                  <10.00

                                    <10.0
                                   (  0.0)
                                   < 0.0 >
                                  < 10.00

                                   < 10.0
                                   (  0.0)
                                   < 0.0 >
                                  <10.00

                                   < 10. 0
                                   (  0.0)
                                   < 0.0 >
                                  < 10.00

                                    < 10.0
                                   (  0.0)
                                   < 0.0 >
                                   <10.00

                                    <10.0
                                   (  0.0)
                                   < 0.0 >
                                  < 10.00

                                    <10.0
                                   (  0.0)
                                   < 0.0 >
                                  < 10.00
 (  0.0)
< 0.0 >
 < 1.00

 < 1.0
 (  0.0)
< 0.0 >
 < 1.00
(  0.0)
< 0.0 >
< 1.00
(  0.0)
< 0.0 >
< 1.00

 < 1.0
(  0.0)
< 0.0 5
< 1.00

<  1.0
{  0.0)
< 0.0 >
< 1.00

   1.2
(  0-»)
< 1.79>
< 1.00
(  0.0)
< 0.0 >
< 1.00
I  0.0)
< o.o •>
< 1.00
  < i.o
 (   0.0)
 <  0.0 >
 < 1.00

  < 1.0
 (   0.0)
 <  0.0 >
 <  1.00

  < 1.0
 (   0.0)
 <  0. 0 >
 <  1.00

  < i.o
 (   0.0)
 <  0.0 >
 <  1.00

  < 1.0
 (   0.0)
 <  0.0 >
 <1.00

 < 1.0
 (   0.0)
 <  0.0 >
 <  1.00
    1.7
 (   1-6)
 <  1.79>
 <  1.00
                     < 1.0
 (   0.0)
 <  0.0  >
 <  1.00
  0.0
    0.0)
  0.0 >
   2.0
(  O.Ot
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
   0.01
  0.0 >
  2.00
   2.0
 I  0.0)
< 0.0 >
  2.00

   2.0
 (  3.0)
< 0. 0 >
  2.00

   2.1
(  0.3)
< U50>
  2.00
   3.3
   3.3t
  U79>
  2.00
   2.0
(  0.0)
< 0. 0 >
  2.00
 < 1.00
   2.0
   0.0)
  0.0 >
  2.00
                       2.8
                    (   2.1)
                    <  1.79>
                    <2.00
  < 2.0
 (  0-0)
 < 0.0 >
 <2.00

  < 2.0
 (   0.0)
 <  0.0 >
 <  2.00

  < 2.0
 (   0.0)
 <  0.0 >
 <2.00

  < 2.0
 (  0.0)
 < 0.0 >
 <2.00

  < 2.0
 (  0.0)
 < 0.0 >
 <2.00

  <2.0
 (  0.0)
 < 0.0 >
 <2.00
   2.4
(  1.0)
< 1.79>
< 2.00
 <2.0
(  0.0)
< 0.0 >

-------
Table  C.27,  continued
06881



06882



06883



06884



06885



06886



06887



06888



06889



06890



06891



06892



06893



IV
SD
S
BD
IV
SD
S
BD
IV
SD
S
BO
IV
SD
S
BD
IT
SD
S
BD
IV
SD
S
BD
IV
SD
S
BD
AV
SD
S
BO
IV
SD
3
BD
AV
SD
S
BO
tv
SD
S
BO
IV
SD
S
BO
IV
SD
S
>«n

«
<


{
<


(
<


(
<


<
<


C
<


(
<


(
<


(
<


(
<


«
<


(
<


(
<

5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
S.OO
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
S.QO
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
0.0)
0.0 >
5.00
5.0
O.O)
o.o >
s. oo
                                   <10. 0
                                  (  0.0)
                                  < 0.0 >
                                  <10.00

                                   <10.0
                                  {  0.0)
                                  < 0.0 >
                                  <10.00

                                  < 10.0
                                  (  0.0)
                                  < 0.0 >
                                 < 10.00

                                  < 10.0
                                  (  0.0)
                                  < 0.0 >
                                  <10.00

                                  < 10.0
                                  (  0.0)
                                  < 0.0 >
                                  <10.00

                                  < 10.0
                                  (  0.0)
                                  < 0.0 >
                                  <10.00

                                  < 10.0
                                  {  0.0)
                                  < 0.0 >
                                 < 10.00

                                  <10.0
                                  (  0.0)
                                  < 0.0 >
                                  <10.00

                                  < 10.0
                                  (  0.0)
                                  < 0.0 >
                                  <10.00

                                  < 10.0
                                  (  0.0)
                                  < 0.0 >
                                 < 10.00

                                  <10.0
                                  (  0.0)
                                  < 0.0 >
                                 < 10.00

                                   <10.0
                                  (  0.0)
                                  < 0.0 1
                                 < 10.00

                                   ,-10.0
                                  C  O. 0)
                                  < O.O 5
 (  0.0)
< 0.0 >
< 1.00
J  0.0)
< o.o •>
< 1.00

 < 1.0
(  0.0)
< 0.0 >
< 1.00
(  0.0)
< 0.0 >
  1.00
 (  0.0)
< 0.0 >
 < 1.00

  < 1.0
 (  0.0)
< 0.0 )
< 1.00

  < 1.0
 (  0.0)
< 0.0 )
< 1.00

  < 1.0
 (  0.0)
< 0.0 )
< 1.00

  < 1.0
 (  0.0)
< o.o •>
 <1.00

  < 1.0
 (  0.0)
< 0.0 *
< 1.00

  < 1.0
 (  0.0)
< 0.0 >
< 1.00

  < 1.0
 (  0.0)
< 0.0 i
 < 1.00
 I  O.OJ
< o.o *
    8.4
 (  18.2)
 <  1.79>
 <1.00
 (   1.1)
 <  1.79>
 < 1.00
    3.2
 (   5.3)
   1.79>
 <1.00
    1.2
 (   0.5)
   1.79>
 <1.00
 <  1.0
 I   0.0)
 <  0.0 >
 <1.00

  < i.o
 (   0.0)
 <  0.0 >
 <1.00

 <  1.0
 (   0.0)
 <  0.0 >
<  1.00

 <  1.0
 (   0.0)
 <  0.0 >
 <1.00

 <  i.o
 (   0.0)
 <  0.0 >
 
 <1.00

 <  1.0
 I   0.0)
 <  0.0 >
 < 1.00

  < 1.0
 {   0.0)
 <  0.0 >
 
  2.00
   2.0
(  O.Ol
< 0. 0 >
  2.00
   2.0
I  0.0)
< 0.0 >
  2.00
   2.0
(  0.01
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
   0.0)
  0.0 >
  2.00
   2.0
I  0.0)
< 0.0 >
  2.00

   2.0
I  0.0)
< 0.0 >
  2.00

   2.0
I  0.01
< 0.0 >
  2.00

   2.0
(  0.0)
< 0. 0 >
  2.00
                    I
    0.01
   O. O  >
   3.0
   2.51
  1. 79>
  2.00

   2.0
   0. 01
  an  •*
   4.3
   5.6)
  1.79>
 <2.00
 <2.0
(  0.0)
< 0.0 >
 <2.00

 < 2.0
C  0.0)
< 0.0 >
 <2.00

   5.7
I  »-0)
< 1.79>
 <2.00

   2.2
(  0.«)
< 1.79>
< 2.00

   2.9
(  1.5)
< 0.73>
< 2.00

   2.5
I  1-2)
< 2.0*>
< 2.00

 < 2.0
(  0.01
< 0.0 >
< 2.00

 < 2.0
(  0.0)
< 0.0 >
< 2.00

 < 2.0
(  0.0)
< 0.0 >
< 2.00

 < 2.0
(  0-0)
< 0.0 >
< 2.00

 < 2.0
(  0. 1)
< 1.79>
< 2.00

   2. 5
<   1-21

-------
Table  C.27, continued
0689*



06896



• ILL
068*8



068«9



06852


-O
^ 0685*



06855



06856



06857



0686*



06870



06880



AT
SD
S
BD
AT
SD
S
BD
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
DIBOItLPBATHALATI
Ct*0t****ft **********
AT
SD
S
BD
AT
SD
S
BD
AT
SD
3
BD
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
BD
<2.0
( 0.0)
< 0.0 >
< 2.00
2.1
( 0.2)
< 1.79>
< 2.00
<2.0
( 0.0)
< 0.0 >
< 2.00
2.1
( 0.2)
< 1.50>
< 2.00
3.0
( 1-9)
< 1. *1>
< 2.00
<2.0
( 0.0)
< 0.0 >
<2.00
<2.0
( 0.0)
< 0.0 >
<2.00
5.5
( 8.7)
< 1.79>
<2.00
<2.0
( 0.0)
< 0.0 >
<2.00
6.4
( 7.0)
< 0.83>
<2.00








<10.0
( 0.0)
< 0.0 >
< 10.00
<10.0
( 0.0)
< 0.0 >
<10.00
2. 3-DICHLOROAIILIIE
• ••499A^*A**A ** •* * ** "

(
<


(



(
<


(
<


(
<


<
<


(
<


(
<•


(
<


(
<

8.0
6.2)
1.68>
5.00
7.7
6.6)
1.79>
5.00
5.0
0.0)
0.0 >
5.00
7.8
6.2)
1.50>
5.00
6.0
2.2)
1.50>
5.00
5.0
0.0)
0.0 >
5.00
7.9
6.5)
1.50>
5.00
«.S
1.2)
• 1 . 7 8>
5.00
5.5
1.3)
1.79>
5.00
5.2
0. 4)
1.79>
5.00
< 1.0
{ 0.0)
< 0.0 >
< 1.00
<1.0
< 0.0)
< 0.0 >
<1.00
3 . 4-DICH LOBCH »ILI IB
f f •••••• •••••• ••• • • 4 •
<2.0
( 0.0)
< 0.0 >
<2.00
< 2.0
( 0.0)
< 0.0 >
<2.00
< 2.0
( 0.0)
< 0.0 >
<2.00
< 2.0
( 0.0)
< 0.0 >
<2.00
<2.0
1 0.0)
< 0.0 >
<2.00
<2.0
( 0.0)
< 0.0 >
<2.00
< 2.0
( 0.0)
< 0.0 >
<2.00
<2.0
( 0.0)
< 0.0 >
< 2.00
< 2.0
{ 0.0)
< 0.0 >
< 2.00
< 2.0
( 0.0)
< 1.79>
< 2.00
< 1.0
( 0.0)
< 0.0 >
<1.00
< i.o
( 0.0)
< 0.0 >
< 1.00
DICBLOBOBBIZZBI
• •••4490t ••••• ••<
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.1)
< 1.79>
2.00
2.0
1 0.0)
< 0.0 >
2.00
2.1
( 0.2)
< 1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
I 0.0)
< 0.0 >
2.00
2.8
( 1.8)
< 1.50>
2.00
2.2
( 0.4)
< 1.79>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
< 0.0)
< 0.0 >
2.00
                                                                                                2.0
                                                                                                0.0)
                                                                                               0.0 >
                                                                                               2.00
                                                                                                2.0
                                                                                             (   0-0)
                                                                                             < 0.0 >
                                                                                              2.00
   < 2.0
   I  0.0)
  < 0.0 >
   <2.00

    <2.0
   (  0.0)
  < 0.0 >
  <2.00
                                                                                    B  DICBLOSOBEK III P  DICHLOiOBIIZIII 0
                                                                                                                        •*»•••*••
                                                                                               2.0
                                                                                            (   0.0)
                                                                                            < 0.0 >
                                                                                             2.00

                                                                                               2.0
                                                                                            (   0.0)
                                                                                            < 0.0 >
                                                                                             2.00
                                                                                              2.0
                                                                                              0.0)
                                                                                             0.0 >
                                                                                             2.00

                                                                                              2.0
                                                                                              0.0)
                                                                                             0.0 >
                                                                                             2.00
                                                                                              2.0
                                                                                            |  0.0)
                                                                                           < 0.0 >
                                                                                             2.00
                                                                                              2.0
                                                                                           C  0.0)
                                                                                           < 0.0 >
                                                                                             2.00
                                                                                              2.0
                                                                                           (  0.0)
                                                                                           < 0.0 >
                                                                                             2.00
                                                                                              2.0
                                                                                           I  0.0)
                                                                                           < 0.0  >
                                                                                             2.00
                                                                                              2.0
                                                                                           (  0.0)
                                                                                           < 0.0 >
                                                                                             2.00
                                                                                              2.0
                                                                                           I  0.0)
                                                                                           < 0.0 >
                                                                                             2.00
    2.5
 (  1.1)
  < 1. 79>
   2.00

    2.3
 (  0.8)
  < 1.79>
   2.00

    2.0
•I  0.0)
  < 0.0 >
   2.00
 (   1.0)
 <  t.50>
  2.00

    2.0
 (   0.0|
 <  0.0 >
  2.00

    2.0
 (   0.0)
 <  0.0 >
  2.00

    2.6
 (   1.3)
 <  1. S0>
  2.00

    3.1
 (   2.7)
 <  1.79>
  2.00
   2.0
   0.0)
 < 0.0 >
  2.00
   2.0
 I  0.0)
 < 0.0 >
  2.00

-------
Table  C.27,  continued
06861  AV
       SO
       S
       HO

06882  »T
       SO
       S
       HD

068BJ  if
       SD
       S
       HD
   4.2
<  4.4)
< 1.74>
  2.*0

  10.5
 12.20

   5.2
(  3-6)
< 0.1«>
  *.65
06884



06885



06686



06887



06886



06(189



06690



068911



06892



IT
SD
S
no
IT
SD
S
BO
IT
SD
S
HD
IT
SD
a
BD
IT
SD
a
HD
AT
SD
S
(ID
IT
SD
S
BD
IT
SD
S
BD
IT
SD
S
BD
3.3
( 3.1)
< 1.79>
< 2.00
14.1
( 20.4)
< 1.41>
3.95
3.4
{ 2.4)
< 1.20>
<2.00
6.3
( «-3)
< 0.00>
6.70
3.5
( 2.3)
< 0.74>
< 2.00
2.5
( 0.6)
< 0. 12>
2.45
2.5
1 1-2)
< 1.79>
< 2.00
2.3
( 0.6)
< 1.50>
< 2.00
3.5
t 2.7)
< 1.35>
< 2.00
   s.o
(  1.4)
<-o.oa>
  s.oo

   5.4
{  0.7)
< 1.23>
  S.OO

   5.2
(  0.4)
< 1.79>
  5.00

   5.3
(  0.7)
< 1.79>
  5.00

   8.1
(  4.3)
< 0.69>
  5.70
                                   5.0
                                (  0.0)
                                < 0.0 >
                                  S.OO
   5.4
   0.7)
  1.48>
  5.00

   5.9
   2.0)
  1.69>
  S.OO

   5.5
   1.1)
  1.15>
  S.OO

   5.1
   0.3)
  1.79>
  S.OO

   6.1
   2.4)
  1.50>
  S.OO
                                   5.0
                                 (  0.0)
                                 < 0.0 >
                                  5.00
 < 2.0
<  0.0)
< 0.0 >
<2.00

  <2.0
(  0.0)
< 0.0 >
<2.00

  <2.0
(  0.0)
< 0.0 >
<2.00

  <2.0
(  0.0)
< 0.0 >
<2.00
                                                        2.6
                                                     (  1-0)
                                                       1.05>
                                                     <2.00
                                          <2.0
                                        (  0.0)
                                        < 0.0 >
                                        <2.00

                                          <2.0
                                        |  0.0)
                                        < 0.0 >
                                        <2.00

                                          <2.0
                                        (  0.0)
                                        < 0.0 >
                                        <2.00

                                        < 2.0
                                        (  0.0)
                                        < 0.0 >
                                        <2.00

                                          < 2.0
                                        (  0.0)
                                        < 0.0 >
                                        <2.00

                                          <2.0
                                        (  0.0)
                                        < 0.0 >
                                        <2.00

                                           2.3
                                        I  0.9)
                                        < 1.79>
                                        <2.00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.5
   1.3)
  1.79>
  2.00

   2.0
   0.0)
  0.0 >
  2.00
                                                                            2.0
                                                                          <  0.0)
                                                                         < 0.0 >
                                                                           2.00
                                                               3.2
                                                               1.9)
                                                              0.82>
                                                              2.00
                       2.0
                       0.0)
                    < 0.0 >
                      2.00
C
                                                                            2.0
                                                                          (  0.0)
                                                                          < 0.0 >
                                                                           2.00

                                                                            2.0
                                                                          (  0.0)
                                                                          < 0.0 >
                                                                           2.00
                       2.0
                     (  0.0)
                    < 0.0 >
                      2.00

                       2.6
                     (  1-5)
                    < 1.79>
                      2.00

                       2.0
                     (  0.0)
                    < 0.0 >
                      2.00

                       2.0
                     (  0.0)
                    < 0.0 >
                      2.00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.01
< 0.0 >
  2.00

   2.0
I  0.0)
< 0.0 >
  2.00

   2. 1
(  0.2)
< 2.04>
  2.00

   2.0
(  0.0)
< 0.3 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
I  0.0)
< 0.0 >
  2.00
                       2.0
                    (   0.0)
                   < 0.0 >
                     2.00

                       2.0
                   (   0.0)
                   < o.o >
                     2.OO
   2.2
(  0.5)
 < 1.79>
  2.00

   4.2
(  4.4)
 < 1.60>
  2.00

   2.3
(  0.7)
 < 1.79>
  2.00

   2.8
<  1.9)
 < 1.79>
  2.00

   4.0
I  3.3)
 < 1.SS>
  2.7S

   2.1
<  0.3)
 < 1.79>
  2.00

   2.8
I  2.0)
 < 2.04>
  2.00

   2.0
I  0.0)
 < 0.0  >
  2.00

   2.0
(  0.0)
 < 0.0  >
  2.00

   2.3
I  0.7)
 < t.79>
  2.00

   2.0
(  0.0)
 < 0.0  >
  2.00

   2. 1
(  0.3)
 < 1.79>
  2. OO

-------
 Table C.27,  continued
06893   A I/       3.O
        SO    (   1.«)
        S      <  O.S7>
        •D    <  2.00
0689*
06894
If
3D
S
BD

IT
3D
S
•0
(
                 3.3
                 2.9)
                1.50>
              < 2.00

                 3.5
              < 1.50>
              < 2.00
                             s.o
                          I   0.0)
                         < 0.0  >
                           5.00
 5.6
 1.3)
1.50>
5.00

 5.1
 0.3)
1.50>
5.00
  <2.0
(  0.0)
< 0.0 >
<2.00

 < 2.0
(  0.0)
< 0.0 >
< 2.00

<  2.0
(  0.0)
< 0.0 >
<2.00
                                                               2.0
                                                             (  0.0)
                                                            < 0.0 >
                                                              2.00
                                                                                   2.0
                                                                                   0.0)
                                                                                  0.0 >
                                                                                  2.00

                                                                                   2.0
                                                                                   0.0)
                                                                                  0.0 >
                                                                                  2.00
                                                                                                      2.0
                                                                                                   (  0.0)
                                                                                                   < 0.0 >
                                                                                                     2.00
                                                              2.0
                                                           I   0.0)
                                                           <  0.0 >
                                                             2.00
                                                                                   2.0
                                                                                <   0.0)
                                                                                < 0.0 >
                                                                                 2.00
                                                                                 2. a
                                                                                 1.7)
                                                                               <  1.50>
                                                                               2.00
  3.2)
< 1.50>
 2.00

  3.3
  2.1)
< 1.11>
 2.00
•BLL         DICBLOIOBCTB1BI  2,4-DICBLOIOPBEROL  DIRBTLPBTBALAH  OIISOOCTTLPUTBlLir B  OIOCTTLPU TUL1TB   DOOSCAIOIC  ACID
• ••••»*••«••••••••••••••••»•»»•••••*•••••»••*•*••••«»•»•••»•••»•«»•»•••••*«•»»•*•»•*••»•••••««*•»»•»•••••*•*»»»••»*»•••««•••••»••
068*8  if         0.0                2.0                3.8               37.6'                10.«               0.0.
        SO      (  0.0)             (  0.0)             (  3.6)             ( 3«. B)              (  20.6)           (   0.0)
        S       < 0.0 >            < 0.0 >            < 1.61>            < 0.08>              <  1.79>           < 0.0 >
        BD        0.0                2.00               2.00              38.15                 2.00             0.0
•P-
K>
 068*9
 «•»
 0685*
 06855
 06856
 06857
 0686*
 06870
AT
SD
S
BD
tT
SD
S
BD
AT
SD
S
BO
AT
3D
S
BD
AT
SD
3
BD
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
BD
0.0
( 0.0)
< 0.0 >
0.0
0.0
< 0.0)
< 0.0 >
0.0
0.0
< 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
o.o
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
   3.2
(  2.9)
< 1.79>
  2.00

   2.8
(  1.9)
< 1.79>
  2.00
                                      2.0
                                   (  0.0)
                                   < 0.0 >
                                     2.00
                               2.0
                            i   0.0)
                            <  0.0 >
                              2.00
                               3.5
                               3.4)
                              1.50>
                              2.00

                               2.0
                               0.0)
                              0.0 >
                              2.00
                                            2.0
                                         (   0.0)
                                         <  0.0 >
                                           2.00

                                            2.4
                                         (   1-0)
                                         <  1.79>
                                           2.00
                                                        11.7
                                                      ( 23.7)
                                                      < 1.79>
                                                        2.00
                                                         5.9)
                                                        1.50>
                                                        2.00
                                        (  5.4)
                                        < 1.SO>
                                          2.00

                                           2.0
                                        (  0.0)
                                        < 0.0 >
                                          2.00
                                                         *.0
                                                         «.6)
                                                        1.50>
                                                        2.00
                                                         2.0
                                                      (  0-0)
                                                      < 0.0 >
                                                        2.00
                                                 3.5
                                                 3.8)
                                                 1.79>
                                                 2.00

                                                 2.0
                                                 0.0)
                                                 0.0 >
                                                 2.00
                    110.8
                   (201.9)
                   < 1.72>
                    29.30

                    110.6
                   <2«8.7)
                   < 1.79>
                     9.95

                     29.2
                   I 31.7)
                   < 0.77>
                    29.00

                     21.7
                   ( 37.5)
                   < 1.«3>
                     2.00
                                                              2.0
                                                              0.0)
                                                             0.0 >
                                                             2.00

                                                              6.3
                                                              7.7)
                                                             1.36>
                                                             2.00
                                                             62.6
                                                           (105.5)
                                                           < 1.42>
                                                             7.30

                                                             23.8
                                                           ( 19.0)
                                                           < 0.26>
                                                            18.90
                                                                                        24.7
                                                                                      (  35.6)
                                                                                      <  0.78>
                                                                                        2.00

                                                                                         9.8
                                                                                      (  17.4)
                                                                                      <  1.50>
                                                                                        2.00
                                                                                         5.7
                                                                                         8.3)
                                                                                        1.50>
                                                                                        2.30
                                                                                                9.8
                                                                                              ( 12.9)
                                                            2.00

                                                             2.0
                                                          (  0.0)
                                                          < 0.0 >
                                                            2.00
                                                             2.0
                                                          I  0.0)
                                                          < 0.0 >
                                                            2.00

                                                             4.8
                                                          I  6.9)
                                                          < 1.79>
                                                            2.30
                                                                                                2.8
                                                                                                2.0)
                                                                                               1-79>
                                                                                               2.00
                                                                                                   0.0
                                                                                                 (  0.0)
                                                                                                 < 0.0 >
                                                                                                  0.0
                                                                                                   0.0
                                                                                                   0.0)
                                                                                                  0.0 >
                                                                                                  0.0
                                                                                                                      0.0
                                                                                                                    I  0.0)
                                                                                                                    < 0.0 >
                                                                                                                     0.0

                                                                                                                      0.0
                                                                                                                    (  o.oi
                                                                                                                    < 0.0 >
                                                                                                                     0.0
                                                           0.0
                                                        (  o.oi
                                                        < 0.0 >
                                                          0.0
                                                           0.0
                                                        (  0.0)
                                                        < 0.0 >
                                                          0.0

                                                           0.0
                                                        (  O.OI
                                                        < 0.0 >
                                                          0.0

                                                           0.0
                                                        (  0.0)
                                                        < 0.0 >
                                                          0.0

-------
Table
06880



06881



06882



06883



06884



06885


4>
N>
hO
06886



06887



06888



06889



06890



06891



C.27,
AV
SO
s
BO
IT
SD
S
HD
if
SD
S
• D
IT
SD
S
•D
IT
SD
S
HD
IT
SD
S
•D


IT
SD
S
•D
IT
SD
3
• D
IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
HD
IT
SD
S
HD
continued
0.0
I 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
{ 0.0)
< 0.0 >
0.0


0.0
I 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
   2.0
 (  0.0)
< 0.0 >
  2.00
   2.0
 (  0.0)
< 0.0 >
  2.00
   2.0
(  0.0)
< 0.0 *
  2.00
   2.0
   0.0)
  0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  1.00
   2.0
{  0.0)
< 0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   4.6
(  7.0)
< 2.04>
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
I  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   3. 1
   2.7)
  1.79>
  2.00

   5.3
  2.00

   3.3
(  3.3)
< 1.79>
  2.00

   4.2
(  5.4)
< 1.79>
  2.00

   3.9
(  4.6)
< 1.79>
  2.00
{  3.9)
< 0.28>
  5.50
                      2.0
                      0.0)
                     0.0 >
                     2.00

                      «. 1
                      5.1)
                     1.79>
                     2.00
   8.5
« 10.4)
< 0.91>
  2.00

   8.9
(  9.8)
< 0.00>
  8.90
   3.8
   4.0)
  1.50>
  2.00

   6. 1
   8.1)
  1.1S>
  2.00
 358.6
(852.7)
< 1.79>
  6.35

 163.0
(359.3)
< 1.76>
  2.70

 757.7
(•**••)
< 1.79>
  7.35

 246.}
(495.4)
< 1.71>
 16.85

  21.7
( 37.5)
< 1.64>
  3.95

  13.7
I 20.8)
< 1.68>
  4.40

  22.2
< 35.5)
< 1.45>
  3.50

  14.9
( 21.7)
< 1.6S>
  7.20

  21.6
( 33.4)
< t.62>
  9.25

  17.1
( 29.0)
< 1.15>
  2.90

  13.9
( 26.9)
< ).78>
  2.95

 305.2
(678.0)
< 1.50>
  2.00
                                                              3.5
                                                           <  2.6)
                                                           < 1.35>
                                                             2.00

                                                             34.3
                                                           ( 79.2)
                                                           < 1.79>
                                                             2.00
                                           3.4
                                           3.6)
                                          1.79>
                                          2.30
                                           2.0
                                        (   0.0)
                                        <  0.0 >
                                          2.00
   3.0
I  2.6)
< 1.79>
  2.00

   6.7
I  9.9)
< 1.75>
  2.45

   3.7
(  «.D
< 1.79>
  2.00

  10.7
« 20.9)
< 2.01>
  2.00

   5.2
I  5.0)
< 0.71>
  2.00
                                           2.0
                                        I  0.0)
                                        < 0.0  >
                                          2.00
                                           2.0
                                        <   0.0)
                                        <  0.0 >
                                          2.00
                                          25.4
                                        (  52.3)
                                        <  1.50>
                                          2.00
                                                            0.0
                                                         (   0.0)
                                                         <  0.0  >
                                                           0.0

                                                            0.0
                                                         (   0.0)
                                                         <  0.0  >
                                                           0.0
                                                                               0.0
                                                                            (  0.0)
                                                                            < 0.0 >
                                                                              0.0
                                                                               0.0
                                                                            (  0.0)
                                                                            < 0.0 >
                                                                              0.0
   0.0
I  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0
                                                            0.0
                                                         (  0.0)
                                                         < 0.0 >
                                                           0.0
                                                                               0.0
                                                                             (  0.0)
                                                                             < 0.0 >
                                                                              0.0

                                                                               0.0
                                                                             (  0.0)
                                                                             < 0.0 >
                                                                              0.0

                                                                               0.0
                                                                             (  0.0)
                                                                             < 0.0 >
                                                                              0.0

                                                                               0.0
                                                                             I  0.0)
                                                                            < 0.0 >
                                                                              0.0

-------
         Table C.27,  continued
N3
06892



06893



06894



06896



• ELL
IT
SD
3
no
IT
SO
S
80
11
SD
S
80
IT
SD
S
no

0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< o.o >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
ITHYL BBIZEIK
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
BBPTiDBCMI
••*•*••••••••**••••*•*•••••••*••*»••••*••**•*• ••••!
06848



068*9



06852



0685*



06855



06856



06857



06864



IT
SD
S
BD
if
SD
S
BD
IT
SD
S
no
IT
SD
S
BD
AT
SD
S
BD
IT
SD
S
BD
IT
SD
S
(ID
IT
SD
S
no
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
i 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
i 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
2.0
( 0.0)
< 0.0 >
2.00
23.7
( M.O)
< 1.67>
2.00
2.0
( 0.0)
< 0.0 >
2.00
29.2
( 60.8)
< 1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
13.8
{ 26.5)
< 1.50>
2.00
2.0
( 0.0)
< o.o •>
2.00
                                                              3.4
                                                              3.5)
                                                            1.79>
                                                            2.00

                                                              3.7
                                                              2.9)
                                                            1.29>
                                                            2.00

                                                              3.8
                                                              4.0)
                                                            1.50>
                                                            2.00
                                                             2.0
                                                           (  0.0)
                                                          < 0.0 >
                                                            2.00
    83.3
  (149.1)
 <  1.70>
  23.75

    61.2
  {126.3)
 <  1.50>
    3.50

    35.3
  (  38.5)
 <  0.38>
  12.90

    39.5
  <  ««.3)
 <  1.09>
  22.90
   2.0
(  0.0)
< 0.0 >
  2.00

   5.3
(  4.7)
< 0.59>
  2.00

   2.3
I  0.8)
< 1.50>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
                     O.I)
                     0.01
                    0.0 >
                    0.0
                     0.0
                  (  0.0)
                  < 0.0 >
                    0.0
                     0.0
                     0.0)
                    0.0 >
                    0.0

                     0.0
                     0.0)
                    0.0 >
                    0.0
                                                         HEI10ECUB     BEI10ECAIOIC ACID  BETBTLBEPTl DBTHOITB   ntTBILBIItDBCUOtTI
                                                        • •••••••«••»»••••»••«••••*•••••»•*«•••••••«•«•«•••••«••••••«••»•••••••»»••••••
                                                             2.0               0.0                 < 2.0                 < 2.0
                                                          (0.0)           (  0.0)               (0.0)               (   0.0)
                                                          < 0.0 >           < 0.0 >               < 0.0 >               <  0.0 >
                                                            2.00              0.0                 <2.00                <  2.00
                                                             2.0
                                                           (  0.0)
                                                          < 0.0 >
                                                            2.00
                                                             2.0
                                                           (  0.0)
                                                          < 0.0 >
                                                            2.00
                                                             2.7
                                                             1.6)
                                                            1.50>
                                                            2.00
                                                             2.0
                                                          (  0.0)
                                                          < 0.0 >
                                                            2.00
                                                             2.0
                                                          (  0.0)
                                                          < 0.0 )
                                                            2.00
                                                             2.0
                                                          (  0.0)
                                                          < 0.0 >
                                                            2.00
   0.0
 (  0.0)
< 0.0 >
  0.0

   0.0
 (  0.0)
< 0.0 >
  0.0

   0.0
 (  0.0)
< 0.0 >
  0.0

  25.6
 (  0.0)
< 0.0 >
• •*•**

 111.0
 (  0.0)
< 0.0 >
*•••••

   0.0
 (  0.0)
< 0.0 >
  0.0
   4.1
 I  5.3)
<  1.79>
 <2.00

   3.3
 I  3.2)
<  t.79>
 <2.00

   «.*
 (  5.3)
<  1.50>
<  2.00

 < 2.0
 (  0.0)
< 0.0 >
<2.00
                        6.9
                     (  12.01
                     <  1.79>
                     <2.00
 (
   2.3
   0.6)
                                                                                                 < 2.00
   4.7
(  6-1)
< 1.50>
< 2.00
                                                             2.0
                                                             0.0)
                                                            0.0 >
                                                            2.00
  26.0
   0.0)
  0.0 >
  <2-0
(  0.0)
< 0.0 )
< 2.00
                      < 2.0
                     (   0.0)
                     <  0.0 >
                     <  2.00

                      <2.0
                     (   0.0)
                     <  0.0 >
                     <2.00

                     < 2.0
                     (   0.0)
                     <  0.0 >
                     <2.00

                      <2.0
                     (   0.0)
                     < 0.0 >
                     < 2.00

                     <  2.0
                     (   0.0)
                     < 0.0 >
                     < 2.00

                     <  2.0
                     (   0.0)
                     < 0.0 >
                     < 2.00

-------
Table  C.27, continued
06870



06880



06881



06882



06883



0688*

.£•
hO
-p-
06885



06886



06887



06888



06889



06890



IV
3D
S
•0
IV
so
S
no
IV
so
S
•0
IV
SD
S
BD
IV
SD
S
(ID
IV
SO
S
BD

»V
SD
S
BD
IV
SD
S
BD
IV
SD
S
•0
IV
SD
S
BD
IV
SD
S
RD
IV
SD
S
HD
1.0
< 0-0)
< 0.0 >
1.00
1.0
• 0.0)
< 0.0 >
1.00
2.1
( 2.7)
< 1.79>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00

1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< o.o >
1.00
1.0
< 0.0)
< 0.0 >
1.00
1.0
< 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.2
i  0.4)
< 1.79>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   0.9)
  1.79>
  2.00

   2.0
   0.0)
  0.0 >
  2.00

   3.7
   3.7)
  1.74>
  2.00
                                 (   3.5)
                                 <  1. 17>
                                   2.95
   2.0
(  0.0)
< 0.0 >
  2.00

   2.9
(  2.4)
< 2.04>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
(  0.0)
< 0. 0 >
  2.00

   2.0
{  0.1)
< 1.79>
  2.00
                                                        2.0
                                                     (   0.0)
                                                     < 0.0 >
                                                      2.00
                                                        2.0
                                                        0.0)
                                                       0.0 >
                                                       2.00
                                                        2.0
                                                     (   0.0)
                                                     <  0.0 >
                                                       2.00
                                                        2.0
                                                        0.1)
                                                       1.79>
                                                       2.00
                                                       2.5
                                                     (   1-1)
                                                     <  1.50>
                                                       2.00

                                                       3.0
                                                     (  2.1)
                                                     <  1.47>
                                                       2.00
                       2.0
                    {  0.0)
                    < O.B >
                      2.00
                       2.3
                       0.5)
                      1.1S>
                      2.00

                       2.8
                       2.2)
                      2.04>
                      2.00
                                                       2.0
                                                     (  0.0)
                                                     < 0.0 >
                                                      2.00

                                                       2.3
                                                     <  0.5)
                                                     < 1.15>
                                                      2.00
                                                       2.0
                                                     I  0.0)
                                                     < 0.0 >
                                                      2.00
  3«.3
(  0.0)
< 0.0 >
   0.0
(  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0

   0.0
1  0.0)
< 0.0 >
  0.0

   0.0
<  0.0)
< 0.0 >
  0.0

   0.0
t  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0
                                                                        50.7
                                                                       (  0.0)
                                                                       < 0.0 >
                                                                       ••••*•
   0.0
(  0.0)
< 0.0 >
  0.0

   0.0
I  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0

  27.1
(  0.0)
< 0.0 >
  <2.0
 I  0.0)
 < 0.0 >
 < 2.00

  14.1
 ( 29.7)
 < 1.79>
 < 2.00

   2.4
 (  0.9)
 < 1.79>
 < 2.00

  <2.0
 (  0.0)
 < 0.3 >
 < 2.00

  < 2.0
 I  0.0)
 < 0.0 >
 <2.00

  < 2.0
 I  0.0)
 < 0.0 >
 <2.00

   3.4
 (  3.5)
 < 1.79>
 < 2.00

   4.8
 (  4.4)
 < 0.79>
 <2.00

   8.4
 ( ".0)
 < 2.04>
 <2.00

   3.4
 (  3.6)
 < 1.79>
 < 2.00

   9.0
 I 14.0)
 < 1.1S>
 < 2.00

   3. 1
 (  2-8)
 < 1.79>
< 2.00
                                                                                 <2.0
                                                                                (  0.0)
                                                                                < 0.0 >
                                                                                < 2.00

                                                                                 <2.0
                                                                                (  0.0)
                                                                                < 0.0 >
                                                                                < 2.00

                                                                                 <2.0
                                                                                (  0.0)
                                                                                < 0.0 >
                                                                                 <2.00
                                                                                   • .0
                                                                                (  4.9)
                                                                                < 1.79>
                                                                                < 2.00
 <2.0
 (  0.0)
 < 0.0 >
 < 2.00

 <2.0
 (  0.0|
 < 0.0 >
 < 2.00

   4.1
 I  4.1)
 < i.sa>
 < 2.00

   2.6
 <  1.5)
 < 1.79>
 < 2.00

 <2.0
 (  0.01
 < 0.0 >
 <2.00

 <2.0
 I  0.0)
 < 0.0 >
 <2.00

 <2.0
 (  0.0)
 < 0.0 >
 <2.00

 <2.0
 I  0.0)
< 0.0 >
 <2. 00

-------
Table  C.27,  continued
06891



06892



0(89)



06894



06896



IBU.
06848



06849



06852



06854



06855



06856



06857



if
SD
3
BO
if
SD
S
BD
if
3D
3
BD
IV
3D
S
BD
IV
SD
S
HD
• •••I
if
SD
3
HD
if
3D
S
HD
IV
SD
S
BD
iV
3D
S
HD
IV
SD
S
HD
if
SD
S
HD
if
SD
S
(ID
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
t.oo
1-HBTHTI.IiPHTlU.llI
Ftg)t9ftf999t944t£tt4t9
2.1
( 0.2)
< 1.79>
2.00
2.2
C 0.4)
< 1.79>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 1.50>
2.00
2.0
< 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.1
( 0.3)
< 1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.1
t 0.2)
< 1.79>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.1
( 0.3)
< 1.50>
2.00
2.4
« 0.9)
< 1.50>
2.00
2-BHBYLPBEIOI.
i£4£g}90999ttttt f 01
2.0
( 0.0)
< 0.0 >
2.00
2.0
I 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.4
( 0.9)
< 1.50>
2.00
 2. 1
 0.2)
1.50>
2.00

 2.1
 0.2)
1.79>
2.00

 2.2
 0.4)
1.50>
2.00

 2.0
 0.0)
0.0 >
2.00

 2.1
 0.2)

2loO
                                                   4-HITBTI.PBHIOL
                                                         5.0
                                                         0.0)
                                                        0.0 >
                                                        5.00
                                                         5.0
                                                      (  0.0)
                                                      < 0.0 >
                                                        5.00

                                                         5.0
                                                      (  0.0)
                                                      < 0.0 >
                                                        5.00
                                                         5.0
                                                         0.0)
                                                        0.0 >
                                                        5.00

                                                         5.2
                                                         o.»)
                                                        1.50>
                                                        5.00

                                                         5.0
                                                         0.0)
                                                        0.0 >
                                                        5.00

                                                         5.0
                                                         0.0)
                                                        0.0 >
                                                        5.00
                                                                           9.0
                                                                        (   0.0)
                                                                       < 0.0 >
                          2.6
                        (  1.3)
                        <  1.50>
                        < 2.00
  41.4
 ( 48.8)
< 0.00>
 41.40

  44.2
 (  0.0)
< 0.0 >
• •*••*

   0.0
 {  0.0)
< 0.0 >
  0.0

  16.8
 (  0.0)
< 0.0 >
                                                                                              <2.0
                                                                                             (   0.0)
                                                                                             < 0.0  >
                                                                                             < 2.00

                                                                                                3.4
                                                                                             I   3.1)
                                                                                             < 1.50>
                                                                                             <2.00

                                                                                              <2-0
                                                                                             (   0.0)
                                                                                             < 0.0  >
                                                                                             <2.00
                       (
                                                                                               3.7
                                                                                               3.4)
                                                                                             <2.00
                         <2.0
                       (  0.0)
                       < 0.0 >
                        <2.00

                         <2.0
                       (  0.0)
                       < 0.0 >
                        <2.00

                       <  2-0
                       (  0.0)
                       < 0.0 >
                       <2.00

                         <2.0
                       (  0.0)
                       < 0.0 >
                       <2.00

                       <  2.0
                       (   0.0)
                       <  0.0 >
                       ,-2.00
 llPHTHiLIIB        4-MOIILPUaOL        OCTiDICilB
• *••**••••••••*••**•»•••»••••**••*••»•*»•••••••*••••**••***•
     7.5                 0.0               <2.0
  C 13.4)              (  0.0)              (  0.0)
  < 1.79>             < 0.0 >              < 0.0 >
    2.00                0.0                <2.00
     2.0
  (   0.0)
  <  0.0 >
    2.00
     2.0
  (   0.0)
  <  0.0 >
    2.00
     2.0
  (   0.0)
  <  0.0  >
    2.00
   0.1
 (  0.0)
 < 0.0 >
  0.0

   0.3
 (  0.0)
 < 0. 0 >
  0.0

   0.0
 (  0.0)
 < 0. 0 >
  0.0
                                                           4.4
                                                        <  5.8)
                                                        < 1.79>
                                                         <2.00

                                                         <2.0
                                                        I  0.0)
                                                        < 0. 0 >
                                                         <2.00
                                                           2.1
                                                        t   0.1)
                                                          1.50>
                                                        <2.00
     2.0
  (   0.0)
  <  0.0 >
    2.00
     2.0
  (   0.0)
  <  0.0 >
    2.00
     6.1
     9.2)
    1.50>
    2.00
   0.0
(  0.0)
< 0. 0 >
  0.0

   0.1
<  0.0)
< 0. 0 >
  0.0

   0.3
(  0.0)
< 0. 0 >
  0. 0
                                                         <2.0
                                                        I   0.0)
                                                        <  0.0 >
                                                        < 2.00

                                                         <2.0
                                                        (   0.0)
                                                        <  0.0 >
                                                        <2-00

                                                         < 2.0
                                                        I   0.0)
                                                        <  0.0 >
                                                        <2  nn

-------
    Table  C.27.  continued
ho
0\
    06864   *T
            SO
            a
            no

    06870   IT
            SD
            3
            HO

    06B80   IV
            SO
            3
            HO

    06681   IF
            SD
            S
            BO

    06882   1*
            SD
            S
            •0

    06883   it
           HO

    0688*  AT
           SO
           S
           •D

    06883  IT
           SD
           S
           BO

    0681*  IT
           SO
           S
           • 0

    06887  IT
           SD
           S
           •D

    06888  AT
           SD
           S
           BD

    06889  AT
           SD
           S
           BD
   2.0
 (  0.0)
< 0.0 >
  2.00
   2.0
   0.0)
  0.0 >
  2.00

   2.1
   0.2)
  1.79>
  2.00
   2.0
(  0.0)
< 0.0 •>
  2.00
   2.0
   0.0)
  0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
I  0.0)
< 0.0 >
  2.00

   2.3
(  0.7)
< 1.79>
  2.00

   2. a
{  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0  >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.7
   1.7)
  1.79>
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.1
   0.3)
  1.79>
  2.00

   2.0
   0.0)
  0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00

   2.1
(  0.3)
< 2.0«>
  2.00

   2.*
<  0.9)
< 1.79>
  2.00

   2.0
{  O.OJ
< 0.0 >
  2.00
   5.0
<  0.0)
< 0.0 >
  s.oo

   5.0
(  0.0)
< 0.0 >
  5.00

   5.0
I  0.0)
< 0.0 >
  5.00
   S.O
   0.0)
  0.0 >
  s.oo

   5.0
   0.0)
  0.0 >
  5.00

   5.2
   0.6)
  1.79>
  5.00

   S.O
   0.0)
  0.0 >
  5.00

   S.O
   0.0)
  0.0 >
  5.00
                 (  1.2)
  5.00

   S.O
(  0.0)
< 0.0 >
  s.oo
                    5.0
                 (  0.0)
                 < 0.0 >
                   5.00

                    5.0
                 (  0.0)
                 < 0.0 >
                   S. 00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
I  0.0)
< 0.0 >
  2.00
                 (  3.2)
                 < 1.78>
                   2.00

                    2.0
                 I  0.0)
                 < 0.0 >
                   2.00
                    2.0
                 (  0.0)
                 < 0.0 >
                   2.00
                    2.0
                 (  0.0)
                 < 0.0 >
                   2.00

                    2.9
                 (  2.1)
                 < 1.79>
                   2.00
                    2.0
                 I  0.0)
                 < 0.0 >
                   2.00

                    2.1
                 I  0.2)
                 < 2.0»>
                   2.00
                    2.0
                 (  0.0)
                 < 0.0 >
                   2.00

                    2.0
                 I  0.01
                 < 0.0 >
                   2.00
   2.0
(  0.0)
< 0. 0 >
• •••*•

   0.0
(  0.0)
< 0.0 >
  0.0

   0.0
(  0.0)
< 0.0 >
  0.0
                       0.1
                    I  0.0)
                    < 0.0 >
                      0.0
                       0.3
                    (  0.0)
                    < 0.0 >
                      0.0
                       0.0
                    (  0.0)
                    < 0.0 >
                      0.0
                       0.)
                       0.0)
                      0.0 >
                      0.0

                       0.)
                       0.0)
                      0.0 >
                       0.0
                     (  0.0)
                     < o. o >
                      0.0

