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
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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.
-------
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
-------
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-
-------
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
-------
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.
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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)
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
ho
CO
Pipeline
Water
= 0.27 km
Figure 4. Gray Farm Land Treatment Site
-------
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
-------
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
-------
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
-------
fFurrow Irrigation
(^Distribution Can
Pipeline
Figure 7. Hancock Farm Land Distribution
System
32
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
BALL VALVE
Modifications Made to Some Center Pivot Irrigation Machines
41
-------
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
-------
SCREEN
Figure 12. Relation of Screen to Flow Meter as Designed and Installed
-------
Figure 13. Position of Flow Meter to Achieve Proper Operation
44
-------
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
-------
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
-------
Type 1
Type 2
Figure 19. Types of Splash-pans Available
51
-------
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
-------
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
-------
To Distribution Can 1
Pump Station
Rvservolr 1
Figure 21. Proper Installation of Flow Transmitter as Described
in the Manufacturer's Manual
55
-------
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
-------
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
-------
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
-------
MD
' ' = O,27 km
—••• Boundary
Road
NON-CONTAMINATED
WELL
Figure 22. Gray Farm Groundwater Monitoring Locations
-------
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
-------
DRINKING WATi
Sampling
Location
/ Road
Hancock
Farm
. 0.62 km
Scale
Figure 24. Hancock Farm Drinking Water Sampling Location
61
-------
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
-------
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
-------
1.22 m (4.01)
r
| -^;?;>%v,'?°. d_. ^-.r
r
t
«8$
^
'1
*•• «Wo'r-.J X' .V/|
MM-
P
_ji
$
•-
5^ Annul us
gravel pa
with 0.64
smaller g
_/— '10.2 cm (
I.D. PVC
8.9 cm (3.5")
O)
Q-
c
o
c/i
c
t.
o
CM
O)
(O
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
-------
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
-------
•Cap
M
I.o ,;• *'* A.' a
',•«;-*
;v*o
-» * «
A
°a
f.
s
V
8&
?0
o.
'S
t-
i!
s
••MM
V
* 10.2 cm (4 in) I.D. PVC Pipe
^'P»0
- Vo 1m X 38 cm (3 ft X 15 in)
^Xrcf ^ Cement Collar
0.?A
'<
b-
6°
ro
$0
O4
^ A
$
$
&
ft
fi
ft'
V.
JD
^
S W> V
r ^' 1 m X 1 m f ^ft 5f 1ft \
P^ff Ai.-0'o-o 4 imA im ^OTlA^nj
'e^ " ^^rk "xV'l * /-» i r» 1
«— Cement
•
Perforated
Zone
Sand
Gravel
f*-Red Beds
Figure 27. Cemented Reservoir Monitoring Well
68
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
/
-------
Sampling Site
Water
= 0.27 km
Figure 35. Crop Sample Locations, Gray Farm
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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.
-------
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
-------
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
-------
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
-------
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)
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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)
-------
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
-------
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
-------
Figure 43. Water Level Contours in feet, December, 1901, Gray Farm
-------
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
-------
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
-------
Reservoir
Playa
1 cm = 0.27 km
CONTOUR ELEVATIONS IN FEET
(.3048 METERS/FT)
Figure 44. Water Level Contours, December
1981, Hancock Site
136
-------
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
-------
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
-------
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
-------
A A •
• -*^L. "•»••«• *»»
0.33
CC
LJ
)
CO
o
LL
O
o.
LU
O
Figure 46. Water
D JF MAM J J A SO
TIME (MONTHS)
Content as Indicated by Neutron Probe LCCIWR #4
140
-------
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
-------
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
-------
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
-------
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)
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
(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
-------
o
o
O'
CM
O
O
CO'
ON
CD
O-
Q-
LU
-------
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
-------
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
-------
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)
-------
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
-------
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
-------
Figure 56. Nitrate Concentration (mg/1) in Well Water under Gray Farm, Baseline Period,
1981-1982.
-------
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
-------
--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
-------
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
-------
§
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
O Well
-»:- Ponded
---" Water
= 0.27 km
Figure 68. Gray Wells which Contain Water with SARad. greater than 9
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
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
-------
o
o.
o
CD
Q_ CM
UJ •'
Q rt
o
ON
O
CO
o
CO
o
•
o
O
o
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
-------
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
-------
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
-------
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
o
|100
1 +
CD
0
.S
100
200
300
400
, 42.2 cm , 52.2cm ,
i
9 •
1 1 •
i
I ;: i
* !
i
i i !
1 1 !
£ m •
^ ^ I
i i •
^ • s •
!j !i
i ! ' i
: ' : i
! - i
i i
i ;
: i
•
I
68.9cm
1
1;
i '
i!
& \
t
t
NIT
SOU
DOGEN
RCES
NITROGEN
LO
1
SSES
Figure 76. Inorganic Nitrogen in 183 cm Profile at the Hancock Farm
211
-------
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
o
o
Q 1981
O 1983
o