                       0.0
                     I  0.0)
                     < 0.0 >
                      0.0
                       0.)
                     (  0.0)
                    < 0.0 >
                      0.0

                       0.1
                    (  o.ot
                    < 0.0 >
                      0.0
                                                                           < 2.0
                                                                          (  0.0)
                                                                          < 0. 0 >
                                                                          < 2.00

                                                                            <2.0
                                                                          (  0.0)
                                                                          < 0.0 >
                                                                          < 2.00

                                                                             2.3
                                                                          (  0.9)
                                                                          < 1.79>
                                                                          <2.00

                                                                             2.2
                                                                          «  0.«)
                                                                          < 1.79>
                                                                          <2.00
                       2.9
                     (  2.1)
                    < 1.79>
                     <2.00
                      <2.0
                     (  0.0)
                    < 0.0 >
                     <2.00

                      <2.0
                     (  0.0)
                    < 0.0 >
                     <2-00
                     (  3.5)
                    <  1.79>
                     <2.00

                       2.6
                     (  1.5)
                    <  1. 79>
                       2.00
                                                                             2.1
                                                                          (  0.3)
                                                                          < 2.0«>
                                                                          < 2.00
                       2. 1
                    <  0-3)
                    < t.79>
                    <2.00

                      <2-0
                    (  0.01
                    < 0. 0 >
                    < 2.00

-------
   Table C.27, continued
N5
06890



06891



06892



06893



06894



06896



BILL
• *•*••<
068*8



068*9



06852



0685*



06855



06856



IT
SD
S
BD
if
SD
S
BD
IT
SD
S
BD
IT
SD
S
BD
IT
3D
3
BD
»T
SD
S
BD


(
<


(
<


(
<


1
<


(
<


(
<

PBBBOL
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.9
2.1)
1.79>
2.00
2.*
0.8)
1.50>
2.00
2.4
1.0)
1.50>
2.00
2.0
0.0)
0.0 >
2.00
PBOP1ZIBB
2.0
( 0.0)
4.5
( 1.2)
< 0.0 > <-1.79>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.5
( 1.3)
< 1.79>
2.00
2.2
( 0.4)
< 1. 50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
1-TBBPIBEOL
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.2
( 0.5)
< 1.79>
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
TITBACHLOBOETBrUBB

(
<


(
<


(
<


(
<


(
<


(


TOLD EBB
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.3
0.8)
1.50>
2.00

1
<


(
<


<
<


<
<


(
<


(
<

TBICBJ.OBOEIH1BK
0.0
0.0)
0.0 >
0.0
0.3
0.0)
0.0 >
0.0
0.)
0.0)
0.0 >
0.0
0.)
0.0)
0.0 >
0.0
0.0
0.0)
0.0 >
0.0
0.3
0.0)
0.0 >
0.0








'















< 2.0
( 0.0)
< 1. 79>
<2.00
<2.0
( 0.0)
< 0.0 >
<2.00
<2.0
( 0.0)
< 0.0 >
<2.00
<2.0
( 0.0)
< 0.0 >
<2.00
3.0
( 2. 1)
< 1.50>
<2.00

<2.00
OICaLOBOBTBILBBB
• ••*••••••••••••»«••••»•»•••«•••••»•••»»•••••*••••••»»»•»•••••••«•*•••••••••»••••»•••««••••*»»••«••••»••«»•••»•»•»»«»»•»»,,
IT
SD
S
BD
AT
SD
S
BD
IT
SD
S
BD
IT
SD
S
BD
AT
SD
S
BD
AT
SD
S
no
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
C 0.0)
< 0.0 >
10.00
10.0
< 0.0)
< 0.0 >
10.00
2.4
J 1-1)
< 1.79>
2.00
2.3
1 0.9)
< 1.79>
2.00
3.0
( 2.5)
< 1.79>
2.00
2.3
( 0.7)
< 1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
7.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
< '-0
1 0.0)
< 0.0 >
< 1.00
1.6
( 1.5)
< 1.79>
< 1.00
5.3
( 10.6)
< 1.79>
<1.00
5.4
( 9-7)
< 1.50>
< 1.00
< 1.0
1 0.0)
< 0.0 >
< 1.00
< 1.0
( 0.0)
< 0.0 >
<1.00
< 1.0
( 0.0)
< 0.0 >
<1.00
1.2
( 0.5)
< 1.79>
<1.00
2.0
( 2.4)
< 1.79>
<1.00
1.3
( 0.6)
< 1.50>
< 1.00
<1.0
( 0.0)
< 0.0 >
<1.00
<1.0
( 0.0)
< 0.0 >
< 1.00
























5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( O-.O)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
S.OO
















'







1.4
( 1.11
< t.79>
1.00
2.0
( 1-4)
< 1.03>
1.60
1.5
I 1.1)
< 1.79>
1.00
2.6
I 2.3)
< 0.76>
1.00
1.6
( 1.1)
< 1. 15>
1.00
1.8
( 2.0)
< 1.79>
1.00

























-------
Table C.27, continued
06857


06864



06870



06880



06881



06882
r;.
1X3
CO
06883



0688*



06885



06886



06887



06888



IT 10.0
SD ( 0.0)
BD 10.00
IT 10.0
SD ( 0.0)
S < 0.0 >
BD 10.00
AT 10.0
SD ( 0.0)
S < 0.0 >
•D 10.00
AT 10.0
3D ( 0.0)
S < 0.0 >
BO 10.00
IT 10.0
3D ( 0.0)
S < 0.0 >
80 10.00
IT 10.0
3D ( 0.0)
S < 0.0 >
•0 10.00
AT 10.0
3D ( 0.0)
3 < 0.0 >
RD 10.00
AT 10.0
SD ( 0.0)
S < 0.0 >
BD 10.00
IT 10.0
SD { 0.0)
S < 0.0 >
BD 10.00
AT 10.0
SD ( 0.0)
S < 0.0 >
RD 10.00
AT 10.0
SD ( 0.0)
3 < 0.0 >
RD 10.00
AT 10.0
SD ( 0.0)
S < 0.0 >
HO 10.00
2.6

2.00
2.0
( 0.0)
< 0.0 >
2.00
2.4
( 0.9)
< 1.79>
2.00
2.0
( 0.0)
< 0.0 >
2.00
3.1
( 2.5)
< 1.76>
2.00
3.0
( 2.6)
< 1.79>
2.00
3.5
( 3.«)
< 1.79>
2.00
3.3
( 3-D
< 1.79>
2.00
4.7
( 3.4)
< 1.00>
3.55
*••*•
(**•**)
< 1.79>
2.00
2.8
i 2.1)
< 2.04>
2.00
3.0
( 2.4)
< 1.79>
2.00
2.0
( 0.0)

2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
I 0.0)
< 0. 0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.3
( 0.7)
< 1.79>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
< i.o
( 0.0)

< 1.00
<1.0
( 0.0)
< 0.0 >
^.oo
<1.0
( 0.0)
< 0.0 >
<1.00
< 1.0
( 0.0)
< 0.0 >
<1.00
< 1.0
( 0.0)
< 0.0 >
<1.00
<1.0
« 0.0)
< 0.0 >
<1.00
<1.0
( 0.0)
< 0.0 >
< 1.00
< 1.0
I 0.0)
< 0.0 >
<1.00
< 1.0
1 0.0)
< 0.0 >
<1.00
< 1.0
( 0.0)
< 0.0 >
<1.00
0.0
( 0.0)

< 1.00
o.o
( 0.0)
< 0.0 >
<1.00
2. 1
( 2.7)
< 1.79>
< 1.00
1.3
( 0.7)
< 1.79>
<1.00
2.8
( *«5)
< 1.79>
<1.00
3.0
< 4.6)
< 1.78>
< 1.00
< '.°
( 0.0)
< 0.0 >
<1.00 .
1.2
( 0.5)
< 1.79>
<1.00
1.7
( 1.*)
< 1.67>
< 1.00
<1.0
( 0.0)
< 0.0 >
<1.00
4.6
( B.4|
< I.7B>
< 1.00
5.0
( 0.0)

S.OO
5.0
( 0.0)
< 0.0 >
S.OO
5.0
I 0.0)
< 0.0 >
S.OO
5.0
( 0.0)
< 0. 0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
S.OO
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
slo
( 0.0)
< 0.0 >
S.OO
5.0
( 0.0)
< 0.0 >
5.00
5.0
I 0.0)
< 0.0 >
S.OO
1.8
< 1-7)
<1 *.fW
1*3 U'
1.00
1.9
( 1.2)
< 0.63>
1.60
4.6
( 7.5)
< 1.71>
1.00
1.9
( 1.6)
< t.2S>
1.00
2.3
I 1.6)
< 0.12>
2.15
1.6
( 1.2)
< 1.63>
1.00
3.2
I 3.5)

iloo
1.5
I 1.1)
< 1.50>
1.00
2.2
( 1.8)
< 0.72>
1.00
3.4
( 3.1)
< 0.48>
2.65
1.6
( 1.4)
< 1.79>
1.00
1.8
I 1.4)

iToo

-------
Table C.27, continued
06889  IT   10.0
       SD  (  0.0)
       S   < 0.0 >
       BD   10.00

06890  IT   8.7
       SD  (  3.3)
       S   <-1.79>
       (ID   10.00

06891  AT  10.0
       SD  (  0.0)
       S   < 0.0 >
       BD  10.00

06892  AT  10.0
       SD  (  0.0)
       S   < 0.0 >
       BD  10.00

06893  AT  10.0
       3D  (  0.0)
       S   < 0.0 >
       BD  10.00

06894  AT  10.0
       SD  |  0.0)
       S   < 0.0 >
       BD  10.00

06896  AT   8.2
       SD  (  4.0)
       S   <-1.50>
       BD  10.00
2.0
I 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.9
I 2.0)
< 1.50>
2.00
2.4
( 0.9)
< 1.79>
2.00
4.9
( 4.0)
< 0.43>
2.00
2.2
1 0.5)
< 1.50>
2.00
2.5
( 1.1)
< 1.50>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
0.0
1 0.0)
< 0.0 >
<1.00
<1.0
I 0.0)
< 0.0 >
<1.00
O.O
( 0.0)
< 0.0 >
< 1.00
O.O
( 0.0)
< 0.0 >
<1.00
<1.0
I 0.0)
< 0.0 >
<1.00
O.O
I 0.0)
< 0.0 >
<1.00
<1.0
( 0.0)
< 0.0 >
o.oo
< 1.0
( 0.0)
< 0.0 >
< 1.00
<1.0
( 0.0)
< 0.0 >
< 1.00
1.8
( 1.7)
< 1.50>
< t.oo
1.2
( 0.4)
< 1.79>
< 1.00
3.4
( 3.9)
< 1.14X
< 1.00
< 1.0
( 0.0)
< 0.0 >
< 1.00
1.8
( 1.8)
< 1.50>
< 1.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
5.0
I 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
5.00
2.2
1 2.1)
< 0.71>
1.00
3.5
( 3.2)
< 0.58>
2.55
1.7
( 1-«)
< 1.50>
1.00
1.5
( 1- K
< 1.74>
1.00
1.5
( 1.1)
< 1.50>
1.00
3.0
( 2.7)
< 0.70>
2.15
1.6
( 1-3)
< 1.50>
1.00
* AV  - Arithmetic Average
  SD  - Standard  Deviation
    S  - Skewness
  MD  - Median

-------
OBGANICS (PPB)
         Table C.28
  Gray Wells After Baseline
Priority Organic  Pollutants
HELL
06848



06809



06852



06854



.p. 06855
WJ
O

06856



06857



0686«



06870



06880



06881



ACERAPHTHTLENE ANTHBACENE/PHE.1ATIIR ENE ATRAZIN6 BKMZEHE/TRICHLOROETHtL ENE
A»*
SO
S
no
AT
SD
S
no
AT
SD
S
NO
AT
SD
S
no
AT
SD
S
no
AT
SD
S
no
IT
SD
S
no
IT
SD
S
HD
IT
SD
S
no
AT
SD
S
HD
AT
SD
S
no
3.0
( 1-7)
< 0.71>
2.00
2.0
t oil)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
3.5
( 2.1)
< 0.0 >
3.50
3.0
( L7)
< 0.71>
2.00
3.0
( 1.7)
< 0.71>
2.00
3.0
( 1.7)
< 0.71>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
3.0
( 1.7)
< 0.71>
2.00
3.0
( 1-7)
< 0.71>
2.00
2.0
( 0.0)
t 0.0 >
2.00
2.0
( 0.0)
< 0.0 )
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
< 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 )
2.00
2.0
( 0.0)
< 0.0 5
2.00
3.5
t 2.7)
< 0.71>
2.00
2.3
( 0.1)
< 0.0 >
2.00
7. 3
( 1.6)
<-0. 71>
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
6.0
( 5.7)
< 0.0 >
A. 00
7.3
I 1.6)

10.00
7.3
( 1.6)
<-0.7 1>
10.00
7.3
( 1.6)
<-0.7 1>
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
7.3
( 1.6)
<-0.7 1>
10.00
7. 1
{ 1 . *)
<-0. 7 1 >
10.00
1.0
( 0.1)
< 0.71>
1.00
1.0
( 0.0)
< 0.0 >
1.00
6.2
( 8.9)
< 0.71>
1.CO
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.14
t 0.5)
< 0.15>
1.30
1.2
( 0.1)
< 0.71>
1.00
' 1.1
( 0.6)
< 0.71>
1.00
1.2
( 0.3)
< 0.0 >
1.20
1. 1
( 0.1)
< 0.71>
1.00
1. 1
( 0.2)
< 0.71>
1.00
BENZENuceric ACIU O-T-DUTYLPHEKOL
0. 0
( d-O)
< o.o >
0.0
0. 0
( 0. 0)
< o.o •>
0.0
o.o
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
1. )
I o.f.)
< J.71>
1.00
1.0
( 0.0)
< J.O >
1.0D
1.0
( 0.0)
< 0.0 >
1.00
1.5
( 0.7)
< 3.0 >
1. 50
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.3
( 0.6)
< 0. 7 1>
1.00
1. J
t 0.6)
< 0. 71>
1.00

-------
label  C.28,  continued
06882



06883



0688*



06885



06886



06887



06888



06889



06890



06891



06892



06893



IT
SD
S
no
IT
SD
S
BD
IT
SO
S
no
AT
SO
S
no
IT
SD
S
ND
IT
SD
S
no
AT
SD
S
(ID
AT
SD
S
HO
AT
SD
S
ND
AT
3D
S
HD
AT
SD
S
no
AT
SD
S
no
).5
( 1.7)
< 0.0 )
3.50
3.5
{ 1.5)
< 0.0 >
3.50
3.5
( 1.7)
< 0.0 >
3.50
3.5
( 1.7)
< 0.0 >
3.50
3.0
( 1.7)
< 0.71>
2.00
3.0
{ 1.7)
< 0.71>
2.00
3.0
( 1.7)
< 0.71>
2.00
3.0
( 1-7)
< 0.71>
2.00
3.0
( 1.7)
< 0.71>
2.00
3.0
( 1.7|
< 0.71>
2.00
3.0
{ 1.7)
< 0.71>
2.00
3.0
« 1-7)
< 0.71>
2.00
                                        5.2
  2.00

   2.0
<  0.0)
< 0.0 •>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
{  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   3.2
(  2.M
< 0.71>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
                                        2.0
                                        0.0)
                                       0.0 >
                                       2.00
                                        2.0
                                     (  0.0)
                                     < 0.0 >
                                       2.00

                                        2.0
                                     (  0.0)
                                     < 0.0 >
                                       2.00
                                        2.0
                                     <  0.0)
                                     < 0.0  >
                                       2.00
                                        2.0
                                        3.0)
                                       0.0 >
                                       2.00
                                                           6.0
                                                        {  «.6)
                                                        < 0.0 >
                                                          A. 00

                                                           7.1
                                                        (  1-6)
                                                        <-0.71>
                                                         10.00

                                                           6.0
                                                        (  1.6)
                                                        < 0.0 >
                                                          6.00
                                                        (  1.6)
                                                        < 0.0  >
                                                          6.00

                                                           7. 1
                                                        (  «.6|
                                                        <-0.7t>
                                                          10.00

                                                           7.3
                                                        (  »•«)
                                                        <-3.7t>
                                                          10.00

                                                           7.3
 10.00

   7.3
(  »-6)
<-0.71>
 10.00

   7.3
(  I.*)
<-0.71>
 10.00

   7.3
(  1-6)
<-0.71>
 10.00

   7.1
(  1-6)
<-0.71>
 10.00

   tt.7
(  1.6)
< 0.71>
  2.00
                      1.5
                   (   0.5)
                   <  0.26>
                     1.50

                      1.1
                   {   0.5)
                   <  o.ia>
                     1.30

                      1.1
                   {   0.7)
                   <  0.90>
                     1.20

                      1. 3
                   (   0.3).
                   <:  0.05>
                     1.25

                      1.0
                   (   0. 1)
                   <  0.71>
                     1.00

                      1.1
                   (   0. 1)
                   <  0.71>
                     1.00

                      1.2
                   (   0.3)
                   <  0.71>
                     1.00
   1.0
(  0.0)
< 0.0 >
  1.00
                                         1.0
                                      (  0.0)
                                      < 0.0 >
                                        1.00

                                         1.7
                                      (  0.8)
                                      < 0.69>
                                        1.30

                                         1. 1
                                      (  0.2)
                                      < 0.71>
                                        1.00

                                         1.1
                                      (  0.6|
                                      < 0.62>
                                        1.20
                           l). J
                           0.0)
                          0.0 >
                          O.I)
                           2.0
                        (  U. J)
                        < 0.0 >
                        ••*#••
                           0.0
                        (  0.0)
                        < 0.0 >
                          0.0

                           0.0
                        (  0.0)
                        < 0.0 >
                          0.0

                           o.a
                        (  0.0)
                        < o.o >
                          0.0

                           0.0
                        (  0.0)
                        < 0.0 >
                          0.0
                           0.0
                        I   0.0)
                        <  0.0  J
                          0.0
                                                                 0.0
                                                              (   0.0)
                                                              <  0.0  )
                                                                0.0
                           3.0
                        I   0.0)
                        <  0.0 >
                          0.0
                          0.0
                          0.0)
                          0.0  >
                          0.0
                           0.0
                        (   0.0)
                        <  0.0  >
                          0.0
                           0.0
                           0.0)
                          0.0  >
                          0.0
 (   0.6)
 <  J.O >
   1.50

    2. fl
 (   2.3)
 <  0.56>
   2.UO

    J.O
 (   3.1)
 <  1.09>
   1.50

    1.5
 (   0.6)
 <  D.O •>
   1.50

    1. ]
 (   0.6)
 <  0.71>
   1.00

    1.3
 (   0.6)
 <  0.71>
   1.00

    1. )
 (   0.6)
 <  0.71>
   1.00

    1.3
 I  0.6)
<  0.71>
   1.00
   2.1
<  1.2)
< 0. I6>
  2.00

   1.3
(  0.6)
< 0.71>
  1.00
   1.3
I   0.6)
<  0.71>
  1.00

   I. J
(   0-M
<  0.71>
  1.00

-------
N>
Table C.28, continued
06894



06896



Af
SO
S
no
AT
SO
S
no
1.8
( 1.5)
<-0.26>
4.05
4.3
( L5)

5.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
I 0.0)
< 0.0 >
2.00
6. 1
( t.b|
< J.O >
6.00
6.0
( *.(>)
< 0.0 >
6.00
SELL CAIBOI TETRACHLOKIDE 4-CHLOBOAIILIRE CFtlOROBZIZ EH E
06848 »T 2.9 10.0 1.0



06849



06852



06854



06855



06856



06857



06864



06870



06880



so
s
no
IT
SD
S
no
IT
50
S
no
IT
SD
S
no
IT
SD
S
no
Af
SD
S
no
IT
SD
S
no
AT
SD
S
no
IT
SD
S
HD
IT
SD
s
no
( 1.8)
< 0.69>
2.00
3.6
( 1.5)

3^90
5.0
( 3-0)
< o.o •>
5.00
6.5
( 2.1)
< 0.0 >
6.50
4.3
( 2.0)
<-0.58>
5.00
3.4
{ 1-5)
< 0. 31>
3.10
3.0
( 1.7)
< 0.58>
2.40
3.9
( 1.7)
<-0.70>
4.90
2.4
( 0.6)
< 0.0 »
2.40
3.3
( 1-5)
< 0.38>
3.00
( 0.0)
< o.n >
10.00
10.0
{ 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
1 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
( 0-0)
< 0.0 >
1.00
1.0
( °-3)
< o.o •>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< o.o •>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< o.o •>
1.0O
1.0
( 0.0)
< 0.0 >
1.00
1.6
( d-6)
< 0.5U>
1.50
CHLOBOPOPn
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.2
( 0.3)
< 0.71>
1.00
1.0
( 0.0)
< 0. 0 >
1.00
1.6
( 1.0)
< 0.71>
1.00
1.5
( 0.8)
< 0.00>
1.55
1.0
( 0.0)
< 0 . 0 >
1 .00
J. J
( 0-0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
2-CHLOR) POE1OL
1.3
( J.6I
< 0.71>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.5
{ 0.7)
< 0.0 >
1.50
1.3
( 0.64
< 0. 71>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0. 71>
1.00
1.0
I 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0. 0 >
1.00
1.J
( 0.6)
< 0.71>
1.OO
t.S
( 0.6)
< 0.0 >
1.50
1.5
( 0.6)
< 0.0 5
1.50
1-CHLUBCTETDADECA1E
2.0
( 0.0)
< 0.0 >
2.00
2.0
I 0.0)
< 0.0 >
2.00
2.8
( 1.3)
< 0.71>
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
I 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( J.O)
< 0.0 >
2.00
2.0
I 0.0)
< 0. 0 >
2.00
2.0
1 0-01
< o.a >
2.00

-------
 Table  C.28,  continued
06881  A»        S.J
       SO      (  1.5)
       S      < 0.17>
       no       5.00
06882



068R3



0688*



06885



06886



06887



06888



06889



06890



06891



06892



IT
SO
S
no
IV
3D
S
no
AT
SO
S
no
IT
3D
S
no
AT
3D
S
RD
AT
3D
S
no
AT
so
S
BD
IT
SO
S
no
IT
3D
S
no
IT
3D
S
NO
AT
3D
S
ID
3.1
( 1-9)
<-0.02>
3. SO
2.9
( 1-8)
< 0.69>
2.00
3.*
( 1-9)
<-0.03>
3. SO
4.5
( 1-8)
<-0.8»>
5.00
3.1
« 1-7)
< 0.68>
2.30
3.0
( 1.7)
< 0.71>
2.00
3.0
( 1.7)
< 0.71>
2.00
«.3
( 2.1)
<-0.53>
S.OO
3.3
( 1-M
< 0.4S>
2.90
3.3
( 1.5)
< o.«s>
2.90
3.2
( 1.«)
< 0.60>
2.60
  10.0
<  O.OJ
< 0.0 >
 10.00

  10.0
(  0.0)
< 0.0 5
 10.00

  10.0
(  O.OJ
< 0.0 >
 10.00

  10.0
(  0.0)
< 0.0 >
 10.00

  10.0
(  0.0)
< 0.0 >
 10.00

  10.0
<  0.0)
< 0.0 >
 10.00

  10.0
(  0.0)
< 0.0 >
 10.00

  10.0
(  0.0)
< 3.0 >
 10.00

  10.0
<  0.0)
< 0.0 >
 10.00

  10.0
(  0.0)
< 0.0 >
 10.00

  10.0
«  0.0)
< 0.0 >
 10.00

  10.0
(  0.0)
< 0.0 >
 10.00
   1.0
(  0.0)
< 0.0 )
  1.00
                                                         1.0
                                                      (  0.0)
                                                      < 0.0 >
                                                        1.00
                                                         1.0
                                                      (  0.0)
                                                      < 0.0 >
                                                        1.00

                                                         1.0
                                                      (  0.0)
                                                      < 0.0 >
                                                        1.00

                                                         1.0
                                                      t  0.0)
                                                      < 0.0 >
                                                        1.00
                                                         1.0
                                                         0.0)
                                                        0.0 >
                                                        1.00

                                                         1.0
                                                         0.0)
                                                        0.0 >
                                                        1.00
                                                         1.0
                                                      (  0.0)
                                                      < 0.0 >
                                                        1.00
                                                         1.0
                                                         0.0)
                                                        0.0 >
                                                        1.00

                                                         1.0
                                                         0.0)
                                                        0.0 >
                                                        1.00

                                                         1.0
                                                         0.0)
                                                        0.0 >
                                                        1.00

                                                         1.0
                                                         0.0)
                                                        0.0 >
                                                        1.00
   1.0
(  0-0)
< 0.0 >
  1.00
                        1.0
                     (   0.0)
                     <  0.0  >
                       1.00

                        1.2
                     (   0.3)
                     <  0.71>
                      ,1.00

                        1.0
                     (   0.0)
                     <  0.0 >
                       1.00
                        1.0
                        0.0)
                      0.0 >
                      1.00

                        1.0
                        0.0)
                      0.0 >
                      1.00

                        1.0
                        0.0)
                      0.0 >
                      1.00
                       1.0
                    {  0.0)
                    < 0.0 >
                      1.00

                       1.0
                    (  0.0)
                    < 0.0 >
                      1.00

                       1.0
                    (  0.0)
                    < 0.0 >
                      1.00
                       2.5
                       2.7)
                      0.71>
                      1.00
                       1.0
                    (  0.0)
                    < 0.0 >
                      1.00
    I. J
 <   0.6)
 <  0. 71>
   1.00

    1.5
 (   0.61
 <  0.0  )
   1.50

    1. 3
 (   0.61
 <  0.71>
   1.00

    3.0
 (   1-tl
 <  1. 09>
   1.50

    1.5
 (   0.6)
 <  3.0 >
   1.50

    1.3
 (  0.61
 <  0. 71>
   1.00

    1.J
 (  0.6)
 <  0.71>
   1.00

    1.3
 I  0.61
 <  0.71>
   1.00

   1.3
 (  0.6|
 <  0.71>
   1.00

   1.3
 I  0.6)
 < 0.71>
   1.00

   1.3
 (  0.6i
 < 0. 71>
   1.00

   1.3
 I  0.6)
< 0.71>
  1.00
    2. J
 (   J.JI
 <  0.0  >
   2.00

    2.0
 (   0.0)
 <  0.0  >
   2.00

    2.0
 (   0.0)
 <  0.0  >
   2.00

    2.6
 (   1-5)
 <  t.15>
   2.00

    2.0
 (   0.0)
 <  0.0  >
   2.00

    2.0
 (   3.0)
 <  0.0  >
   2.00

    2.0
 (   0.0)
 <  0.0  >
   2.00

    2.0
 (   0.0)
<  0.0 >
   2.00

   2.0
 I   0.0)
< 0.0 )
  2.00

   2.0
 (  0.0)
< 0.0 >
  2.00
                                          2.0
                                          0.0)
                                         0.0 )
                                         2.00

                                          2.0
                                          0.0)
                                         0.0 >
                                         2.00

-------
Table C.28, continued
06893



0689*



06896



• ELL
• ••• •*
068*8



068*9



06852


4>
VjJ
"^ 0685*



068S5



06856



06857



0686*



06870



AT
SD
S
no
AT
SD
S
BD
AT
SD
S
no












3.0
( 1-7)
< 0.71>
2.00
3.*
( 1.8)
<-0.01>
3.50
3.5
( 1-7)
< o.o >
3.50
DIBOTTLPHATHALAT!
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
BD
AT
SD
S
RD
AT
SD
S
BD
IT
SD
S
BO
AT
SD
s
no
W V
(



(
<


(
<


(
<


(



(
<


(
<


(



{
<

VVVVVVVVVVVV
8.8
7.9)
0.«3>
6.80
2.0
0.0)
0.0 >
2.00
3.*
2.*)
0.71>
2.00
2.0
0.0)
0.0 >
2.00 x
2.9
1.5)
0.71>
2.00
».»
*.1)
0.71>
2.00
2.0
0.0)
0.0 >
2.00
3.7
2.9)
0.71>
2.00
2.0
0.0)
0.0 >
2.00












10.0
1 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
2,3-DICHLOROiJrLIH'
3.0
(



(
<


(
<


(
<


(



(



<



(
<


(
<

1.7)
0.71>
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
3.5
2-1)
0.0 >
3.50
3.0
1.7)
0.71>
2.00
3.0
1.7)
0.71>
2.00
3.0
1.7)
0.71>
2.00
2.0
0.0)
0.0 )
2.00
2.0
0.0)
0.0 >
2.00

(
<


(
<


(
<

1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
3,4-DicrioRtuffiun::

(
<


(
<


(
<


(
<


(
<


(
<


(
<


(
<


(
<

2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
2.00

(
<


(
<


(


1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
• 1.2
0.3)

UOO
DICULOROEENZEIE fl
1.3
(



(
<


(
<


(
<


I
<


(



(
<


(
<


(
<

0.6)
0.71>
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1.5
0.7)
0.0 >
1.50
1.3
0.6)
0.71>
1.00
1.3
0.6)
0.7t>
1.00
1.3
0.6)
0.71>
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
1. J
( O.b)
< 0. 71>
1.00
1.5
( 0.6)
< 0.0 >
1.50
1.5
( 0.6)
< 0. 0 >
1.50
DICHLORODEIZENE P
1.3
( 0.6)
< 0.7 1>
1.30
1.0
( 0.0)
< 0.0 >
1.00
1.0
1 0.0)
< 0.0 >
1.00
1.5
J 0.7)
< 0.0 >
1.50
1.)
1 0.6)
< 0.71>
1.00
1. J
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.0
1 0.0)
< 0.0 >
1.00
1.0
1 0.0)
< 0.0 >
t.OO
4. •*
( ">. J)
< 0.71>
2.00
2.0
( 0.0)
< 0.0 >
2.JO
2.1)
1 3.0)
< 0.0 >
2.30
DICHLOU05EMZEKE O
1.3
( 3.6)
< 0.71>
1.))
1.3
1 0.3)
< 3.0 >
1.30
1.3
( 0.3)
< 0.3 >
1.03
1.5
( 0.7)
< 0.3 >
1.50
1. 1
' ( 0*6)
< 0.71>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0.7I>
1.00
1.0
( 0.0)
< 0.3 >
1.30
1.3
( 0.0)
< 0.0 >
1.00

-------
 Table  C.28,  continued
06880
06881
AT
SD
S
HO

IT
SD
S
HD
06882  IT
       SD
       S
       BD

06883  IT
       SD
       S
       BD

0688*  IT
       SD
       S
       HD

06885  IT
       SD
       S
       RD

06886  AT
       SD
       S
       BD

06887  IT
       SD
       S
       no

06888  AT
       SD
       S
       HD

06889  IT
       SD
       S
       HD

 06890  AT
       SD
       S
       HD

 06891  AT
       SD
       S
       HD
   6.2
(  5.2)
< 0.52>
  •.60

   2.8
{  1.«)
< 0.71>
  2.00

   3.3
(  2.6)
< 1.15>
  2.00
      < 0.71>
        2.00

         5.1
      (  6.3)
      < 1.15>
        2.00

         5.1
      (  6.3)
      < 1.1S>
        2.00

         5.3
      t  5.7)
      < 0.71>
        2.00
       I   «•«)
       <  0.71>
         2.00

          2.7
       (   1-2)
       <  0.71>
         2.00

          6.0
       (   7.0)
       <  0.71>
         2.00

          4.0
       <   3.»)
       <  0.71>
         2.00

          2.6
       (   1-0)
       <  0.71>
         2.00
   1.0
(  1.7)
< 0.71>
  2.00

   3.0
(  1.7)
< 0.71>
  2.00

   3.5
(  1-7)
< 0.0 >
  3.50

   3.*
(  1.5)
< 0.2«>
  3.20

   8.9
( 12.0)
< l.11>
  3.50
                                    3.5
                                    1.7)
                                   0.0 >
                                   3.50
                       3.0
                    (   1-7)
                    <  0.71>
                      2.00

                       3.0
                    (   1.7)
                    <  0.71>
                      2.00

                       3.0
                    {   1.7)
                    <  0.71>
                      2.00

                       6.3
                    (   5.1)
                    <  0.45>
                      5.00

                       3.0
                    <   L7)
                    <  0.71>
                      2.00

                       3.0
                    (   1-7)
                    <  0.71>
                      2.00
                                                         2.0
                                                      {   0.0)
                                                      <  0.0 >
                                                        2.00
   2.0
   0.0)
  0.0 >
  2.00
   2.0
{  0.0)
< 0.0 >
  2.00

   2.0
C  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 •>
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00

   2.0
<  0.0)
< 0.0 >
  2.00

   2.0
(  0.0)
< 0.0 >
  2.00
                                                         2.0
                                                      (  0.0)
                                                      < 0.0 t
                                                        2.00

                                                         2.2
                                                      (  0.3)
                                                      < 0.71>
                                                        2.00

                                                         2.6
                                                      (  1-0)
                                                      < 0.71>
                                                        2.00
    1. J
   0.6)
  0.71>
  1.00

    1.3
   0.6)
  0.71>
  1.00

    1.5
   0.6)
  0.0 )
  1.50

   1.3
   0.6)
  0.71>
  1.00
   1.5
(  0.6)
< 0.0 >
  1.50

   1.5
(  0.6)
< 0. 0 >
  1.50

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00
                                                         2.0
                                                         0.0)
                                                        0.0 >
                                                        2.00
                                             1.3
                                             0.6)
                                            0.71>
                                            1.00

                                             1.1
                                             0.5)
                                            0.60>
                                            1.20
                                                                                                1.3
                                                                                              I  0.6)
                                                                                              < 0.71>
                                                                                               1.00

                                                                                                1.3
                                                                                              I  0.6)
                                                                                              < 0.71>
                                                                                               1.00
                                                                                                1.5
                                                                                              I  0.6)
                                                                                             < 0.0 >
                                                                                               1.50

                                                                                                1.3
                                                                                              (  0.6)
                                                                                             < 0.71>
                                                                                               1.00
                                                                                                1.5
                                                                                             (  0.6)
                                                                                             < 0.0 >
                                                                                               1.50
                                                                1.5
                                                             I   0.6)
                                                             <  0.0 >
                                                               1.50

                                                                1.3
                                                             <   0.6)
                                                             <  0.71>
                                                               1.00

                                                                1.3
                                                             (   0.6)
                                                             <  0.71>
                                                               1.00

                                                                1.3
                                                             (   0.6)
                                                             <  0.71>
                                                               1.00
                                          1.7
                                        (  0.6)
                                        <-0.63>
                                         2.00

                                          1. 3
                                        t  0.6)
                                        < 0.71>
                                         1.00

                                          1.3
                                        I  0.6)
                                        < 0.7t>
                                         1.00
   1. 1
 I  0.6)
 < 0.71>
  1.00

   1.5
 (  0.5)
 < 0.0 >
  1.50

   1.6
 (  0.5)
 <-0.17>
  1.65

   1.7
 (  0.6)
 <-0.71>
  2.00

   1.9
 (  0.6)
 <-0.65>
  2.00

   1.6
(  0.5)
 <-0.31>
  1.70

   1.3
(  0.6)
 <  0.71>
  1.00

   1.4
I  0.5)
 <  0.«5>
  I.JO

   1.6
(  0.5)
 <-0.«5>
  1.70

   1.3
I  0.6)
 <  0.71>
  1.00

   1.8
(  0.7|
 <-O.U7>
  2.00

   1. )
(  0.6)
 <  0.71>
  1.00

-------
  Table C.28,  continued
06892



06893



06894



06896



IT
SO
s
no
»t
so
s
NO
»T
30
S
NO
IT
SO
S
no
J.7
( 2-9)
< 0.71>
2.00
8.0
( 10. 5)
< 0.71>
2.00
2.7
( 1-«>
< 1.15>
2.00
3.1
( 2.3)
< 1.15>
2.00
                                    1.0
                                 <  1.7|
                                 < 0.71>
                                   2.00

                                    J.O
                                 (  1.7)
                                 < 0.71>
                                   2.00
                                    3.5
                                    1.7)
                                   0.0 >
                                   3.50
                                    3.5
                                 (   1-7)
                                 <  0.0  >
                                   3.50
   2.0
{  0.0)
< 0.0 >
  2.JO

   2.0
(  0.0)
< 0.0 >
  2.00
   2.0
   0.0)
  0.0 >
  2.00

   2.0
   0.0)
  0.0 >
  2.00
   1.5
(  0.5)
< 0.0 >
  1.50

   1.3
(  0.6)
< 0.71>
  1.00

   1.7
I  0.5)
<-1.03>
  1.90

   1.6
(  0.5)
<-0.17>
  1.65
   1.3
I  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00
   1.5
I  0.6)
< 0.0 >
  1.50
   1.5
(  0.6)
< 0.0 >
  1.50
                                                                                                                         1.6
                                                                                                                      I   0.6)
                                                                                                                      <-0.68>
                                                                                                                        1.90

                                                                                                                         1. 3
                                                                                                                      I   0.6)
                                                                                                                      <  0.71>
                                                                                                                        1.00

                                                                                                                         1.5
                                                                                                                      (   0.6)
                                                                                                                      <  0.0  >
                                                                                                                        1.50

                                                                                                                         1.9
                                                                                                                      (   0.6)
                                                                                                                      <-0.65>
                                                                                                                        2.00
WELL        DICHLOBOHBTHtlB   2,4-DICHLOEOPHEIOL  DIETHf LPHTHiliTE  IUISOOCTTLPHTIIALJITE  OIOCTTLPHTIIlLiTE   DODZC1XGIC ICID
•••••••••••••••••••••••••••••ft***************************************************************************************************
068*8  AT         0.0                 2.7               16.3                2.0                  2.0               0.0
       SO       (  0.0)             (   0.6)             ( 24.8)             (  0.0)              (   0.0)           (   0.0)
       3       < 0.0 >             <-0.71>             < 0.71>            < 0.0 >              < 0.0 >           <  0.0 >
       HO        0.0                 3.00               2.00             ••••••               *«•*•«              o.O
4>
Vd
06849  AT
       SD

       ND

06852  »T
       SD
       S
       no

06854  IT
       3D
       S
       90

06855  AT
       SD
       S
       BD

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       SD
       S
       no

06857  IT
       SD
       S
       no

06864  if
       SD
       S
       no
  0.0
  0.0)
 0.0 >
 0.0

  0.0
  0.0)
 0.0 >
 0.0

  0.0
  0.0)
 0.0 >
 0.0

  0.0
  0.0)
 0.0 >
 0.0

  0.0
  0.0)
 0.0 >
 0.0

  0.0
  0.0)
 0.0 >
 0.0

  0.0
  0.0)
: o.O  >
 O.O
   3.0
(  0.0)
< 0.0 >
  3.00

   3.0
(  0.0)
< 0.0 >
  3.00

   2.5
(  0.7)
< 0.0 >
  2.50

   2.7
(  0.6)

  3*.00

   2.7
(  0.6)

  3."00

   2.7
i  0.6)

  3^00

   3.0
(  0.0)
< O.O  >
  1.00
                                                         2.0
                                                      (  0.0)
                                                      < 0.0 >
                                                        2.00

                                                        14.8
                                                      ( 22.2)
                                                      < 0.71>
                                                        2.00

                                                         2.0
                                                      (  0.0)
                                                      < 0.0 >
                                                        2.00

                                                        15.2
                                                      ( 12.7)
                                                      <-0.16>
                                                       16.30

                                                         9. ft
                                                      ( 13.2)
                                                      < 0.71>
                                                        2.00

                                                        10.0
                                                      ( 13.8)
                                                      < 0.71>
                                                        2.00

                                                        12.9
                                                      { 1«.9)
                                                      < 0.71>
                                                        2.0O
                     04.7
                    (  0.0)
                   < 0.0 >
                   **•»*•

                     44.0
                    (  0.0)
                   < 0.0 >
                   »•••*• ,

                     74.4
                    (  0.0)
                   < 0.0 >
                     40.3
                    (  0.0)
                   < 0.0 >
                   *••••»

                      2.0
                    (  0.0)
                   < 0.0 >
                   ******

                     83.5
                    I  0.0)
                   < 0.0 >
                   ••**«•

                    190.0
                    (  0.0)
                   < O.O >
                      2.0
                    (  0.0)
                    < 0.0  >
                    ******

                      2.0
                    I  0.0)
                    < 0.0 >
                    ******

                      2.0
                    (  0.0)
                    < 0.0 >
                    ******

                      2.0
                    I  0.0)
                    < 0.0  >
                    • •»*••

                      2.0
                    (  0.0)
                    < 0.0  >
                    ******

                      2.0
                    «  0.0)
                    < 0.0 >
                    *«••*•

                      2.0
                    (  0.0)
                    < 0.0 >
                    0.0
                  (  0.0)
                  < 0.0  >
                   0.0
                    0.0
                  (  0.0)
                  < 0.0 >
                   0.0
                    0.0
                    0.0)
                   0.0 >
                   0.0
                    0.0
                  (  0.0)
                  < 0.0  >
                   J.O

                    0.0
                  (  0.0)
                  < 0.0  )
                   0.0

                    0.0
                  (  0.01
                  < 0.0 >
                   0.0

                    0.0
                  (  0.01
                 < 0.0 1
                   3.0

-------
  Table  C.28, continued
06870  AT         0.0
       SO      (  0.0)
       S       < 0.0 >
       NO        0.0
06880



06881



06882



06883



0688*



06885



06886



06887



06888



06889



06890



it
SD
3
no
AT
SD
S
no
AT
SD
S
no
AT
SD
9
HO
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
(ID
AT
SD
S
BD
AT
SD
S
HD
AT
SD
S
NO
AT
SD
S
HD
0.0
( 0.0)
< 0.0 >
0.0
0.0
1 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 J
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
   3.0
C  0.0)
< 0.0 >
  3.00

   2.7
(  0.6)
<-0.71>
  3.00

   2.7
I  0.6)
<-0.71>
  3.00

   2.5
(  0.6)
< 0.0 >
  2.50

   2.7
(  0.6)
<-0.71>
  3.00

   2.5
(  0.6)
< 0.0 >
  2.50

   2.5
(  0.6)
< 0.0 >
  2.50

   2.7
(  0.6)
<-0.71>
  3.00

   2.7
(  0.6)
<-0.71>
  3.00

   2.7
(  0.6)
<-0.71>
  3.00

   2.7
(  0.6)
<-0.71>
  3.00

   2.7
(  0.6)
<-0.71>
  3.00
   2.0
(  0.0)
< 0.0 >
  2.00
                                                        15.8
                                                      (  21-0)
                                                      <  0.71>
                                                        2.00

                                                        25.7
                                                      (  23.8)
                                                      <  0.01>
                                                      25.50

                                                        22.9
  2.00

   6.5
I  S.3)
< o.«s>
  5.10

  29.7
( «3.5)
< 1.01>
 11.65

   2.0
(  0.0)
< 0.0 >
  2.00

 175.0
                                                       0.70>
                                                       31.90

                                                       11.4
                                                      ( 1«-3)
                                                      < 0.71>
                                                       2.00

                                                       95.2
                                                      (129.5)
                                                      < 0.60
                                                       »0.50

                                                       862. 1
                                                      (*•*••)
                                                      < 0.71>
                                                       6.40

                                                       «3.5
                                                      ( »2.8)
                                                      < O.«0>
                                                       33.70
   0.0
 (  0.0)
< 0.0 >
  0.0

  18.6
 «  0.0)
< 0.0 >
••*•••

  18.6
 (  0.0)
< 0.0 >
******

  25. 1
 { 32.7)
< 0.00>
 25. 10

   2.0
 (  0.0)
< 0.0 >
******
                   ( 17.9)
                   < 0.0 >
                    1«.65

                     78.5
                   (108.2)
                   < 0.0 >
                    78.50

                     31.2
                   (  0.0)
                   < 0.0 >
                   *•••*•

                     69.9
                   (  0.0)
                   < 0.0 >
                   ••*••*

                      2.0
                   (  0.0)
                   < 0.0 >
                   ******

                     71.1
                   (  0.0)
                   < 0.0 >
                   *«•*••

                     39.9
                   (  0.0)
                   < 0.0 >
                   *»»«»*
   0.0
(  0.0)
< 0.0 >
  0.0

   2.0
I  0.0)
< 0.0 >
******

   2.0
I  0.0)
< 0.0 >
•*«»•*
                                                                                                2.0
                                                                                                0.0)
                                                                                               0.0 >
                                                                                               2.00

                                                                                                2.0
                                                                                                0.0)
                                                                                               0.0 >
                                                                                             • »*•**

                                                                                                2.0
                                                                                             (  0.0)
                                                                                             < 0.0 >
                                                                                               2.00
                                                                                                5.8
                                                                                             I   5.3)
                                                                                             <  0.0 >
                                                                                               5.75
                                                                                                2.0
                                                                                                0.0)
                                                                                               0.0 >
                    • •••*•

                       2.0
                    (  0.0)
                    < 0.0 >
                    ••• »**

                       2.0
                    (  0.0)
                    < 0.0 >
                    •••»»*

                       2.0
                    I  0.0)
                    < 0.0 >
                       2.0
                    (   0.0)
                    <  0.0 >
                    »**•*•
                                                            0.0
                                                            0.0)
                                                           0.0 >
                                                           0.0

                                                            0.0
                                                            0.01
                                                           0.0 >
                                                           o.c
                                                           I 0.0
                                                         (   0.0)
                                                         <  0.0 >
                                                           0.0
                                                            0.0
                                                         (   0.0)
                                                         < O.J  >
                                                          0.0
                                                           2.0
                                                           0.0)
                                                          0.0 >
                    0.0
                 (   0.0)
                 <  0.0  >
                   0.0

                    0.0
                 (   0.0)
                 <  0.0  >
                   0.0

                    0.0
                 (   0.0)
                 <  0.0  >
                   0.0

                    0.0
                 I   0.0)
                 <  0.0  >
                   o.c
                   0.0
                 (  0.0)
                 < 0.0 >
                  0.0

                   0.0
                 {  0.0)
                 < O.J >
                  0.0

                   0.0
                 (  0.01
                 < 0.0 >
                  0.0

-------
     Table C.28, continued
CO
06891
06892
06893
06894
06896
It
SD
S
BD
IV
SD
S
HO
IV
SD
S
HO
IV
SD
S
RD
IV
SD
S
BD
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
J 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
2.7
( 0.6)
lioo
2.7
C 0.6)
1*00
2.7
< 0.6)
3*00
2.5
( 0.6)
< o.o •>
2.50
2.5
( 0.6)
< 0.0 )
2.50
7MO.O
< 0.71>
2.00
4.7
( 4.7)
< 0.7I>
2.00
78.2
(116.2)
< 0.
20.60
14. 1
< 0.04>
13.20
35.7
( 63.6)
4*95
79. 1
( 0.0)
< 0.0 >
•»•*••
2.0
( 0.0)
< 0.0 >
475.0
( 0.0)
< 0.0 >
*•••»«
2.0
( 0.0)
< 0.0 >
2.00
J33.5
(•68. 8)
< 0.0 >
333.50
2.0
( 0.0)
< 0.0 >
»*••»•
2.0
( 0.0)
< 0.0 >
••*«••
2.0
1 0.0)
< 0.0 >
••»•»*
2.0
I 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
0.0
( 0.0)
< 0.0 J
0.0
'o.o
( 0.01
< 0.3 1
0.3
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
3.0
0.0
I 0.0)
< 0.0 >
0.0
VEIL nHTL BBIZEVE HBPTIDICIM BEIIDZCMC HEXiDEClHOIC 1CID HETIITLHEPTIDECIHO «TE HETHTLHEXADECIIIOITB
«••••»•••••••••••••••«»•»••••••««••••••*«••••«•••••«••»•»••••*•»»•»••••••••••*••••»•••«•»••»••»•*•«•••«•»•»»«»••»«••••••••»«•«»»«
06848 IV 1.0 1.3 2.0 0.0 2.0 2.0
SD ( 0.0) ( 0.6) ( 0.0) ( 0.0) ( 0.0) ( 0.0)
S < 0.0 > < 0.71> < 0.0 > < 0.0 > < 0.0 > < 0.0 >
RD 1.00 1.00 •••**• o.o 2.00 2.00
06849
06852
068S4
0685S
06856
06857
IV
SD
S
BO
IV
SO
S
BO
IV
SD
S
HD
IV
SD
S
SD
IV
SD
S
no
IV
so
S
no
1.7
( 0.6)
2*00
1.7
( 0.6)
2! oo
1.5
1 0.7)
< 0.0 >
1.50
1.7
( 0.6)
2*00
1.7
( 0.6)
2*00
1.7
( 0.6)
2.0O
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.5
C 0.7)
< 0.0 >
1.50
1.3
( 0.6)
< 0.71>
1.00
1.3
C 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0.71>
1.0O
2.0
( 0.0)
< 0.0 >
0.0
( 0.0)
< 0.0 >
0.0
2.0
( 0.0)
< 0.0 >
«••«*»
2.0
( 0.0)
< o.o •>
2.0
( 0.0)
< 0.0 >
••••••
2.0
{ 0.0)
< o.o •>
*• • *•*
0.0
I 0.0)
< 0.0 >
0.0
0.0
{ 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
0.0
i 0.0)
< 0.0 >
0.0
0.0
( 0.0)
< 0.0 >
0.0
2.0
1 0.0)
< 0.0 >
2.00
2.0
< 0.0)
< 0.0 >
2.00
2.0
< 0.0)
< 0.0 >
2.00
2.0
1 0.0)
< 0.0 >
2.00
2.0
< 0.0)
< 0.0 >
2.00
2.0
1 0.0)
< o.o >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0)
< 0.0 >
2.00
2.0
( 0.0) .
< 0.0 >
2.00
2.0
( 0.0)
< 0. 0 >
2. no

-------
Table C.28,  continued
0«86«  If       1.7
       SD    (  0.6)
       S     <-0.71>
       HO      2.00
06870



06880



06881



06882



06883



0688*



06885



06886



06887



06888



06889



IT
3D
S
RD
»T
SD
S
RD
»T
SD
S
RD
IT
SD
S
HD
AT
SD
S
HD
IT
SD
S
RD
IT
SD
S
RD
»T
SD
S
RD
if
SD
S
RD
IT
SD
S
no
if
SD
S
HD

(
<


{
<-


(
<-


(
<


(
<-


«
<


(
<


(
<-


(
<-


(
<


(
<-

2.0
0.0)
0.0 >
2.00
1.7
0.6)
0.71>
2.00
1.7
0.6)
0.71>
2.00
1.5
0.6)
0.0 >
1.50
1.7
0.6)
0.71>
2.00
1.5
0.6)
0.0 >
1.50
1.5
0.6)
0.0 >
1.50
1.7
0.6)
0.71>
2.00
1.7
0.6)
0.71>
2.00
2.1
1.2)
0.20>
2.00
1.7
0.6)
0.71>
2.00
   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00
 1.5
 9.6)
0.0 >
1.50

 1.3
 0.6)
0.71>
1.00
   1.5
(  0.6)
< 0.0 >
  1.50

   1.5
(  0.6)
< 0.0 >
  1.50

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00
   2.0
(  0.0)
< 0.0 >
                                                         0.0
                                                      (   0.0)
                                                      <  0.0  >
                                                        0.0
                                                         2.0
                                                      (   0.0)
                                                      <  0.0 >
                                                      •*»••»
                                                         2.0
                                                      (   0.0)
                                                      < 0.0 >
                                                        2.0
                                                      (  0.0)
                                                      < 0.0 >
                                                       2.00
                    {
                                                         2.0
                                                         0.0)
                                                     < 0.0  >
                                                         2.0
                                                      (   0.0)
                                                      < 0.0 >
                                                       2.00
                                                        2.0
                                                        0.0)
                                                       0.0 •>
                                                       2.00
                                                        2.0
                                                      (  0.0)
                                                      < 0.0 >
                                                      •••**•
                                                        2.0
                                                      (  0.0)
                                                     < 0.0 >
                                                     ••••*•
                                                        2.0
                                                        0.0)
                                                       0.0 >
                                                       2.00

                                                        2.0
                                                        0.0)
                                                       0.0 >
   0.0
(  0.0)
< 0.0 >
  0.0

   0.0
I  0.0)
< 0.0 >
  0.0
                     0.0
                     0.0)
                    0.0 >
                    0.0

                     0.0
                     0.0)
                    0.0 >
                    0.0
                                         0.0
                                      (  0.0)
                                      < 0.0 )
                                        0.0

                                         0.0
                                      (  0.0)
                                      < 0.0 >
                                        0.0

                                         0.0
                                      {  0-0)
                                      < 0.0 >
                                        0.0

                                         0.0
                                      (  0.0)
                                      < 0.0 >
                                        0.0

                                         0.0
                                      (  0.0)
                                      < 0.0 >
                                        0.0

                                         0.0
                                      (  0.0)
                                      < 0.0 >
                                        0.0

                                         0.0
                                      (   0.0)
                                      <  0.0 >
                                        0.0
                                         0.0
                                      (   0.0)
                                      <  0.0 >
                                        0.0
                                                               2.0
                                                            (  0.0)
                                                            < 0.0 >
                                                              2.00

                                                               2.0
                                                            <  0.0)
                                                            < 0.0 >
                                                              2.00

                                                               2.0
                                                            I  0.0)
                                                            < 0.0  >
                                                              2.00

                                                               2.0
                                                            (  0.0)
                                                            < 0.0  >
                                                              2.00

                                                               2.0
                                                            (   0.0)
                                                            <  0.0  >
                                                              2.00
                                          2.0
                                       I  0.0)
                                       < 0.0 >
                                         2.00
                                          2.0
                                       I  0.0)
                                       < 0.0 >
                                         2.00
                                          2.0
                                       I  0.0)
                                       < 0.0 >
                                         2.00

                                          2.0
                                       (  0.0)
                                       < 0.0 >
                                         2.00

                                          2.3
                                       <  0.5)
                                       < 0.71>
                                         2.00
                                          2.0
                                          0.0)
                                         0.0 >
                                         2.00

                                          2.0
                                          0.0)
                                         0.0 >
                                         2.00
                                                                                  2.0
                                                                               (   0.0)
                                                                               <  3.0 >
                                                                                 2.00

                                                                                  2.0
                                                                               (   0.0)
                                                                               <  0.0 >
                                                                                 2.00
                                              2.0
                                              0.01
                                            0.0 >
                                            2.00
                                             2.0
                                           (  0.0)
                                          < 0.0 >
                                            2.00
                                                               2.0
                                                               0.0)
                                                              0.0 >
                                                              2.00
                                             2.0
                                          (  0.0)
                                          < 0.0 >
                                            2.00
                                             2.0
                                          (   0.0)
                                          <  0.0 >
                                            2.00
                                             2.0
                                          (   0.0)
                                          < 0.0 >
                                           2.00
                                             2.0
                                          1   0.0)
                                          < 0.0 >
                                           2.00
                                            2.0
                                          (  0.0)
                                          < J.O >
                                           2.00
                                            2.0
                                            0.0)
                                           0.0 >
                                           2.00

                                            2.0
                                            0.0)
                                           0.0 >
                                           2.00

-------
       Table  C.28,  continued
 06890  AT
       SD
       S
       no

 06891  AT
       SD
       S
       no

 06892  AT
       SD
       3
       80

06893  AT
       3D
       S
       no

06894  AT
       SD
       S
       HD

06896  AT
       SO
       S
       80
   1.7
 (  0.6)

  2! oo

   1.7
 (  0.6)

  2.00

   1.7
 «  0.6)

  2^00

   1.7
 (  0.6)

  2! oo

   1.5
 (  0.6)
< 0.0 >
  1.50

   1.5
 (  0.6)
< 0.0 >
  1.50
                                          1.3
                                       {   O.S)
                                       <  0.71>
                                         1.00

                                          1.3
                                       (   0.«)
                                       <  0.71>
                                         1.00

                                          1.3
                                       (   0.6)
                                       <  0.71>
                                         1.00

                                          1.3
                                       (   0.6)
                                       <  0.71>
                                         1.00
                                          1.5
                                          0.6)
                                         0.0 >
                                         1.50

                                          1.5
                                          0.6)
                                         0.0 >
                                         1.50
                                       2.0
                                    (  0.0)
                                    < 0.0 •>
                                       2.0
                                    (  0.0)
                                    < 0.0 >
                                    *••»••

                                       2.0
                                    (  0.0)
                                    < 0.0 >
                                       2.0
                                    (  0.0)
                                    < 0.0 >
                                       2.0
                                    (  0.0)
                                    < 0.0 >
                                      2.00
                                       2.0
                                       0.0)
                                      0.0 >
                                      2.00
                                     0.0
                                  (  0.0)
                                  < 0.0 >
                                    0.0

                                     0.0 .
                                  (  0.0)
                                  < 0.0 >
                                    0.0
                                     0.0
                                  (  0.0)
                                  < 0.0 )
                                    0.0
                                     0.0
                                     0.0)
                                    0.0 >
                                    0.0
                                     0.0
                                  (  0.0)
                                  < 0.0 >
                                    0.0

                                     0.0
                                  (  0.0)
                                  < 0.0 >
                                    0.0
                                                                            2.0
                                                                          I  0.0)
                                                                          < 0.0 >'
                                                                           2.00

                                                                            2.0
                                                                          I  0.0)
                                                                          < 0.0 >
                                                                           2.00

                                                                            2.0
                                                                          I  0.0)
                                                                          < 0.0 >
                                                                           2.00

                                                                            2.0
                                                                          I  0.0)
                                                                          < 0.0 >
                                                                           2.00
                                                        2.0
                                                     (  0.0)
                                                     < 0.0 >
                                                       2.00

                                                        1.9
                                                     I  0.1)

                                                       2.00
                                                                             2.0
                                                                          (   0.0)
                                                                          <  0.0 >
                                                                            2.00

                                                                             2.0
                                                                          (   0.0)
                                                                          <  0.0 >
                                                                            2.00
                                                                             2.0
                                                                          (  0.0)
                                                                          < 0.0 >
                                                                            2.00
                                                                             2.0
                                                                             0.0)
                                                                            0.0 >
                                                                            2.00
                                                                                                 2.0
                                                                                               (  0.0)
                                                                                               < 0.0 >
                                                                                                2.00
                                                                                                 2.0
                                                                                               I  0.0)
                                                                                               < 0.0 >
                                                                                                2.00
-P-
O   IB1L        1-HETHTLRAPBTHALERE   2-SrmLPBESOL   »-«THTLPHEROt      RAPHTHALERE         U-KCHILPHOIOL        OCT1DBCARE
     •••••••••••••ft*******************************************************************************************************************
                         1.3                  1.3               3.0               1.5                  0.0                  2.0
     068*8  AT
            SO
            S
            BD
     068*9  AT
            3D
            3
            HD

     06852  AT
            3D
            S
            BD

     06854  AT
            SD
            S
            no

     06855  AT
            SD
            S
            80
(  0.6)
< 0.71>
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00
 1.5
 0.7)
0.0 >
1.50

 1.3
 0.6)
0.71*
1.00
(  0.6)
< 0.71>
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
{  0.0)
< 0.0 >
  1.00
 1.5
 0.7)
0.0 >
1.50

 1.3
 0.6)
0.71>
1.00
                                   (  1.7)
                                   < 0.71>
                                     2.00

                                      2.0
                                   (  0.0)
                                   < 0.0 >
                                     2.00

                                      2.0
                                   (  0.0)
                                   < 0.0 )
                                     2.00
                                                         3.5
                                                         2-1)
                                                        0.0 >
                                                        3.50

                                                         3.0
                                                         1.7)
                                                        0.71>
                                                        2.00
                                <  0.5)
                                <-0.24>
                                  1.60

                                   1.0
                                (  0.0)
                                < 0.0 >
                                  1.00

                                   1.0
                                (  0.0)
                                < 0.0 >
                                  1.00
                                                             1.5
                                                          t  0.7)
                                                          < 0.0 >
                                                            1.50

                                                             1.6
                                                          {  0.5)

                                                            K70
                                                                                            (  0.0)
                                                                                            <  0. 0  >
                                                                                              0.0

                                                                                              0.0
                                                                                            (  0.0)
                                                                                            <  0.0  >
                                                                                              0.0
                                                                                               0.0
                                                                                            (   0.0)
                                                                                            <  0.0 >
                                                                                              0.0
                                                                             0.0
                                                                             0.0)
                                                                             0.0 >
                                                                             3.0
                                                                             0.0
                                                                           (  o.oi
                                                                           < 0. 0 >
                                                                            0.0
                                                                                                   (  0.0)
                                                                                                   < 0.0  >
                                                                                                    2.00

                                                                                                     2.0
                                                                                                   (  0.0)
                                                                                                   < 0.0  >
                                                                                                    2.00

                                                                                                     2.4
                                                                                                   (  0.7)
                                                                                                   < 0.71>
                                                                                                    2.00
                                                                             2.0
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                            2.00

                                                                             2.0
                                                                           (  0.0)
                                                                           < 0.0 >
                                                                            2.00

-------
06856   IT
        SD
        S
        HD

06857   IT
        SD
        S
        HD

0686*   IT
        3D
        S
        HD

06870   IT
        SD
        S
        HD

06880   IT
        SD
        S
        HD

06881   IT
        SD
        S
        RD

06882   IT
        SD
        5
        HD

06883   IT
        SD
        S
        no

0688*   IT
        SD
        S
        no

06885   IT
        SO
        S
        HD

06886   IT
        SD
        S
        HD

06887   IT
        SD
        S
        no
    1.7
(  0.6)
<-0.69>
  2.00

   1.3
<  0.6)
< 0.71>
  1.00
(  0.8)
< 0.71>
  1.00

   1.0
(  0.0)
< 0.0 >
  1.00

   1.3
I  0.6)
< 0.71>
  1.00

   1.3
<  0.6)
< 0.71>
  1.00

   1.8
i  0.5)
<-1.13>
  2.00

   1.5
(  0.5)
<-0.2«>
  1.60

   1.9
(  0.7)
<-0.37>
  2.00

   1.9
(  0.6)
<-0.65>
  2.00

   1.6
(  0.6)
<-0.68>
  1.90

   1.3
(  0.6)
< 0.71>
  1.00
   I. 1
   0.6)
  0.71>
  1.00
   1.3
(  0.6)
< 0.71>
  1.00
   1.0
(  0.0)
< 0.0 >
  1.00

   1.0
(  0.0)
< 0.0 )
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.7
(  0.5)
<-1.03>
  1.90

   1.3
(  0.6)
< 0.71>
  1.00

   1.8
{  0.5)
<-1.13>
  2.00

   1.8
(  0.5)
<-1. I5>
  2.00

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.6)
< 0.71>
  1.00
   3.0
(  1.7)
< 0.71>
  2.00

   3.0
(  1-7)
< 0.71>
  2.00

   2.0
I  0.0)
< 0.0 >
  2.00
                    2.0
                    0.0)
                   0.0 >
                   2.00

                    3.0
                    1-7)
                   0.71>
                   2.00
   3.0
{  1.7)
< 0.71>
  2.00

   3.5
(  1.7)
< 0.0 >
  3.50
                    2.0
                    0.0)
                   0.0 >
                   2.00
                   31.0
                  ( 56.0)
                                        3.50

                                         3.5
                                         1.7)
                                        0.0 >
                                        3.50

                                         3.0
                                         1.7)
                                        0.71>
                                        2.00
                    3.0
                 «  1.7)
                 < 0. 71>
                   2.00
   1.6
(  0.6)
<-0.68>
  1.90

   1.3
(  0.6)
< 0.71>
  1.00

   1.3
(  0.5)
< 0.71>
  1.00
                     1.0
                  <   0.0)
                  <  0.0 >
                    1.00

                     1.3
                  (   0.6)
                  <  0.71>
                    1.00
                                      1.3
                                   (   0.6)
                                   <  0.71>
                                     1.00
   1.5
(  0.6)
< 0.0 >
  1.50

   1.9
(  0.9)
<-0. 1«>
  2.00
                  (   3.8)
                  < 0.89>
                   2.80
                                      2.0
                                   <   0.9)
                                   <  0.19>
                                     2.00
                                      1.7
                                   (   0.6)
                                   <-0.69>
                                     2.00
                     1.3
                  (   0.6)
                 < 0.71>
                   1.00
                                         0.0
                                         0.0)
                                        0. 0  >
                                        0.0

                                         0.3
                                         0.0)
                                        0.0  >
                                        0.0
                        0.0
                     (  0.0)
                     < 0.0 >
                       0.0

                        0.0
                     (  0.0)
                     < 0. 0 >
                       0.0

                        3.3
                     (  0.0)
                     < 0.0 >
                       0.0

                        0.0
                     (  0.0)
                     < 0. 0 >
                       0.0
                                                          0.0
                                                          0.0)
                                                         0.0 >
                                                         0.0
                                         2.0
                                      I   0.0)
                                      <  0. 0 >
                                      * **• •*
                       0.0
                     (  0.01
                     < 0.0  >
                      0.0
                                         0.0
                                         0.0)
                                        0.0 >
                                        0.0

                                         0.0
                                         0.0)
                                        0.0 >
                                        0.0
                       0.3
                     (  0.0)
                     < 0.0 >
                      0.0
                                            2.0
                                            0.0)
                                           0.0  >
                                           2.00

                                            2.0
                                            0.0)
                                           0.0  >
                                           2.00
                                                                                                   2.0
                                                                                                 (  0.0)
                                                                                                 < 0.0 >
                                                                                                  2.00

                                                                                                   2.0
                                                                                                 (  0.0)
                                                                                                 < 0.0 >
                                                                                                  2.00

                                                                                                   2.0
                                                                                                 (  0.0)
                                                                                                 < 0.0 >
                                                                                                  2.00

                                                                                                   2.0
                                                                                                 (  0.0)
                                                                                                < O.I) >
                                                                                                  2.00
                                                                                                   3.6
                                                                                                I  3.2)
                                                                                                < 1. 1S>
                                                                                                  2.00

                                                                                                   1.0
                                                                                                I  3.5)
                                                                                                < 0.71>
                                                                                                  2.00
                                                                                                   2.0
                                                                                                (   0.0)
                                                                                                <  0.0  >
                                                                                                  2.00
                                           2.0
                                         I  0.0)
                                         < 0.0 >
                                          2.00
                                           3.2
                                           2.1)
                                          0.71>
                                          2.00
                                                                                                   2.0
                                                                                                (   0.0)
                                                                                                <  0.0  >
                                                                                                  2.00

-------
      Table  C.28,  continued
        ObHbtf
               »»
               SD
               s
               ID
    1.5
    0.5)
  0.2»>
  1.60
   I. i
   0.6)
  0.71>
  1.00
   J.U
(  1.7)
< 0.7t>
  2.00
   1. 7
   0.6)
 -0.71>
  2.00
   O.il
(  0.0)
< 0.0 >
  0.0
   1.0
I  0.0)
< 0.0 1
  2.00
        06689  If
               SD
               S
               HO
   1.7
   0.6)
 -0.71>
  2.00
   1.1
   0.6)
  0.71>
  1.00
   1.0
   1.7)
  0.71>
  2.00
   i.a
<  0.7)
<-O.S6>
  2.00
   0.0
   0.0)
  0.0 >
  0.0
   2.0
(  0.0)
< 0.0 >
  2.00
        06890  if
               3D
               5
               no
   2.1
(  1.M
< o.m
  2.00
   1.3
{  0.6)
< 0.71>
  1.00
   3.1
{  1-5)
< 0.38>
  1.00
   i.e
   0.9)
 -o.ie>
  2.00
   0.0
(  0.0)
< 0.0 >
  0.0
   J. 2
(  2.0)
< 0.71>
  2.00
        06891  If
               SD
               s
               no
   i.)
   0.6|
  0.71>
  1.00
   1.1
   0.6)
  0.71>
  1.00
   3.0
   1-7)
  0.71>
  2.00
   1.5
   0.5)
  0.2»>
  1.10
   0.0
(  0.0)
< 0.0 >
  0.0
   2.2
   0.«)
  o. ; i>
  2.00
        06892
               IT
               SD
               S
               no
   1.7
(  0.6)
<-0.6J>
  2.00
   1.6
<  0.6)
<-0.68>
  1.90
   1.0
   1.7)
  0.71>
  2.00
   1.3
   0.6)
  0.71>
  1.00
   0.0
(  0.0)
< 0. 0 >
  0.0
   2.0
I  0.0)
< 0.0  >
  2.00
NJ
        06893  IT
               SD
               S
               no
   1.6
(  0.5)
<-0.45>
  1.70
   1.]
(  0.6)
< 0.71>
  1.00
   3.0
   1.7)
  0.71>
  2.00
   1.6
(  0.6)
<-0.68>
  1.90
   0.3
   0.0)
  0. 0 >
  J. 0
   2.6
   1.0)
  0.71>
  2.00
        0689*  IT
               SD
               S
               SD
   1.5
(  0.6)
< 0.0 >
  1.50
   1.5
(  0.6)
< 0.0 >
  1.50
   3.5
   1.7)
  0.0 >
  3.50
   1.9
«  0.7)
<-0.37>
  2.00
   0.0
   0.0)
  0. 0 >
  0.0
   3.5
   2.9)
  1.15>
  2.00
        06896  »T
               3D
               S
               no
   1.6
   0.5)
  1.15>
  2.00
   1.9
(  0.6)
<-0.65>
  2.00
   3.5
(  1.7)
< 0.0 3
  3.50
   1.9
I  0.7)
<-0. 37>
  2.00
   0.0
(  0.0)
< 0.0  >
  0.0
   2.8
 (  1.6)
 <  1. I5>
   2.00
        • ELL      P HE HOI   PBOPAZIIE    1-TERPIHBOL  TETBACHLOROETHTLCIE  TOLOEIE     TBICHLOBOETHAIE   Tt ICIILOBOETUILEHE
        • ••»•*•*•*•••••»••*•••••*«»••»•••••••«»•••••«•«•»«••*••»••••••*•••«••«»*«••••»•••«•»•.«»•••«»•«».«»«*«.»«*»»»»,«»«,,,„,,„,,„„
        068*8
        068«9
        06852
        0685*
AT
SD
S
no
AT
SD
S
BD
IT
SD
S
II D
IT
3D
S
HD
(
<

1
<


(
<


(
<

«.o
5.2)
0.71>
1.00
1.0
0.0)
0.0 >
1.00
1.0
0.0)
0.0 >
1.00
5.5
«.•)
o.o >
5.50
7.3
10.00

(
<


(
<


10.0
0.0)
0.0 >
10.00
10.0
0.0)
o.o •>
10.00
6.0
«
1
0
1
.
0
•
•
3
.6)
71>
00
1.0
(
<


(
<



0
1
1

0
1
1
0
•
•
.
0
.
.
.
.0)
0 >
00
0
• 0)
0 5
00
5
( 1.7) ( 0.71
<

o.o >
6.OO
<

0
1

.
o >
50
                                   2.5
                                  (   1.«)
                                  < 0.52>
                                   1.90

                                   2.2
                                  (   2.1)
                                  < 0.71>
                                   1.00
                                                             0.71>
                                                             1.00
                                                           I  5-3)
                                                           < O.O  >
                              1.0
                            (  0.0)
                            < 0. 0 >
                              1.00

                              1.1
                            (  0.2)
                            < 0.71>
                              1.00

                              1.0
                            (  0.0)
                            < 0.0 >
                              1.00

                              1. 0
                            I   0.01
                            <  o.o >
                              i. oo
                              5.0
                            (  0.0)
                            <  0. 0 >
                            •*•»*•

                              5.0
                            (  0.0)
                            <  0.0 >
                            »•»*«•

                              5.0
                            <  0.0)
                            <  0.0 >
                            ••••*•

                            10. «
                            (  7.7|
                           < O.0f»
                            JO- US
                                2.7
                              (   2.5)
                             <  0.67>
                                1.50

                                1.5
                              (   2.U)
                             <-0.51>
                                5.20

                                2.1
                             (
                             < -
                                                                                       1-2)
                                                                                       .iio
                                                                                      2.60
                                                                                      3.3
                                                                                    I   3.2)
                                                                                    <  O.O  >
                                                                                      J.J5

-------
Table C.2S, continued
OC8S5



06856



06857



0686*



06870



06880



-P> 06881
^


06882



06883



06884



06885



06886



if 4.0
SD ( 5.2)
3 < 0.11>
(ID 1.00
if 4.0
SD | 5.2)
S < 0.71>
(ID 1.00
iT 4.0
SD { 5.2)
S < 0.71>
RD 1.00
iT 1.0
SD ( 0.0)
S < 0.0 >
SO 1.00
iT 1.0
SD ( 0.0)
s < o.o >
(ID 1.00
if 4.2
SD ( 5.1)
S < 0.70>
80 1.50
IT 4.0
SD | 5.2)
S < 0.71>
SD 1.00
iT 5.5
SO ( 5.1)
S <-0.00>
ao s.60
IT 4.0
SD ( 5.2)
S < 0.71>
(ID 1.00
iT 10.5
SD ( 13.7)
S < 0.66>
BD 5.55
iT 5.5
SD ( 5.2)
S < 0.0 >
(ID 5.50
iT 4.1
SD ( 5.1)
S < 0.70>
no 1.40
7. 1
( 4.6)
<-0.7 1>
10.00
7.3
( *-fi)
<-0.71>
10.00
7.1
( *• M
<-0.71>
10.00
10.0
( 0.0)
< 0.0 >
10.00
10.0
( 0.0)
< 0.0 >
10.00
7.3
( 4.6)
<-0.71>
10.00
7.3
( 4.6)
<-0.71>
10.00
6.0
( 4.6)
< 0.0 >
6.00
7.3
( 4.6)
<-0.7 1>
10.00
10.1
( 11.5)
< 0.83>
6.00
8.4
( «. -M
< 0.5fl>
6.00
7.3
( *.«)

10.00
1,3
( 0.6)
< 0. 71>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.4
( 0.5)
< 0.45>
1.30
1.3
( 0.6)
< 0.71>
1.00
1.5
( 0.6)
< 0.0 >
1.50
1.3
( 0.6)
< 0.71>
1.00
1.5
( 0.6)
< 0.0 >
1.50
1.5
( 0.6)
< 0.0 >
1.50
1.3
( 0.6)
< 0. 71>
1.00
3.7
( *.6)
< 0.71>
1.00
2.5
C 2.3)
< 0.69>
1.30
1.4
« 0.8)
< 0.71>
1.00
2.9
( 2.5)
< 0.59>
2.00
2. S
{ 2.5)
< 0.00>
2.80
3.2
I 2.8)
< 0.54>
2.30
5.3
( «-8)
< 0.32>
4.40
1.8
( 1*0)
< 0.28>
1.65
1.6
, t 0.8)
< 0.50>
1.40
1.3
I 0.6)
< 1. 15>
1.00
2.4
I 2.5)
< 1.09>
1.35
2.1
1 1-0)
<-0.42>
2.30
1.0
( 0.0)
< 0. 0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 )
1.00
1.0
( 0.0)
< 0.0 )
1.00
1.0
( 0.1)
< 0.71>
1.00
1.0
( 0. 1)
< 0.71>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
2.2
( 2.4)
< 1. 15>
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
5.0
( 0.0)
< d.O >
••••*•
5.0
( 0.0)
< 0.0 >
•*••*•
5.0
( 0.0)
< 0.0 >
••••••
5.0
( 0.0)
< 0.0 >
»•»••*
0.0
( 0.0)
< 0.0 >
0.0
5.0
( 0.0)
< 0.0 >
••»••»
5.0
( 0.0)
< 0.0 >
••**»*
5.0
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
•••*•*
5.0
< 0.0)
< 0.0 >
5.00
5.0
< 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 >
••••••
6.7
( 6.2)
< 0 . 1 5>
5.10
1.2
( 0.3)
< 0.71>
1.00
2.9
( 3.1)
< 0.70>
1.30
2.0
< 1.4)
< 0.60>
1.50
1.4
( 0.6)
< 0.0 >
1.45
3.8
( 3.2)
< 0.37>
3.10
7.2
( 7.6)
< 0.49>
5.00
2.0
( 1.7)
< 0.71>
1.00
1.0
( 0.0)
< 0.0 >
1.00
3.1
« 2.5)
< 0.03>
3.00
3.5
1 5.1)
< 1.15>
1.00
2.3
I 2.3)
< 0.71>
1.00

-------
Table C.28, continued
06897
06888
06889
06890
06891
06892
06893
0689*
06896
* AV
SD
S
MD
AT 4.0
SD ( 5.2)
S < 0.71>
no i.oo
AT 4.0
SD ( 5.2)
S < 0.71>
HD 1.00
AT 4.0
3D ( 5.2)
S < 0.71>
HD 1.00
AT 5.1
SD ( 4.5)
S < 0.29>
HD 4.40
AT 4.1
SD ( 5.1)
S < 0.71>
HD 1.20
AT 4.0
SD ( 5.2)
S < 0.71>
HD 1.00
IT 4.3
SD ( 5.0)
S < 0.68>
BD 1.90
IT 5.5
SD < 5.2)
S < 0.0 >
RO 5.50
IT 5.5
SO ( 5.2)
S < 0.0 >
no s.so
7.3
( 4.6) (
<-0.71> <
10.00
7.3
(4.6) (
<-0.71> <
10.00
7.3
( 4.6) (
<-0.71> <
10.00
7.1
( ».6) (
<-0.71> <
10.00
7.3
( 4.6) (
<-0.71> <
10.00
9.1
( 6.7) (
<-0.23> <
10.00
7.3
{ 4. 6) (
<-0.71> <
10.00
6.0
( 4.6) (
< 0.0 > <
6.00
6.0
( «.6) J
< 0.0 > <
6.00
2. 1
1.1)
0.11>
2.00
1.3
0.6)
0.71>
1.00
1.3
0.6)
0.71>
1.00
1.3
0.6)
0.71>
1.00
1.3
0.6)
0.71>
1.00
2.1
1.2)
0.20>
2.00
1.3
0.6)
0.71>
1.00
1.5
0.6)
0.0 >
1.50
1.5
0.6)
0.0 >
1.50
1.9
( 1.*)
< 0.71>
I.OO
1.4
( 0.7)
< 0.71>
1.00
4.0
( 5.3)
< 0.71>
1.00
2.9
1 2.1)
< 0.54>
2.10
2.8
( 1.9)
< 0.10>
2.70
1.8
• LI)
< 0.65>
1.30
1.0
C 0.0)
< 0.0 >
1.00
1.4
( 0.8)
< 1. 1S>
1.00
1.4
I 0.7)
< 1.14>
1.05
1.0
( 0.0)
< 0.0 1
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0. 0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0. 0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
5.0
( 0.0)
< o.o •>
******
5.0
( 0.0)
< 0. 0 >
»**•••
5.0
( 0.0)
< 0.0 >
• ••*••
5.0
( 0.0)
< 0.0 >
******
5.0
( 0.0)
< 0.0 >
*«•»••
5.0
( 0.0)
< 0.0 >
******
5.0
( 0.0)
< 0.0 )
*»**»•
s.o
( 0.0)
< 0.0 >
5.00
5.0
( 0.0)
< 0.0 )
5.00
1.7
( 1.2)
< 0.71>
1.00
).«
( 2.7)
< 0.29>
J.OO
7.0
( 5.5)
< O.J3>
6.00
3.3
( 3.6)
< 0.70>
1.40
1.0
1 0.0)
< 0.0 >
1.00
2.9
( 3.3)
< 0.71>
1.00
1.0
» 0.0)
< 0.0 >
1.00
2.4
( 2.8)
< 1.15>
1.05
1.9
( 1.8)
< 1.15>
1.00
- Arithmetic Average
- Standard Deviation
- Skewness






- Median Value

-------
 o
 o
 CM
                                       Precipitation Events
                                                                        KEY
                                                                 Q  Well 11032
                                                                 O  Well 40421
                                                                 A  Well 10521
                                                                 O  Well 20842
                                                                     Well 21323
<»
O
O
o
o
  1.00
June 1980
               6.00       11.00       16.00      21.00      26.00       31.00
                                          MONTH SflMPLED
Figure C.1.  Nitrite+Nitrate  Concentrations in  Well Water Over Time, Hancock Site
36.00
   m.oo
October
    1983

-------
O
O
                                                 D
                                                 O
                                                 A
                                                 O
                 KEY

               Well 10211
               Well 10821
               Well 10842
               Well 40231
                                                                    31.00
  cvl
   1.00        6.00       11.00
 June 1980
Figure  C.2.  Nitrite^Nitrate Concentrations In Well Water Over Time,  Hancock Site
 T	T
16.00      21.00      26.00
    MONTH SflMPLED
36.00
    m.oo
October
    1983

-------
 o
 o
                                          Precipitation
                             KEY
                        Q Well 20243
                        O Well 30312
                        A Well 10112
                        O Well 20112
   1.00
June 1980
  I           I
16.00      21.00      26.00
    MONTH SflMPLEO
              6.00       11.00       16.00      21.00      26.00      31.00

Figure C.3.  Nitrite+Nitrate Concentrations  in Well Water over Time, Hancock  Site
36.00      Ul.OO
       October 1903

-------
co
                                                                             KEY
                                                                        D Well  10931
                                                                        O Well  10721
                                                                        A Well  20711
                                                                        O Well  10232
                                                                                10541
                                             Precipitation Events
  "1.00        6.00        11.00      16.00      21.00      26.00      31.00
June 1900                                MONTH  SflMPLEO
Figure C.4.   Nitrite+Nitrate Concentrations in Well Water over  Time, Hancock Site
                                                                                        36.00
  41.00
October
  1983

-------
I
           1.00
        June 1900
                                                    Precipitation
                                                         Events
                                                    KEY
                                                Q Well 21234
                                                O Well 21141
                                                A Well 20721
                                                O Well 40331
  I
a. oo
                         11.00       16.00      21.00      26.00       31.00
                                         MONTH SflMPLEO
Figure C.5.   Nitrite+Nitrate Concentrations in Well Water  over Time,  Hancock  Site
36.00
   1
  ui. oo
October
  1983

-------
                                                            KEY

                                                       D Well 10731

                                                       O Well 10932

                                                       A Well 21132
  1.00
June 19UO
 T
6.00
                        11.00      16.00      21.00      26.00       31.00
                                       MONTH SflMPLEO

Figure  C.6.  Nitrite+Nitrate Concentrations in Well  Water over Time,  Hancock Site
  i
36.00
                                                                                              I
   141.00
October
   1983

-------
§
                                                        Precipitation
                                                           Event
                                                                          KEY

                                                                     D  Well 10232

                                                                     O  Well 10721

                                                                     A  rtell 1U931

                                                                     O  Well 11032

                                                                        Well 20711
1.00
June 1980
 Figure C.7.
6.00
                         11.00
                                     16.00      21.00       26.00
                                         MONTH SflMPLED
             TKN Concentration in Well  Water over Time, Hancock Farm
31.00
36.00       41.00
      October  1983

-------
   8.
   o
   (O
 I
O
z:
CE
O
_J
UJO
o
I—

  o
  J.
  o
                                          KEY

                                      D Well 10731

                                      O Well 10932

                                      A Well 21152
                                      T
                       T
                                                             T
               6.00
11.00
    1.00

 June 1900

Figure C.8.  TKN Concentration in Well Water over Time, Hancock Farm
16.00      21.00      26.00
    MONTH SflMPLEO
-T	1	1
 31.00      36.00      41.00
                 October 1903

-------
                                                                                       KEY	
                                                                                    D  Well  20112
                                                                                    O  Well  20243
                                                                                    A  Well  20721
                                                                                    O  Well  21141
                                                                                        Well  21234
VJ1
                                            1           '
       1.00        6.00        11.00      16.00       21.00      26.00
    June  1980                                   MONTH SflMPLED
    Figure C.9.  TKN Concentration in Well Water over  Time, Hancock Farm
  I
31.00
 T
36.00       41.00
       October  1903

-------
                                       KEY
                                     D Weil 10112
                                     O Well 10211
                                     A Well 10821
                                        Well 10842
   1.00
June 1980
Figure C.10.
6.00        11.00

TKN Concentration in  Well Water over Time, Hancock Farm
16.00      21.00      26.00
    MONTH SflMPLED
             1           I
31.00      36.00       m,00
                  October  190.3

-------
                                                                                  KEY

                                                                              D Well  30312

                                                                              O Well  40231
    1.00
June 1980
Figure C.11
                                   T	r
 6.00        U.OO       16.00      21.00       26.00
                            MONTH SflMPLED
TKN Concentration  in Well Water over Time, Hancock Farm
 r
31.00
 T
36.00
. oo

-------
                                                                            KEY

                                                                           D  Well 21323

                                                                           O Well 40331

                                                                           A Well 40421
   1.00
June 1980
Figure  C.12.
                        T           i           I
 6.00       11.00      16.00      21.00      26.00
                           MONTH  SflMPLEO
TKN Concentration in Well Water over Time, Hancock Farm
                        1
31.00      36.00      UJ.OO

                October 1983

-------
                                                      Pr«clp|tatl0n Ev*nt
                                                                             KEY
                                                                        Q Well 40421
                                                                        O Well 10232
                                                                        A Well 10931
                                                                        O Well 11032
  1.00
June 1900
6.00
11.00
16.00      21.00       26.00
    MONTH  SflMPLED
31.00      36.00      >11.00
                 October 19U3
Figure C.13.  Ammonia Concentration  in Well Water over Time, Hancock Farm

-------
 8
 I*
 W
    • °"
   >"
   C!J

   ZS
   '»•
   CL
Ul jfS
CO S
  CtO-
                                         KEY
                                     D  Well  1U721
                                     O Well  20711
                                     A Well  30312
                                     O  Well  40231
                                     O Well  40331
                                                         Precipitation Ev«nt
  1.00        6.00        11.00       16.00       21.00       26.00       31.00
June 1980                                  MONTH SflMPLED
 Figure  C.14.   Ammonia Concentration in Well Water over Time, Hancock Farm
                                                                                          36.00      UK 00
                                                                                                October

-------
  0
  (O
CD
 Id
0.
                             Precipitation
                               Event
     KEY
D Well 10112
O Well 10211
A Well 10821
O Well 10842
   Well 20112
 8%.
 °i.oo
June 1980
Figure C.15.
                 I
               6.00
  I           I           I           I
11.00      16.00      21.00      26.00
                MONTH  SflHPLED
      I           r           i
    31.00      36.00      Ul.OO
                       October 19H3
               Ammonia Concentration in Well Water over Time,  Hancock Farm

-------
                                                                        KEY
                                                                  D  Well 20243
                                                                  O  Well 20721
                                                                  A  Well 21141
                                                                  O  Well 21234
                                                                  O  Well 21323
                                                   Precipitation Event
 1.00        6.00
June 1980
11.00
16.00      21.00      26.00
    MONTH SflMPLEO
31.00      36.00      m.OO
                October  1983
  Figure C.16.  Ammonia Concentration in Well  Water over Time,  Hancock Farm

-------
  o
  CM.
  (D
CE
2Im
•c- 00
*= o.
CL  .-
   o
   o
   o
   o
     KEY



D Well  10731


O Well  10932


   Well  21152
    1.00

  June 1980

   Figure C.17.
  I           I           I           \           I

6.00        11.00       16.00      21.00      26.00

                           MONTH SflMPLED

 Ammonia Concentration  in Well Water over  Time, Hancock  Farm
    _1           I           I

    31.00       36.00       41.00

                    October 1983

-------
                                                                                       KEY
                                                                                   O Well 10232
                                                                                   O Well 1U721
                                                                                   A Well 10931
                                                                                    QWell 11032
                                                                                   <> Well 20711
  8
   i.oo
June 1900
 Figure C.1I
 T	   I	T
16.00      21.00      26.00
    MONTH SflMPLED
6.00        11.00      16.00      21.00      26.00       31.00
Total  Phosphorus Concentration in Well  Water over Time, Hancock Farm
 T	1
36.00      m.OO
      October 1903

-------
   O

    •
   O
ON
    Q_

     I
O a
H
Q_
to
O
    cc"

    O
    I—


      o

      O*
      8
                                                                              D Well  10731


                                                                              OWell  1U932


                                                                              A Well  21152
        1.00

     June 1900
               6.00
 l           I           I
11.00      16.00      21.00      26.00
               MONTH SflMPLEO
31.00
36.00      41.00

      October  1903
      Figure C.19.  Total Phosphorus  Concentration  in Well Water  over Time,  Hancock Farm

-------
                                                             Precipitation Event
                                                                                         KEY
                                                                                    D Well 10112
                                                                                    O Well 10211
                                                                                    A Well 10821
                                                                                    O Well 10842
                                                                                     Well 20112
ON
6.00
11.00
16.00      21.00       26.00
    MONTH  SRMPLED
                                                                              31.00
   1.00
June 1980
Figure C.20.   Total  Phosphorus Concentration in Well Water over  Time, Hancock Farm
36.00       41.00
      October 1983

-------
                                                                     KEY
                                                                D Well 20721
                                                                O Well 21141
                                                                A Well 21234
                                                                O Well 21323
                                                                   Well 20243
   1.00
 June 1980
Figure  C.21
 6.00        11.00      16.00      21.00      26.00       31.00
                            MONTH SflMPLEO
Total  Phosphorus Concentration in Well Water over Time,  Hancock Farm
36.00      41.00
    October  1983

-------
                                                                                 KEY

                                                                             D  Well 30312

                                                                             O  Well 40231

                                                                             A  Well 40331

                                                                             O  Well 40421
cr\
        1.00
       June 1980
        Figure  C.22.
  I
6.00
                                  i           i
         11.00       16.00      21.00      26.00      31.00
                         MONTH SflMPLED
Total  Phosphorus Concentration in Well Water over Time,  Hancock Farm
36.00      41.00
     October  1983

-------
                                                                      Q Well  10211
   1.00
June 1980
6.00
16.00      21.00      26.00
    MONTH SflMPLED
31.00
                        11.00



Figure  C.23.  Ortho Phosphorus Concentration in Well Water over  Time, Hancock Farm
36.00      41.00
     October 1983

-------
   =r
   o
   o
   ™,
    •
   o
-o
ON
03
LD
Z:

Q_
 I
J-
Q_
in
310
I—
O

  O.
    •
  a
  O
  O
                                                                                      KEY
                                                                                  D Well 10112
                                                                                   OWell 10232
                                                                                   AWell 10842
                                                                                   OWell 10931
                            I
                                                                              I
    1.00
 June 1980
   Figure C.24.
                   6.00
11.00
31.00
                       I            I           I
                      16.00      21.00      26.00
                          MONTH SflMPLED
Ortho  Phosphorus Conc.entratipn in Well Water  over Time, Hancock  Farm
  I           I
36.00      41.00
      October 1983

-------
        in
        CM.
ON
MD
     X




     Q_

      I

     UJ
Q_
(S)
O
o

 4
O
     O
        in
        o
        a
        o
                                                                                  KEY

                                                                               D Well 40421

                                                                               O Well 10731

                                                                               A Well 10413

                                                                               O Well 10932

                                                                               O Well 21152
         1.00
      June 1980
      Figure C.25.
               6.00
                        —1	1	1	1	1	
                        11.00       16.00       21.00      26.00      31.00
                                        MONTH SflMPLED
—I	1
 36.00      m.oo
      October 1983
               Ortho Phosphorus  Concentration in  Well Water over Time, Hancock Farm

-------
      o
      a*
       •
      o
   O CM

   *=*!•
   '*~* O

   Q_


    I
   Q_
   cn
   o
o    JJjJ
   o
     8.
                                                       KEY	


                                                    D Well 11032


                                                    O Well 20711


                                                    A Well 20842
      1.00

   June 1980
6.00
  i           I           I            [

16.00      21.00      26.00      31. (70

    MONTH SflMPLEO
                                                                                       T
                                                                                 1
36.oo      m.oo

      October 1983
      Figure C.26.  Ortho Phosphorus Concentration  in Well Water over  Time, Hancock harm

-------
   o
   «-*
   d
Q_
 I
LU
I—

-------
K)
o
=r,
 •
o
    Q_
    I
    UJ
    h— i
    $•
    Q_
    CO
   310
      §.
       1.00
   June 1900
                                                                                   KEY	
                                                                                D Well 2U243
                                                                                O Well 20721
                                                                                A Well 21141
                                                                                O Well 10821
                                                                                C3 Well 21234
            6.00
  i           i           i           i
11.00      ]S.OO      21.00       26.00
                MONTH  SRMPLED
                                                                                        i
31.00
                                                                                             l
36.00      m.OO
     October 1983
     .Figure C.28.   Ortho Phosphorus  Concentration in  Well Water over  Time, Hanocck Farm

-------
       KEY	
   D Well 30312
   O Well 40231
   A Well 40331
   O Well 10721
   Q Well 20112
6.00
11.00
16.00      21.00      26.00
    MONTH SflMPtEO
31.00
  1.00
June 1980
Figure  C.29.  Ortho Phosphorus Concentration in Well Water over Time,  Hancock Farm
36.00      41.00
     October 1983

-------
o
o
                                                                       KEY	
                                                                   O  Well 10931
                                                                   O  Well 41)421
                                                                   A  Well 11032
                                                                   O  Well 21323
                                                                       Well 10721
                                                                     31.00
  1.00        6.00       11.00       16.00       21.00      26.00
June i9ou                                 MONTH SRMPLED
 Figure  C.30.  Chemical Oxygen Concentration in Water Wells  over Time, Hancock Farm
36.00      41.00
     October  1983

-------
                                                           KEY	
                                                        D Well 10842
                                                        O Well 10821
                                                        A Well 30312
                                                        O Well 21141
                                                        A Well 40331
  1.00
 June  1980
Figure C.31
6.00        11.00       16.00      21.00      26.00      31.00
                           MONTH SAMPLED
Chemical Oxygen Concentration  in Well Water  over Time,  Hancock Farm
36.00      Ul.OO
     October  1983

-------
 o
 o
                                                                           KEY	
                                                                       Q Well 20243
                                                                       O Well 20112
                                                                       A Well 10211
                                                                       O Well 10112
                                                                         > Well 40231
             6.00        11.00      16.00      21.00       26.00      31.00
                                         MONTH  SRMPLEO
Figure  C.32.  Chemical Oxygen Concentration in Water Wells over Time,  Hancock Farm
  1.00
June 1900
36.00      Ul.OO
     October 1983

-------
 o
 o
                                                            KEY
                                                         D  Well 10232
                                                         O  Well 20711
                                                         &  Well 20721
                                                         O  Well 21234
   1.00
June 1980
6.00
11.00
16.00      21.00      26.00
    MONTH SPMPLEQ
31.00
36.00      HI.00
      October 1983
 Figure C.33.   Chemical Oxygen Concentration in Water Wells over  Time, Hancock Farm

-------
       s
CD
                                                                                 KEY	
                                                                              Q  Well 21)112
                                                                              O  Well 20243
                                                                              A  Well 20721
                                                                              O  Well 20842
        1.00
     June 1980
6. On
11.00
             r           r
16.00      21.00      26.00       31.00
    MONTH  SflMPLED
36.00      41.00
     October 1983
     Figure C.34.   Total Organic Concentration in Water Wells over Time, Hancock Farm

-------
                                                                          KEY	
                                                                       D Well 21141
                                                                       O Well 30312
                                                                       A Well 40231
                                                                       O Well 40331
   1.00
June 1980
6.00
IK 00
15.00      21.00      26.00
    MONTH SflMPLED
31.00
36.00      m.OO
     October  1983
  Figure C.35.   Total Organic Concentration in  Well Water over  Time, Hancock  Farm

-------
   o
   o
                                                                       KEY	
                                                                    D Well 11)232
                                                                    O Well 10542
                                                                    A Well 20711
                                                                    O Well 21323
    1.00
June 1980
           6.00        11.00      16.00      21.00      26.00       31.00
                                      MONTH SRMPLED
Figure  C.36.  Total Organic Concentration  in Well Water  over Time,  Hancock Farm
36.00      41.00
      October 1983

-------
CD
                                                                            KEY	
                                                                         D Well 10112
                                                                         O Well IU211
                                                                         A Well 10541
                                                                         O Well 10721
                                                                         £3 Well 10931
  1.00       6.00
June 1980
                             1J.OO       16.00      21.00      26.00      31.00
                                             MONTH SflMPLED
     Figure C.37.  Total Organic Concentration in Well Water over Time,  Hancock Farm
36.00
      October 1983

-------
co
N5
      1.00
  June 1980
                                                                                  KEY
                                                                              Q Well  10821

                                                                              O Well  10842

                                                                              A Well  21234
             \           I
16.00      21.00      20.00
    MONTH SRMPLEO
                       11.00       16.00       21.00      20.00      31.00


Figure  C.38.  Total Organic Concentration in Well Water over Time,  Hancock Farm
36.00      41.00
      October 1983

-------
                                                                                   KEY

                                                                               D Weil 4U311

                                                                               O Well 40421

                                                                               A Well 11032
•P-
co
       1.00
   June 19(30
     Figure C.39.
6.00
             i           i           i
11.00      16.00      21.00       26.00
                MONTH  SflMPLEO
31.00      36.00       lil. 00
                 October 1983
Total Organic Carbon Concentration in Well Water over Time,  Hancock Farm

-------
                                                                               KEY	
                                                                           D Well 10731
                                                                           O Well 10932
                                                                           A Well 21152
                                                                           O Well 10413
  1.00
June 1980
Figure C.40.
6.00        11.00       16.00      21.00      28.00      31.00
                           MONTH SflMPLED
Total Organic Concentration in Well Water Over Time,  Hancock Farm
36.00      lll.OO
     October 1983

-------
                                                             KEY
      8
CD
VJ1
      8-
      g
      §
      g
      o*
      CM
       1.00
     June 1980
     Figure C.41
                                                          D Well 10731
                                                                 10932

                                                                 21152
  1           II           I           I           I           I          1
6.00        11.00      16.00      21.00      26.00      31.00      36.00       41.00
                           MONTH SflMPLEO                             October 1903
Total  Dissolved Solids  Concentration in Well Water over Time,  Hancock Farm

-------
                                                                    KEY
       8
OD
ON
    8
      8
      8
  8i.w
June 1980
Figure  C.42.
                                                              QWell 10931
                                                              O Well 40421
                                                                Well 11032
                                                                Well 21323
                                                              O Wel1
                                             Prec.p.tat.on Event.
                    I
                   6.00
11.00      16.00       21.00      26.00      31.00      36.00
                MONTH SRMPLEO
                                                                                            October 1983
                 Total Dissolved Solids Concentration in Well Water over  Time, Hancock Farm

-------
                                              Precipitation Eventa
en
      8
                                                                                  KEY
      8
   (O
   o
    o
    CO
o
CO

28
                                                                           Q Well 40231


                                                                           O Well 10842


                                                                           A Well 10821


                                                                           O Well 30312
                    I

                   6.00
  I           I           1

16.00      21.00      26.00

    MONTH SPMPLED
  I

31.00
                                                                                     I
    1.00       6.00        11.00      16.00      21.00      26.00       31.00      36.00      HI.00

 June 1900                                 MONTH SPMPLED                             October  1903

 Figure C.43.   Total Dissolved Solids Concentration in Well Water  over Time, Hancock  Farm

-------
       O)
    *—, 00

    
-------
                                                                        KEY
CD
M3
   8
   Ss-
   o
   8s
   »-«  .
   QO.
   ^*
                                                                     D Well 20711
                                                                     QWell 20721
                                                                     A Well 21234
                                                                     OWell 10721
       1.00
    June 198U
    Figure C.45,
            11.00
16.00      21.00      26.00
    MONTH SflMPLEO
31.00
            1
36.00      41.00
      October I9U3
Total Dissolved  Solids Concentration in Well Water over Time, Hancock  Farm

-------
•o
VO
o
                                                                              KEY
                                                                          D  Well 10542
                                                                          O  Well 20711
                                                                          A  Well 20042
                                                                          0  Well 10932
       1.00
    June  1980
    Figure  C.46.
 6.00        11.00      16.00      21.00       26.00      31.00
                            MONTH  SflMPLED
Chromium Concentrations  in Well Water over Time, Hancock  Farm
36.00
     October 1983

-------
CJ —.
*•___!••  fe
   o
O

CJ
  CD
  O
                                                                                KEY	

                                                                           D  Well  10211
                                                                           O  Well  20112
                                                                           A  Well  20243
                                                                           +  Well  20721
                                                                           X  Well  21141
                                                              ,
   1.00
June 1980
Figure C.47.
6.00
11.00
                                      16.00      21.00      26.00
                                          MONTH SflMPLED
              Chromium Concentrations in Well Water over Time, Hancock Farm
31.00      36.00       41.00
                 October 1983

-------
       CNJ

       O
       O
       CM
       to
       •—f
        •
       O
MD
K)
    QQ
    O
    CE
    LU
      oo
      O
      O,
       •
      O
      O
      O
                                                           U  Well 10232

                                                           O  Well 10542

                                                           A Well 10721

                                                              Well 20711

                                                           X  Well 21323
         I
      J.OO
     June 1980
   Figure C.48.
6^00
11JOO
                         16.00       21.00      26J00
                             MONTH SflMPLED
Lead Concentration in Well Water over Time,  Hancock Farm
                                             31.00       36.00      41.00

                                                               October 1983

-------
   1.00
 June 1980
                                                                       D Well 20112
                                                                       O Well 20721
                                                                       A Well 21141
                                                                       0 Well 40331
11.00
16.00      21.00      26.00
    MONTH SflMPLED
31.00
             1
36.00      41.00
     October 1983
Figure  C.49.  Lead Concentration in Well Water over Time, Hancock Farm

-------
MD
       o
       CD
      O
      in
      o
      zr
      O
    *-^ (O

    £='
    a
    a:
    LU
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      »-<_
       •

      O
                                                        KEY



                                                     D  Well  10211


                                                     O  Well  20243


                                                     A  Well  21234


                                                     0  Well  30312


                                                     O  Well  40231
       1.00

    June 1980

    Figure C.50.
                         I           I            I

 6.00       11.00      16.00       21.00       26.00

                            MONTH SflMPLED

Lead Concentration in  Well Water over Time,  Hancock Farm
31.00
36.00
    Ul.OO

October  1983

-------
   oo
   o
CD
n
*•—*•


s <°
s°.
'-' O

s:
ZD
  sj
  o
  o
  o.
                       KEY	



                   D Well 10413


                   O Well 10731


                   A Well 10932


                   0 Well 21152
0

A

O
    1.00

 June 1980

 Figure C.51
             i           i  "      ~  i         "i           r

6.00        11.00       16.00      21.00      26.00      31.00

                           MONTH  SflMPLEO

Cadmium Concentration in Well Water over Time, Hancock Farm
                                  36.00      11.00


                                         October 1983

-------
ON
                                                                       KEY	


                                                                   D  Well 40331

                                                                   O  Well 40311

                                                                   A  Well 40421
       1.00
    June 1980
     Figure C.52.
6.00
11.00
                                   T           T
                       16.00      21.00      26.00
                           MONTH SflMPLEO
Cadmium Concentration in Well Water over Time,  Hancock Farm
31.00
 r
36.00
     m.oo
October  1983

-------
      o
      Cvl
   O
   «— I
    *
      u>
MD
   O CM
   U~-
   s-^ o
   Q oo
      o
      o
      o
                                                          KEY
                                                      d  Well  20112
                                                      O  Well  20721
                                                      A  Well  21141
                                                      0  Well  30312
                                                      Q  Well  40231
       1.00
   June 1980
6.00
  I           I           I            I
11.00      16.00       21.00      26.00
                MONTH  SflMPLED
  I           I            i
31.00      36.00       41.00
                 October 1983
   Figure C.53.   Cadmium Concentration in  Well Water over Time, Hancock Farm

-------
        J-
        f^
         •
        o
        o
        c\/
        {£>
        «—i
         •
        O
     CD
     O C\J
MD
CD
     51
     Q oo
     CL°.
       zr
       o
       o
       o
                                      KEY
                                 D Well 10112
                                 O Well 10211
                                 A Well 10821
                                 0 Well 10842
                                 G Well 20243
v
         l.OO        6.00        11.00       16.00      21.00       26.00
      June 1980                                  MONTH  SflMPLED
    Figure C.54.  Cadmium Concentration in Well  Water  over Time, Hancock Farm
                                         ~I	1	:	1
                                         31.00      36.00      41.00
                                                           October  1982

-------
    o
     •
    o
7
 O
 «—i
  K
    CM
     •
    O
 <_>*:-
 O to
 (X —.
    o
    o
                                                                   KEY
                                                               O  Well 10232
                                                               O  Well 10541
                                                               A  Well 10542
                                                               0  Well 10721
                                                               O  Well 10931
                             I
     1.00
  June 1900
  Figure  C.55,
6.00
11.00
                          I           I           I
                        16.00      21.00      26.00
                            MONTH SflMPLED
Cadmium  Concentration in  Well Water over  Time, Hancock  Farm
  I           I           I
31.00      36.00       m.OO
                 October 1983

-------
 g
  1.00
June 1980
                                                                   KEY
                                                                D  Well 6884
                                                                O  Well 6883
                                                                &  Well 6880
                                                                O  Well 6888
                                                                   Well 6890
            6.00        11.00      16.00      21.00       26.00      31.00
                                       MONTH SflMPLEO
Figure  C.56.  Nitrite+Nitrate Concentration in Well  Water over Time,  Gray Farm
36.00      Ul.OO
        October 1903

-------
     KEY
Q Well 6855
O Well 6857
A Well 6870
   Well 6892
    1.00       6.00       11.00       16.00      2J.OO       26.00      31.00
 June 1980                                 MONTH  SflMPLED
Figure C.57.   Nitrite+Nitrate Concentration in Well  Water over Time, Gray Farm
          36.00       HI.00
               October 1983

-------
O
 •
O'
  B-
 0.
 (O"
 8.
                                                                            KEY
                                                                        D Well 6052
                                                                        O Well 6S49
                                                                        A Well 6882
                                                                        O Well 6856
   1.00
June 1980
                                    I           I           I
                                   16.00      21.00      26.00
                                       MONTH SflMPLED
                                                                        r
              6.00       11.00      16.00      21.00       26.00      31.00

Figure C.58,  Nitrite+Nitrate Concentration in Well  Water over Time,  Gray Farm
  I           I
36.00      41.00
        October 1983

-------
 8
                                                          KEY	

                                                       O Well 6083

                                                       O Well 6064

                                                       A Well 6881

                                                       O Well 6886
   1.00
 June 1980
Figure C.59.
6.00
11.00
                        T	1	r
                       16.00      21.00      26.00       31.00
                           MONTH  SflMPLEO
Nitrite+Nitrate Concentration in Well  Water over Time, Gray Farm
36.00      41.00

     October  1983

-------
                                                KEY
                                            D Well 6892
                                            O Well 6084
                                               Well 6890
                                            O Well 6805
   1.00        6.00       11.00
June 1980
Figure C.60.  Ammonia Concentration in Well Water over Time, Gray  Farm
16.00      21.00      26.00
    MONTH SRMPLEO
31,00      36.00      41.00
                 October 1903

-------
                                                                KEY
  1.00        6.00       11.00
 June 1980

Figure  C.61.  Ammonia Concentration in Well Water over Time, Gray Farm
16.00      21.00      26.00
    MONTH SflMPLED
31.00
  1           I
36.00      41.00
     October  1983

-------
Ul
a
                                                                             KEY
                                                                          D Well 6855
                                                                          O Well 6857
                                                                          A Well 6882
                                                                          O Well 6886
       1.00
   June 19HO
   Figure  C.62
16.00      21.00      26.00
    M0NTH SflMPLED
             11.00
Ammonia Concentration  in Well Water  over Time,  Gray Farm
31.00
36.00
                 October 1903

-------
                                                                                        KEY
                                                                                    D Well 6884
                                                                                    O Well 6890
                                                                                    A Well 6891
                                                                                    0 Well 6892
   1.00
 June 1980
Figure C.63.
6.00
31.00
            11.00       16.00       21.00       26.00
                            MONTH SflMPLED
Ortho Phosphate Concentration in Well Water over Time, Gray Farm
36.00
                                                                         October 1983

-------
  1.00
 June 1980
Figure C.64.
6.00
11.00
31.00
                       16.00      21.00      26.00
                           MONTH SflMPLED
Ortho  Phosphate Concentration in Well Water over Time,  Gray Farm
36.00      41.00
     October 1983

-------
                                                                         KEY
                                                                     D  Well 6000
                                                                     O  Well 6802
                                                                     A  Well 6883
                                                                     0  Well 6885
                                                                     £3  Well 6806
    1.00
 June 1980
Figure  C.65.
6.00
11.00
                         I-J I  *jl ..«•*	  ^ .— •-! . .    -.•.. I ,.,,.-
                        16.00      21.00       26.00
                             MONTH  SflMPLEO
Ortho  Phosphate Concentration- in Well Water over Time,  Gray Farm
31.00
36.00      41.00
      October  1983

-------
                                                 D  Well 6894
                                                 O  Well 6896
                                                 A  Well 6889
                                                 0  Well 6893
                                                    Well 7000
   1.00
 June 1980
Figure C.66.
6.00
11.00
31.00
                       16.00      21.00       26.00
                            MONTH  SflMPLED
Ortho  Phosphate Concentration in Well  Water over Time, Gray Farm
36.00
                                                                          October  1983

-------
                                                                              KEY
                                                                          D Well 6854
                                                                          O Well 6855
                                                                          A Well 6857
                                                                          0 Well 6870
                                                                          t3 Well 6881
    1.00
 June 1980
Figure  C.67.
6.00
11.00
                          i	1	r
                         16.00      21.00      26.00
                             MONTH SflMPLED
Ortho  Phosphate Concentration in Water Wells over Time, Gray Farm
31.00
36.00      m.OO
     October 1983

-------
N)
                                                                          KEY
                                                                      D  Well 6888
                                                                      O  Well 6895A
                                                                      A  Well 6895B
                                                                      0  Well 6895C
                                                                      O  Well 6895D
        1.00        6.00        11.00       16.00      21.00       26.00       31.00
      June 1980                                 MONTH  SflMPLED
      Figure C.68.   Ortho Phosphate Concentration in Water Wells over Time,  Gray Farm
              1
36.00       HI. 00
      October  1983

-------
                                                                 KEY
                                                              D  Well  6848
                                                              O  Well  6849
                                                              A  Well  6852
                                                              0  Well  6856
                                                                 Well  6864
               6.00       11.00       16.00       21.00      26.00      31.00
                                          MONTH SflMPLED
Figure C.69.  Ortho Phosphate Concentration  in Well Water over Time, Gray  Farm
   1.00
June 1980
36.00      41.00
      October 1983

-------
TABLE D.1.  CALCULATED BALANCE OF PERCOLATION POTENTIAL


(1)Non Runoff
Precipitation
1982 (cm)
Jan
Feb
Mar
Apr
May
Jun
3ul
Aug
Sep
Oct
Nov
Dec
1983
3 an
Feb
Mar
Apr
May
3un
Oul
0.8
0.6
3.2
2.2
14.2
15.7
8.1
2.5
5.1
0.8
3.0
3.1

1.3
2.0
0.8
2.6
6.2
1.6
2.0

Irrigation
(cm)
	
1.6
3.1
2.9
2.0
3.2
6.9
3.6
	
	

	
1.8
4.4
10.7
1.5
0.4
6.6

Hydraulic
Loading
(cm)
'0.8
1.2
6.3
5.1
16.2
15.7
11.3
9.4
8.7
0.8
3.0
3.1

1.3
3.8
5.2
13.3
7.6
2.1
8.6

(3)
(2)Efc
f
(cm)
0.6
0.6
0.6
0.6
0.6
1.0
1.0
0.85
0.75
0.6
'0.6
0.6

0.6
0.6
0.6
0.75
1.0
0.85
0.6




Calculated (4) (Balance) cm
ET of H20 in
cm) 1 .88 m2 Profile
1
2
3
4
6
11
16
15
11
3
1
1

1
2
3
6
10
9
9
.95
.33
.45
.95
.37
.75
.38
.3
.25
.67
.95
.80

.95
.33
.45
.19
.62
.99
.83
19
19
21
22
31
35
30
24
22
19
21
22

21
23
25
32
29
21
20
.2
.1
.9
.0
.8
.8
.7
.8
.2
.3
.3
.6

.9
.4
.2
.3
.3
.4
.2



Calculated %
Moisture in
1 .88 m Profile
13.7
13.6
15.6
15.7
22.7
25.5
21.9
17.7
15.8
13.8
15.2
16.1

15.6
16.7
17.9
23.0
20.9
15.3
14.4


:r
O-
-s
a
o
CD
o
o
rt-
P"
PJ
D-
-TI
id
c
-5
fD
in













1 m
o
t — t
X
o










                                                                    (Continued)

-------
  Table  D.1,  continued
^Non Runoff
Precipitation
1982 (cm)
Aug 	
Sep 	
Oct 15.5
Nov 	
Dec 	
Hydraulic (2) ( ^Calculated
Irrigation Loading ^f ET
(cm) (cm) (cm) cm)
7.9 7.9 0.6
1.3 1.3 0.6
15.5 0.6
0.6
0.6
10.8
9.0
3.67
1.95
1.8
(Balance) cm Calculated %
of H20 in Moisture in
I. 88 m2 Profile 1.88 m Profile
17.3
9.6
21.4
19.4
17.6
*12.3
*6.8
15.3
13.8
12.6

     -"•Calculated Wilting Point = 14.3
These may drop below ETf of 0.6
(1)   Calculated from:  Engineering Technical Note,  U.S.D.A.
                       Subject:  Hydraulogy
                       No:  210-18-TX5
     Runoff from precipitation event is already subtracted

(2)   From telephone communication with Dr. Zartman (Dept. of Plant and Soil Science, Texas Tech University
             <75% of Maximum Available Water in Profile ETf = 0.85
             <50?o of Maximum Available Water in Profile ETf = 0.75
             <25?o of Maximum Available Water in Profile ETf = 0.60

(3)   ET0 x Kc = ET  (ET from Pan Evap x Crop factor = ET)

     ET x (2)ETf - Calculated ET

(4)   Calculated field capacity from "Guidelines to an Understanding of Your Soil Fertility Report".
          Field Capacity = 0.027 x Percent Sand + 0.187 x Percent Silt + 0.555 x Percent Clay
          Field Capacity - Wilting Point = Available Water
          Calculated Field Capacity = 26.5% = 37.2 cm H20/1.88 m Soil
          Calculated Wilting Point = 14.3% = 20.0 cm H20/1.88 m Soil

-------
Table D.1,  continued
Date
5/06
5/12
5/23
5/24
5/25
5/28
6/11
6/20
6/24
6/28
7/05
7/09
8/17
9/19
11/25
Precipitation
(cm) (in)
2.79
4.39
0.66
0.73
2.79
5.99
3.20
7.54
7.29
1.29
4.67
4.49
2.69
3.18
2.24
1.10
1.73
.0.26
0.29
1.10
2.36
1.26
2.97
2.87
0.51
1.84
1.77
1.06
1.25
0.88
FielcK1)
Moisture
II
II
I
I
I
II
I
I
II
II
I
' II
II
I
I
(1)
Curve
79
79
62
62
62
79
62
62
79
79
62
79
79
62
62
Runoff
(cm) (in)
0.25
0.94



1.96

0.91
2.79

0.10
1.04
0.25


0.10
0.37
— ^_
	
	
0.77
	
0.36
1.10
	
0.04
0.41
0.10
	
	
1982 YEAR TOTAL
8.26
                                                                     3.25
                                 516

-------
Table D.1   continued
Date
1/06
2/06
5/10
5/29
6/04
7/15
10/02
10/08
10/09
10/16
10/18
10/19
10/20
" 10/25-

( 1 )D . . . . .
Precipitation
(cm) (in)
1 .27
1 .98
3.61
2.89
1.65
2.01
0.71
0.68
2.54
3.56
3.30
13.79
1.27
1.39

0.50
0.78
1.42
1.14
0.65
0.79
0.28
0.27
1.00
1 .40
1.30
5.43
0.50
0.55

Field Runoff
Moisture Curve (cm) - (in)
I
I
II
I
I
I
I

I
I
II
III
III
I

57 	
57 	
75 0.33 0.13
57 	
57 	
57 — -
57 	
	 	
57
57
88 0.25 0.10
88 10.29 4.05
88 0.43 0.17
57 	
1983 YEAR TOTAL 11.30 4.45

(1)   Taken from Engineering Technical Note
            Subject:  Hydrology
            Nunber:   210-18-TX5
            Reference Estimating Runoff for Conservation Practices
               March 1983
               Soil Conservation Service U.S.D.A.
                                   517

-------
TABLE D.2.   IRRIGATION WATER APPLIED TO TEXAS TECH RESEARCH PLOTS
       AT HANCOCK SITE DURING SOIL MOISTURE TEST PERIOD
              (See Figure 29 for Plot Locations)

Amount in cm (in)
Date
09-08-82
09-13-82
09-14-82
09-15-82
09-20-82
09-21-82
09-27-82
09-28-82
10-04-82
10-06-82
10-11-82
10-12-82
10-18-82
10-20-82
10-25-82
10-27-82
03-11-83
03-14-83
03-23-83
04-25-83
04-26-83
04-28-83
05-09-83
05-18-83
05-25-83
05-26-83
06-07-83
06-14-83
06-15-83
06-21-83
Plot

2
1

3
1
1
2
1


3




5
4
2
6
2

6
2
4
3
5
1
5
6

.87
.60

.78
.72
.57
.44
.65


.20




.03
.62
.66
.32
.69

.30
.16
.37
.45
.77
.68
.26
.65

(1
(0

(1
(0
(0
(0
(0


(1




(1
(1
(1
(2
(1

(2
(0
(1
(1
(2
(0
(2
(2
1

.13)
.63)

.49)
.69)
.62)
.96)
.65)


.26)




.98)
.82)
.01)
.49)
.06)

.48)
.85)
.72)
.36)
.27)
.66)
.07)
.62)
Plot
1.35 (0


1.55 (0
3.94 (1
1.30 (0
1.73 (0
1.91 (0
1.50 (0

3.00 (1

3.84 (1
2.77 (1
4.11 (1
3.45 (1





4.60 (1








2
.53)


.61)
.55)
.51)
.68)
.75)
.59)

.18)

.51)
.09)
.62)
.36)





.81)








Plot 3
1.70 (0
1.68 (0
1.75 (0

4.25 (1
1.45 (0
0.99 (0
1.88 (0
4.37 (1
'2.06 (0
4.60 (1
2.46 (0







5.61 (2
1.02 (0








4.88 (1

.67)
.66)
.69)

.87)
.57)
.39)
-74)
.72)
.81)
.81)
.97)







.21)
.40)








.92)
                            5-}g                          (Continued!

-------
Table D.2,  continued
Date
06-22-83
06-28-83
07-06-83
07-07-83
07-08-83
07-13-83
07-14-83
07-26-83
' 07-27-83
08-01-83
08-03-83
08-16-83
08-17-83
08-18-83
08-25-83
08-29-83
09-13-83
09-14-83
09-21-83
09-26-83
09-27-83
09,-28-83
09-30-83

Plot
1.27
4.34
3.43
2.90
2.13

7.14
4.32


3.71



4.72

15.24

13.97
15.24
15.24


Amount in cm (in)
1 Plot 2
(0.50)
(1.71)
(1.35)
(1.14)
(0.84)

(2.81)
(1.70)

5.51 (2.17)
(1.46)

6.63 (2.61)
1.91 (0.75)
(1.86)

(6.00)

(5.50)
(6.00)
(6.00)



Plot 3





3.30 (1.30)
4.85 (1.91)

6.50 (2.56)

4.24 (1.67)
6.63 (2.61)



5.16 (2.03)

15.24 (6.00)



15.24 (6.00)
10.16 (4.00)
                                     519

-------
                               Appendix D.3
               Surface  Runoff and Percolation Calculations

                   1982 Runoff and Percolation Calculations
     262.8 gal/m3      Acre Feet x 0.1234 = hectare meters     2.47 acres/ha
   1376 ha      10.54 cm              -,
(Water Shed)  *   ~7^	=  1,136,600 m3  Total Runoff
14.6 ha       50.8                   ,
(Ponds) x (Evaporation)  = 75,117.8 mj Loss
Total Runoff -  Evap. Loss = Calculated Percolation
1,136,600 m3 -  74,168 m3 -  1,062,400 m3
106.2 hectare meters   = yQ8 hectgre mefcerg Qf Rise
     15% Porosity
708 hectare meters of Rise                   Rise
           1376 ha
                     1983 Run-off an Percolation Calculatons
     264.2 gal/m3    Acre Feet x 0.1234 = Hectare Meters    2.47 Acres/ha

   1376 ha      11.05 cm
x "•"; °"   = 1,520,050 m3
 (Water Shed)       ha        ',-^u,u^ ...   Totgl Runoff

 14.6 ha      50.8 cm     ...  ,,_  3
 i o  A ^  x r	r7"  = 74,168 m  ,
 (Ponds)    Evaporation             loss
 Total Run-off - Evap. Loss = Calculated Percolation
 1,520,050 m3 - 74,168 m3 = 1,445,882 m3
 144.6 hectare meters
      15% Porosity
            964 hectare meters of rise
          = 964 hectare meters of rise

                            = 0.70 meters of rise
                    1376 hectares
                                520

-------
                            Reproduced from      iF"^
                            best available copy.    |T * S
Figure  D.1.  Location of  State Observation Wells in Vicinity of Gray Site


                                      521

-------
                     ^^—^^i^   m _
                                     .,      •      :            .   jU   -3?-. --ferSS^-.
Figure D.2.  Location of State Observation Wells  in  Vicinity of Hancock Site



                                    522

-------
    8.6
CC
L4J
O
I-
H
QL
LU
Q
   18.4
         r + 2.!>
         --2.5
                                           GRAY
                                           WELL
                                         NUMBER
                                  -MEAN— 688U
                                            6883
                                            6882
                                            6881
                                            6880
         1980   1981     1982
                       DATE

 Figure D.3.  Depth to Water, Gray Site
                                    1983
                   523

-------
   14.9
        --2.
~ 22.4
CC
UJ
   12.8
o
h-
UJ
Q
   16.9
    7.1
  GRAY
  WELL
NUMBER
   6889
                                        A
^  6888
   6887
   6886
   6885
         1980   1981     1982     1983
                      DATE

 Figure D.4. Depth to Water, Gray Site
                     524

-------
          r + 2.1)
     13.9  :
           --2.5
~  11.9
DC
HI
H


^   9.0

O
      5.7
  UJ
  O
      5.1
                                           GRAY
                                           WELL
                                         NUMBER

                                         =• 6896
                                             6893
                                             6892
                                           6891
                                            6890
           1980   1981    1982     1983
                         DATE
Figure D.5. Depth to Water, Gray Site


                       525

-------
   7.8
~  8.0
CC
UJ
H-
    7.9
0,  7.
LU
Q
   10.9
        r + 2.i
        --2
                        4ig^^
 GRAY
 WELL
NUMBER
  7000
1980   1981     1982
             DATE
                                   1983
  Figure D.6.  Depth to Water,  Gray Site

                   526

-------
   23.2
~  23.9
CC
UJ


   26.0
   39.9
 UJ
 Q
   35.4
         --2.5
                    r
                                           HANCOCK
                                            WELL
                                           NUMBER
                                           10731
         1980   1981     1982
                       DATE
Figure D.7. Depth to Water, Hancock Site
                     527
                                            10721
                                            10521
                                           10211
                                           10112
                                    1983

-------
  30.0
-  18.4  :
oc
LU
H
  20.6   :
  27.5   :
UJ
Q
   21.8   i
        1980   1981    1982
                      DATE
Figure D.8.  Depth to Water, Hancock Site
                                       HANCOCK
                                         WELL
                                        NUMBER

                                          11032
                                          10932
                                           10931
                                           108U2
                                          10821
                                    1983
                     528

-------
   30.7
~ 29.2
QC
HI
   33.9
 tu
 O
   38.1
          -2
         1980   1981     1982
                       DATE
Figure D.9. Depth to Water, Hancock Site

                     529
                                         HANCOCK
                                           WELL
                                          NUMBER
      ;208i42
       20721
                                           :202U3
      •20112
1983

-------



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34. 2
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-------



i
QC
LJJ
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5









1















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MEAN





H;
i
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	 S~* 	 	 — . 	 	





        1980   1981    1982
                      DATE
Figure D.11.  Depth to Water, Hancock Site
                     531
                                        HANCOCK
                                         WELL
                                        NUMBER
                                          40231
1983

-------
             5.5
                -H2%
            27
            25.7
                  SONDJFMAMJJASO
                         TIME (MONTHS)
Figure D.12.  Water Content as Indicated by Neutron Probe #TTU 1

                           532

-------
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Figure D.13.
     SONDJFMAMJJASO

            TIME (MONTHS)

Water Content as Indicated by Neutron Probe #TTU 2


                533

-------
           23.7
  74

5.91
                 SONDJFMAMJJASO
                        TIME (MONTHS)
                                                       o
                                                       h-
                                                       cc
                                                       ai
                                                       
-------
Figure D.15.
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                                                        cc
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     SONDJFMAMJJASO

            TIME (MONTHS)
Water Content as Indicated by Neutron Probe #TTU 4
                             535

-------
        UJ
        CD
z
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z
o
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cc
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              5
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13.6
19.9
22.6
22.8
23.0
22.6
21.4
19.9
19.1
18.6
19.6
20
21
23.7
25.5
26.7
27.8
28.4
28
28
29
28.9
29.6
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31
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29
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             .8
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        <  29.2
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           27.5
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           26.6
           26.2
           25.9
           25.6
           25.0
           24.6
           23.7
           23.2
           23.8
           25.3
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                                     0.49
                                     0.66
                                     0.82
                                     0.98
                                        15
                                        31
                                        48
                                        64
                                        80
                                        97
                                        13
                                        30
                                        46
                                        62
                SONDJFMAMJJASO
                       TIME (MONTHS)
O
P

>
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UJ

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LL
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Figure D.16. Water Content as Indicated by Neutron Probe #TTU 5
                         536

-------
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  13.4
  20.5
  20.7
  19.1
  17.6
  18.4
  19.2
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                               TIME (MONTHS)
         Figure D.17. Water Content as Indicated by Neutron Probe LCCIWR # 8

                                 537

-------
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                  SONDJFMAMJJASO
                         TIME (MONTHS)

Figure D.18.  Water Content as  Indicated by Neutron Probe LCCIWR #9
                          538

-------
                                                Table E.1
                             Soil Physical Characteristics - Hancock Farm
M3
Particle
Depth Density
(q/cc)
Pivot 1
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm
Pivot 2
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm
Pivot 3
30 cm
61 cm
91 cm
122 cm

152 cm

183 cm
Pivot 4
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm
Pivot 5
30 cm
61 cm
91 cm
122 cm
I 52 cm
183 cm
(Code 00160)
(1 ft) 2
(2 ft) 2
(3 ft) 2
(4 ft) 2
(5 ft) 2
(6 ft) 2
(Code 02141)
(1 ft) 2
(2 ft) 2
(3 ft) 2
(4 ft) 2
(5 ft) 2
(6 ft) 2
(Code 04154)
(1 ft) 2
(2 ft) 2
(3 ft) 2
(4 ft) 2

(5 ft) 2

(6 ft)
(Code 02141)
(1 ft) 2
(2 ft) 2
(3 ft) 2
(4 ft) 2
(5 ft)
(6 ft)
(Code 05071)
(1 ft) 2
(2 ft) 2
(3 ft) 2
(4 ft) 2
(5 ft) 2
(6 ft) 2
Texture
B
.54
.49
.46
.60
.60
.56

.72
.57
.57
.57
.72
.59

.54
.45
.50
.50 (5'/6')

.54



.44
.42
.61
.48 (3'/6')
Clay Loam
Clay Loam
Clay
Clay
Clay
Clay

Sandy
Sandy
Sandy
Sandy
Sandy





Clay
Clay
Clay
Clay
Loam
Sandy Loam

Sandy
Clay
Clay
Clay

Clay



Clay
Clay
Clay
Clay

Clay Loam
I

Sandy Clay Loam
Clay
Clay
Clay
Clay
Clay

Sandy
Clay
Sandy
Sandy
Sandy
Sandy

Sandy
Loam
Loam




Clay Loam
Loam
Clay Loam
Clay Loam
Clay Loam
Clay Loam

Loam
Sandy Clay Loam
Loam






Loam



Clay
Clay

Clay



Loam


Loam



Clay Loam
Clay
Clay
Clay
Loam
Loam

Bulk
Density
(q/cc)

1.34
1.37
1.29
1.39
1,44
1.48

1.47
1.39
1 .38
1.40
1.49
1.44

1.37
1.35
1.33
1.39

1.43



1.35
1.32
1.34
1.41
Color
Description Code

Reddish Brown
Yellowish Red
Pink
Pink
Pink
Pink

Reddiish Brown
Yellowish Red
Yellowish Red
Yellowish Red
Reddish Yellow '
Light Reddish Brown

Dark Brown
Pinkish Gray
Brown
Pink

Light Red



Dark Brown
Brown

Light Brown

5YR4/4
5YR5/6
7.5YR7/4
7.5YR8/4
7.5YR7/4
7.5YR7/4

5YR4/4
5YR5/8
5YR5/8
5YR5/8
5YR6/8
5YR6/4

7.5YR4/2
7.5YR7/2
7.5YR5/2
7.5YR8/4

2.5YR6/8



7.5YR4/4
7.5YR5/4

7.5YR6/4
Porosity

47.4
44.9
47.7
46.4
44.5
42.3

46.0
46.0
46.2
45.7
45.3
44.4

45.7
44.7
44.6
44.4

43.9



44.6
45.2
48.6
43.1





O
l!l
o
Cu
CU
o
t-t-
CD
	 1. ^pa
N ~O
Qj ~O
(-+ rn
Or — j
+ — '
3 i— i
X
QJ m
r+

cu
3
Q-

~n
— t.
CO
c
-5
CD
(/>

Clay


.56
.58
.59
.65
.60
.65


Sandy
Clay
Clay
Clay.
Clay
Clay


Clay Loam
Loam
Loam



Clay

Sandy
Clay


Clay Loam
Loam
Clay Loam
Clay
Clay
Clay
Loam

Loam


1 .39
1.38
1.37
1.58
1 .40
1.42


Dark Brown
Strong Brown
Reddish Yellow
Pink
Pink
Pink


7.5YR4/4
7.5YR5/6
5YR6/6
7.5YR7/4
7.5YR7/4
7.5YR7/4


45.8
46.3
47.3
48.1
46.1
46.6









-------
Table E.1, continued
Particle
Depth Density
(g/cc)
Pivot 6 (Code 13171)
30 cm (1 ft) 2.64
61 cm (2 ft) 2.71
91 cm (3 ft) 2.71
122 cm (4 ft) 2.77
152 cm (5 ft) 2.76 (5'/6')
183 cm (6 ft)
Pivot 7 (Code 11164)
30 cm (1 ft) 2.51
61 cm (2 ft) 2.56
91 cm (3 ft) 2.48
122 cm (4 ft) 2.55 (4'/6')
152 cmm (5 ft)
183 cm (6 ft)
4> Pivot 8 (Code 08122)
30 cm (1 ft) 2.49
61 cm (2 ft) 2.41
91 cm (3 ft) 2.50
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Pivot 9 (Code 11083)
30 cm (1 ft) 2.59
61 cm (2 ft) 2.46
91 cm (3 ft) 2.53
122 cm (4 ft) 2.52 (4'/6')
152 cm (5 ft)
183 cm (6 ft)
Pivot 10 (Code 13171)
30 cm (1 ft) 2.52
61 cm (2 ft) 2.60
91 cm (3 ft) 2.58
122 cm (4 ft) 2.59
152 cm (5 ft) 2.71
183 cm (6 ft) 2.64
Texture
B
Clay Loam
Clay Loam
Clay/Clay Loam
Clay
Clay

Sandy Clay Loam
Clay Loam
Clay Loam
Clay


Clay Loam
Clay
Clay Loam


Clay
Clay Loam
Clay
Clay
Clay


Sandy Clay Loam
Clay Loam
Sandy Clay Loam
Clay
Clay
Clay

I
Sandy Clay Loam
Clay Loam
Clay
Clay
Clay

Sandy Clay Loam
Clay Loam
Clay Loam
Clay Loam
Clay
Clay
Sandy Clay Loam
Clay Loam
Clay Loam
Clay
Clay

Clay Loam
Clay Loam
Clay Loam
Clay Loam
Clay
Clay
Sandy Clay Loam
Sandy Clay Loam
Sandy Clay Loam
Clay Loam
Clay Loam
Clay
Bulk
Density
Jg/cc)
1.36
1.34
1 .32
1.36
1.26

1.44
1.42
1.38
1.42


1.47
1.38
1..44



1.45
1.36
1.35
1.46


1.45
1.38
1.39
1.45
1.44
1.46
Color
Description
Reddiah Brown
Yellowish Red
Pink
Pink
Pink

Reddish Brown-
Light Reddish Brown
Light Red
Pink


Brown
Dark Brown
Brown



Brown





Reddish Brown
Yellowish Red
Light Red
Pink
Pink
Pink
Code
5YR5/4
5 YR5/6
5YR7/4
5YR8/4
5YR8/4

5YR4/4
5YR6/4
2.5YR6/B
5YR7/4


7.5YR5/4
7.5YR4/4
7.5YR5/2



7.5YR5/2





5YR4/4
5YR5/6
2.5YR6/8
5.YR6/B
5YR7/4
5YR7/4
Porosity
(;;)
48.6
50.5
51.2
54.0.
54.2

42.6
44.7
44.2
44.1


41.1
42.7
42.5



44.0
44.6
46.7
42.1


42.5
47.0
46.3
46.3
47.0
44.5

-------
Table E.1, continued
Depth
Pivot
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm
Pivot
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm
Pivot
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm
Pivot
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm
Pivot
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm
11 (Code
(1
(2
(3
(4
(4
(6
ft)
ft)
ft)
ft)
ft)
ft)
12 (Code
(1
(2
(3
(4
C5
(6
ft)
ft)
ft)
ft)
ft)
ft)
13 (Code
(1
(2
(3
(4
(5
(6
ft)
ft)
ft)
ft)
ft)
ft)
14 (Code
(1
(2
(3
(4
(4
(6
ft)
ft)
ft)
ft)
ft)
ft)
15 (Code
(1
(2
(3
(4
(5
(6
ft)
ft)
ft)
ft)
ft)
ft)
Particle
Density
(g/cc)
13123
2.
2.
2.
2.
2.
2.
14073)
2.
2.
2.
2.
2.

15053)
2.
2.
2.
2.
2.

17161)
2.
2.
2.
2.
2.
18133)
2.
2.
2.
2.
2.
2.
49
43
55
49
44
52
58
52
55
63
57 (4'/6')

62
49
53
53
65 (5V61)

57
60
63
56
67 (5V61)
50
44
52
56
61
57
Texture
B
Clay Loam
Clay Loam
Clay
Clay
Clay
Clay
Sandy Clay Loam
Clay/Clay Loam
Clay Loam
Clay Loam
Clay

Clay Loam
Clay
Clay Loam
Clay Loam
Clay

Clay Loam
Clay Loam
Clay Loam
Clay

Clay Loam
Clay
Clay
Clay
Clay
Clay
I
Sandy Clay Loam
Clay
Clay
Clay
Clay
Clay
Loam
Loam



Sandy Clay Loam
Clay
Clay
Clay
Clay
Clay
Clay
Clay
Clay
Clay
Clay
Clay
Clay
Clay
Clay
Clay
Clay
Clay
Loam
Loam
Loam
Loam
Loam
Loam
Loam
Loam
Loam


Loam
Loam
Loam

Loam
Loam
Sandy Clay Loam
Clay
Clay
Clay
Clay
Loam
Loam
Loam
Loam
Bulk
Density
(g/cc)
1.42
1.33
1.33
1.47
1.44
1.51
1.41
1 .38
1.37
1.39
1 .40

1.38
1.36
1.36
1.33
1.40

1.43
1.41
1.46
1.43
1.42
1.56
1.40
1.54
1..39
1.39
1.45
Color
Description Code
Reddish Bfown
Reddish Brown
Pink
Pink
Pink
Light Reddish Brown
Dark Brown
Brown
Brown
Reddish Yellow
Pink

Dark Brown
Reddish Brown
Reddish Brown
Light Reddish Brown
Pink

Brown
Reddish Yellow
Reddish Brown
Pink

Dark Brown
Reddish Brown
Light Reddish Brown
Pink
Pink
Pink
5YR4/4
5YR5/4
5YR7/4
5YR7/4
5YR7/4
5YR6/4
7.5YR4/4
7.5YR5/4
7.5YR5/4
5YR6/6
7.5YR7/4

7.5YR4/4
5YR5/3
5YR5/3
5YR6/4
7.5YR8/4

7.5YR5/4
5YR6/6
5YR5/4
5YR7/4

7.5YR4/2
5YR5/4
5YR6/4
5YRS/4
5YR8/4
5YR8/3
Porosity
42.9
45.3
48.0
40.9
41.1
40.1
45.5
46.4
47.1
47.1
45.4

47.4
45.2
46.3
47.5
47.0

44.5
45.7
44.7
44.1
46.7
37.7
42.3
46.8
47.6
46.6
43.6

-------
Table E.1, continued
Depth
Pivot 16 (Code
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm
(1 ft)
(2 ft)
(3 ft)
(4 ft)
(5 ft)
(6 ft)
Pivot 17 (Code
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm
(1 ft)
(2 ft
(3 ft)
(4 ft)
(5 ft)
(6 ft)
Pivot 18 (Code
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm
Pivot 19
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm (
Pivot 20
30 cm
61 cm
91 cm
122 cm
152 cm
183 cm
(1 ft)
(2 ft)
(3 ft)
(4 ft)
(5 ft)
(6 ft)
(Code
(1 ft)
(2 ft)
(3 ft)
(4 ft)
(5 ft)
6 ft)
(Code
(1 ft)
(2 ft)
(3 ft)
(4 ft)
(5 ft)
(6 ft)
Particle
Density
(q/cc)
1B101

2.59
2
.50
2.59
2.65
2.65


Texture
B
Clay Loam
Clay
Clay
Clay
Clay

Clay
Clay
Clay
Clay
Clay
Clay
I
Loam

Loam
Loam
Loam
Loam
Bulk
Density
(q/cc)
1.35
1.35
1.35
1.30
1.40

Color
Description
Dark Brown
Brown
Light Brown
Pink
Pink

Code
7.5YR4/4
7.5YR5/4
7.5YR6/4
7.5YR7/4
7.5YR7/4

Porosity
(1)
47
46
47
50
47

.9
.1
.9
.8
.2

22171)
2.61
2.44
2.55
2.59
2.
2'.
22114)
2.
2.
2.
2.
2.
2.
21083)
2.
2.
2.
2.
2.

21042)
2.
2.
2.
2.
2.

67
60
51
54
50
42
63
49
61
56
67
62
67 (5V61)

65
60
65
71
72 (5','6')

Clay Loam
Clay
Clay
Clay
Clay
Clay
Sandy Clay Loam
Clay Loam
Clay Loam
Clay
Clay
Clay
Sandy Clay Loam
Clay Loam
Clay Loam
Clay Loam
Clay

Sandy Clay Loam
Sandy Clay Loam
Clay Loam
Sandy Clay Loam
Clay

Clay
Clay
Clay
Clay
Clay
Clay
Sandy
Clay
Clay
Clay
Clay
Clay
Sandy
Sandy
Sandy
Sandy


Sandy
Sandy
Sandy
Sandy
Clay
Clay
Loam
Loam
Loam
Loam
Loam

Clay Loam
Loam
Loam
Loam


Loam
Clay Loam
Clay Loam
Clay Loam (41


Clay Loam
Clay Loam
Clay Loam
Clay Loam


1.44
1.40
1.39
1.43
1.45
1.48
1.36
1.39
1.31
1.34
1.33
1.37
1.45
1.39
1.33
/6') 1.34
1.44

1.40
1.39
1.38
1.36
1.38

Brown
Reddish Brown
Yellowish Red
Light Reddish Brown
Pink
Light Reddish Brown
Dark Brown
Brown
Yellowish Red
Pink
Pink
Pink
Reddish Brown
Reddish Brown
Red
Red
Pink

Reddish Brown
Reddish Brown
Red
Red
Pink

7.5YR5/4
5YH5/4
5YR5/6
5YR6/4
5YR7/4
5YR6/4
7.5YR4/2
7.5YR5/4
5YR5/6
5YR7/3
5YR8/3
5YR7/4
5YR4/4
5YR5/4
2.5YR5/6
2.5YR5/8
5YH7/4

5YR4/3
5YR5/4
2.5YR5/6
2.5YR5/8
5YR7/4

44
42
45
44
45
43.
46
45
47
44
49
45
44
45
50
49
46

47
46
47
49
49

.8
.6
.6
.6
.8
0
.0
.5
.4
.5
.4
.0
.4
.8
.3
.0
.2

.0
.5
.9
.8
.2


-------
Table E.1, continued
Depth
Particle
Density
(q/cc)
Pivot 21 (Code 02003}
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
2.61

2.63
2.66


Texture
B
Clay Loam
Clay Loam
Clay
Clay


I
Sandy Clay Loan
Clay Loam
Clay Loam
Clay
Clay
Clay
Bulk
Density
(q/cc)
1.35
1.36
1.28
1.31


Color
Description
Dark Brown
Reddish Brown
Light Reddish Brown
Pink


Code
7.5YR4/4
5YR5/4
5YR6/4
5YR7/4


Porosity
( «}
48.2


50.6


Pivot 22 (Code 11022)
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
•£• Playa Lake/Pivot
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Playa Lake/Pivot
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
2.61
2.57
2.61
2.63


2 (Code 01141)
2.54
2.57
2.77



18 (Code 23143)
2.36
2.38
2.34
2.44


Sandy Clay Loam
Clay/Clay Loam
Clay Loam
Clay Loam
Clay (5'/6')
Clay
Clay
Clay
Clay



Clay
Clay
Clay
Clay


Loam
Clay Loam
Clay Loam
Clay
. Clay

Sandy Loam
Sandy Clay Loam
Sandy Clay Loam
Sandy Loam
Sandy Loam
Sandy Loam
Clay
Clay
Clay
Clay
Clay Loam
Clay
1.37
1.36
1.38
1.33


1.43
1.47
1.48



1.43
1.34
1.42
1.44


Dark Brown
Reddish Brown
Yellowish Red
Yellowish Red
Pink

Brown
Grayish Brown
Grayish Brown



Dark Gray
Dark Gray
Gray
Gray


7.5YR4/4
5YR5/4
5YR5/6
5YR5/8
5YR8/4

7.5YR5/2
10YR5/2
10YR5/2



10YR4/1
10YR4/I
10YR5/I
10YR6/1


47.6
47.3
47.1
49.3


43.2
42.7
46.4



39.5
43.5
39.3
40.9



-------
                                      Table E.2
                Nitrogen in Hancock Soils Receiving 42.2 cm Hydraulic Loading
     DEPTH          TKW           N02/N03             NH3              ORG  H
       CM         HG-N/G           BG-H/G            1G-N/G            MG-N/G
                1991    1983     1981    1983      1981    1983      1931     19B3
     ***********************************************************************
       30  AV*  0.65    0.55    .00854  .00337    .00161  .00192    .65303  .54891
           SD   0.17    0.15    .00467  .00277    .00114  .00130    .17252  .14960
           CV    26.    27.      55.     82.       71.     67.       26.      27.
Ul
-o
       60
       91
      121
      152
SD
CV

AV
3D
CV

AV
SD
CV

AV
SD
CV
     182   AV
           SD
           CV
0.59
0. 11
 18.

0.40
0.07
 18.

0.23
0. 10
0.20
0.05
 26.

0.19
0.06
 33.
0.48
0. 17
 35.

0.29
0. 12
 43.

0.20
0. 17
 86.

0.23
0. 17
 73.

0.20
0. 17
 8B.
 00895
,00816
  91.

 00946
 00874
  92.

 01 179
 01321
 112.

 00992
 00924
  93.

 00782
 00673
  86.
,00162
.00101
  62.

,00158
.00096
  61.

,00399
,00627
 157.

,00706
,00983
 139.

,00951
.01353
 142.
 00117
,00080
  69.

 001 12
,00098
  87.

,00098
,00104
 106.

,00107
,00084
  79.

,00107
,00084
  78.
,00190
.00123
  65.

.00121
.00067
  56.

.00131
.00082
  62.

.00100
.00060
  60.

.00333
.00804
 241.
,55860
,16197
  29.

.39613
,07188
  •18.

.22361
.09506
  42.

.19955
.05120
  26.

.18748
.06130
  33.
 47475
 16924
  36.

,28795
 12377
  43.

,20118
,17397
  86.

.22983
, 16796
  73.

. 19632
,17500
  89.
 * AV - Arithmetic Average; SD - Standard  Deviation; CV - Coefficient of Variation as Percent

-------
                                   Table E.3
            Nitrogen in Hancock Soils  Receiving 52.2  cm Hydraulic Loading
DEPTH           TKN          H02/N03             NH3              ORG  N
  CM          HG-N/G          MG-N/G            HG-N/G            flG-N/G
            1981    1983    1981     1983      1931    1^83      1981     1983
***********************************************************************
  30  AY*   0.67   0.51   .01322  .00327    .00230  .00145    .66991   .51231
      SD    0.20   0.18   .00804  .00185    .00279  .00080    .20233   .18273
      CV     30.     36.     61.     56.      121.     56.      30.      36.
  60
  91
 121
 152
 182
AV
SD
CV

AV
SD
CV

AV
SD
CV

AV
SD
CV

AV
SD
CV
0.53
0.09
 16.

0.40
0.08
 19.

0.26
0.09
 37.

0.21
0. 10
 46.

0.20
0. 10
 50.
0.44
0.12
 28.

0.30
0.13
 42.

0.25
0. 11
 45.

0.19
0.09
 46.

0.19
0.08
 43.
.00835
.00346
  41.

.00932
.00692
  74.

.01386
.11160
 805.

.01794
.01078
  60.

.01609
.01263
  79.
.00191
.00175
  92.

.00130
.00075
  58.

.00153
.00123
  80.

.00401
.00481
 120.

.00877
.00811
  92.
.00168
.00112
  66.

.00213
.00196
  92.

,00170
.00141
  83.

,00172
.00161
  94.

.00177
,00159
  90.
.00119
.00064
  53.

.00074
.00040
  55.

,00100
,00061
  61.

.00069
.00041
  59.

.00085
,00054
  63.
.52796
.08699
  16.

.39384
.07484
  19.

.25523
.09451
  37.

.20467
.09514
  46.

. 19947
,09979
  50.
.43756
.12215
  28.

.30301
. 12784
  42.

.24900
, 11175
  45.

. 18931
,08714
  46.

, 19414
08395
  43.
  AV - Arithmetic Average
  SD - Standard Deviation
  CV - Coefficient of Variation as Percent

-------
                                      Table E.4

                 Nitrogen in Hancock Soils Receiving 68.9 cm Hydraulic Loading
    DEPrH           TKN           N02/N01             NH3              OR3  N
      CP          MG-N/G           MG-N/G            MG-N/G            HG-N/G
                1981   1983    1981     1983      1981    1983      1981     1983
    ********************************************** *********** **************
      30  AV*   0.75   0.57   .01352   .00317   .00130  .00220    .74559   .57032
          SD    0.05   0.06   .00779   .00220   .00076  .00119    .05112   .06602
          CV      7.    11.     58.     69.       42.     67.        7.      12.
Ul
-P-
ON
      60
      91
     121
     152
     182
AV
SD
CV

AV
SD
CV

AV
SD
CV

AV
SD
CV

AV
SD
CV
0.59
0.09
 15.

0.37
0.0t»
 10.

0.22
0.08
 37.

0. 18
0.05
 28.

0. 16
0.04
 22.
0.49
0.09
 18.

0.34
0.08
 23.

0.21
0.06
 30.

0. 14
0.04
 28.

0.21
0.16
 75.
.01124
.00566
  50.

.01293
.00787
  61.

.01232
.00998
  81.

.01115
.00455
  41.

.01013
.00503
  50.
.00124
.00079
  64.

.00266
.00262.
  98.

,01073
.01907
 178.

.01964
.02447
 125.

.02001
.01520
  76.
,00143
,00091
  61.

,00096
 00089
  92.

,00042
 00066
 155.

,00048
 00061
 127.

,00047
 00061
 128.
,00082
.00064
  78.

.00191
.00272
 142.

,00067
.00034
  50.

.00033
.00033
 102.

.00028
.00020
  70.
,58857
.08682
  15.

.36899
.03717
  10.

.22433
.08369
  37.

.18183
.05007
  28.

.16365
.03674
  22.
 49417
,09096
  18.

,34057
,07728
  23.

 20682
,06216
  30.

,14215
.04050
  28.

,21225
. 15991
  75.
  * AV - Arithmetic Average
    SD - Standard Deviation
    CV - Coefficient of Variation as Percent

-------
                                      Table E.5
      Phosphorus and Organic Carbon in  Hancock Soils Receiving 42.2 cm Hydraulic Loading
 DEPTH       TOTAL  P         ORTHO P          ORG.  P       OPG.  C    ORG.  MATTER
   CM         KG-P/G          MG-P/G          MG-P/G       MG-C/G          %
           1981    1983     1981     1983     1981   1983   1981   1983    1981  1983
 ***************************************************************** * * ****
   30   AV*0.19    0.15    .00093  .0        0.08   0.04   5.80   6.06    0.34  1.04
        SD 0.06    0.04    .00072  .0        0.04   0.01   0.80   0.97    0.04  0.17
        CV  33.     25.      78.    .0  0.      56.    38.    13.    16.     13.   16.

   60
   91
  121
  152
  182
* AV  - Arithmetic  Average
  SD  - Standard Deviation
  CV  - Coefficient of Variation aa percent
AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
0.20
0.05
26.
0.21
0.06
27.
0.20
0.07
36.
0.20
0.06
30.
0.21
0.04
20.
0.16
0.04
28.
0.16
0.05
30.
0.16
0.06
38.
0.16
0.06
37.
0. 15
0.06
40.
.00085
.00093
110.
.00100
.00093
93.
.00080
.00096
121.
.00073
.00095
130.
.00079
.00097
123.
.0
.0
.0 0.
.0
.0
.0 0.
.0
.0
.0 0.
.0
.0
.0 0.
.0
.0
.0 0.
0.09
0.06
66.
0.09
0.06
67.
0.05
0.06
113.
0.04
0.05
102.
0.04
0.04
88.
0.05
0.03
53.
0.04
0.02
48.
0.02
0.02
85.
0.01
0.01
51.
0.01
0.01
49.
4. 34
0.75
17.
3. 10
1.07
34.
1.91
0.56
29.
1.71
0.64
37.
1.58
0.77
49.
4.64
0.69
15.
2.92
0.78
27.
2. 10
0.51
24.
1.67
0.50
30.
1.26
0.44
35.
0.25
0.04
17.
0. 18
0.06
34.
0. 10
0.05
56.
0. 10
0.04
40.
0.09
0.05
52.
0. 80
0. 12
15.
0.84
1.26
150.
0.36
0.09
24.
0.29
0.08
29.
0.22
0.08
35.

-------
                                              Table E.6

          Phosphorus and Organic Carbon in Hancock Soils Receiving 52.2 cm Hydraulic Loading
Ul
4>
CD
DEPTH
CH


TOTAL
P
MG-P/G

1981
1983
OKTHO
P
HG-P/G
1981
1983
OEG.
P
riG-p/G
1981
1983
OHG,
C
HG-C/G
1981
1983
OHG. MATTES
*
1981

1983
•ft*********************************************************************
30


60


91


121


152


182


AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
0.26
0. 16
64.
0.22
0. 15
6B.
0.23
0.16
68.
0.27
0. 16
60.
0.21
0.09
as.
0.22
0.09
39.
0.15
0.04
25.
0.18
0.05
29.
0.17
0.04
26.
0.19
0.08
43.
0.16
0.09
58.
0.19
0.09
47.
.00388 .
.00444 .
114.
.00304 .
.00402 .
132.
.00276 .
.00314 .
114.
.00261 .
.00249 .
95.
.00156 .
.00161 .
103.
.00152 .
.00163 .
107.
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0.10
0.07
72.
0.08
0.07
88.
0.07
0.05
78.
0.07
0.08
105.
0.04
0.05
104.
0.05
0.04
82.
0.03
0.02
68.
0.03
0.02
56.
0.02
0.01
65.
0.01
0.01
38.
0.01
0.00
31.
0.03
0.05
175.
6.24
2.09
34.
4.59
0.35
8.
2.85
0.99
35.
2.35
1.07
46.
1.85
1.00
54.
1.78
1. 10
61.
6.37
1.09
17.
4.72
0.68
14.
2.85
0.51
18.
1.86
0.56
30.
1.54
0.43
28.
1.27
0.29
23.
0.36
0. 12
34.
0.26
0.02
9.
0. 16
0.06
35.
0.13
0.06
47.
0.11
0.06
55.
0. 10
0.06
64.
1. 10
0. 19
17.
1.56
2.09
134.
0.49
0.09
18.
0.32
0. 10
30.
0.27
0.07
27.
0.23
0.05
21.
      AV -  Arithmetic  Average
      SD -  Standard  Deviation
      CV -  Coefficient of Variation as Percent

-------
                                            Table E.7

          Phosphorus and Organic Carbon in Hancock Soils Receiving 68.9 cm Hydraulic Loading
•o
vo
DEPTH
CH
******
T^ * T -n
30


60


91


121


152


182



TOTAL
P
NG-P/G

AV*
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
1981
A**** **
^ ^ -T ^ T ^ ^
0.18
0.03 •
16.
0.22
0.05
23.
0.23
0.07
28.
0.28
0.14
49.
0.27
0.13
47.
0.27
0.13
47.
1983
* * * * *- 4
V ^ * ^ f ^
0. 15
0.01
9.
0. 16
0.00
3.
0.18
0.02
12.
0.19
0.04
20.
0. 17
0.03
20.
0.20
0.04
22.
ORTHO
P
1G-P/G
1981
r*********
C^J^^^^^I^^CT^;
.00106
.00135
128.
.00076
.00041
54.
.00063
.00042
67.
.00062
.00036
57.
.00048
.00023
48.
.000^6
.00049
87.
1
•* *- •
^ ^ •
.0
.0
.0
.0
.0
.0
.0
.0
.0
.0
.0
.0
.0
.0
.0
.0
.0
.0
                                            1983
OB3. P
WG-P/G
1981 1983
******* ***••*••*• 1
^ ^ ^ ^ T
0.08
0.02
29.
0.12
0.05
45.
0.11
0.05
46.
0.09
0.04
42.
0.08
0.01
18.
0.08
0.04
47.
T- <** 1* -r- T- T» '
0.04
0.01
23.
0.05
0.01
20.
0.05
0. 03
60.
0.03
0.01
55.
0.02
0.01
55.
0.02
0.03
120.
ORG. C
H G- C/G
1981 1983
fc *-•*<* *<*• **•*•**• *•*• i
f T^ V T " ~
6.93
0.37
5.
4.62
0.41
9.
2.92
0.53
18.
1.96
0.65
33.
1.57
0.29
18.
1.26
0. 07
6.
T- T" T- 1» -T* •*• '
6.35
0.95
15.
5.65
0.77
14.
3.23
0.33
10.
2. 15
0.34
16.
1.38
0.22
16.
1. 15
0.38
33.
ORG. HATTER
%
1981 1983
fc * ** * **
r- * •T V f + V
0.40
0.02
5.
0.26
0.03
10.
0. 17
0.03
18.
0. 11
0.04
33.
0.09
0.02
19.
0.07
0.01
8.
1.09
0. 17
15.
0.97
0. 13
14.
0.56
0.05
10.
0.37
0.06
15.
0.24
0.04
17.
0.20
0.07
34.
    * AV - Arithmetic Average
      SD - Standard Deviation
      CV - Coefficient of Variation  as  Percent

-------
                                 Table  E.8

                          Minerals  in Hancock  Soils
                     Receiving  42.2 cm  Hydraulic  Loading
DEPTH
CM

****
30


60


91


121


152


182


CONDUCTIVITY
DS/M

1981
1983
TDS
PR
MG/G
1981
1983
1981
1933
CL
MG/G
1981
1983
SO4
MG/G
1981
1983
********************** ******************** ** * * ***** ****************
AV
3D
CV
AV
3D
CV
AV
3D
CV
AV
3D
CV
AV
SD
CV
AV
3D
CV
* 0.308
0.057
19.
0.443
0.089
20.
0.582
0.354
61.
0.678
0.378
56.
0.584
0.200
34.
0.584
0.188
32.
0.620
0. 128
21.
0.649
0.159
24.
0.643
0.152
24.
0.721
0.243
34.
0.650
0. 183
.28.
0.626
0.169
27.
0.24
0.06
25.
0.31
0.08
26.
0.40
0.27
66.
0.48
0.29
61.
0.40
0.15
37.
0.40
0.13
33.
0.56
0.10
18.
0.56
0.15
26.
0.52
0.20
39.
0.54
0.19
36.
0.43
0.18
42»
0.41
0.16
40.
7.94
0.16
2.
7.99
0.13
2.
8.04
0.19
2.
8.05
0.21
3.
8.07
0.19
2.
8.08
0.19
2.
7.81
0.21
3.
7.66
0.19
2.
7.72
0.17
2.
7.76
0.21
3.
7.80
0.19
2.
7.86
0.18
2.
.026
.046
177.
.020
.010
48.
.050
.066
132.
.074
.076
104.
.055
.042
76.
.049
.032
66.
. 042
.028
67.
.075
.034
45.
. 076
.040
53.
.080
.042
52.
. 061
.039
63.
.048
.041
84.
.023
.01 1
45.
. 198
.364
183.
.112
.222
198.
.237
.470
198.
.238
.448
189.
.243
.446
184.
.061
.027
45.
.081
.032
40.
.055
.022
40.
.080
.058
72.
.078
.038
49.
.080
.048
60.
AV - Arithmetic Average
SD - Standard Deviation
CV - Coefficient of variation in percent

-------
           Table E.9

    Minerals in Hancock Soils
Receiving 52.2 cm Hydraulic Loading
DEPTH
CM
* ** * *
^ * T T T1
30
60
91
121
152
182
coworrcTiviTY
DS/H
1981 1983
fc *******+*•********<
* ^ ^ * T
AV*
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
•. ff ^, -f. T* ^» ^ ^
0.301
0. 154
51.
0.367
0.220
60.
0.469
0.395
84.
0.733
0.586
80.
0.832
0.541
65.
0.842
0.492
58.
1 T- ft 4fb tf ^« .-^
0.642
0.219
34.
0.805
0.248
31.
0.693
0.157
23.
0.704
0.217
31.
0.765
0.381
50.
0.777
0.379
49.
                              TDS
                              MG/G
                           1981  1983
                         L***********
                           0.27  0.61
                           0.16  0.18
                            57.  29.

                           0.34  0.68
                           0. 17  0.20
                            50.  29.

                           0.34  0.58
                           0.25  0.07
                            72.  12.

                           0.49  0.60
                           0.36  0.19
                            73.  32.

                           0.56  0.61
                           0.33  0.19
                            59.  32.

                           0.56  0.62
                           0.30  0.26
                            53.  42.
* AV - Arithmetic Average
  SD - Standard Deviation
  CV - Coefficient of Variation in percent
                     PR           CL            S04
                                 !fG/G           MG/G
                  1981  1983   1981  1983     1981  1983
                  *********************************
                  7.76  7.86   .016  .053     .038  .098
                  0.27  0.22   .012  .029     .029  .052
                    3.    3.    73.   54.     78.   53.
                  7.90 7.45
                  0.35 0.32
                    4.   4.

                  7.94 7.51
                  0.29 0.41
                    4.   5.
                  7.91 7.65
                  0.36 0.33
                    5.   4.

                  8.10 7.74
                  0.18 0.30
                    2.   4.
.020  .098
.028  .045
141.   46.

.044  .087
.068  .027
155.   31.
                  8.07 7.63   .067
                  0.12 0.26   .135
                    1.   3.   201.
.087
.073
 84.

.075
.071
 95.
.076
.026
 34.

.058
.034
 58.

.055
.031
 57.
.075  .127
.062  .050
 83.   39.

.040  .085
.022  .047
 55.   55.

.116  .094
.277  .074
238.   78.

.141. 148
.134  .150
 95.  101.

. 170  . 145
. 144  . 150
 84.  104.

-------
                                 Table £.10

                          Minerals in Hancock Soils
                     Receiving 68.9 cm Hydraulic Loading
DEPTH       CONDUCTIVITY       TDS         PH          CL            SOU
  CM            DS/P!           HG/G                   MG/G           MG/G
            1981     1983    1981  1983   1981  1983  1981  1983     1981  1983
**************** ********** ****************** ***************************
  30  AV*  0.320    0.685    0.24  0.55   7.96  7.72  .010  .037     .027  .092
      3D   0.061    0.196    0.04  0.14   0.08  0.25  .0    .052     .005  .048
      CV     19.      29.      17.  25.     1.    3.    0.  140.      13.   53.

  60  AV   0.370    0.884    0.30  0.64   8.09  7.37  .010  .104     .051  .146
      SD   0.080    0.120    0.10  0.15   0.16  0.28  .0    .059     .019  .051
      CV     22.      14.      32.  23.     2.    '4.    0.   56.      37.   35.

  91  AV   0.427    1.075    0.32  0.64   8.21  7.43  .017  .162     .026  .130
      SD   0.107    0.190    0.11  0.17   0.16  0.17  .005  .010     .021  .050
      CV     25.      18.      33.  27.     2.    2.   29.    6.      83.   38.

 121  AV   0.582    1.040    0.41  0.65   8.31  7.49  .037  .154     .052  .146
      SD   0.233    0.167    0.16  0.19   0.32  0.12  .027  .026     .036  .037
      CV     40.      16.      38.  30.     4.    2.   73.   17.      69.   25.

 152
AV
SD
CV
0.622
0.217
35.
1.
0.

044
239
23.
0.43
0.16
36.
0.60
0.30
50.
8.17
0.07
1.
7.59
0.12
2.
.045
.037
82.
. 107
.035
32.
.096
.067
69.
. 165
.120
73.
 182  AV  0.575    0.910    0.39  0.55   8.18 7.69  .042   .078    .038 .162
      SD  0.164    0.220    0.09  0.21   0.12 0.08  .033   .028    .055 .124
      CV     28.      24.     22.   39.     1.   1.   78.    36.      62.  77.

* AV - Arithmetic Average
  SD - Standard Deviation
  CV - Coefficient of Variation in  percent

-------
                                                   Table  E.11

                         Metals in  Hancock Soils Receiving 42.2 cm  Hydraulic  Loading
BBT1L5, TOTAL (HG/KG)
DEPTH       AL            AS         BA        B          CA          CD       CO       CB
  CH    1981    1983   1981  1983  1981 1983  1981 1983   1981   1983   1981 1983  1981 1983   1981 1983
    CD        TL
1981  1983  1931 1983
****** *********
30 A7*25317.
SD 8132.
C7 32.
60 A7 30891.
3D 7393.
C7 24.
91 A7 27575.
3D 8799.
C7 32.
121 A7 19191.
SD 10163.
C7 53.
152 A7 18630.
SD 7019.
C7 38.
182 A7 19280.
SD 7026.
C7 36.
DEPTH F
CM 1981
+^^*^* •$$££$ t4
30 A715742.
SD 2456.
C7 16.
60 A719309.
SD 3933.
CT 20.
91 A716358.
SD 3365.
C7 21.
121 1710518.
SD 5044.
C7 48.
152 A710330.
SD 3212.
C7 31.
182 A710770.
SD 3036.
C7 28.
k********
17032.
4450.
26.
18042.
3966.
22.
15863.
3855.
24.
11410.
3467.
30.
13564.
5303.
39.
12870.
3017.
23.
E
1983
$tt444£44i
10993.
2933.
27.
10989.
5276.
48.
11860.
5654.
48.
9593.
3795.
40.
8513.
2686.
32.
9533.
3020.
32.
9. 33
4.22
45.
8.71
3.17
36.
7.27
2.44
34.
3. 30
4.73
143.
3.39
3.54
104.
3.06
3.41
112.
I
1981
4.83
1.54
32.
4.61
1.83
40.
5.57
9.05
162.
1.26
1.95
154.
1.35
0.59
44.
1.30
0.64
49.
15.78 906.
12.43 1612.
79. 178.
15.48 *****
13.04 *****
84. 332.
8.67 504.
8.02 258.
93. 51.
0.0 1178.
0.0 1293.
0. 110.
0.0 1285.
0.0 1221.
0. 95.
0.0 1388.
0.0 1154.
0. 83.
>B
1983 1981
6.73 3125.
1.99 1196.
30. 38.
6.78 3900.
2.08 1179.
31. 30.
5.54 3983.
2.09 1056.
38. 26.
0.0 5191.
0.0 1965.
0. 38.
0.0 5510.
0.0 1865.
0. 34.
0.0 5620.
0.0 1897.
0. 34.
85.
34.
40.
114.
48.
42.
101.
73.
72.
0.
0.
0.
0.
0.
0.
0.
0.
0.
8G
1983
2623.
405.
15.
3212.
593.
18.
3605.
806.
22.
3699.
755.
20.
4185.
795.
19.
4685.
917.
20.
150.
112.
75.
****
****
332.
386.
812.
210.
502.
977.
195.
216.
327.
151.
****
****
246.
nv
1981
229.
51.
22.
232.
59.
25.
206.
86.
42.
105.
58.
55.
102.
27.
26.
108.
26.
25.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.

1983
201.
121.
60.
170.
38.
22.
152.
73.
48.
0.
0.
0.
0.
0.
0.
0.
0.
0.
9433.
19305.
205.
17055.
25134.
147.
35800.
32948.
92.
73343.
43522.
59.
67028.
29006.
43.
68858.
28323.
41.

1981
25.5
15.7
61.
21.3
10.9
51.
20.9
17.2
83.
51.5
93.1
181.
44.3
87.5
197.
42.2
88.3
209.
1701. 0. 14 0. 10
1228. 0.05 0.07
72. 38. 64.
12339. 0.14 0.09
11930. 0.05 0.06
97. 37. 66.
58234. 0.14 0.31
49152. 0.05 0.32
84. 39. 104.
153041. 0.13 0.05
100151. 0.06 0.0
65. 41. 0.
173559. 0.14 0.0
81981. 0.05 0.0
47. 38. 0.
157479. 0.12 0.0
61471. 0.04 0.0
39. 36. 0.
HI K
1983 1981 1983
13.2 4633. 3116.
6.7 599. 592.
51. 13. 19.
15.2 5264. 3168.
8.8 991. 596.
58. 19. 19.
12.1 4833. 2937.
5-4 955. 889.
44. 20. 30.
0.0 3809. 2193.
0.0 1291. 679.
0. 34. 31.
0.0 3760. 2253.
0.0 723. 500.
0. 19. 22.
0.0 3900. 2567.
0.0 645. 913.
0. 17. 36.
:***********'
3.89 6.91
1.74 1.47
45. 21.
4.85 8.08
2.07 2.77
43. 34.
4.46 6.54
2.13 1.27
48. 19.
3.14 0.0
1.71 0.0
55. 0.
3.26 0.0
1. 17 0.0
36. 0.
3.39 0.0
1.30 0.0
38. 0.
SB
1981 1983
0.3 0.5
0.1 0.0
20. 0.
0.3 0.5
0.0 0.0
0. 0.
0.5 0.5
0.0 0.0
0. 0.
1.0 0.0
0.4 0.0
44. 0.
0.9 0.0
0.2 0.0
22. 0.
0.9 0.0
0.2 0.0
22. 0.
25.48 18.03 9.78
16.97 20.47 2.87
67. 114. 29.
26.82 16.43 12.72
15.19 12.28 3,30
60. 75. 26.
22.20 13.88 11.97
13.72 12.98 4.73
62. 94. 40.
17.15 3.0 7.66
12.65 0.0 3.68
74. 0. 48.
15.46 0.0 7.25
9.27 0.0 2.37
56. 0. 33.
17.85 0.0 7.25
7.55 0.0 2.76
42. 0. 38.
1C HA
1981 1983 1981 1983
0.0 0.09 202. 388.
0.0 0.14 91. 139.
0. 149. 45. 36.
0.0 0.05 307. 223-
0.0 0.01 104. 115.
0. 12. 34. 52.
0.0 0.07 329. 220.
0.0 0.05 104. 101.
0. 65. 32. 46.
0.0 3.0 305. 244.
0.0 0.0 130. 125.
0. 0. 43. 51.
0.0 0.0 287. 250.
0.0 0.0 92. 113.
0. 0. 32. 45.
0.0 0.0 301. 229.
0.0 0.0 102. 85.
0. 0. 34. 37.
6.61 1.0 1.6
3.89 3.5 2.7
59. 51. 168.
7.54 1.7 1.2
4.97 1.2 1.7
66. 68. 136.
7.86 3.1 2.5
3.55 3.4 4.8
45. 107. 195.
3.0 0.6 0.0
0.0 3.9 0.0
0. 595. 0.
0.0 0.6 0.0
0.0 0.1 0.0
0. 11. 0.
0.0 0.6 0.0
0.0 0.1 0.0
0. 11. 0.
ZB
1981 1983
112.8 36.0
252.5 8.3
224. 23.
60.6 39.7
43.4 8-4
72. 21.
52.3 60-3
24.9 95-5
48. 158.
39.3 25. 1
37.2 4.2
95. 17.
39.7 25.8
24.2 4.9
61. 19.
41.3 27.0
23.1 4.6
55. 17.
 *AV - Arithmetic Average; SD -  Standard Deviation; CV -  Coefficient of  Variation in  percent

-------
                                                  Table E.12

                        Metals  in Hancock Soils Receiving 52.2 cm Hydraulic Loading
  HETALS, TOTAL  (1G/KG)
  DEPTH       AL           AS
   CH    1981    1983    1981 1983
   BA       B          CA          CD        CO        ZK          CO       TL
1981 1983  1981 1983   1981   1983  1981  1983  1981 1983  1981 1983  1981  1933  1981  1933
30 AV*22913. 18325.
SD 9344. 3961.
CV 41. 22.
60 AV 32563. 23711.
SD 8099. 4925.
CV 25. 21.
91 AV 30250. 20174.
SD 7624. 6350.
CV 25. 31.
121 AV 22286. 14625.
SD 11182. 3233.
CV 50. 22.
152 AV 15517. 13689.
SD 6093. 3935.
CV 39. 29.
182 AV 14867. 13863.
SD 6376. 4219.
CV 43. 30.
DEPTH FE
CH 1981 1983
30 AV12741. 14182.
SD 7754. 3718.
CV 61. 26.
60 AV20200. 15998.
SD 3176. 1369.
CV 17. 27.
91 AV18738. 17353.
SD 1620. 9312.
CV 25. 54.
121 AV13429. 10100.
SD 6202. 3108.
CV 96. 31.
152 AV10367. 9984.
SD 4906. 3844.
CV 47. 39.
182 AV11117. 9810.
SD 4542. 4170.
CV 41. 43.
12. 96
6.93
53.
11. 54
6.55
57.
11.25
7.38
66.
5.84
7.36
126.
1.60
4.69
102.
3.75
3.99
106.
F
1981
5.99
3.60
60.
5.49
3.31
60.
5.34
3.67
69.
3.06
2.93
96.
2.93
2.70
92.
2.52
2.56
102.
7.32
7.91
108.
9.67
9.87
102.
12.14
10. 16
84.
0.0
0.0
0.
0.0
0.0
0.
0.0
0.0
0.
'B
1983
5.70
3.25
57.
5.63
1.93
34.
5.64
3.25
?8.
0.0
0.0
0.
0.0
0.0
0.
0.0
0.0
0.
477.
321.
67.
635.
343.
54.
515.
266.
52.
770.
450.
58.
739.
498.
67.
761.
522.
69.

1981
2863.
877.
31.
3825.
892.
23.
3975.
932.
23.
4457.
1763.
40.
4417.
1729.
39.
4750.
1583.
33.
83.
23.
34.
100.
26.
26.
118.
60.
51.
0.
0.
0.
0.
0.
0.
0.
0.
0.
KG
1983
2875,
970.
34.
3484.
987.
28.
3631.
1075.
30.
3771,
1424.
38.
3989.
1437.
36.
44fiO.
1490.
33.
249.
304.
122.
189.
267.
142.
225.
274.
122.
178.
257.
144.
247.
416.
169.
153.
194.
127.
BS
1981
270.
112.
42.
?55.
99.
39.
250.
104.
41.
180.
128.
71.
131.
118.
90.
148.
109.
74.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.

1983
199.
60.
30.
227.
108.
47.
276.
145.
53.
0.
0.
0.
0.
0.
0.
0.
0.
0.
3225.
296 1.
92.
11013.
14852.
135.
17088.
22707.
133.
49886.
47107.
94.
53365.
40870.
77.
58833.
38990.
66.

1981
13.6
7.0
52.
15.9
6.6
41.
13.8
7.3
52.
10.8
7.1
66.
10.8
5.4
50.
10.1
5.7
57.
2497
3860
155.
12625
24946
198.
37016
55550
150.
79511
79806
100.
96555
81180
84.
80423
68579
85.
NI
1983
10.2
2.5
24.
11.2
2.6
23.
10.9
3.8
35.
0.0
0.0
0.
0.0
0.0
0.
0.0
0.0
0.
. 0.14 0.20
. 0.08 0.11
55. 58.
. 0. 13 0.21
. 0.05 0.13
38. 59.
. 0. 14 0.22
. 0.05 0.26
39. 116.
. 0.18 0.0
. 0.08 0.0
41. 0.
. 0. 16 0.0
. 0.05 0.0
34. 0.
. 0. 18 0.0
. 0.04 0.0
25. 0.
K
1981 1983
4775. 3509.
1058. 1442.
22. 41.
5675. 4004.
1417. 1271.
25. 32.
5413. 3645.
1508. 1159.
28. 32.
4214. 2946.
1980. 1126.
47. 38.
3633. 2799.
1839. 1159.
52. 41.
3967. 3023.
1715. 117B.
43. 39.
5.14 6.07
2.94 1.25
57. 21.
4.64 7.61
1.92 1.81
42. 24.
4.81 8.31
2.08 2.60
43. 31.
3.60 0.0
1.96 0.0
55. 0.
2.77 0.0
1.07 0.0
39. 0.
3.02 0.0
1.12 0.0
37. 0.
SE
1981 1983
0.0 0.5
0.0 0.0
0. 0.
0.0 0.5
0.0 0.0
0. 0.
0.0 0.5
0.0 0.0
0. 0.
0.0 0.0
o.o o'.o
0. 0.
0.0 0.0
0.0 0.0
0. 0.
0.0 0.0
0.0 0.0
0. 0.
27.00 13.49 10.85 5.06 1.8 0.5
9.33 3.15 3.24 1.13 0.5 0.0
35. 23. 30. 22. 25. 0.
33.25 12.41 11.31 6.55 1.1 2.0
9.05 2.06 2.58 1.48 0.3 2.6
27. 17. 23. 23. 29. 126.
23.25 11.16 10.87 5.09 2.4 0.5
7.98 4.03 3.49 2.38 1.2 0.0
28. 36. 32. 39. 50. 0.
25.00 0.0 9.69 D.O 0.8 0.0
12.94 0.0 3.89 0.0 3.2 0.0
52. 0. 40. 0. 403. 0.
22.18 0.0 10.57 0.0 0.8 0.0
10.82 0.0 7.09 0.0 0.3 0.0
49. 0. 67. 0. 33. 0.
24.90 0.0 7.12 3.0 0.6 0.0
13.23 0.0 3.31 ).0 0.3 0.0
41. 0. 47. 0. 33. 0.
AG HA ZH
1981 1983 1981 1983 1981 1983
0.0 0.05 203. 414. 50.1 39.9
0.0 0.00 79. 61. 21.8 8.7
0. 9. 39. 15. 44. 22.
0.0 0.10 274. 342. 57.0 46.8
0.0 0.09 124. 143. 11.5 6.5
3. 91. 45. 42. 20. 14.
0.0 0.08 296. 281. 56.6 40.7
0.0 0.07 138. 132. 14.6 8.0
0. 93. 47. 47. 26. 20.
0.0 0.0 273. 241. 43.9 32.1
0.0 0.0 143. 94. 21.8 10.2
0. 0. 52. 39. 50. 32.
0.0 0.0 261. 211. 31.0 32.9
0.0 0.0 120. 101. 11.4 10.5
0. 0. 46. 48. 37. 32.
0.0 0-0 285. 223. 38.2 32.1
0.0 0.0 130. 85. 15.1 11.0
0. 0. 45. 38. 40. 34.
* AV -  Arithmetic  Average; SD  - Standard  Deviation;  CV - Coefficient of Variation in percent

-------
1ETAI.S, TOTAL (KG/FG)
                                                  Table E.13

                       Metals in Hancock Soils  Receiving 68.9  cm Hydraulic Loading
DEPTH       AL            V         PA        n
  CH    1981   1983   1981  19R3  1931  1983  19B1 1^83
                                                      Ci         CD        CO        CB          CD        TL
                                                  1981  1983   1981 1983  1981 1983  1931 1983  1981  1993  1931  1983
30 AV*29250.
SD 1317.
CV 15.
60 AV 35100.
SD 1169.
CV 3.
91 JV 26650.
SD 3381.
CV 13.
121 AV 16500.
SD 6189.
CV 39.
152 AV 16850.
SD 5712.
CV 31.
182 AV 18225.
SD 5616.
CV 31.
DEPTH F
CH 1981
30 AV16300.
SD 2061.
CV 13.
60 AV19675.
SD 913.
CV 5.
91 AV11575.
SD 7011.
CV 61.
121 AV 8327.
SD 6092.
CV 73.
152 AV 9500.
SD 3135.
CV 13.
182 AV 9925.
SD 279U.
CV 28.
21108.
1581.
22.
27375.
2185.
8.
21510.
3511.
16.
16253.
2993.
18.
11635.
1730.
12.
15310.
2609.
17.
E
1983
10193.
1285.
12.
13115.
3885.
30.
12815.
1160.
35.
9350.
1370.
11.
5913.
P125.
101.
9fl15.
173fi.
18.
11.92
5.75
18.
11. 37
8.06
71.
5.37
3.81
71.
3.15
3.11
109.
3.25
3.61
111.
3.93
3.72
95.

1981
1.82
2.53
52.
1.15
3.06
71.
2.30
1.96
85.
1.05
0.70
f,6.
1. 10
P. 26
"3.
1. 10
T. ?6
-•3.
2P.31
5.81
21.
2P. 87
2.35
8.
21.99
10.08
16.
0.0
0.0
0.
0.0
0.0
0.
0.0
0.0
0.
PB
1983
10.01
5.77
58.
10.02
1.12
13.
9.06
1.18
11.
0.0
0.0
0.
0.0
n.o
0.
0. 0
0.0
0.

319.
51.
815.
336.
11.
828.
576.
70.
871.
1051.
120.
1179.
918.
80.
1269.
959.
76.

1981
3175.
525.
17.
1050.
976.
23.
1375.
1187.
27.
5050.
2117.
13.
C175.
1615.
30.
r-ooo.
1301.
??.
130.
97.
75.
11^.
13.
37;
122.
58.
18.
0.
0.
0.
0.
0.
0.
0.
0.
0.
"3
inm
2515.
289.
1 1.
3373.
53?.
1f,.
3525.
131.
1?.
378r'.
117.
11.
1103.
281.
r,.
50 1r..
91.
?.
35S.
r26.
IIP.
121.
156.
108.
137.
101.
73.
171.
97.
57.
131.
109.
81.
117.
101.
68.
.IN
1981
216.
23.
1 1.
216.
12.
5.
180.
11.
23.
112.
53.
17.
10U.
31.
q?-
1 10.
C, 1
'Ifi.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.

19P3
202.
35.
17.
205.
35.
"1.
17U.
r, 5.
37.
0.
0.
0.
0.
0.
0.
0.
0.
n.
5600.
^56 5.
16.
21250.
22116.
93.
61100.
37701.
59.
78925.
19173.
25.
81650.
13281.
16.
71825.
16097.
22.
M
1981
21.6
11.7
18.
23.1
11.3
61.
22.5
18.3
81.
52.0
82.1
158.
71.1
66.0
92.
19. f
68.9
112.
5110. 0.12 0.27
1359. 0.05 0.11
85. 10. 153.
13988. 0. 10 0.07
8000. 0.0 0.03
57. 0. 13.
83090. 0.10 0.28
51990. 0.0 0.12
66. 0. 152.
109878. D. 12 0.0
70621. 0.07 0.0
61. 53. 0.
199525. 0. 12 0.0
15065. 0.05 0.0
23. 10. 0.
128725. 0. 12 0.0
22591. 0.05 0.0
18. 10. 0.
II K
1983 1981 1983
16.2 1900. 2728.
3.3 365. 319.
20. 7. 13.
11.5 5150. 3323.
3.2 656. 511.
17. 13. 16.
15.6 1150. 2835.
B.6 621. 631.
55. 11. 22.
3.3 3130. 2215.
0.0 929. 216.
0. 27. 11.
3.0 3330. 2118.
0.0 775. 102.
0. 23. 5.
0.3 3150. 2673.
0.0 656. 500.
0. 19. 19.
1.52
0.99
22.
1.82
1.51
31.
3.87
1.11
30.
2.92
1.01
35.
2.92
1.27
13.
3.05
1.33
11.
S
1981
0.5
0.0
0.
0.1
0.0
0.
0.1
0.0
0.
1.3
0.0
0.
1.3
0.0
0.
1.3
0.0
0.
7.93
1.26
16.
10. 29
2. 38
23.
9.52
1.82
19.
0.0
0.0
0.
0.0
0.0
0.
0.0
0.0
0.
IE
1983
0.0
0.0
0.
0.0
0.0
0.
0.0
0.0
0.
0.0
0.0
0.
0.0
0.0
0.
0.0
0.0
0.
16.22 15.70 8.30
3.61 3.71 2.31
22. 21. 28.
13.10 11.18 11.35
5.36 5.37 5.62
29. 37. 50.
16.55 16.69 13.88
5.25 2.19 6.61
32. 15. 18.
13.32 0.0 8.17
3.95 0.0 1.83
30. 0. 57.
16.32 0.0 7.37
6.62 0.0 3.99
11. 0. 51.
13.07 0.0 7.07
2.37 0.0 1.09
18. 0. 58.
AG NA
1381 1983 1981 1983
0.0 0.05 211. 170.
0.0 0.00 73. 73.
0. 0. 31. 15.
O.»0 0.05 219. 326.
0.0 0.00 78. 60.
0. 0. 31. 19.
0.30 0.11 278. 303.
0.0 0.11 62. 71.
0. 107. 22. 21.
0.0 0.0 300. 253.
0.0 0.0 15. 85.
0. 0. 15. 31.
0.0 0.0 293. 310.
0.0 0.0 78. 151.
0. 0. 27. 19.
0.0 0.0 281. 302.
0.0 0.0 85. 97.
0. 0. 30. 32.
5.61 0.0 3.9
5.01 0.0 1.5
89. 0. 37.
S.18 0.0 0.5
2.68 0.0 0.0
11. 0. 0.
5.93 3.9 1.1
1.09 0.0 0.9
16. 0. 63.
3.0 3.2 0.0
0.0 0.0 0.0
0. 0. 0.
0.0 8.0 0.0
0.0 0.0 0.0
0. 0. 0.
0.0 0.9 0.0
3.0 3.0 0.0
0. 0. 0.
ZH
1981 1983
78.1 52.5
16.0 31.1
59. 59.
55.0 13.6
11.2 6.8
20. 16.
13.1 38.0
1.1 9.6
10. 25.
51.5 32.7
28.6 7.5
53. 23.
»»*»• 30.1
**•»* 10.3
200. 31.
17.3 29.0
20.1 1.3
13. 15.
*AV-Arithmetic Average;  SD-Standard Deviation;  CV-Coefficient  of Variation  in Percent

-------
                             Table E.14
Priority Organics  in  Hancock Soils Receiving 42.2 cm Hydraulic Loading
 1981
 1983
  1981
 1983
Degth
30


60


91


121


152


182


30


60.


91


121


152


182


°cBth
30


60

91

121

152

182


30

60


91

121




182



AV *
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD

AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SO
AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
rp
r n
SD
AV
rp
r n
cr\
MJ
Acenaphthylene
<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


23.63
1/12

<20.0


<20.0


<20.0


<20.0


<20.0


4-chloroaniline
< 100.0


< 100.0

< 100.0

<100.0

< 100.0

<100.0


< 100.0

< 100.0


< 100.0

< 100.0


< IOO.O

<100.0


Anthracene Atrazine Benzene
<20.0 <100.0 12.19
10/12
(14.44)
<20.0 <100.0 8.29
7/12
(5.76)
<20.0 <100.0 4.83
8/12
(3.46)
<20.0 107.75 2.69
1/12 8/12
(1.07)
<20.0 <100.0 2. 98
7/12
(2.17)
<20.0 <100.0 2.90
7/12
(2.05)
<20.0 <100.0 1.99
10/12
(0.88)
<20.0 <100.0 1.42
6/12
(0.61)
<20.0 <100.0 1.05
2/12
(0.12)
<20.0 <100.0 1.07
1/12

<20.0 <100.D <1.0


<20.0 <100.0 <1.0


4-t-butylphenol
17.35
2/12
(19.21)
18.45
2/12
(25.59)
12.98
2/12
(6.88)
<10.0


<10.0


<10.0


<10.0


<-10.0


<10.0


<10.0


<10.0


<10.0


Carbon tetrachl
<1 .0


<1 .0


<1.0


<1 .0


<1.0


<1 .0


8.46
7/12
(8.60)
13.08
9/12
(15.12)
7.55
9/12
(7.07)
5.U7
3/12
(3.16)
5.90
3/12
(3.18)
5.77
3/12
(3.26)
Chlorobenzene Chloroform '2-chlorophenol 1-chloruietradecane
<1.0 11.25
6/12
(15.07)
<1.0 y.;>3
3/12
(12.46)
<1.0 8.81
4/12
(16.40)
<1.0 7.96
2/12
(17.53)
<1.0 3.81
2/12
(5.77)
<1.0 2.87
2/12
(3.95)
<1.0 20.28
5/12
(63.55)
<1.0 4.62
4/12
(7.89)
<1.0 4.38
5/12
(5.97)
<1.0 7.20
3/12
(1.35)
<1.0 6.90
3/12
(0.36)
<1.0 6.03
3/12
(1.59)
11.96
2/12
(6.33)
13.66
2/12
(10.51)
12.10
1/12
(6.97)
<10.0

<10.0

<10.0


<10.0

<10.0


<10.0

<10.0


<10.0

<10.0


<20.0


<2U.U

<20.0

<20.0

<20.0

<20.0


33.12
5/12
(23.06)
20.39
1/12

<20.0

<20.0


<20.0

<20.0


                               556

-------
Table  E.14,  continued
1981
                 Dibutylphthalate   2,3-dichloroaniline   3,4-dichloroaniline  Dichloroben:
30
60
91
121

152

182

1983 30

60

91


121


152


182


1981 Oeott
30


60


91


121


152


182


1983 30


60


91


121


152


182


AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FH
SO
AV
FR
SD
AV
FR
SO
AV
FH
SD
AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
1
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
33.92
1/12
<20.0
47.50
1/12
27.91
2/12
(25.01)
27.80
2/12
(23.93)
40.43
3/12
(40.28)
<20.0

<20.0

<20.0


21.13
1/12

21.13
1/12

21.13
1/12

Dichlorobenzene P
22.99
1/12

<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


26.39
1/12
21.22
1/12
24.53
1/12
<20.Q

<20.0

<20.0

21.12
1/12
<20.0

<20.0


<20.0


<20.0


<20.0


Dichlorobenzene 0
17.93
2/12
(19.05)
24.76
3/12
(25.34)
18.57
2/12
(19.44)
37.31
3/12
(59.64)
33.63
1/12
(66.82)
39.36
2/12
(66.47)
11.26
3/12
(2.42)
13.58
4/12
(7.14)
12.23
2/12
(5.22)
,17.93
1/12
(13.74)
17.93
1/12
(13.74)
17.93
1/12
(13.74)
40.33
1/12
<20.0
<20.0
<20.0

<20.0

<20.0

22.09
1/12
<20.0

<20.0


<20.0


<20.0


<20.0


2 , 4-dichlorophenol
<30.0


<30.0


<30.0


<30.0


<30.0


<30.0


<30.0


<30.0


<30.0


<30.0


<30.0


<30.0


10.66
1/12
12.53
1/12
12.83
1/12
<10.0

<10.0

<10.0

10.29
1/12
<10.0

10.23
1/12

<10.0


<10.0


<10.0


Diethylphthalate
79.60
3/12
(178.83)
24.00
2/12
(10.49)
32.26
2/12
(34.59)
33.90
2/12
(32.85)
47.50
2/12
(51.15)
47.50
2/12
(51.15)
<20.0


55.75
2/12
(67.17)
80.83
3/12
(129.08)
<20.0


<20.0


31.83
1/12


























Diisooctylphthalate
182.24
8/12
(210.99)
164.92
10/12
(183.61)
98.96
9/12
(85.85)
85.19
8/12
(77.13)
152.80
8/12
(134.45)
188.5
8/12
(153.97)
<20.0


<20.0


<20.0


<20.0


<2D.O


<20.0


                                              557

-------
Table  E.14,  continued





1981   Depth      Dioctylphthalate   Ethyl benzene   Heptadecane   Methylheptadecanoate  Methylhexadecanoate


















1983

















1981












1983











30


60


91


121


152


182


30


60


91


121


152


182


°8R
30

60

91

121

152

182

30

60

91

121

152

182

AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FH
SO
AV
FR
SD
AV
FH
SD
AV
FR
SO
AV
FR
SD
th
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SO
AV
FR
SO
AV
FR
SO
AV
FH
SO
AV
FR
SO
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SD
1 31 . 80
3/12
(153.84)
114.00
2/12
(162.81)
275. QU
4/12
(283.09)
107.90
5/12
(86.53)
226.23
3/12
(223.86)
168.20
3/12
(195.18)
<20.D


<20.0


<20.0


<20.0


<20.0


<20.0


1-methylnaphthalene
<10.0

<10.0

<10.0

<10.0

<10.0

<10.0

<10.0

<10.0

<10.0

<10.0

<10.0

<10.0

3.50 <1Q.O
2/12
(4. BO)
<1.5 <10.0


<1.5 <10.0


4.74 13.99
2/12 1/12
(7. 06)
1.56 <10.0
1/12

<1.5 <10.0


<1.5 11.37
1/12

<1.5 10.48
1/12

<1.5 <10.0


<1.5 <10.0


<1.5 <1Q.O


<1.5 <10.0


2-methylphenol 4-methylphenol
<10.0 * <20.0

<10.0 <20.0

<10.0 <20.0

<10.0 <20.0

<10.0 <20.0

<10.0 <20.0

<10.0 <20.0

<10.0 <20.0

<10.0 <20.0

"=10.0 <2Q.Q

<10-° <20.0

<10.0 <20.o

<20.0


<20.0


40.38
1/12

72.08
1/12

38.75
1/12

38.75
1/12

<20.0


<2D.O


<20.0


<20.U


<20.0


<20.0


Napthale.,i
<10.0

<10.0

<10.0

<10.0

<10,0

<10.0

<10.0

<10.0

<10.0

<10.0

<10.0

<1U.O

<20.0


32.83
1/12

<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<2D.O


<20.0


<20.0


<20.0


Octadecane Phenol
<20.0 <100.0

23.02 <100.0
1/12
26.00 <100.0
2/12
22.27 172.92
1/12 1/12
<20.0 223.63
2/12
(306.21)
<20.0 224.30
2/12
(306.19)
<20.0 <100.0

<20.0 <100.0

<20.0 <100.0

<20.0 <100.0

<20.0 <100.0

<20.0 <100.Q

                                             558

-------
    Table  E.14,  continued
1981
1983
Oegth
30


60


91


121


152


182


30


60


91


121


152


182


Propazine a-terpineol
AV
FH
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SO
AV
FR
SO
AV
FR
SD
AV
FH
SO
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR -
SD
101.00
2/12

<100.0


111.33
1/12

115.83
1/12

<100.0


<100.0


<100.0


<100.0


<100.0


<100.0


<100.0


<100.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


Tetrachloroethylene Toluene Tnchloroetnane Trichloroet
1.27 <1.0 <1.0 <1.0
3/12
(0.75)
1 .16 <1 .0 <1 .0 <1 .0
3/12
(0.27)
1.03 <1.0 <1.0 <1.0
1/12

1 .06 <1 .0 <1 .0 <1 .0
2/12
(0.13)
<1.0 <1.0 <1.0 <1.0


<1.0 <1.0 <1.0 <1.0


2.39 <1.D <1.0 1.68
7/12 1/12
(1.15)
1.67 <1.0 <1.0 <1.0
5/12
(0.73)
1.79 <1.0 <1.0 <1.0
5/12
(0.72)
1.09 <1.0 <1.0 <1-0
1/12

1.09 <1.0 <1.0 <1-0
1/12

1.09 <1.0 <1.0 <1.0
1/12

              * AV - Arithmetic Average
                FH   Frequency of Detection Greater Than Detection Limit
                SD - Standard Deviation
                                              559

-------
                          Table E.15
Priority Organics in Soils Receiving 52.2 cm Hydraulic Loading
1981


















1983

















1981


















1983















Degth
30


60


91


121


152


182


30


60


91


121


152


182


Death
cm
30


60


91


121


152


182


30

60


91


121


152


182


AV*
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
•FH
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD

AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FH
SD
AV
FR
SD
AV
FR
SO
Acenaphthylene
21.99
1/8

<20.0


<20.0


22.43
2/8

<20.0


<20.0


21.11
1/8

<20.0


<20.0


<20.0


<20.0


<20.0


4-chloroaniline
<100.


<1DO.


<100.


<100.


<100.


<100.


<100.

<100.


<100.


<100.


<100.


000.

Anthracene
40.88
1/8

20.10
1/8

<20.0


36.75
1/8

36.75
1/8

36.75
1/8

<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


Atrazine Benzene
<1UO. 14.74
5/8
(11.11)
<100. 11.33
6/8
(8.42)
<100. 4.85
6/B
(5.72)
<100. 4.63
6/8
(3.26)
<100. 4.23
4/8
(3.54)
<100. 4'. 20
4/8
(3.56)
<100. 2.14
6/8
(1.24)
<100. 1.46
2/8
(0.77)
<100. 1.09
3/8
(0.16)
<100. <1.0


<1UO. <10.0


<100. <10.0


4-t-butylphenol
28.37
2/8
(33.96)
33.03
3/8
(39.26)
20.6
2/8
(20.76)
28.08
1/8

<20.0


20.19
1/8

<20.0


<20.0


<20.0


<20.0


<20.0


<20.D


Carbon tetrach
<1.0


<1 .0


<1 .0


<1 .0


<1 .0


<1 .0


12.54
5/8
(10.56)
12.13
4/8
(9.81)
8.75
4/8
(8.3)



<1 .0


<1.0


Chlorobenzene Chloroform 2-chlorophenol 1-chlorotetradecane
<1.0


<1 .0


1.29
1/8

1.29
1/8

1.29
1/8

1.29
1/8

<1.0"

<1.0


<1.D


<1.U


<1.U


<1.0

9.76
5/U
•(8.23)
17.88
6/8
(17.42)
6.61
4/8
(8.84)
5.79
3/8
(8.21)
12.12
3/U
(19.15)
4.22
2/8
(7.31)
1.69
3/8
(1.21)
1.UO
3/8
(1.08)
1.19
2/8
(0.37)
1.40
1/8

1.23
1/8

1.21
1/8
<10.0


<10.0


<10.0


24.38
1/8

<10.0


<10.0


11.43
1/8
<10.0


<10.0


<1U.O


<10.0


<10.D

26.48
1/8

24.60
1/8

39.00
1/8

32.63
1/8

<20.U


29.67
2/8
(17.37)
70.13
2/8
(94.95)
<20.0


<20.0


<2D.O


<20.0


<2U.O

                             560

-------
Table E.15, continued
1981
















1983
















1981


















1983














Depth
30

60


91


121


152


182


30


60


91


121

152


182


DHT
30


60


91


121


152


182


30

60


91


121

152

182


AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FH
SD
AV
FR
SD
AV
FH
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
i
AV
FH
SD
AV
FR
SD
AV
FR
SD
AV
FH
SD
AV
FH
SD
AV
FR
50
AV
FK
SD
AV
FR
50
AV
FR
SD
AV
FH
SO
AV
FR
SD
AV
FR
SD
Dibutylphthalate 2,3-dichloroaniline

-------
      Table  E.15,  continued




1981   Death      Dioctylphthalate   Ethyl benzene   Heptadecane   Methylheptadecanoata  Methylhexadecanoate

















1983

















1981
















1983










30

60


91


121


152


182


30


60


91


121


152


182


Dgfith
30

60

91


121


152


182


30

60

91

1 91
I L \
152
182

AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FH
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD

AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FH
SD
AV
FR
SO
AV
FR
SD
AV
FR
SO
AV-
FR
SD
AV
FH
SD

AV
FR
SD
AV
FR
SD
AV
FR
SD
379.38
1/8

96.13
1/8

66.75
1/8

89.2
3/8
(62.9)
332.00
3/0
(391.45)
951.00
2/8
(1332.19)
<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


1-methylnaphthalene
14.36
1/8
11.48
1/8
<10.0


<10.0


<10.0


<10.0


<10.0

<10.0

<10.0


<10.0
<10.0
<10.0

2.00 14.49 175.50
1/8 1/8 1/8

<1.5 <10.0 <20.0


<1.5 <10.0 <20.0


1.69 28.35 23.63
1/8 2/8 1/8
(33.10)
1.69 <10.Q 62.63
1/8 1/8

1.69 13.51 62.63
1/8 1/8 1/8

<1.5 <10.0 <20.0


<1.5 <10.0 <20.0


<1.5 <10.0 <20.0


<1-5 <10.0 <20.0


<1-5 <10.0 <20.0


<1.5 <10.0 <20.0


2-methylphenol 4-methylphenol NapthaJene
<20.0 <20.0 12.84
1/0
<20.0 <20.0 <10.0

<20.0 <20.0 <1Q.Q


<20.0 <20.0 .<10.0


<20.0 <20.U <10.0


<20.0 <20.0 <10.0


<20.0 <20.0 <10.Q

<20.0 <20.0 <1Q.Q

<20.0 <20.Q <10.0


<20-0 <20.0 <1Q.o
<2U.U <20.0 
-------
Table  E.15,  continued
1981 °g°,th
30


60


91


121


152


182


1983 30


60


91


121


152


182


Propazine a-terpineoi Tetracnioruethyiene Toiuene Triuiiiuruethane Tricnlurut
AV
FR
SD
AV
FH
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
50
AV
FH
SD
AV
FR
SD
AV
FR
SD
<100.


102.25
1/8

102.88
1/8

111.38
1/8

<100.


<100.


<100.


<100.


<100.


<100.


<100.


<100.


<10.0


12.21
1/8

<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<1U.O


<1.0 <1.0 <1.0 <1.0


<1.0 <1.0 <1.0 <1.0


<1.0 <1.0 <1.0 <1.0


<1.Q <1.0 <1.0 <1.0


<1.0 <1.0 <1.U <1.0


<1.0 <1.0 <1.0 <1.0


2.00 <1.0 <1.0 <1-0
4/8
(1.03)
1.71 <1.0 <1.0 <1.0
3/8
(0.92)
1.61 <1.0 <1.0 <1-°
5/8
(0.69)
1.09 <1.0 <1.0 <1.D
1/8

1.21 <1.0 <1.0 <1.C
1/8

1.24 <1.0 <1.0 <1.C
1/8

             * AV   Arithmetic Average
              FR - Frequency of Detection  Greater than Detection Limit

              SD - Standard Deviation
                                               563

-------
                              Table  E.16
 Priority Organics in  Soils  Receiving  68.9  cm Hydraulic  Loading
1981  °§Eth      Acenaphthylene  Anthracene  Atrazine   Benzene  4-t-butylpnenol  Carbon tetrachloride


















1983

















1981
















1983











30


60


91


121


152


182


30


60


91


121


152


182


°?Rtr
30


60


91


121

152


182

30

60
91

121

152

182


AV*
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FH
SD
AV
FR
SD
i
AV
FH
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FK
SD
AV
FH
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FH
SD
<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.J


<20.0


<20.0


4-chloroaniline
<100.


<100.


<100.


<100.

<100.


<100.

<100.

<100.
<100.

<100.

<100.

<100.


<20.0 167.50 13.2 <10.0 <1 .0
2/4 3/4
(122.03) (13.1)
<20.0 119.75 9.50 <10.0 <1.0
1/4 3/4
(6.14)
<20.0 145.00 2.70 14.05 <1.0
1/4 3/4 1/4
(1.5)
<20.0 <100. 1.75 53.38 <1.0
3/4 2/4
(0.54) (80.54)
<20.0 <100. 1.45 <10.0 <1.0
2/4
(0.71)
<20.0 <100. 1.33 <10.0 <1.0
3/4
(0.97)
<20.0 <100. <1.0 <10.0 5.93
1/4

<20.0 <100. <1.0 <10.0 5.08
1/4

<20.0 <100. <1.0 
-------
Table E.16,  continued





1981   °|Rth      Dibutylphthalate   2,3-dichloroaniline   3,4-dichloroaniline   Oichlorobenzene H


















1983
















1981


















1983
















30


60


91


121


152


182


30


60


91


121


152

182


Degth
30


60


91


121


152


182


30


60


91


121


152

182


AV
FR
SO
AV
FR
SD
AV
FR
SO
AV
FR
SO
AV
FR
SD
AV
FR
SO
AV
FR
SO
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
50
AV
FR
SD

AV
FH
SD
AV
FR
SO
AV
FR
SO
AV
FR
en
JU
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
<20.0


<20.0


<20.0


<20.D


<20.0


<20.U


89.50
1/4

62.00
1/4

68.75
1/4

<20.0


<20.0

<20.0


Dichlorobenzene P
<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.D


<10.0


<10.0


<10.0

<10.0


<20.0


<20.0


<20.0


<20.0


<20.Q


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0

<20.0


Dichlorobenzene 0
<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


13.90
1/4

11.28
1/4

10.95
1/4

<10.0


<10.0

<10.0


<20.0


<2Q.O


<20.0


60.25
1/4

<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0

<2D.O


2 , 4-dichlorophenol
<30.0


<30.0


<30.0


64.50
1/4

<30.0


<30.0


<30.0


<30.0


<30.0


<30.0


<30.0

<30.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


12.90
1/4

<10.0


<10.0


<10.0


<10.0

<10.0


Diethylphthalate
<20.0


49.75
1/4

31.65
1/4

<20.0


<20.0


<20.0


96.75
3/4
(97.75)
54.75
1/4

59.50
1/4

<20.0


<20.0

<20.0





































Diisooctylphthalate
222.25
4/4
(103.86)
101.43
3/4
(18.98)
80.93
3/4
(54.52)
1 1 3 . 80
2/4
(160.10)
30.80
1 /4


30.80
1/4

NR


NR


MR


NR


NR

NR


                                                565

-------
Table E.16,  continued
1981


















1983

















1981


















1983

















Death
Cm
30


60


91


121


152


182


30


60


91


121


152


182


Deoth
cfn
30


60


91


121


152


182


30


60


91


121


152


182


Dioctylphthalate Ethyl benzene Heptadecane Methylheptadecanoate Metnyihexadecanoati
AV
FH
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FH
SO
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SO

AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FH
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SD
103.33
2/4
(73.92)
129.93
2/4
(135.27)
71.47
2/4
(53.62)
93.23
2/4
(104.66)
37.75
1/4

37.75
1/4

NR


NR


NR


NR


NR


NR


1-methylnaphthalene
<10.0


<10.0


<1D.O


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.U


<1 5 <10.0 65.75
1/4

6.50 <10.0 52;00
2/4

4.78 <10.0 73.50
1/4 1/4

<1.5 <10.0 <20.0


<1.5 <10.Q <20.0


<1.5 <10.0 <20.0


<1.5 <10.0 <20.0


<1.5 13.48 <20.0
1/4

<1.5 <10.0 <20.0


<1.5 <10.0 <20.0


<1.5 <10.0 <2D.O


<1.5 <10.0 <20.0


2-methylphenol 4-methylphenol Napthalene
<10.0 <20.0 <10.0


<10.0 <20.0 <10.0


<10.0 <20.0 <10.0


<10.0 <20.0 <10.0


<10.0 <20.0 <10.Q


<10.0 <20.0 <10.0


<10.0 <20.0 <10.0


<10.0 <20.0 <10.0


<10.0 <20.0 <10.0


<10.0 <20.0 <10.0


<10.0 <20.0 <10.0


<10.0 <20.0 <10.0


<20.0


<20.0


27.28
1/4

<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


Octadecane Phenol
<2U.I) <1UO.


<20.0 105.50
1/4

<2U.O <100.


<20.0 <100.


<20.0 <100.


<2U.O <100.


<20.0 <100.


23.10 <100.
1/4

<20.0 <100.


<20.0 <100.


<20.0 <100.


<20.0 <100.


                                 566

-------
Table  E.16,  continued


                     Propazine   a-terpineol    Tetrachiuruethylene   Toluene   Trichloruethane  Trichloroethylene
1981
30


60


91


121


152


182


1983 30


60


91


121


152


182


AV
FH
SO
AV
FH
SO
AV
FR
SO
AV
FR
SO
AV
FR
SO
AV
FH
SO
AV
FR
SO
AV
FR
SO
AV
FR
SD
AV
FR
SO
AV
FR
SO"
AV
FR
SO
<100.


<1QO.


<100.


<100.


<100.


<100.


<100.


<100.


<100.


<100.


<100.


<100.


<10.D


<10.Q


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<1.0


<1.U


<1.Q


1.40
V4

1.40
1/4

1.40
1/4

2.33
2/4
(1.62)
:• . 1 3
3/4
(7.20)
2.43
3/4
(1.11)
<1.0


<1.0


<1.0


<1.0 <1.0


<1.0 <1.0


<1.0 <1.0


<1.0 <1.0


<1.0 <1.0


<1.0 <1.0


<1.0 <1.U


<1.0 <1.0


<1.0 <1.0


<1.0 <1.0


<1.0 <1.0


<1.0 <1.D


                * AV - Arithmetic  Average
                  FR - Frequency of Detection Greater than Detection Limit
                  SD - Standard Deviation
                                                  567

-------
Ul
Ox
en
                                Table E.17
Bacteriological Data for Hancock Soils Receiving 42.2  cm Hydraulic  Loading
                              (CFU/g soil    )
                            Fecal Coliform

                              <2320
                                (0)
                                0/12
                              <2420
                                (0)
                                0/12
                              <2400
                                (0)
                                0/12
                              <2320
                                (0)
                                0/10
                              <2260
                                (0)
                                0/10
                              <2260
                                (0)
                                0/10

                              <2340
                                (0)
                                0/12
                              <2380
                                (0)
                                0/12
                              <2340
                                (0)
                                0/12
                              <2240
                                (0)
                                0/1
                              <2240
                                (0)
                                0/1
                              <2240
                                (0)
                               0/1

 *  AV  -  Arithmetic Average
   SD  -  Standard Deviation
   FR  -  Frequency of Detection of organisms  at concentration
        Greater than analytical  detection  limit
1981 Depth
cm
30


60


91


121


152


182


1983 30


60


91


121


152


182




AV*
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FH
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
Total Colifc

<2320
(0)
0/12
<2420
(0)
0/12
<2400
(0)
0/12
<2320
(0)
0/10
<2260
(0)
0/10
<2260
(0)
0/10
248,000
(597,000)
2/12
2618-
(1050)
1/12
5283-
(10,400)
1/12
<2240
(0)
0/1
<2240
(0)
0/1
<2240
(0)
0/1
Fecal Strep

2535
(966)
1/12
1.3 x 109
(4.5 x 109)
1/12
<2360
(0)
0/12
<2320
(0)
0/10
<2260
(0)
0/10
<2260
(0)
0/10
8334
(11,300)
5/12
2615
(2260)
2/12
2774
(1706)
1/12
<2240
(0)
0/1
<2240
(0)
0/1
<2240
(0)
0/1
Actinomycetes
^2
1.0 x 10
(1.8 x 10 )
12/12
2.0 x 10'"
(1.1 < 10")
11/11
5.5 x 1010
(1.4 x 10")
12/12
1.3 x 10"
(2.1 x 10")
10/10
1.1 x 10"
(2.2 x 10")
10/10.
1.3 x 10"
(2.2 x 10")
10/10
3.0 x 10"
(2.7 x 10U)
12/12
1.2 < 10"
(2.1 < 10*)
12/12
1.2 x 10
(2.2 x 10U)
12/12
1.79 x 109
(0)
1/1
6.72 x 101"
(0)
1/1
2.24 x 10 '°
(0)
1/1
Fungi
1*
2.3 x 10
(2.5 x 10')
12/12
1.3 x 10*
(1.3 x 10")
11/11
9.3 x 10s
(9.2 x 10s)
12/12
1.6 x 10"
(1.8 x 10')
10/10
1.1 x 10"
(9.7 x 10s)
10/10 ^
7.2 x 10
(2.0 x 10 )
10/10
2.4 x 10"
(1.7 x 10 )
12/12
1 .0 x 10
(1.3 x 10')
12/12
8.3 x 10
(8.8 x 10 )
12/12
7.8 x 10
(0)
1/1
4.5 x 10
(0)
1/1
1.1 x 1Q3
(0)
1/1

-------
                                Table E.18
Bacteriological Data  for Hancock Soils Receiving 52.2  cm  Hydraulic  Loading
                               (CFU/g soildwfc)
1981 Depth
cm
30


60


91


121


152


182


1983 30


60


91


121


152


182



AV*
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
Total Coliform
<2420
(0)
0/8
<2500
(0)
0/8
<2420
(0)
0/8
2271
(47)
1/7
<2260
(0)
0/6
<2260
(0)
0/6
261,000
(654,000)
2/8
12,900
(20,800)
3/8
2766
(1247)
1/8
<2260
(0)
1/1
<2260
(0)
1/1
<2260
(0)
1/1
Fecal Coliform
<2420
(0)
0/8
<2500
(0)
0/8
<2420
(0)
0/8
<234Q
(0)
0/7
<2260
(0)
0/6
<2240
(0)
0/6
3963
(4598)
1/8
5578
(9084)
1/0
<2440
(0)
0/8
<2260
(0)
1/1
<2260
(0)
1/1
<2260
(0)
1/1
Fecal Strep
<2420
(0)
0/8
<2500
(0)
0/8
<2420
(0)
0/8
<2340
(0)
0/7
<2260
(0)
0/6
<2260
(0)
0/6
42,016
(97,521)
3/8
3119
(2106)
2/8
3646
(3727)
'1/8
<2260
(0)
1/1
<2260
(0)
1/1
<2260
(0)
1/1
                                                                Actinomycetes     Fungi

                                                                  1.4  x  10",2     6.3  x  10*
                                                                  (1.6 x  10  )     (8.7 x io")
                                                                  8/8      u      8/8
                                                                  2.4  x  10        1.4  x  10*
                                                                  (3.3 x  10  )     (1.9 x 10')
                                                                  8/8      n      8/8
                                                                  1.4 x  10        1.4  x  10"
                                                                  (2.1 x  10 ')     (1.2 x  10*)
                                                                  8/8             8/8
                                                                  9.0 x 10        1.7  x  10*
                                                                  (2.3 x  1012)     (2.2 x  10*)
                                                                  7/7             7/7
                                                                  2.4 x 10U       7.2  x  10S
                                                                  (4.2 x  10U)     (5.4 x 103)
                                                                  6/6            6/6
                                                                  1 .9 x 10"      9.1  x 10S
                                                                  (3.9 x  10")     (3.9 x 10')
                                                                  6/6            6/6
                                                                 4.5 x 10U      7.6 x 10"
                                                                  (3.4 < 10U)    (1.1  x  105)
                                                                 8/8            8/8
                                                                 3.0 x 10*      9.5 x 105
                                                                  (3.4 x 1012)    (2.0  x  106)
                                                                 8/8            8/8
                                                                 2.4 x 10U      8.5 x 10'
                                                                 (2.2 x  10*)'    (7.1  x,105)
                                                                 8/8     '       0/8
                                                                 9,04 x  10"     1.1  x 103
                                                                 (0)            (0)
                                                                 1/1            1/1
                                                                 2.26 x  10"     3.4 x 10
                                                                 (0)            (0)
                                                                 1/1            1/1
                                                                 9.04 x  Kj"     6.8 x 10*
                                                                 (0)            (0)
                                                                 1/1            1/1
* AV - Arithmetic Average
  SD - Standard Deviation
  FR - Frequency of Detection of  organisms  at  concentration
       Greater than analytical detection  limit

-------
o
                                                           Table  E.19
                            Bacteriological  Data  for  Hancock  Soils  Receiving  68.9  cm  Hydraulic  Loading
                                                         (CFU/g soildwt)
Fecal Coliform

   <2280
    (0)
    0/4
   <23UO
    (0)
    0/4
   <2380
    (0)
    0/4
   <2280
    (0)
    0/4
   <22130
    (0)
    0/4
   <22BO
    (0)
    0/4

    5545
    (6530)
    V4
    2365
    (19)
    2/4
   <2360
    (0)
    0/4
    NR
                                                          NK
                                                          NR
1981 Dejath
30


60


91


121


152


182


1983 30


60


91


121


152


182



AV*
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
Total Coliform
<2240
(0)
0/4
<2380
(0)
0/4
<2380
(0)
0/4
<2280
(0)
0/4
<2280
(0)
0/4
<2280
(0)
0/4
18,700
(14,600)
3/4
3250
(1767)
3/4
<2360
(0)
0/4
NR


NR


NR


, Fecal Strep
<2280
(0)
0/4
<2380
(0)
0/4
•<2380
(0)
0/4
<2280
(0)
0/4
<2280
(0)
0/4
<2280
(0)
0/4
25,400
(35,800)
3/4
8508
(12., 300)
1/4
4985
(3365)
2/4
NR
Actinomycetes
3.9 x 10"
(7.2 x 10")
4/4
2.0 x 10"
(4.8 x 109)
4/4
1.2 x 10'°
(5.4 x 109)
4/4
2.8 x 10"
(5.5 x 10")
4/4
3.9 x 10"
(4.7 x 10l°)
4/4
4.1 x 10'"
(4.6 x 10l°)
4/4
6.3 x 10'2
(2.2 x 10 )
V4
1.2 x 10 u
(1.3 x 10 .)
4/4
1.3 x 10
(1.3 x 10 )
4/4
NR
Fungi
2.1 x 1011
(2.4 x 10")
4/4
6.8 x 10'
(2.4 x 103)
4/4
5.0 x 10
(5.2 x 103)
4/4
9.4 x 103
(1.0 x 10")
4/4
1.8 x 10"
(1.2 x 10")
4/4
2.2 x 10"
(9.6 x 103)
4/4
5.4 x 10"
(5.1 x 10 )
4/4 3
1.3 x 10 3
(1.5 x 10 )
4/4
1.1 x 10 ,
(1.1 x 10 )
4/4
NR
                                                                             NR
                     NR
                                    NR
                                                                                            NR
                         * AV - Arithmetic Average
                           SD - Standard Deviation
                           FR - Frequency of Detection  of  organisms  at  concentration
                                Greater than analytical detection  limit

-------
                                                Table E.20
                                 Soil Physical Characteristics - Gray Farm
Vjn
Depth
Code 01062
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Code 02093
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Code 05084
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Code 07072
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Code 09052
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Particle
Density
(q/cc)
2.44
2.41
2.53
2.63 (3'/6')


2.58
2.53
2.57
2.70 <3'/6')


2.53
2.59
2.68
2.63 C3'/6')


2.56
2.57
2.61
2.59 (3'/6')


2.51
2.51
NR
2.55 (V/61)


Texture
B
Sandy Clay Loam
Clay Loam
Sandy Clay Loam
Clay


Sandy Clay Loam
Sandy Clay Loam
Clay Loam
Clay Loam


Sandy Loam
Sandy Clay Loam
Clay
Clay


Sandy Loam
Sandy Clay Loam
Clay Loam
Clay Loam


Sandy Clay Loam
Sandy Clay Loam
Sandy Clay Loam
Sandy Clay Loam


I
Sandy Loam
Sandy Clay Loam
Clay Loam
Clay


Sandy Loam
Sandy Clay Loam
Sandy Clay Loam
Clay Loam


Sandy Loam
Sandy Loam
Sandy Clay Loam
Loam


Sandy Loam
Sandy Clay Loam
Sandy Clay Loam
Clay Loam


Sandy Loam
Sandy Clay Loam
Sandy Loam
Sandy Loam
Sandy Loam
Sandy Loam
Bulk
Density
(g/cc)
1.40
1.39
1.41
1.32


1 .43
1.37
1.45
1. 26


1.44
1.37
1.37
1.39


1.46
1.41
1.38
1.40


1.43
1.36
NR
1.40


Color
Description
Dark Brown
Strong Brown
Light Reddish Brown
Pinkish White


Dark Braown
Strong Brown
Light Brown
Pink


Brown
Pinkish Gray
Pinkish White
Pinkish White


Dark Brown
Pinkish Gray
Pinkish Gray
Pinkish Gray


Brown
Yellowish Red
Light Red
Light Red


Code
7.5YR4/4
7.5YR4/6
5YR6/4
•5YR8/2


7.5YR4/4
7.5YR4/6
7.5YR6/4
7.5YK7/4


7.5YR5/2
7.5YT6/2
7.5YR8/2
7.5YR8/2


7.5YR4/2
7.5YR6/2
7.5YR8/2
7.5YR7/2


7.5YR5/4
5YR5/6
2.5YR6/8
2.5YR6/8


Porosity
(SO
42.7
42.3
44.2
50.0


44.6
45.7
43.5
53.3


43.3
42.5
48.9
47.0


43.1
45.3
47. 1
46.0


43.0
45.9
NR
45.0



-------
     Table E.20, continued
K>

Depth
Code 10093
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Code 14071
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Code 19084
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Code 18121
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Code 23132
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Particle
Density
(q/cc)
2.66
2.46
2.53
2.55
2.52

2.48
2.45
2.53
2.52 (3'/6')


2.54
2.50
2.47
2.59 O'/6')


2.57
2.44
2.48
2.55
2.39 (4'/6')

2.57
2.54
2.40
2.53



Texture
B
Sandy Clay Loam
Sandy Loam
Sandy Clay Loam
Sandy Clay Loam
Sandy Clay Loam

Sandy Loam
Sandy Clay Loam
Clay Loam
Clay


Sandy Clay Loam
Sandy Clay Loam
Clay Loam
Clay


Sandy Clay Loam
Sandy Clay Loam
Clay Loam
Clay
Clay Loam

Sandy Clay Loam
Sandy Clay Loam
Sandy Clay Loam
Clay Loan




I
Sandy Loam
Sandy Loan
Sandy Loam
Sandy Clay Loam (3'/6')


Sandy Loam
Sandy Clay Loam
Sandy Clay Loam
Clay Loam


Sandy Loam
Sandy Clay Loan
Sandy Clay Loam
Sandy Clay Loam


Sandy Loam
Sandy Clay Loam
Sandy Clay Loam
Sandy Clay Loam
Sandy Clay Loam

Sandy Loam
Sandy Loam
Sandy Clay Loam (2'/4')



Bulk
Density
(q/cc)
1.48
1.49
1.42
1.45
1.43

1.43
1.38
1.39
1.29


1.42
1.32
1.37
1.33


1.38
1.41
1.34
1.29
1.35

1.46
1.46
1 .45
1.40



Color
Description
Dark Brown
Strong Brown
Reddish Brown
Yellowish Red
Light Red

Reddish Brown
Yellowish Red
Light Reddish Brown
Pinkish White


Brown
Yellowish Red
Reddish Yellow
Pink


Dark Brown
Yellowish Red
Light Reddish Brown
Pink
Pink

Dark Brown
Brown
Reddish Brown
Pink



Code
7.5YR4/4
7.5YR4/6
5YR4/4
5YR5/6
2.5YR6/8

5YR4/3
5YR5/6
5YR6/4
7.5YR8/2


7.5YR5/4
5YR5/6
5YR6/6
7.5YR8/4


7.5YR4/4
5YR5/6
5YR6/4
7.5YRB/4
7.5YR8/4

7.5YR4/2
7.5YR5/4
5YR5/4
7.5YR7/4


Porosity
(S)
44.5
39.3
44.1
43.3
43.4

42.3
43.9
45.1
48.8


43.9
47.1
44.7
48.5


46.4
42.3
46.2
49.4
43.6

43.4
42.6
39.8
44.6



-------
    Table E.20, continued
Depth
Code 24163
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Code 21163
30 cm (1 ft)
61 cm (2 ft)
91 cm (3 ft)
122 cm (4 ft)
152 cm (5 ft)
183 cm (6 ft)
Particle
Density
Cg/cc)
2.58
2.46
2.44
2.44
NR
2.38
2.49
2.50
2.60
2.64
NR (4V61)

Texture
B
Sandy Clay Loam
Sandy Clay Loam
Sandy Clay Loam
Sandy Clay Loam
Clay
Clay Loam
Sandy Clay Loam
Sandy Clay Loam
Sandy Clay Loam
Clay Loam



I
Sandy Loam
Sandy Clay Loam
Sandy Clay Loam
Sandy Clay Loam
Sandy Clay Loam
Sandy Clay
Sandy Laom
Sandy Clay Loam
Clay Loam
Clay
Clay Loam

Bulk
Density
(g/cc)
1.47
1.36
1.39
1.33
1.35
1.36
1.49
1.44
1.50
1.50
NR

Color
Description
Brown
Reddish Brown
Yellowish Red
Reddish Yellow
Pink
Pink
Reddish Brown
Reddish Brown
Light Reddish Brown
Pink
Pink

Code
7.5YR5/4
5.YR5/4
5.YR5/8
5YR6/6
7.5YR7/4
7.5YR7/4
5YR4/4
5YR5/4
5YR6/4
7.5YR7/4
7.5YR8/4

Porosity
42.9
44.8
43.)
45.5
47.9
42.9
40.3
42.4
42.5
43.2
NR

\n

-------
                                           Table E.21

                             Nitrogen in Gray Soils flood Irrigated
Ul
-^j
-O
DEPTH
CM
30 AV *
SD
CV
60 AV
SD
CV
91 AV
SD
CV
121 AV
SD
CV
152 AV
SD
CV
182 AV
SD
CV
TKN
PIG-N/G
1981 1983
**:*****•*•*•*•*• **• ^
^ T" ^ T- -^ T ™
0.75
0. 11
15.
0.54
0. 12
22.
0.34
0.06
19.
0.28
0. 10
36.
0.20
0.08
41.
0.18
0.10
53.
r*T"T»T'*r'*T*T-!
0.68
0.35
52.
0.43
0. 13
31.
0.24
0.05
20.
0,20
0.09
46.
0.20
0.08
41.
0.23
0.09
39.
N02/N03
HG- H/G
1981 1933
^**#****:fr+*****-**J
.01181
.00638
54.
.00930
.00367
39.
.0087r-
.00451
52.
.00997
.00768
77.
.00975
.00594
61.
.01091
.00483
44.
.00545
.00855
157.
.00301
.00466
155.
.00210
.00210
104.
.00542
.00813
150.
.00197
.00147
75.
.00366
.00279
76.
NH3
HG-N/G
1981 1983
fc £ :fr £ 4c 4t ^c4c^e*'***i*'*tJ'*''J
.00250
.001 18
47.
.00202
.00182
90.
.00172
.00059
34.
.00123
.00108
.00057
.00044
77.
.00081
.00038
47.
-^ T T* -T- ^* T- T- •T' 1
.00340
.00151
44.
.00373
.00423
113.
.00160
.00102
64.
.00128
.00138
108.
.00200
.00238
119.
.00172
.00149
87.
ORG N
NG-N/G
1981 1983
k^Afe^AfeAfr*1* *• Jr a.
F^^^T^**^
.74480
.11283
15.
.54035
.12011
22.
.34329
.06395
19.
.27625
.09990
36.
.19607
.08157
42.
.18250
.09747
53.
•T- T- ^ ^- T-
.67410
. 35152
52.
.42375
. 12714
30.
.20500
.09988
49.
. 19870
.09061
46.
.20137
.08150
40.
.23327
.09148
39.
        * AV - Arithmetic Average
          SD - Standard Deviation
          CV - Coefficient of Variation in percent

-------
                                Table E.22

                  Nitrogen in Gray Soils Sprinkler Irrigated
DEPTH           TKN          N02/N03             NH3              ORG N
  CH          HG-N/G          MG-N/G            «!G-N/G            NG-N/G
            1981   1983    1981     1983      1981     1983      1981     1983
***********************************************************************
  30  AV*   0.71   0.52   .01964   .00170   .00198   .00209    .70511  .51490
      3D    0.16   0.09   .01004   .00029   .00102   .00228    .16240  .08885
      CV     23.    17.     51.      17.       51.     109.       23.      17.
  60
  91
 121
 152
 182
AV
3D
CV

AV
3D
CV

AV
3D
CV

AV
3D
CV

AV
3D
CV
0.59
0.15
 25.

0.39
0.14
 35.

0.25
0.13
 52.

0.26
0.14
 53.

0.24
0.13
 56.
0.39
0.09
 24.

0.28
0.11
 41.

0. 10
0.02
 19.

0.10
0.02
 19.

0.10
0.02
 19.
 00794
 00292
  37.

 01131
 01036
  92.

.0154Q
 00971
  63.

,01558
,00966
  62.

,01629
,01020
  63.
.00175
,00103
  59.

.00190
,00082
  43.

.01941
,04503
 232.

.01948
,04449
 228.

.01942
,04451
 229.
.00096
,00059
  61.

.00175
,00281
 161.

,00087
,00057
  66.

.00080
,00055
  68.

,00081
,00059
  73.
.00099
.00064
  65.

.00087
.00027
  31.

.00094
,00028
  29.

.00082
 00024
  29.

.00088
,00017
  20.
.59147
.14873
  25.

.38439
.13652
  36.

,25391
, 13334
  53.

,25653
,13631
  53.

,23618
,13346
  57.
. 39151
.09281
  24.

.27911
.1 1403
  41.

, 10406
.02017
  19.

,10417
,02006
  19.

 10412
,02007
  19.
   AV - Arithmetic Average
   SD - Standard Deviation
   CV - Coefficient of Variation in percent

-------
                                         Table E.23
                   Phosphorus  and Organic Carbon in  Gray Soils Flood Irrigated
Ox
    DEPTH       TOTAL P         OFTHO P          ORG. P        ORG. C     3RG. MATTER
      CM         MG-P/G          PG-P/G          l"IG-P/G        MG-C/G          %
              1981    1983     1981     1983     1981  1983    1981   1983   1981   1983
    ******:****************«************************************************
      30  AV*0.49    0.86    .02502   .01275    0.10  0.04    7.11   9.11   0.41   1.57
          SD  0.20    0.80    .00892   .00948    0.08  0.03    2.33   3.28   0.14   0.56
          CV   39.     93.      ?6.      74.      77.   69.     33.   36.    34.    36.

      60
      91
     121
    152
    182
     * AV - Arithmetic Average
       SD - Standard Deviation
       CV - Coefficient of Variation in percent
AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
0.32
0.22
69.
0.29
0.15
53.
0.19
0.26
139.
0.07
0.04
53.
0.07
0.04
52.
0.39
0.19
48.
0.27
0.09
33.
0.24
0.04
17.
0.25
0. 15
57.
0.42
0.23
54.
.03080
.02188
71.
.01524
.01 142
75.
.00474
.00775
163.
.00071
.00051
72.
.00120
.00129
108.
.01273
.008?7
65.
.01085
.01496
138.
.00895
.01230
137.
.01018
.01387
136.
.00330
.00455
138.
0.09
0.07
75.
0.06
0.04
65.
0.05
0.11
209.
0.02
0.02
65.
0.03
0.02
57.
0.04
0.02
67.
0.03
0.03
108.
0.01
0.0
0.
0.01
0.01
41.
0.02
0.01
56.
4.06
0.47
12.
3. 25
0.81
25.
4. 49
5.28
118.
1.82
0. 77
42.
1.69
6.96
56.
4.92
1.31
27.
3. 10
0.83
27.
2.04
0.30
14.
1.85
0.61
33.
2.45
1.02
42.
0.23
0.03
11.
0.18
0.05
26.
0.26
0.31
119.
0. 10
0.05
44.
0. 10
0.06
57.
0.85
0.23
27.
0.54
0. 15
27.
0.35
0.05
14.
0.32
0. 11
33.
0.42
0. 18
43.

-------
                                              Table E.24

                    Phosphorus and Organic Carbon in Gray Soils Sprinkler Irrigated
Ul
DEPTH
CM
**** *
30
60
91
121
152
182
TOTAL P
HG-P/G
1981 1983
<:***********•*•*•*•*'*
T ^ ^•^^•T^T^T
AV*0.37
SD 0.13
CV 35.
AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
0.26
0,06
23.
0.25
0.07
28.
0. 17
0.07
43.
0.18
0.07
39.
0.19
0.07
40.
"^••^T»T'^*'^T
0.41
0.17
43.
0.21
0.08
39.
0.20
0.06
31.
0.13
0.09
66.
0.13
0.06
49.
0.13
0.06
49.
OPTHO P
MG-P/G
1981 1983
r********^ik**'*^*'*J
1 ^ v ^ T ^ ^ T *
.01953
.01292
66.
.02556
.03537
138.
.00951
.01232
130.
.00157
.00271
173.
.00081
.00091
112.
.00065
.00085
131.
•^•T-T'T'^'T'^^^
.00551
.00357
65.
.00517
.00869
168.
.00276
.00504
183.
.00152
.00354
233.
.00128
.00352
275.
.00127
.00353
277.
ORG. P
MG-P/G
1981 1983
* + +"+•+++•*> lit *A. ^. -4. *Ar .
r T W T T *
0.10
0.04
40.
0.11
0.06
53.
0.10
0.04
36.
0.07
0.04
57.
0.08
0.04
46.
0.08
0.04
47.
^ ^ T- -» -^ -^ *
0.05
0.03
53.
0.06
0.03
42.
0.06
0.03
51.
0.02
0.01
63.
0.02
0.01
67.
0.02
0.01
67.
ORG. C
MG-C/G
1981 1983
k *A 4 *•**•**•*• * •** i
FT* * V V ^f
6.60
1.47
22.
5.18
1. 19
23.
3.71
1.01
27.
3. 15
1.61
51.
3.18
1.60
50.
3.24
1.72
53.
• •** ^ f Jf' •T' f- *
7.27
1.30
18.
5.09
1. 12
22.
3.81
1.33
35.
1.78
0.76
43.
1.73
0.62
36.
1.65
0.71
43.
OKG. MATTER
%
1981 1983
0.38
0.09
23.
0.30
0.07
23.
0.21
0.06
29.
0. 18
0.09
52.
0. 18
0.09
51.
0. 18
0. 10
54.
1.25
0.22
18.
0. 88
0.19
22.
0.66
0.23
35.
0. 31
0. 11
35.
0. 32
0.08
24.
0. 31
0. 10
33.
            AV - Arithmetic Average
            SD - Standard Deviation
            CV - Coefficient of Variation  in  percent

-------
                                             Table E.25

                                   Minerals in Gray Soils Sprinkler Irrigated
CO
DEPTH
CM
A A A A A
T T T ^ T
30


60


91


121


152


182


r* A*A 4
'^ ^ ^ ^ ^
A?*
SD
CV
AV
SD
CV
AV
3D
CV
AV
SD
CV
AV
SD
CV
AV
SD
CV
CONDUCTIVITY
DS/H
1981
k A* * *** 4
F^^T^^^I
0.719
0.174
23.
0.779
0.281
36.
0.813
0.373
46.
1.107
0.608
55.
1.142
0.571
50.
1.204
0.587
49.
1983
k * *******
F ^ T ^ ^ ^ ^ * -T
0.435
0.093
21.
0.639
0.179
28.
0.959
o.aei
18.
1.714
1.211
71.
1.729
1.163
67.
1.813
1.096
60.
TDS
MG/G
1981
* * ** A* J
V * ^ ^ ^ ^ ^
0.60
0. 17
28.
0.53
0. 16
30.
0.66
0.23
35.
0.79
O.U7
59.
0.80
0.45
56.
0.86
0.46
53.
1983
k 4:* ***
F ^ T T * ^
0.52
0.09
17.
0.60
0.11
18.
0.73
0.28
38.
1.13
0.7U
65.
1.1U
0.71
62.
1.18
0.67
57.
PH
1981
<£ £ £4t4r4
8.17
0.17
2.
8.18
0.23
3.
7.93
0.23
3.
8.05
0.32
4.
8.11
0.28
3.
8.11
0.30
H.
1983
r dc ** * * •
* ^ ^ T T ™
7.97
0.23
3.
8.06
0.28
3.
8.10
0.29
4.
8.23
0.19
2.
8.23
0.16
?..
8.23
0.16
2.
CL
HG/G
1981
Jc *ik * **
* ^ ^ ^ ^ ^
. 059
.032
55.
.081
.061
79.
. 132
.077
58.
. 187
. 137
73.
.189
.135
72.
.207
. 135
65.
1983
* * * *4c**
W- *• T ^ * ^ *
.011
.005
49.
.035
.029
83.
. 108
.078
72.
.283
.283
100.
.287
.270
94.
.311
. 256
83.
504
MG/G
1981
* **** * *
.056
.033
59.
. 102
.079
77.
.208
.127
61.
.240
.101
42.
.221
.105
48.
.240
.101
42.
1983
r* **
.042
.009
21.
.057
.030
54.
. 156
.129
83.
.237
.199
84.
.238
.195
82.
. 252
. 185
73.
           *  AV  -  Arithmetic Average
             SD  -  Standard  Deviation
             CV  -  Coefficient of Variation in percent

-------
                               Table E.26

                   Minerals  in Gray Soils Flood Irrigated
DEPTH
CM
* *** *
^ T V T T
30
60
91
121
152
182
CONDUCTIVITY
DS/M
1981 1983
^
-------
        HETALS, TOTAL  (HC/KG)
                                                              Table E.27
                                             Metals in  Gray Soils  Flood  Irrigated
DEPTH        AL             AS          BA         B
  CH    1981     19B3     1981  1983  1981 1983  1981 1983
                                                                      CA           CD        CO         CB            CD          TL
                                                                 1981   1983   1981  1983   1981  1983   1981 1983   1981   1983   1981  1983
CO
O
30 AT*20225. 7700. 6.25 2.87
SD 2949. 2665. 1.30 1.77
CV 15. 35. 21. 62.
60 AT 21375. 8750.
SD 4315. 4029.
CT 20. 46.
91 AT 16800
SD 10185
CT 54.
121 AT 13250
SD 7005
CT 53.
152 AT 15000
SD 7203
CT 48.
182 AT 13933,
SD 7128
CT 51.
. 13200.
4101.
31.
. 15050.
1202.
8.
. 10933.
7247.
66.
8925.
3238.
36.
DEPTH Tl
CH 1981 1983
30 AT10550. 9950.
SD 772. 597.
CT 7. 6.
60 AT 63*>0.
SD 3903.
CT 47.
91 AT11500.
SD 2780.
CT 24.
121 AT 7500.
SD 4610.
CT 61.
152 AT 7900.
SD 4392.
CT 56..
182 AT 7700.
SD 4358.
CT 57.
12055.
2150.
18.
14020.
1160.
8.
12015.
6795.
57.
10990.
4665.
42.
9160.
4318.
47.
6.12 1.09
3.42 O.B3
56. 77.
7.55 2.34
3.40 0.0
45. 0.
5.62 0.0
3.66 0.0
65. 0.
6.27 0.0
2.21 0.0
35. 0.
6.73 0.50
2.05 0.0
30. 0.
PB
1981 1983
3.62 9.61
2.93 3.03
81. 32.
1.47 6.75
0.93 3.20
63. 47.
2.97 7.39
0.46 0.0
16. 0.
1.47 0.0
1.64 0.0
111. 0.
0.63 0.0
0.42 0.0
66. 0.
0.73 2.38
0.59 0.0
RO. 0.
184. 86. 601;.
46. 1. 496.
2"i. 1. 82.
180. 94.
38. 1.
21. 1.
187. 117.
34. 0.
18. 0.
249. 0.
115. 0.
46. 0.
260. 0.
27. 0.
10. 0.
233. 127.
73. 0.
32. 0.
HG
1981 1983
2350. 2198.
387. 644.
16. 29.
2625. 2583.
512. 372.
20. 14.
2575. 2780.
465. 764.
16. 27.
3450. 2054.
747. 2865.
22. 139.
3867. 3883.
666. 1661.
17. 43.
3000. 4573.
1353. 966.
45. 21.
512.
395.
77.
443.
549.
124.
493.
495.
101.
693.
144.
21.
717.
104.
15.
1981
173.
101.
59.
203.
47.
23.
166.
114.
69.
121.
99.
81.
79.
46.
58.
86.
57.
66.
*
o o o *
• • • »
»
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
1
1983
169.
177.
105.
145.
63.
44.
288.
0.
0.
0.
0.
0.
0.
0.
0.
96.
0.
0.
3500. 4561. 0.30 0.37 2.75 5.04
3189. 7595. 0.0 0.12 1.06 1.40
91. 167. 0. 32. 39. 28.
38500.
38033.
99.
44825.
66907.
149.
80375.
73482.
91.
80867.
78317.
97.
60533.
90764.
150.
14519. 0.0 0.35
20181. 0.0 0.10
139. 0. 28.
1419. 0.10 0.31
1288. 0.0 0.0
91. 0. 0.
2742. 0.0 0.0
3152. 0.0 0.0
115. 0. 0.
76517. 0.0 0.0
72076. 0.0 0.0
94. 0. 0.
194550. 0.0 1.32
109448. 0.0 0.0
56. 0. 0.
2.82 5.71
1.57 2.96
56. 52.
3.05 10.37
0.78 0.0
25. 0.
1.60 0.0
1.29 0.0
72. 0.
1.80 0.0
1.32 0.0
73. 0.
1.60 16.24
0.98 0.0
62. 0.
69.20 15.91
62.71 5.60
91. 35.
26.87 12.52
25.30 0.54
94. 4.
41.05 15.95
29.72 0.0
69. 0.
52.00 0.0
55.01 0.0
106. 0.
IS. 60 0.0
5.74 0.0
34. 0.
17.13 11.40
5.52 0.0
32. 0.
II K SE AC
1981 1983 1981 1983 1981 1983 1961 1983
>»•••«•**»*»»«»»**«»*»**»**»•**•*•»***••«*••*•***
16.0 8.6 3350. 2475. 0.0 2.3 0.13 0.46
4.6 2.7 252. 253. 0.0 2.1 0.06 0.60
29. 31. 8. 10. 0. 94. 43. 124.
12.4
7.0
56.
12.6
7.3
58.
8.8
6.2
92.
3.9
0.4
9.
5.7
3.3
59.
9.1 3550. 2668.
1.2 436. 413.
13. 12. 16.
10.1 3675. 3045.
0.0 1024. 247.
0. 28. 8.
0.0 1925. 3720.
0.0 772. 14.
0. 40. 0.
0.0 1600. 2687.
0.0 700. 1106.
0. 39. 41.
5.8 2000. 2185.
0.0 1044. 1086.
0. 52. SO.
0.0 0.9
0.0 0.3
0. 39.
0.0 0.5
0.0 0.0
0. 0.
2.2 0.0
0.0 0.0
0. 0.
0.0 0.0
0.0 0.0
0. 0.
0.0 0.5
0.0 0.0
0. 0.
0.0 0.14
0.0 0.13
0. 93.
0.0 0.07
0.0 0.0
0. 0.
0.0 3.0
0.0 0.0
0. 0.
0.0 0.0
0.0 0.0
0. 0.
0.0 0.24
0.0 0.0
0. 0.
17.02 7.62 0.2 0.0
10.88 5.37 0.0 0.0
64. 70. 0. 0.
16.37 5.90 0.2 0.0
7.20 0.80 0.0 0.0
44. 14. 0. 0.
14.00
5.90
42.
11.55
6.79
59.
12.53
1.75
14.
12.20
1.39
11.
IA
1981 1983
370. 368.
74. 66.
20. 18.
416. 420.
33. 42.
8. 10.
413. 551.
109. 98.
26. 10.
320. 501.
91. 114.
28. 23.
303. 651.
55. 417.
18. 64.
253. 512.
71. 166.
28. 33.
5.00 9.3 0.0
0.0 0.0 0.0
0. 0. 0.
J.O 0.3 0.0
0.0 0.0 0.0
0. 0. 0.
1.0 0.0 0.0
0.0 0.0 0.0
0. 0. 0.
6.41 0.0 0.0
1.0 0.0 0.0
0. 0. 0.
ZR
1981 1983
38.3 28.3
17.9 4.4
47. 15.
19.7 27.2
13.5 6.8
68. 32.
11.5 33.6
1.6 6.7
14. 20.
16.0 35.2
4.5 2.2
25. 6.
18.8 24.9
3.3 11.0
17. 44.
20.8 23.0
6.4 9.4
31. 41.
          AV - Arithmetic Average; SD - Standard Deviation; CV - Coefficient ul Viiriuliun in percent

-------
      •mis, TOTIL (NG/KG)
                   Table  E.28

Metals  in  Gray Soils  Sprinkler  Irrigated
      DEPTH        IL             IS           BA         B            en            CD         ro         C»            CO         TL
        CH    1981    1983    1981   1983   1981  1983  1981 1"»83   1981   1983   1981 1983   1981  1983   1931 1933   1981  1983  1981  1983
CD
•a*********************
30 1T*16588. 12250.
SD 3868. 2690.
CT 23. 22.
60 IT 19625. 16013.
SD 5708. 5910.
CT 29. 37.
91 IT 17838. 12400.
SD 8214. 3656.
CT 46. 29.
121 IT 9263. 8350.
3D 5181. 3364.
CT 56. 40.
152 IT 9588. 7313.
SD 5659. 3009.
CT 59. 41.
182 IT 8429. 7188.
SD 4983. 3035.
CT 59. 42.
DEPTH PE
CH 1981 1983
30 IT10038. 11496.
SD 2164. 1623.
CT 22. 14.
60 IT12263. 14231.
SD 3456. 4118.
CT 28. 29.
91 IT 9813. 11741.
SD 4576. 3342.
CT 47. 28.
121 IT 4988. 7849.
SD 3322. 5562.
CT 67. 71.
152 IT 5113. 6235.
SD 3553. 3094.
CT 69. 50.
182 IT 4257. 6074.
SD 2811. 3101.
CT 66. 51.
»*»•*»••»»•
6.60 0.0
5.11 0.0
77. 0.
6.21 0.0
4.13 0.0
66. 0.
4.06 0.0
2.78 0.0
69. 0.
3.27 0.0
3.45 0.0
105. 0.
3.35 0.0
3.45 0.0
103. 0.
3.30 0.0
3.73 0.0
113. 0.
PP
1981 1983
3.10 0.0
1.52 0.0
49. 0.
2.75 0.0
1.38 0.0
50. 0.
1.76 0.0
1.32 0.0
75. 0.
1.40 0.0
1.17 0.0
84. 0.
1.39 0.0
1. 15 0.0
83. 0.
1.10 0.0
0.87 0.0
79. 0.
178.
166.
93.
113.
37.
33.
153.
56.
36.
209.
116.
56.
207.
117.
57.
218.
122.
56.

1981
2263.
450.
20.
2588.
479.
19.
3025.
851.
28.
3238.
1497.
46.
3275.
1456.
44.
3457.
1471.
43.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
KG
1983
2484.
575.
23.
2866.
665.
23.
3185.
1061.
33.
4696.
1993.
42.
4850.
1952.
40.
4934.
,1796.
36.
236.
191.
81.
242.
265.
110.
135.
80.
60.
194.
186.
96.
195.
185.
95.
205.
197.
96.
(IV
1981
192.
45.
23.
183.
42.
23.
138.
55.
40.
91.
65.
71.
90.
61.
69.
73.
42.
57.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.

1983
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
0.
11616.
12662.
109.
19675.
19895.
101.
35063.
23613.
67.
92563.
81332.
88.
92688.
81170.
88.
105743.
78076.
74.

1981
14.9
9.6
64.
14.2
10.5
74.
13.1
8.8
67.
8.8
7.4
84.
8.7
7.6
87.
9.7
7.6
79.
9052. 0.17 0.0
15511. 0.05 0.0
171. 29. 0.
19564. 0.20 0.0
47260. 0.10 0.0
242. 50. 0.
59316. 0.20 0.0
69842. 0.0 0.0
118. 0. 0.
177100. 0.13 0.0
152858. 0.06 0.0
86. 43. 0.
206803. 0. 13 0.0
133756. 0.06 0.0
65. 43. 0.
210688. 0.13 0.0
127264. 0.06 0.0
60. 43. 0.
II K
1983 1981 1983
0.0 3313. 3126.
0.0 608. 414.
0. 18. 13.
0.0 3888. 35711.
0.0 1209. 1079.
0. 31. 30.
0.0 3305. 2931.
0.0 1601. 743.
0. 48. 25.
0.0 3119. 2214.
0.0 2492. 1127.
0. 80. 51.
0.0 3181. 1896.
0.0 2503. 918.
0. 79. »8.
0.0 3093. 1873.
0.0 2691. 922.
0. 87. «9-
3.10 0.0
1.39 0.0
45. 0.
3.15 0.0
1.32 0.0
42. 0.
2.35 0.0
0.91 0.0
39. 0.
1.79 0.0
0.49 0.0
27. 0.
1.80 0.0
0.48 0.0
27. 0.
1.80 0.0
0.52 0.0
29. 0.
SB
1981 1983
0.0 0.0
0.0 0.0
0. 0.
0.0 0.0
0.0 0.0
0. 0.
2.5 0.0
0.1 0.0
3. 0.
2.6 0.0
0.0 0.0
0. 0.
2.6 0.0
0.0 0.0
0. 0.
2.6 0.0
0.0 0.0
0. 0.
48.91 0.0
33.56 0.0
69. 0
39.25 0.0
17.85 0.0
45. 0
35.81 0.0
22.16 0.0
62. 0
25.29 0.0
22.78 0.0
90. 0
23.04 0.0
22.22 0.0
89. 0
18.90 0.0
11.98 0.0
79. 0.
1C
1981 1983
0.10 0.0
0.0 0.0
0. 0.
0.0 0.0
0.0 0.0
0. 0.
0.0 0.0
0.0 0.0
0. 0.
0.0 0.0
0.0 0.0
0. 0.
0.0 0.0
0.0 0.0
0. 0.
0.0 0.0
0.0 0.0
0. 0.
7.79
2.52
32.
9.02
2.65
29.
6.71
3.67
55.
5.59
2.97
53.
5.70
2.97
52.
5.64
3.21
57.
Ill
1981 1983
368. 313.
89. 77.
2U. 25.
460. 426.
101. 149.
22. 35.
451. 465.
86. 108.
19. 23.
338. 412.
131. 237.
39. 58.
342. 408.
131. 159.
38. 39.
340. 414.
141. 155.
41. 37.
0.0 0.4 0.0
0.0 0.1 0.0
0. 25. 0.
0.0 0.4 0.0
0.0 0.1 0.0
0. 25. 0.
0.0 0.4 0.0
3.0 0.2 0.0
0. 35. 0.
8.0 0.3 0.0
0.0 0.1 0.0
0. 17. 0.
0.0 0.3 0.0
0.0 0.1 0.0
0. 17. 0.
0.0 0.3 0.0
0.0 0.1 0.0
0. 20. 0.
II
19S1 1963
24.6 37.2
3.1 9.3
13. 25.
33.5 46.7
16.0 20.0
48. 43.
22.5 42.2
5.7 15.5
25. 37.
16.1 34.6
4.8 13.6
30. 39.
16.4 32.0
5.3 13.3
33. 41.
14.8 33.5
3.4 13.2
23. 39.
         * AV - Arithmetic Average; SD - Standard Deviation; LV - L'oefliciunt of Variation in |iun-nnl

-------
                                Table E.29
            Priority Organics  in  Flood Irrigated  Gray Soils
1981
1983
1981
1983
Deoth
30

60


91


121


152


182


30


60


91


121


152


182


Death
cm
30


60


91


121


152


182


30


60


91


121


152


182


AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SO
AV
FR
SO
AV
FR
SO
AV
FR
SD
AV
FR
SO

AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
FR
SD
Prooazine a-terpineol Tetracnloroethylene Toluene Trichloroethane Trichloroethy.
<100.0 <10.0 <1.0 <1.0 <1.0 <1.0

<100.0


137.25
1/4
(74.50)
<100.0


<100.0


<100.0


<100.0


<100.0


<100.0


<100.0


<100.0


<100.0


Acenaphthylene
<20.0


45.75
1/4
(51.50)
21.88
1/4
(3.75)
26.90
1/4

<20.0


<20.0


21.13
1/4
(2.25)
24.70
1/4
(9.40)
<20.0


<20.0


<20.0


<20.0



<10.0


17.60
1/4
(15.20)
<10.0


220.75
1/4

291.00
1/4
(486.71)
11.05
1/4
(2.10)
<10.0


<10.0


<10.0


<10.0


<10.0


Anthracene
<20.0


<20.0


<20.0


<20.0


33.10
1/4
(26.2)
33.10
1/4
(26.2)
<20.0


<20.0


<20.0


<20.0


<20.0


<20.0



<1 .0


<1 .0


<1.0


<1 .0


<1 .0


2.88
4/4
(0.82)
2.80
4/4
(1.04)
6.38
4/4
(7.90)
6.43
4/4
(7.86)
2.43
3/4
(1.40)
2.37
2/4
(1.35)
Atrazine
<100.


<100.


141.75
1/4
(03.50)
<100.


<100.


<100.


<100.


<100.


<100.


<100.


<100.


<100.




































Benzene
11.50
4/4
(8.79)
11.48
3/4
(8.71)
5.48
4/4
(1,15)
4.83
4/4
(2.05)
2.20
3/4
(0.92)
2.10
3/4
(1.05)
2.03
4/4
(0.81)
3.73
4/4
(3.12)
1.08
2/4
(0.15)
1.13
2/4
(0.24)
1.43
1/4
(0.85)
1.08
2/4
(0.10)

1.75 <1.0
1/4
(1.50)
<1 .0 <1.0


<1.0 <1.0


<1.0 <1.0


<1.0 <1.0


<1.0 <1.0


<1.0 <1.0


<1.0 <1.0


<1 .0 <1 .0


<1.0 <1.0


<1.0 <1.0


4-t-butylphenoI
<10.0


<10.0


<10.0


<10.0


28.43
1/4
(31.93)
28.43
1/4
(31.93)
<10.0


<10.0


<10.0


<10.0


<10.0


<10.0



<1.0


<1 .0


<1.0


<1 .0


<1 .0


<1.0'


<1 .0


<1 .0


<1.0


<1.0


<1 .0


Carbon tetrachloride
<1 .0


<1 _Q


<1 .0


<1 .0


<1 .0


<1 .0


3.05
4/4
(1.16)
2.87
3/4
(2.11)
2.65
4/4
(0.97)
2.68
4/4
(1.57)
2.17
3/4
(0.93)
2.33
3/4
(1.29)
                                   582

-------
Table  E.29,  continued
       1981    Deoth       4-chloroaniline   Chlorobenzene   Lniorororm   i-cniorupnenui   1-chlorotetradecane
                                                                                              <20.0



                                                                                              <20.0


                                                                                              <20.0


                                                                                              <2D.O


                                                                                              <20.0


                                                                                              <20.0




        1983    30     AV      <100.            <-LU           ^"          ~	               ^'05

                                                                                              (28.79)
                                                                                               33.08
                                                                                               1/4
                                                                                              (27.70)
                                                                                               <20.0


                                                                                               <2Q.O


                                                                                               <20.0


                                                                                               <20.0
teeth
Cm
30

60


91


121


152


182


30


60


91


121


152

182


°cT3th.
30


60


91


121


152


182


30


60


91


121


152


182



AV
FR
SO
AV
FR
SO
AV
FR
SO
AV
FR

AV
FR
en
JU
AV
FR
SO
AV
FR

AV
FH
SO
AV
FR
en
of
AV

FR
SO
AV
FR
SO
AV
FH
SD

AV
FR
SO
AV
FR
SO
AV
FR
SO
AV
FH
SO
AV
FR
SO
AV
FR
SO
AV
FR
SO
AV
FR
SO
AV
FR
SO
AV
FR
SO
AV
FR
SO
AV
FR
SO
4-chloroanil ins
<100.

112.75
1/4
(25.50)
<100.


<100.


<100.


<100.


<100.


<100.


<1UO.


<100.


<100.

<100.


Dibutylphthalate
91.75
2/4
(91.83)
49.50
1/4
(59.00)
34.65
2/4
(17.16)
63.58
2/4
(64.72)
66.40
3/4
(25.25)
63.57
2/4
(39.H6)
41.75
1/4
(43.50)
34.48
1/4
(28.95)
<20.0


35.23
1/4
(30.45)
28.60
1/4
(14.89)
28.40
1/4
(14.55)
Chlorobenzene
<1.0

5.60
1/4
(9.20)
<1.0


<1.0


<1.0


<1.0


<1.0


<1.0


<1.0


<1.0


<1.0

<1.0


Chloroform
17.90
2/4
(20.22)
14.73
2/4
(11.97)
5.48
3/4
(4.96)
9.43
3/4
(7.56)
11.47
3/4
(7.47)
8.17
2/4
(9.70)
24.95
2/4
(36.62)
41.12-
3/4
(69.69)
137.75
2/4
(212.60)
130.63
2/4
(214.84)
157.68
1/4
(271.35)
1.93
1/4
(1.62)

2-chlorophenol
35.50
1/4
(51.00)
<10.0


<1D.O


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.U


<10.0

<10.0


2,3-dichloroaniline 3,4-dichloroaniline
<20.0


36.15
1/4
(32.30)
35.83
1/4
(31.65)
<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


20.2
1/4
(0.40)
<20.0


<20.0






































<20.0


71.25
2/4
(88.44)
32.90
1/4
(25.95)
<20.0


<20.0


<20.0


33.38
2/4
(20.52)
<20.0


<20.0


<20.0


<20.0


<20.0


        1981   °gBth^      Dibutylphthalate   2,3-dichloroaniline   3,4-dichloroaniline   Dichlorobenzene M

                                                                                            20.93
                                                                                            1/4
                                                                                           (21.85)
                                                                                           <10.0



                                                                                           <10.0



                                                                                           <10.0



                                                                                           <10.0



                                                                                           <1U.U
       1983    30     AV         41.75            <20.0                   33.38               <10.0


                                                                                           <10.0


                                                                                           <10.0


                                                                                           <10.0


                                                                                           <10.0


                                                                                           <10.0




                                                        583

-------
  Table  E.29. continued
1981
1983
 1981
 1983
De th
30
60
91
121
152

182


30

60

91


121


152


182


Depth
cm
30 -


60


91


121


152


182

30


60


91


121


152


182



AV
FR
SD
AV
FH
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD

AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SO
AV
FR
SO
AV
FH
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SO
Dichlorobenzene P
16.75
1/4
(13.50)
22.25
1/4
(24.50)
<10.0
18.13
1/4
(16.25)
<10.0

<10.0


11.1
1/4
(2.20)
<10.0

<10.0


10.15
1/4
(0.30)
11.43
1/4
(2.48)
<10.0


Dioctylphthalate
364.23
3/4
(339.90)
170.03
4/4
(110.03)
64.05
4/4
(54.04)
64.4
2/4
(24.89)
486. U
1/4
(0)
486.0
1/4
(0)
NR


NR


NR


NR


NR


NR


Dichlorobenzene 0 2,4-d
15.58
1/4
(11.15)
36.75
1/4
(53.50)
87.25
1/4
(154.50)
<10.0
<10.0

<10.0


<10.0

<10.0

<10.0


<10.0


<10.0


<10.0


Ethyl benzene
3.05
2/4
(2.42)
3.58
1/4
(4.15)
2.33
1/4
(1.65)
3.03
1/4
(3.74)
<1.5


<1.5

<1.5


<1.5


<1.5


<1.5


<1.5


<1.5


























lichlorophenol Diethylphth;
<30.0 <20.0
<30.0 78.5
1/4
(82.73)
65.75 25.30
1/4 1/4
(71.50) (7.50)
47.75 <20.0
1/4
(35.50)
<30.0 <20.0

<30.0 <20.0


<30.0 <20.0

<30.0 <20.Q

<30.0 52.25
1/4
(64.50)

<30.0 35.53
1/4
(31.05)
<30.0 <20.0


<30.0 <20.0


Heptadecane Methylheptadecanoate
38.75
1/4
(57.50)
12.13
1/4
(4.25)
<10.0


12.25
1/4
(4.50)
<10.0


<10.0

17.53
2/4
(8.71)
15.15
1/4
(10.30)
<10.0


<10.0


<10.0


<10.0


44.18
2/4
(39.74)
<20.0


110.65
2/4
(176.92)
27.55
1/4
(15.10)
<20.0


97.33
1/4
(133.95)
23.45
1/4
(6.90)
40.75
1/4
(41.50)
<20.0


<20.0


<20.0


<20.0


alate uiisooctyipni
347.3
3/4
(267.4)
277.0
4/4
(177.3)
229.75
4/4
(283.70)
383.00
3/4
(103.50)
1814.6
2/4
(2506.5)
1262.1
3/4
(2U13.4)

NH

NR

NR


NR


NR


NR


Methylhexadecanoate
22.43
1/4
(4.85)
1130.25
3/4
(1258.4)
663.43
2/4
(1281/1)
<20.0


<20.0


<20.0

<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


                                      584

-------
Table E.29,  continued
cm
30


60


91


121


152


182


1983 30


60

91

121

152

182



AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FH
SD
AV
FH
SD
AV
FH
SD
AV
FR
SD
AV
FH
SD
AV
FR
SD
AV
FR
SD
AV
FH
SD
AV
FR
SD

<10.0


55. 2B
3/4
(54.31)
<10.0


<10,0


<10.0


<10.0


13.98
2/4
(7.75)
<1Q.Q

<10.0

<10.0

<10.0

<10.0



62.23
2/4
(61.36)
56.50
174
(93.00)
14.25
1/4
(a. so)
43.75
1/4
(67.50)
<10.UU


30.47
1/4
(35.45)
<10.00


<10.00

<1U.UU

<10.00


-------
                    Table E.30
Priority Organics in Sprinkler Irrigated Gray Soils
1981
















1983

















1981













1983








Death
cm
30


60


91

121

152


182


30


60


91


121


152


182


"SB01
•30

60

91

121

152

182


30
60
91

121
152

182


AV *
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FH
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD

AV
FR
SD
AV
F R
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
ru
r n
SD
AV
FR
SD
AV
FR
SO
AV
FR

SD
AV
FR
SO
AV
FR
SD
AV
FR
SD
Acanaphthylene
24.76
1/7
(12.59)
<20.0


<20.0

<20.0

<20.0


<20.0


38.91
2/7
(33.27)
<20.0


<20.0


<20.0


<20.0


<20.0


4-chl'oroaniline
<100.

<100.

<100.

<100.

<100.

<100.


<100.
<100.
<100.

<100.
<100.

<100.

Anthracene Atrazine Benzene
<20.00 <100. 9.76
' 7/7
(7.51)
<20.0 <100. 5.40
6/7
(5.25)
<20.0 <1UO. 7.16
7/7
(2.75)
<20.0 <100. 3.46
7/7
(1.64)
<20.Q <1GO. 3.03
7/7
(1.07)
<20.0 <100. 3.03
6/7
(1.07)
<2U.U <10U. 1.U3
b/7
(1.06)
<20.0 <100. 1.27
4/7
(0.44)
<20.0 <1DO. 1.27
5/7
(0.36)
<20.0 <100. 1.04
6/7
(0.08)
<20.0 <100. 1.04
6/7
(0.08)
<20.0 <100. 1.04
6/7
(O.OB)
4-t-butylphenol
15.48
1/7
(14.48)
<10.0


<10.0

13.29
1/7
(8.69)
13.29
1/7
(8.69)
13.29
1/7
(H. 69)
<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


Carbon tetracl
<1.0


1.06
1/7
(0.15)
<1.0

<1.0

<1 .0


<1 .0


3.94
7/7
(1.88)
2.67
6/7
(1.21)
2.86
7/7
(0.42)
2.49
6/7
(0.92)
2.57
6/7
(0.95)
2.44
6/7
(0.80)
Chlorobenzene Chloroform . 2-chlorophenol 1-chlorotetradecanc
<1.0 23.39
5/7
(21.78)
<1-0 26.54
5/7
(28.19)
<1.0 30.74
5/7
(51.60)
<1.0 5.23
3/7
(5.95)
<1.0 7.78
3/7
(10.00)
<1.0 7.78
3/7
(10.00)
<1-0 1.50
2/7
(0.91)
<1-0 1.07
2/7
(0.15)
<1.0 1.Q9
2/7
(0.19)
<1-0 < 1.0

<1.0
<1-Q < 1.0
586
13.93
1/7
(10.39)
15.51
1/7
(14.59)
<10.0

12.86
1/7
(7.56)
12.86
1/7
(7.56)
12.86
1/7
(7.56)
30.71
1/7
(75.97)
<10.0
<10.0

<10.0

<10.0
<10.0

21.23
1/7
(3.25)
<20.0

<20.0

<20.0

<20.0

<20.0


80.34
4/7
(12.95)
92.74
2/7
(158.1)
<20.0

<20.0

<20.0
<20.0


-------
 Table  E.30,  continued
1981
1983
 1981
 1983
Ctegth Dibutylphthalate 2,3-dichloroaniline
30


60


91


121


152


182


30


60


91


121


152


182


Death
cm
30


60


91


121


152


182


30


60


91


121


152

182


AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
FR
SO
AV
FR
SO
AV
FH
SD
AV
FH
SD
AV
FR
SD
AV
FR
SO
AV
FR
SD
AV
n V
rp
T n
SD

AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FH
SO
AV
FK
SD
AV
FH
SO
AV
FH
SO
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FK
SD
51.31
2/7
(69.69)
<20.0


S20.0


<20.0


<20.0


<20.0


134.71
2/7
(231.77)
36.14
2/7
(31.03)
<20.0


28.97
3/7
(11.66)
26.90
2/7
(11.79)
26.90
2/7
(11.79)
Dichlorobenzene P
14.69
2/7
(10.32)
13.67
2/7
(10.58)
<10.0


<1U.O


<10.0


<10.0


<10.0


<10.0


<10.0


10.66
1/7
(1.74)
10.66
1/7
(1.74)
10.66
1/7
(1.74)
22.23
1/7
(5.90)
<20.0


<20.0


24.60
2/7

25.31
2/7-
(9.16)
22.75
1/7
(6.74)
27.39
1/7
(20.00)
40.04
2/7
(47.82)
23.57
1/7
(9.45)
37.77
3/7
(24.52)
37.77
3/7
(24.52)
37.77
3/7
(24.52)
Dichlorobenzene 0
21.81
2/7
(20.55)
24.74
3/7
(31.60)
17.53
1/7
(19.92)
<10.U


<10.0


<10.0


<10.0


<10.0


<10.0


11.46
1/7
(3.86)
11.46
1/7
(3.86)
11.46
1/7
(3.86)
3 , 4-dichloroaniline
<20.0


<20.0


<20.0


<20.0


<20.0


<20.0


26.09
1/7
(16.10)
<20.0


<20.0


<20.0


<20.0


22.57
1/7
(6.80)
2 , 4-dichlorophenol
37.39
1/7
(19.54)
34.60
1/7
(12.17)
<30.0


39.93
1/7
(26.27)
39.93
1/7
(26.27)
39.93
1/7
(26.27)
<30.0


<30.0


<30.0


49.14
1/7
(50.65)
49.14
1/7
(50.65)
49.14
1/7
(5U.65)
Dichlorobenzene M
17.41
3/7
(13.18)
14.71
2/7
(11 .00)
<10.0


<10.0


<10.0


•OO.U


25.73
4/7
(14.85)
13.21
2/7
(7.58)
<10.l)


11 .07
1/7
(2.84)
11 .07
1/7
(2.84)
11.07
1/7
(2.84)
Diethylphthalate
254.0
1/7
(0)
227.0
1/7
(0)
66.00
1/7
(fi'j.M'j)
61.67
1/7
(72.17)
61.67
1/7
(72.17)
61.67
1/7
(72.17)
21.50
1/7
(3.97)
105.00
5/7
(96.92)
38.71
1/7
(49.51)
93.43
6/7
(89.47)
89.00
6/7
(87.10)
90.43
6/7
(U7.74)
Diisooctylphthalate
     1291.0
     7/7
    (2467.)
     302.43
     7/7
    (254.4)
     348.29
     7/7
    (2112.1)
     1099.2
     6/7
    (2010.6)
     1112.8
     6/7
    (2002.8)
     1295.8
     5/7
    (21U2.5)

    <20.0


    <20.0


    <20.0


    <20.0


    <20.0


    <20.0
                                                  587

-------
Table E.30,  continued
1981


















1983














1981



















1983















Ofgth
30


60


91


121


152


182


30

60


91


-121


152


182
Death
cm
30


60


91


121


152


182


30

60

91


121


152


182



AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FH
SO
AV
FR
SO
AV
FR
SD
AV
FR
SD
AV
FR
SD

AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FH
SD
AV
FR
SD
AV
FR
SO
AV
FH
SD
AV
FH
en
jU
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SO
Dioctylphthalate E
46.17
3/7
(37.18)
46.7
2/7
(20.00)
66.43
3/7
(26.00)
162.9
3/7
(135.7)
137. B
4/7
(121.6)
248.0
3/7
(119.5)
<20.0

<20.0


<20.0


<20.0


<20.0


<20.0
1-methylnaphthalene

<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0

<10.0

<10.0


<10.0


<10.0


<10.0


thyl benzene H
2.97
2/7
(3.76)
<1.5


<1.5


<1.5


<1.5


<1.5


1.90
1/7
(1.06)
1.63
1/7
(0.34)
<1.5


<1.5


<1.5


<1.5
2-fliethylphenol

<10.0


34.19
3/7
(39.40)
21.71
2/7
(27.71)
11.63
1/7
(4.31)
11.63
1/7
(4.31)
11.63
1/7
(4.31)
<10.0

<10.0

<10.H


<10.0


<10.0


<10.0


leptadecane Methylheptadecanoati
34.00 25.99
3/7 2/7
(10.00) (11.43)
<10.0 39.86
1/7
(52.54)
<10.0 26.57
1/7
(17.39)
13.00 <20.0
1/7
(7.90)
15.21 <20.0
2/7
(9.02)
13.48 <20.0
1/7
(8.53).
10.90 67.14
2/7 2/7
(1.95) (115.7)
<10.0 <20.0


<10.0 <20.0


11.11 <20.0
1/7
(2.95)
11.11 <20.0
1/7
(2.95)
11.11 <20.0
1/7
( f QC. i
I, L . yj 1
4-methylphenol Napthalane

<20.0 <10.0


<20.0 25.00
1/7
(39.69)
<20.0 14.57
1/7
(12.13)
<20.0 <10.0


<20.0 <1U.O


<20.0 <10.0


<20.0 <10.0

24-14 11.58
1/7 1/7
(10.96) (4.16)
<20.0 <1U.O


<20.0 <10.0


<20.0 <10.0


<20.0 <10.0


2 Methylhexadecanoal
20.63
1/7
(1.66)
<20.0


20.46
1/7
(1.21)
<20.0


<20.0


<20.0


24.07
1/7
(10.77)
<20.0


<20.0


<20.0


<20.0


<20.0
Octadecane Phenol

<20.0 100.57
1/7
(1.51)
<20.0 <100.


<20.0 103. 2B
1/7
(8.70)
<20.0 <100.


<20.0 <1UU.


<20.0 <100.


<20.0 108.57
1/7
(22.68)
<20.0 126.71
1/7
(70.6U)
<20.0 <100.


<20.0 <100.


<20.0 <100.


<2U.O <100.


                                 588

-------
   Table E.30,  continued



1981    Dcfnth       Propazine   4-terpineol   Tetrachloroethylene   Toluene   Tricnioroecnane   Trichloroethylene
1983
30


60


91


121


152


182


30


60


91


121


152


182
AV
FR
SD
AV
FH
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
AV
FR
SD
<100.


<100.


<100.


<1UO.


<100.


<100.


<1QO.


<100.


<100.


<100.


<100.


<100.
<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0


<10.0
<1.0


1.B3
1/7
(2.19)
<1 .0


<1 .0


<1 .0


<1 .0


2.U7
7/7
(1.37)
2.23
5/7
(1.1H)
2.10
7/7
(0.46)
2.07
6/7
(O.BO)
2.14
6/7
(o.ao)
2.17
6/7
(0.80)
<1.0


<1.0


<1.0


<1.0


<1.0


<1.0


<1.0


<1.0


<1 .0


<1.0


<1.0


<1.0
<1.0


1.13
1/7
(0.34)
<1.0


<1.U


<1 .0


<1.0


<\ .0


<1.0


<1 .0


<1.0


<1.0



-------
MD
O
                                          Table t.?t
                      Microbiological Data for Flood Irrigated Gray Soils
                                        (CFO/cj soil   )

                                                   Fecal Strep     Actinomycetea      Fungi
                                                      2155            1.7 x 10"        1.1 x 10s
                                                      (184)           (1.4 x 10")      (1.0 x 105)
                                                      1/4             4/4              3/4
                                                      2250            4.2 x 10"        2.0 x 10*
                                                      (170)           (5.8 x 10'')      (2.3 x 10*)
                                                      1/4             4/4              2/4
                                                     <2360            5.4 x 10"^       3.5 x 10"
                                                      (0)             (5.8 x 10")      (5.2 x 10")
                                                      0/4             4/4              3/4
                                                     <2400            5.6 x 10"J       9.6 x 10s
                                                      (0)             (5.9 x 10")      (1.1 x 10*)
                                                      0/4             4/4              2/4
                                                      2127            3.3 x 10'"        9.9 x 10s
                                                      (219)           (1.2 x 10'°)      (1.7 x 10")
                                                      1/3             3/3              1/3
                                                      2127            3.0 x 1010        9.9 x 10°
                                                      (219)           (1.7 x 10'°)      (1.7 x 10*)
                                                      1/3             3/3              1/3

                                                      18             2.2 x 10U        1.1 x 105
                                                      (27,900)       (4.3 x 10")      (1.4 x 10s)
                                                      3/4             4/4              4/4
                                                      11,500         4.0 x 10'°        3.1 x 10'
                                                      (18,500)       (1.2 x 101")      (2.1 x 10*)
                                                      1/4             4/4              4/4
                                                      3823            5.3 x 1010        8.6 x 103
                                                      (3006)         (3.5 x 10'°)      (1.0 x 10*)
                                                      1/4             4/4              4/4
                                                      4337            5.6 x 101"        5.8 x 10*
                                                      (3459)         (4.9 x 101")      (5.0 x 10*)
                                                      1/3             3/3              3/3
                                                     <2240            4.5 x 10l°        2.3 x 10*
                                                      (0)             (3.2 x 101")      (3.1 x 10*)
                                                      0/2             2/2              2/2
                                                     <2260            3.4 x 10"        1.3 x 10*
                                                      (0)             (3.4 x 10W)      (1.4 x 10*)
                                                      0/2             2/2              2/2

* AV - Arithmetic Average
  SD - Standard Deviation
  FR - Frequency of Detection of organisms at concentration
       Greater than analytical detection limit
1981 Defltl
30


60


91


121


152


182


1983 30


60


91


121


152


182


h
AV *
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
Total Coliform
23,300
(37,300)
4/4
<2320
(0)
0/4
<2360
(0)
0/4
4195
(3874)
1/4
3317
(2281)
1/3
3317
(2281)
1/3
495,000
(971,000)
2/4
162,000
(320,000)
1/4
11,600
(18,500)
1/4
14,600
(21,300)
1/3
94,600
(131,000)
1/2
<2260
(0)
0/2
Fecal Coliform
5360
(4857)
2/4
<2320
(0)
0/4
<2360
(0)
0/4
<2400
(0)
0/4
<2380
(0)
0/3
<2380
(0)
0/3
8040
(11,700)
1/4
3783
(3032)
1/4
2335
(66)
1/4
2343
(55)
1/3
<2240
(0)
0/2
<2260
(0)
0/2

-------
1981 De^th
30


60


91


121


152


182


1983 30


60


91


121


152


182


i
AV*
50
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FH
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
AV
SD
FR
Total Coliform
7860
(14,800)
1/7
<2400
(0)
0/7
<2380
(0)
0/7
<2400
(0)
0/7
<2400
(0)
0/7
<2400
(0)
0/6
11,500
(18,800).
5/7
10,100
(20,800)
2/7
<2340
(0)
0/7
<2340
(0)
0/7
<2340
(0)
0/7
<2340
(0)
0/7
                                          Table  E.32

                   Microbiological Data  for Sprinkler  Irrigated  Gray  Soils
                                       (CFU/g soildwt)

                               Fecal Coliform     Fecal Strep
                                   4081
                                   (4793)
                                   1/7
                                  <2400
                                   (0)
                                   0/7
                                  <2380
                                   (0)
                                   0/7
                                  <2400
                                   (0)
                                   0/7
                                  <2400
                                   (0)
                                   0/7
                                  <2400
                                   (0)
                                   0/6

                                   2240
                                   (26)
                                   2/7
                                   2200
                                   (59)
                                   1/7
                                  <2340
                                   (0)
                                   0/7
                                  <2340
                                   (0)
                                   0/7
                                  <2340
                                   (0)
                                   0/7
                                  <2340
                                   (0)
                                   0/7
<2360
 (0)
 0/7
<2400
 (0)
 0/7
<2380
 (0)
 0/7
<2400
 (0)
 0/7
<2400
 (0)
 0/7
<2400
 (0)
 0/6

 54,600
 (66,800)
 6/7
 7219
 (6947)
 6/7
 22,800
 (34,700)
 3/7
 3070
 (2259)
 2/7
 3033
 (2275)
 3/7
 3039
 (2273)
 2/7
Actinomycetes
1.0 x 10U
(1.3 x 10U)
7/7
8.8 x 10"
(1.3 x 10U)
7/7
2.7 x 10
(3.2-x 10")
7/7
4.3 x 10"
(3.5 x 10")
7/7
4.5 x 10
(3.7 x 10 a)
7/7
3.8 x 10"
(3.4 x 10")
6/6
6.5 x 10U
(7.2 x 1012)
7/7
3.9 x 10"
(8.5 x 10")
7/7
6.8 x 10
(4.1 x 10'")
7/7
3.8 x 10
(4.5 x 10'°)
7/7
4.1 x 10'°
(4.8 x 101")
7/7
4.1 x 10"
(9.8 x 10")
7/7
Fungi
3.3 x 10*
(4.4 x 10*)
7/7
4.7 x 10"
(8.1 x 10*)
7/7
3.9 x 10
(8.5 x 10*)
7/7
2.8 x 10
(3.9 x 10")
6/6
2.8 x 10"
(3.6 x 10*)
7/7
2.8 x 10"
(3.9 x 10*)
6/6
8.8 x 10*
(7.0 x 10*)
7/7
2.4 x 10"
(2.7 x 10*)
7/7
2.6 < 10
(2.4 x 10*)
7/7'
3.6 x 10*
(8.6 x 10")
7/7
4.5 x 10
(4.4 x 10S)
7/7
4.6 x 10
(4.7 x 103)
7/7
* AV - Arithmetic Average
  SD - Standard Deviation
  FR - Frequency of Detection of organisms al  concentration
       Greater than analytical detection limit

-------
                                                           42.2
                                                                                                   52.2 on
                                                                                                                                           68.90
MD
K3
Priority Detection Calculated Calculated Calculated
Organic limits Haae Applied Concentration Haas Applied Concentration Haaa Applied Concentration
Compound Concentration (q/ha) In 30 tn of Soil !g/he) In 30 on of Soil Cg/ha) In 30 cm of Soil
(ppb)
Acenephthylene <20
Anthrecene/penathrene <20
Atrezlne <100
Benzene <1
4-t-butylphenol <10
Carbon Tetrechlorlde <1
4-chloroenlllne <100
Chlorobenzene <1
Chloroform <1
2-chlorophenol <10
1 -chlorotetradecene <20
Olbutylphatehalata <20
2,3-dichloroenlllne <20
3,4-dlchloroenlline <20
Oichlorobenzene M <10
F <10
0 OO
2,4-dlchlorophenol et«nce

-------
              APPENDIX F




Crop Characterization Data and Figures
                  593

-------
                         Table F.1
Hydraulic Pivot
Loading Mo.
1
3
7
42.2 cm 8
10
14
16
17
19
20
21
22

2
9
52.2 cm 11
12
13
18

4
5
68.9 cm
6
15


Area
:na)
22.7
29.8
38.9
21 .2
56.1
50.3
53.0
55.5
35.5
42.5
40.0
15.4
z 470.9
30.2
50.5-
53.8
24.4
48.9
55.5
I 263.3
57.5
51.4
24.5
26.1
I 159.7
1982
Crop
Mi 1.0
Oats
Milo
Sunflowers
Milo
Milo
Milo
Sun flowers
Milo
Milo
Milo
Milo
Wt . Av .
Soybeans
Milo
Soybeans
Milo
Milo
Soybeans
Wt. Av.
Soybeans
Milo
Oats
Soybeans
Wt . Av .

kg/ha
Uptake
-116
75
112
*70
84
33
•75
»75
-136
111
53
110
32.6
256
75
196
89
67
173
141.0
254
131
*87
267
190.7

Area
Cha)
22.7
29.8
38.9
42.5
56.1
60.3
53.0
27.7
71.0
42.5
40.0
15.4
£ 499.9
30.2
50.5
53.8
48.9
48.9
55.5
I 287.8
57.5
25.7
24.7
26.1
I 134.0

Crop
Cotton
Oats
Milo
Cotton
Cotton
Cotton
Milo
Milo
Cotton
Cotton
Cotton
Cotton
Wt . Av .
Cotton
Milo
Cotton
Cotton
Cotton
Cotton
Wt . Av .
Wheat -H
Milo
Wheat +
Milo
Oats +
Milo
Oats +
Milo
Wt. Av.

kg/ ha
Uptake
*75
69
152
56
65
*75
110
101
57
46
82
68
78.4
45
145
84
72
63
39
76.4
*72 +
104 -
107 +
42 +
214.0


















120
«• 99
173
169

Estimation of Nitrogen based on A * L Laboratory's Soil and Plant Analysis Handbook

                          Table F.2
  Percentage of  Organic-N  in Plants  Harvested in 1982
                Incorporated into the  Soil
Hydraulic Loading
(cm)

42.2

52.2


68.9

Crop
Milo
Oats
Sunflowers
Soybeans
Milo
Soybeans
Milo
Oats
Percent N
Returned to Soil
50
33
50
24
50
24
50
33
in Plant
After Harvest








                               594

-------
                 Table F.3
Phosphorus Uptake by Crops on Hancock Farm
Hydraulic
Loading Pivot
(cm) NO.
1
3
~
a
10
42.2 14
16
17
19
20
21
22
2
9
52.2 11
12
13
• 18
4
68.9 5
6
15
Area
'ha)
22.7
29.8
38.9
21.2
56.1
60.3
53.0
55.5
35.5
42.5
40.0
15.4
30.2
50.5
53.8
24.4
48.9
55.5
57.5
51.4
24.7
26.1
1982
Crop
Milo
Oats
Milo
Sunflowers
Milo
Milo
Milo
Sunflowers
Milo
Milo
Milo
Milo
Soybeans
Milo
Soybeans
Milo
Milo
Soybeans
Soybeans
Milo
Oats
Soybeans
Uotake
(kg/ha)
40.1
12.2
37.4
35.7
29.6
11.3 -
25.7
47.7
47.0
43.6
34.2
37.6
62.2
23.3
55.8
37.7
29.2 .
43.2
56.8
46.3
15.0
59.2
Area
(ha)
22.7
29.8
38.9
42.5
56.1
69.3
53.0
27.7
71.0
42.5
40.0
15.4
30.2
50.5
53.8
24.4
48.9
55.5
57.5
51.4
24.7
26.1
1983
Crop
Cotton
Oats
Milo
Cotton
Cotton
Cotton
Milo
Milo
Cotton
Cotton
Cotton
Cotton
Cotton
Milo
Cotton
Cotton
Cotton
Cotton
Wheat +
Milo
Wheat +
Milo
Oats 1-
Milo
Oats -r
Milo
Uptake
^kg/ha)
' 5.4
10.2
19.7
7.2
11.3
6.7
17.5
13.2
8.7
6.6
10.8
3. 5
7.2
19.5
10.7
9.7
10.5
5.3
26.4
28.3
36.9
20.4
                       595

-------
           Table F.4

Potassium Uptake by Crops Grown
      on the Hancock Farm
Hydraulic Pivot
Loading No.
1
3
7
a
10
42.2 cm 14
16
17
19
20
21
22

2
9
52.2 11
12
13
18

4

5
63.9 on
6

15



Area
.'ha)
22.7
29.8
38.9
21.2
56.1
60.3
53.0
55.5
35.5
42.5
40.0
15.4
470.9
30.2
50.5
53.3
24.4
48.9
55.5
263.3
57.5

51.4

24.7

26.1

159.7
1982
Crop
Milo
Oats
Milo
Sunflowers
Milo
Milo
Milo
Sunflowers
Milo
Milo
Milo
Milo
Wt . Av .
Soybeans
Milo
Soybeans
Milo
Milo
Soybeans
Wt . Av .
Soybeans

Milo

Oats

Soybeans

Wt. Av.

Uptake
140.8
186.8
116.3
87.8
104.2
39.8
108.8
117.7
165.3
152.9
119.9
132.0
107.0
167.9
76.6
167.4
132.4
102.8
116.6
124.1
153.2

158.7

173.3

159.8

159.2

Area
22.7
29.8
38.9
42.5
56.1
60.3
53.0
27.7
71.0
42.5
40.0
15.4
449.9
30.2
50.5
53.3
24.4
48.9
55.5
263.3
57.5

51.4

24.7

26.1

159.7
I983
Crop
Cotton
Oats
Milo
Cotton
Cotton
Cotton
Milo
Milo
Cotton
Cotton
Cotton
Cotton
Wt. Av.
Cotton
Milo
Cotton
Cotton
Cotton
Cotton
Wt. Av.
Wheat +
Milo
Wheat 4-
Milo
Oats +
Milo
Oats +
Milo
Wt. Av.

Uptake
(kg/ha)
6.6
186.8
112.4
19.0
39.7
14.6
77.6
64.8
13.3
14.3
17.9
14.0
44.8
10.9
91.5
42.4
16.0
15.5
12.2
34.4
169.5 +

279.9 +

173.8 +

101.9 +

262.5


















77.3

61.4

74.0

53.8


               596

-------
                             Table  F.5
            Cotton Plant Analysis, Stalk  and Seed
                              (mg/g)
Pivot
No . Date
1
2
3
5
6
a
10
11
12
13
14
15
18
19
20
21
22
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
1981
1983
Referenced
Average**
TKN
Stalk Seed
18,240
9,610
13,500
2,390
12,600
4,600
18,040
5,050
14,850
3,760
13,350
6,330
13,650
2,360
15,900
3,670
17,250
7,650
16,050
4,670
8,640
12,000
12,600
10,140
15,600
7,690
13,650
6,490
18,150
7,680
16,350
8,880
14,400
5,880
»*#
33,000
46,610
31,280
8,680
34,140
40,500
30,300
33,900
34,950
34,500
32,700
34,500
33,460
32,850
33,210
45,000
35,920
35,850
38,290
29,100
30,550
45,000
39,640
35,250
33,070
33,750
37,670
34,800
35,800
34,050
33,540
47,700
36,450
34,050
35,850
40,000
Stalk
2,760
840
1,120
990
1,110
1,040
1,830
870
2,060
920
2,190
750
2,160
1,100
1,690
940
2,350
1,070
1,520
880
2,930
1,440
1,770
1,110
2,020
1,120
1,470
790
2,550
950
2,470
990
2,060
880
2,400
IP
Seed
11,300
5,200
4,980
6,620
5,200
5,960
9,320
6,420
5,940
6,440
6,210
5,350
5,360
7,210
5,030
5,730
6,530
4,290
6,400
7,750
5,960
5,740
5,790
6,070
6,400
5,790
6,770
6,070
6,030
6,030
6,040
5,090
5,610
5,000
Ca
Stalk Seed
19,400
18,020
21,2BO
15,900
13,840
16,700
9,420
14,200
1,860
11,280
10,790
12,040
14,510
21,530
14,300
5,110
12,670
9,780
11,200
15,890
13,370
17,640
8,700
11,390
20,750
12,080
11,210
12,440
11,480
39,000
2,700
2,070
2,13D~
2,400
2,100
2,800
1,490
3,300
1,870
2,580
1,570
1,720
2,110
1,800
1,680
2,200
1,810
2,250
1,460
4,600
1,590
1,950
1,340
1,500
1,640
1,560
2,800
1,490
1,930
1,700
1 ,020
1,620
1,650
•<
Stalk
7,600
6,800
22,400
5,700
13,300
9,120
9,400
9,320
20,600
9,380
24,430
11,510
29,720
18,460
21 ,810
26,300
7,100
9,300
30,720
7,510
13,500
13,010
24,080
26,260
10,540
22,100
9,480
23,630
12,770
25,110
9,570
26,030
8,510
29,000
Seed
8,310
3,600
11 ,400
9,900
6,880
10,170
9,570
9,900
12,320
12,840
10,130
2,540
10,440
9,500
9,350
11,970
9,950
3,500
9,040
12,490
11 ,350
9,490
9,600
9,440
11,860
8,860
12,580
9,520
11,710
8,820
11.850
Na
Stalk Seed
1 ,580
339
200
330
1,220
406
1,700
453
1,730
223
3,780
797
4,290
459
3,790
666
3,340
547
4,000
494
2,650
521
10,700
11,170
370
610
627
5,570
618
3,150
511
4,510
377
1,200
1 ,290
92
100
443
2,360
126
2,320
179
1 ,770
148
3,260
43
2,990
139
4,720
90
1,660
<3
3,420
8
2,340
20
3,700
5,590
<3
70
6
3,300
<3
3,420
<3
4,380
<7
300
 »» From A 4 L Labs Feed Manual
*** Not stalks but leaf tissue (will alter some analysis)
                               597

-------
Table  F.5,  continued
Fe As
Pivot
No. Date
1 1981
1985
2 1981

1983
3 1981
1983
5 1981
1 Qflf
1 7OJ
6 1981
8 1981
1983
10 1981
1983
11 1981
1983
12 1981
1983
13 1981
1983
14 1981
198-
15 1981
1983
18 1981
1983
19 1981
1983
20 1981
1983
21 1981
1983
22 1981
198J
Referenced
verage-*_
Stalk
407
349

498
323
214
193
1 "\7
I J L
182
56
216
78
141
33
1 58
230
69
830
209
284
194
188
163
154
	
169
277
172
148
133
36
224


Seed Stalk Seed
91 <.5 <.5


32 	 	
68 <.5 <.5
62 <-5 <.5
82 <.5 <.5
54 <.5 <.5
56 <.5 <.5
26 <-.5. <.5
9 <.5 <.5
85 <.5 <.5
60 <-5 <.5
66 <.5 <.5
69 <.5 <.5
21 <.5 <.5
50 <.5 <,5
27 <-5 <.5
155 <-5 <.5
19 <-5 <.5
66 <-5 <.5
22 <-5 <.5
34 <-5 <.5
<.5 <.5
28 <-5 <,5
19 <-5 <.5
38 <-5 <.5
19 <.5 <.5
18 <-5 <.5
<.5 <-5 <.5
31 <.5 <.5

	 = 	
8a
Stalk
22.8
14.89

29.4
10.86
27.1
28.7
26.2
13.2
•30.0
14.4
30.0
12.7
23.1
28.2
28.2
7.01
25.97
7.67
18.9
29.8
3.5
9.62
3.44
28.2
4.43
16.7
8.3
25.3
7.9


Seed
5.8
3.31

6.2
6.06
7.7
6.5
4.4
4.5
5.7
17.86
7.0
17.85
5.8
11.6
4.5
3.5
7.5
7.5
4.9
3.8
0.49
1.74
2.62
6.3
1.47
3.4
3.35
5.9
3.4


Cd
Stalk
0.2
0. 1

0.1
<.Q5
0.1
<.05
.1
.06
.1
<.05
.7
.08
.2
<.05
0.4
.11
.2
<.05
0.1
0.1
<.05
0.08
<.05
.2
<.05
.6
<.05
.1
<.05


Seed
0.2
.24

0.2
<.Q5
0.2
.1
.5
.08
0.2
0.06
.3
<.Q5
2.5
0.06
1.2
<.05
.09
.09
0.1
0.4
0.49
0.29
<-05
.4
<.05
.2
<.05
.1
<.05


Cr Cu Pb
Stalk Seed Stalk
2.3 1.7 5.0
.5 .6 5.25

<.5 2.2 5.7
.77 .54 3.35
<.5 <.5 6.4
.8 <.5 7.3
<.5 <.5 7.5
<.5 <.5 .18
<.5 <.57 9.6
<.5 .97 <.5
<.5 <.5 10.2
3.0 .66 <.5
<.5 <.5 8.1
<.5 <.5 <.5
<.5 <.5 11.9
.78 .75 1.58
2.5 1.1 9.9
.88 .8 .18
0.8 <.5 5.7
2.4 <.5 8.2
0.53 1.12 0.54
1.12 <.5 5.28
0.77 0.88 <.5
.5 <.5 7.3
.67 <.5 1.37
.5 <.5 6.9
.61 <.5 <.5
<.5 <.5 6.0
.75 .53 <.5

	 	 12.0
Seed Stalk Seed
6.1 1.9 1.9
4.46 <.5 <.5

14.6 1.7 <.5
0.94 <.2 <.2
6.5 1.3 1.5
5.1 2.1 .3
<.5 <.5 <.5
.95 <.2 
-------
                                               Table  F.6

                               Plant  Analysis,  Stalk  and  Seed
                                                 (/ng/g)
                  Milo-
                               TKN             TP             Ca              K               Na
             Pivot
              No.   Date    Stalk    Seed  Stalk   Seed    Stalk  Seed    Stalk     Seed   Stalk   Seed

               5    1982     	      -—   —_   ...    6,390    490   25,200   2,700     393     62
                   1983    2,360   12,610   900   2,970   4,580    510   17,000   2,510     845     88

               6    1982     	      	    	   	    6,340    470   24,100   4,170     418     76
                   1983    3,770   13,260   880   2,590   4,970    390     	    2,590     	     55

               7    1982     	      —-    —   —    5,440    520   22,900   2,420     432    130
                   1983   12,620   15,720  1,180  2,420   6,430    174   14,960   2,190   1,114    156

               9    1982     	      —    —   	    a,400    820    2,100   5,270     175     64
                   1983    3,630   11,630    730  2,490   7,490    440   13,120   2,980     306    106

              15    1982     	      	    —-   —-    6,420    980   16,100   5,260     256     54
                   1983   12,090   17,640    990  2,880

              16    1982     	      	    	   	    6,000  1,160   27,900   6,100     473    201
                   1983    2,980   10,960    650  2,770   7,240    410   12,460   2,960     239     69


              Referenced
              Averaae ** 27,000    19,200  3,800  3,300   4,200    400   21,000   3,900     200     50
                  Fe          As            Ba              Cd             Cr             Cu             Pb
Pivot
 No.  Date  Stalk  Seed Stalk  Seed   Stalk   Seed    Stalk   Seed    Stalk   Seed   Stalk   Seed    Stalk   Seed
  5   1982   419   114   1.12   1.03    	      ---     0.24   < .05
      1983   422    63
  6   1982   328    14   1.11   <.5     	      —     0.46    0.3
      1983   337    70   <.5    <.5    16.02     2.5     0.16   <.05    0.83    <.5    <.5    1.79     <.2    < .2

  7   1982   618     4   <.5    <.5     	      —      	-     	-
      1983   355    66   <.5    <.5     7.55     3.04    0.14   <.05    2.35    <.5    6.45    1.11     <.2    < .2

  9   1982   195    11    .64   <.5     	      	     0.14    	-	—
      1983   389    65   <.5    <.5    13.38     1.84    0.07   <.05    1.55    1.28   <.5    <.5          -"
  •• A 4 L Labs Feed Manual


                                                   599

-------
                                  Table  F.7
Plant Analysis  for  Cotton and Milo Samples  Obtained from  Gray Farm 1981
TKN
Stalk Seed
COTTON
81001 18,900 15,450
81002 24,450 21,580
81003 13,200 54,900
81004 26,850 53,540
81007 17,230 19,330
81010 18,680 20,540
81011 No Data 36,950
81012 15,420 36,720
81013 16,870 35,270
RefAvg* 23,000 72,000
Gray
Mean 17,700 32,698
SO 5,782 14,645
Hancock
Mean 14,871 35,652
SD 2,493 8,864
MILO
81002 11,600 23,400
RefAvg* 14,000 19,000
As
Stalk
COTTON
81001 <.5
81002 <.5
81003 <.5
81004 <.5
81007 <.5
81010 <.5
81011 <.5
81012 <.5
81013 
-------
                  Table F.8

Plant Analysis for Alfalfa Samples Collected  from
           Gray Farm in 1982 and 1983
Yr/ Loc
83 004
83 07E
83 08E
83 10E
83 10W
83 11W
83 012
83 013
MEAN
S.D.
NORMAL
WHEAT
83 001
83 015
83 016
MEAN
S.D.
NORMAL
TKN
32,010
31,460
24,360
32,410
52,900
46,710
38,740
47,990
38,322
9,952
46,000

44,390
40,650
39,710
41,583

28,000
TP
3,380
3,470
3,790
3,260
5,630
5,480
3,710
4,490
4,151
944
4,000

8,730
8,940
6,370
8,013

3,600
Ca
15,510
18,670
17,270
19,730
11,580
10,850
23,520
15,790
16,615
4,184
18,000

2,100
3,590
8,240
4,643

4,500
K
19,970
20,340
23,300
22,900
32,500
35,000
20,080
30,400
25,561
6,111
27,000

46,900
44,700
25,100
38,900

26,000
Na
2,218
1,468
1,850
1,287
570
1,716
1,668
883
1,458
533
200

416
1,258
2,394
1 ,356

200
Fe As
118 <.5
224 <.5
337 <.5
217 <.5
223 <.5
352 <.5
239 <.5
178 <.5
236 <.5
77
105

— <.5
1,258 <.5
1,247 <.5
1,252

60
Ba
20.1
23.2
31.1
27.6
27.4
28.4
27.4
30.5
26.9
3.7


21.4
15.4
23.1
19.96


Cd
.07
.08
<.05
.06
<.05
.09
.05
0.05
.06
.02


0.1
0.1
<.05



Cr Cu Pb
<.5 .51 <.2
1. 08 .55 <.2
0.64 <.5 <.2
<.5 <.2
<.5 .81 <.2
.72 .62 <.2
2.62 1.74 <.2
<.5 <.5 <.2
.86 .75 <.2
.66 .45
12

.94 4.6 <.2'
1.02 3.2 <.2
2.63 0.8 <.2
2.87

9

-------
           APPENDIX d

Land Application System Operation Data
               and
   System Expansion Cost Data
              602

-------
TABLE G.1
	 • — 	 	 ' .1.1- I-K LJI \ in 1 uu 1 ^U^ 1 l_l\ 1 1L1AUH lUlHL-J UI^JULU 1 1VUIJ
Treat &
Pivot
Location
14-No Fert


Average
4-Nitrogen


Average
14-Sulfur



1-No Fert


Average
11-Nitrogen


Average
11 -Sulfur +
Nitrogen

Average
5-No Fert


Average
5-Nitrogen


Average

No/m2
Plant Count
6
8
12
8.67
6
17
9
10.67
17
11
16
14.67
21
17
19
19.0
19
21
18
19.33
25
20
20
21 .67
8
13
11
10.67
8
11
11
10.0

No/m2
Boll Count
38
30
29
32.33
39
41
42
40.67
31
34
36
33.66
74
62
69
68.33
82
69
67
71 .67
90
59
63
70.33
34
40
47
40.33
40
40
32
37.33

No/m2
Yield Lint
65
58
42
55.0
81
77
53
70.33
59
54
63
58.67
115
85
105
101 .67
130
100
95
108.33
115
95
80
96.67
58
66
83
69.0
64
70
56
63.33

gr/m2
Field Wt.
475
400
550
475.0
510
500
500
503.3
455
425
465
448.33
745
520
615
626.67
775
720
650
731 .67
645
605
565
605.0
400
450
465
438.3
380
445
415
413.3

Percent
Moisture
42.4
43.4
55.7
47.17
11 .6
18.6
27.2
19.13
16.4
14.2
18.9
16.5
17.0
10.5
11 .1
13.2
15.6
23.0
16.7
18.43
9.3
10.2
17.6
12.53
10.2
6.1
5.7
7.33
6.9
7.3
12.7
8.97
                            603
                                                           (Continued)

-------
Table G.1,  continued
5-Sulfur +
Nitrogen

Average
12
14
16
14.0
47
40
40
42.33
84
74
68
75.33
505
460
435
466.67
5.8
6.3
8.4
6.83

No Pert
15
14
11
Average
Nitrogen
15
14
11
Average
Sulfur
15
14
11
Average
10.67
8.67
19.0
12.78

10.0
10.67
19.33
13.33

14.0
14.67
21.67
16.78
40.33
32.33
68.33
47.0

37.33
40.67
71 .67
49.89

42.33
33.66
70.33
48.77
69.0
55.0
101 .67
75.22

63.33
70.33
108.33
80.66

75.33
58.67
96.67
76.89
438.3
475.0
626.67
513.32

413.3
503.3
731 .67
549.4

466.67
448.33
605.0
506.67
7.33
47.17
13.2
22.57

8.97
19.13
18.43
15.51

6.83
16.3
12.53
11.95
                                        604

-------
                                 Table G.2
	Total Construction  and  Land Acquisition  Costs  1982

 I.  Construction
     A.  Engineering
         1.   Design                      $405,607.98
         2.   Special  Costs                 36,305. 11
         3.   Resident  Engineer             149,922.68
                              Subtotal   $  592,325.77
     B.  Contracts
         1.   Pump Station &  Force Main   2,658,554.50
         2.   Reservoirs                  1,691,208.87
         3.   Farm Distribution  System    1,433,801.64
         4.   Electrical  Hookup             41,171.00
         5.   Monitoring  Wells               4,000.00
                              Subtotal $ 5,828,736.01
                                  Total                      $6,421,071.78
II.  Land Purchase                Total                       1,460,000.00
                           Grand  Total                      $7,881,071.78

               Amortized Construction and  Land  Purchase  Costs
No Cost Sharing
     Construction amortized  over  20  yrs  $754,219.08/yr
     Land Purchase amortized over 20 yrs   171 ,491.60/yr
                                  Total                      $925,710.68/yr
City's Share of Cost  Sharing  (85%  Federal,  15%  City  for  Innovative
Technology Treatment)
     Construction, amortized  over  20  yr   $113,132.80
                   (i =  10%)
     Land Purchase, amortized over 20 yr   $25,723.74
                   (i =  10%)
                                Total                        $138,856.60/yr
                                 605

-------
                                 Table G.3
                      Operational Costs - City and Farm
 I.   1982  Operational  Costs
     A.   City
         1 .   Water  Treatment
             25.587 cents/1000  gal              $286,685.00
             (including  pumping costs  and
              maintenance)
         2.   Chemical                             5,093.00
                                 Subtotal       $291,778.00
     B.   Farm
         1 .   Improvements
             a.   Owner & LCCIC                    32,369.94
             b.   Farmers                         43,350.00
         2.   Irrigation  Expense                  63,701.04
         3.   Interest, Depreciation               36,457.86
         4.   Repairs,  Tires,  Oil,  Gas             71,542.10
         5.   Seed,  Fertilizer,  Chemicals         46,624.78
         6.   Labor                                56,121.31
                                 Subtotal       $350,167.03
                                    Total                         $641,945.03
II.   1983  Operational  Costs
     City
     A.   Water Treatment Plant
         25.587  cents/1000 gal                  $259,931.81
         (including pumping  cost
         chemicals  and maintenance)
     B.   Farm
1.


2.
3.
4.
5.
6.
Improvements
a . Owner
b. Farmers
Irrigation Expense
Interest, Depreciation
Repairs, Tires, Oil, Gas
Seed, Fertilizer, Chemicals
Labor
Subtotal
Total

23,919.91
7,347.29
101,206.23
34,119.56
70,022.75
65,173.14
63,548.21
$365,337.09
$625,268.90
606

-------
               Table G.4
Farm Operation Costs Prior to Effluent
1980
Interest, Depreciation
Repairs, Gas
Seed, Fertilizer
Labor
TOTAL


$34,766.
97,668.
62,901 .
19,218.
$214,555.
99
72
48
69
88
Average

Table
G.5

1981
$59,498
87,454
64,395
16,768
$228,117
$221,336


.00
.59
.82
.95
.36
.62

Farming Expenses

Name
19BD
Farmer A
Farmer B
Farmer C
Farmer 0
Farmer F_
Farmer F
Farmer G
Farmer H
Farmer I
Farmer J**
Farmer K**
Total
1981
Farmer A
Farmer 8
Farmer C
Farmer D
Farmer E
Farmer F
Farmer G
Farmer H
Farmer I
Total
» Total/Acre
*• Left aFter
Equipment Repair,
Purchase Tires,
Budget Gas 4 Oil
3910.40 3942.40
7497.70 3744.72
20,365.52
7872.03 16,322.84
9208.80 9867.46
5870.00
4403.06 6750.49
7696.82
6583.47
1875.00 7285.00
10,240.00
34,766.99 97,668.72

3840.00 4484.80
3051.16 5580.99
22,361.86 11,759.94
14,184.00 17,448.54
8880.80 9024.74
13,420.08
7180.18- 8986.50
11,012.68
5736.32
59,498.00 87,454.59
x 2.47 Total/hectare
1980 season
Seed,
Fertil izer
Chemicals
5947.20
5923.92
5837.10
8667.28
5831.16
4750.00
6084.40
8394.04
5212.38
6418.00
5086.00
68,151.72

4475.00
5351.17
6911 .21
8089.08
4888.99
10,033.80
5133.32
14,877.70
4635.55
64,395.82


Total/*
Labor
2361 .60
2940.66
812.00
1264.00
4092.40
4160.00
1057.23
213.80

2317.00

19,218.69

2673.00
1091.83
367.25
982.60
5261.58
5696.09
1195.56
501.04

17,768.95


Total
Acre
20,198.40 132.88
24,015.58
30,320.48
39,466.93
31 ,082.98
15,380.00
25,048.96
16,641.00
13,196.51
20,488.00
16,772.00
33.10
64.93
75.60
77.51
48.82
61.09
46.48
40.36
106.15
71 .98
252,610.84 808.90

17,074.00
22,854.65
40,501.05
43,800.63
30,844.96
31/443.98
29,856.65
26,512.45
10,371 .87
253,260.24



112.32
79.08
86.72
108.68
76.92
99.82
72.33
74.05
31.71
741.63


                   607

-------
                                         Table G.6
                                     Farming Expenses
Name
1982
Farmer A
Farmer B
Farmer C
Farmer E
Farmer F
Farmer G
Farmer H
o Farmer I
CD
Total
1983
Farmer A
Farmer B
Farmer C
Farmer E
Farmer F
Farmer G
Farmer H
Farmer I
Total
Interest ,
Depreciation or Repairs
Irrigation Equipment Tires,
Expense Purchase Gas A Oil
$1,660.80
8,492.55
12,017.39
16,451.88

7,575.58
9,635.25
7,867.59
$63,701.04
1,574.40
22,729.80
19,817.45
24,694.82
10,269.48
10,600.00

11,520.28
$101,206.23
$3,859.20
5,613.76
5,582.69
15,269.99

5,826.73
305.49

$36,457.86
3,524.80
2,973.43
2,391.05
14,924.28
3,554.00
6,752.00


$34,119.56
$4,250.00
6,283.81
21,553.28
14,082.89

7,189.62
12,182.04
6,000.46
$71,542.10
3,416.00
6,749.97
26,730.68
13,740.78
3,140.40
11,334.00

4,910.92
$70,022.75
Seed
Fertilizer
Chemicals Labor
$3,944.00
8,592.43
6,558.00
7,881.99

5,408.17
8,695.59
5,544.60
$46,624.78
4,889.60
8,708.18
11,243.36
18,160.17
4,791.54
8,852.00

8,528.29
$65,173.14
$5,468.80
7,173.97
8,574.28
16,575.49

6,027.12
9,905.81
2,395.84
$56,121.31
2,961.60
13,975.12
8,355.20
22,936.16
7,866.13
5,964.00

1,490.00
$69,548.21
Total
$19,182.80
36,156.52
49,285.64
70,202.24
21 ,562.68
32,027.22
40,724.18
21,807.60
$290,948.88
16,366.40
55,136.50
68,537.74
94,456.20
26,821.89
43,502.00
32,401.00
26,449.49
$363,671.22
Total/*
Acre
$123.76
102.14
127.68
132.21
86.59
156.23
141.89
100.49
$970.99
105.59
99.17
177.56
158.48
107.72
156.48
112.88
121.89
$1039.77
* Total/Acre x  2.47 =  Total/hectare

-------
       Table G.7
Gross Income of Tenants

1980
Farmer A
Farmer B
Farmer C
Farmer D
Farmer E
Farmer F
Farmer G
Farmer H
Farmer I
Farmer 3
Farmer K
Total
1 981
Farmer A
Farmer B
Farmer C
Farmer 0
Farmer E
Farmer F
Farmer G
Farmer H
Farmer I
Total
Average 1980
Farmer A
Farmer B
Farmer C
Fanner 0
Farmer E
Farmer F
Farmer G
Farmer H
Farmer I
Total
Cotton

$3,035.13
9,291.63
21,609.63
18,070.79
13,242.19
6,660.00
26,355.72
35,121.00
7,343.00
26,962.00
7,660.00
$ 168,081.52

11 ,623.11
15,676.38
28,207.38
22,561 .00
25,925.26
25,491.47
23,491.47
21,010.00
19,854.56
$193,840.63
+ 1981
$7,329.12
12,484.06
24,908.25
20,315.89
19,583.72
16,075.73
25,176.28
28,065.50
13,598.80
$167,537.35
Other Government
Croos Proarams

513,333.75
2658.38 M 8,186.93
3,186.93
227.26 M 9,500.00
9,490.02

634.51 M 552.41

6,350.24
2,196.00
7,127.00
53,520.15 $66,198.70

7,194.99
12,692.78
11 ,987.57
16,207.00
12,092.96

1,494.79 M 14,568.94
17,309.14
6,250.82
$1,536.20 $98,304.20

$10,514.37
$1,329.19 10,439.85
10,225.46
113.63 12,853.50
20.71 10,791.49
4,500.00
1,064.65 7,560.67
8,654.57
6,550.54
$2,528.18 $82,090.45
"sr.al

516,668.38
- 20,136.94
30,072.47
27,570.25
23,104.97
15,660.00
27,542.64
55,121 .00
! a , 1 9 3 . 29
29,157.00
14,788.00
6254,215.44

18,818.10
28,369.28
40,194.95
38,768.00
38,059.63
25,491.4-7
40,060.58
38,319.14
26,105.38
$294,186.53

$17,843.49
24,266.61
35,133.71
33,169.12
29,082.30
20,575.73
33,801.61
36,720.07
20,149.33
$250,741.97
T3C31 *

5 1 10.57
69.67
54.59
68.41
57.61
49.71
67.17
98.10
43.40
151.07
63.47
$843.97

123.80
98.16
86.07
96.20
94.91
80.92
97.70
107.03
79.83
$864.62

$117.39
117.39
75.23
82.30
72.51
65.32
82.44
102.57
61 .62
$743.35
            609

-------
Table G.7,  continued

1982
Farmer A
Farmer B
Farmer C
Fanner E
Farmer F
Farmer G
Farmer H
Farmer I
Total
19B3
Farmer A
Farmer B
Farmer C
Farmer E
Farmer F
Farmer G
Farmer H
Farmer I
Total
Other
Cotton Crops

17,660.27
8,102.34 SF
16,476.52 SB
1,727.63
35, 626. 93
18,752.33 SB
12,788.56 M
9,812.53
25,491.i7 M
1,918.91 5,990.68 SB
6,441.91 M
16,534.28
22,181.04
1,918.91 197,586.49

32,174.51
76,200.00 2,094.00 0
13,644.30 M
13,131.05 W
40,977.64 29,191.94
107,174.98 3,489.02 M
5,504.97
34,600.00 24,000.00 M
8,400.00 W
8,280.00 0
43,399.57 3,869.00 M
5,040.00 W
7,009.00 0
37,847.00
16,521.24 18,021 .32 M
13,212.01 W
388,894.94 154,886.61
Government
Programs


18,111 .31
17,558.87
20,544.90

12,411 .00
24,534.28
9,549.20
102,709.56


15,202.30
5,717.25
13,1 15.60


7,782.00
7,422.50
49,239.65
Total

23,889.27
44,417.30
42,185.80
61 ,898.32
25,491 .47
26,762.00
41,044.52
31,730.24
297,419.42

32,174.51
105,069.35
75,888.00
129,284.57
75,280.00
59,417.00
45,629.00
55,177.07
593,021.20
Total/*
Acre

154.94
125.47
109.29
116.57
102.37
130.00
143.01
146.22
1,027.87

207.57
188.97
196.60
21-.92
302.33
254.27
158.97
228.14
1,712.88

Key:
        SF   Sunflower
        SB = Soybeans
        0   Oats
        M   Milo
        W   Wheat
        ?   Data not Reported
      Left = Farmer no longer farmed on Hancock Farm
          * Total/Acre x 2.47   Total/hectare
                                                 610

-------
                     Table G.8
                Tenants'  Net  Income

1980
Farmer A
Farmer B
Farmer C
Farmer D
Farmer E
Farmer F
Farmer G
Farmer H
Farmer I
Farmer 3
Farmer K
Farmer A
Farmer B
Farmer C
Farmer D
Farmer E
Fanner F
Farmer G
Farmer H
Farmer I
1982
Farmer A
Farmer B
Farmer C
Farmer E
Farmer F
Farmer G
Farmer H
Farmer I
1983
Farmer A
Farmer B
Farmer C
Farmer E
Farmer F
Farmer G
Farmer H
Farmer I
Tenant
Expenses/ acre

$132.88
83.10
64.93
75.60
77.51
48.82
61.09
46.48
40.36
1 06 . 1 5
71.98
112.32
79.08
86.72
108.68
76.92
99.82
72.33
74.05
31 .71

$ 123.76
102.14
127.68
132.21
86.59
156.23
141.89
100.49

105.59
99.17
177.56
15B.48
107.72
156.48,
115.30
121.89
Tenant
Gross Income/acre

$110.97
69.67
64.39
68.41
57.61
49.71
67.17
98.10
43.40
151.07
63.47
123.80
98.16
86.07
96.20
94.91
80.92
97.70
107.03
79.83

$154.94
125.47
109.29
116.57
102.37
130.00
143.01
146.22

207.57
188.97
196.60
216.92
302.33
213.38
15B.97
254.27
Tenant
Net Income/ acre

$ -21.91
-13.43
0.54
7.19
-19.90
+ 0.89
+ 6.08
+51.62
+ 3.04
+ 44.92
8.51
+11 .48
+ 19.08
0.65
-12.48
+17.99
-18.90
+25.57
+32.98
•+48.12

$+31.18
+23.33
-18.39
-15.64
+15.78
-26.23
+ 1.12
+45.73

+101.98
+ 89.80
+ 19.04
+ 58.44
+194.61
+ 56.90
+ 43.67
+132.38
	 	 — — — 	 • 	
$/acre x 2.47 - $/hectare
                           611

-------
  T
                     Reservoir
                 -i---- Playa
                 • MHO
                  ::::;: Soybeans

                  **l Sun Flowers
                  1 cm = 0.27 km
Figure G.1.
Summer 1982 Cropping Pattern
for Hancock Farm
                                612

-------
                       July Irrigation
                        Showing Source
    Numbers  inside  pivot  out-
    lines  denote  dates  that
    pivot  was operated.
Figure G.2.  July 1982 Irrigation Showing Source

                       613

-------
                          August  Irrigation
                           Showing  Source
                    Reservoir

                    Pipeline
    Numbers  inside  pivot  out-
    lines  denotes dates that
    pivot  was  operated.
Figure G.3.   August 1982  Irrigation  Showing  Source

                           614

-------
                       September Irrigation
                           Showing Source
                    Reservoir

                &H Pipeline
    Numbers inside pivot out
    lines denote dates that
    pivot was operated.
Figure G.4.  September 1982 Irrigation Showing Source

                         615

-------
                   Reservoir
                   Playa
                   Wheat/Oats
j        	
                1 cm = 0.27 km
Figure G.5.
Winter 1982 Hancock Farm
Wheat and Oats Production

                   616

-------
                      DISTRIBUTION CAN

                      DISTRIBUTION LINE
        HANCOCK  LAND
       DISPOSAL SITE
Figure G.6.  Summer 1983 Cropping Pattern, Hancock Farm
                              617

-------
o\
	!t

CD
          Figure G.7.  Type of  Irrigation  Used  at  Gray  Farm 1982 and 1983

-------
o\
VO
                                                                ALFALFA
                                                               1982-1983
                    Figure G.8.   Winter  and  Summer 1982-1903 Alfalfa Production,  Gray Farm

-------
ON
N)
O
                                                            WINTER  CROP

                                                            1982-1983
                    Figure G.9.   Winter 1982 and 1983 Wheat Production, Gray Farm

-------
ON
                                                        SOYBEANS
                                                         1982
                    Figure G.10.  Summer 1982 Soybean Production,  Gray Farm

-------
                                  Appendix H

              Calculation of the Adjusted SAR of Irrigation Water
                         (Stromberg and Tisdale 1979)

           	Na
adj. SAR =   \ I Ca + Mg~   [1 + (8.4 - pHc) ]
             N    2
pHc = (pK'2 - pK'c) +'p(Ca + Mg) + pAlk

pK'  is the second dissociation constant for hLSCL and pH  is the solubility
        constant for CaCCL both corrected for ionic strength obtained.

p(Ca +Mg) is the negative logarithm of the molal concentration of calcium plus
          magnesium.

pAlk is the negative logarithm of the molal concentration of the total bases
        (CO  + HCCL).  Based on pH levels between 7 and 8.  It was assumed the

        bases were primarily HCCL and CCL was negligible.

pHc is a theoretical, calculated pH of irrigation water in contact with lime in
        equilibrium with soil CCL.

(pK'  - pK1 ) is obtained from using the sum of Ca + Mg + Na in meq/1 and the
        following table:
Sum of Concentration
(meq/1)
.05
.10
.15
.20
.25
.30
.40
.50
.50
.75
1.00
1.25
1.5
2.0
pK'2 - pK'c
2.0
2.0
2.0
2.0
2.0
2.0
2.0
2.1
2.1
2.1
2.1
2.1
2.1
2.2
Sum of Concentration
(meq/1)
2.5
3.0
4.0
5.0
6.0
8.0
10.0
12.5
15.0
20.0
30.0
50.0
80.0
PK'2 - PK'c
2.2
2.2
2.2
2.2
2.2
2.3
2.3
2.3
2.3
2.4
2.4
2.5
2.5
                                      622

-------
Appendix H, continued
An example of calculating PHc:
   A water contains:



Ca + Mg
Ca
co3 +


From the


Ca -
Mg =
Na =
+ Na =
+ Mg =
HCO =
C03 =
HC03 =
table:


1 .82 meq/1
0.75 meq/1
6.70 meq/1
9.27 meq/1
2.57 meq/1
0.35 meq/1
0.05 rneq/1
0.30 meq/1
PK'9 - PK'
p(Ca + Mg)c
p(Alk)
                                        2.3
                                        2.9
                                        3.5
                                       '8.7
To calculate  SAR  ,.,  substitute in  formula:
                aaj
         SAR
6.70 meq/1
2.57 meq/r   (1 + (8.4 - 8.7)  = 4.1
            adj

       Values  of pHc  greater than 8.4 indicates  a  tendency  to  dissolve  lime  from
       the  soil  matrix;  values below 8.4 indicate  a  tendency to  precipitate  lime
       from the  applied  water.
                                       623

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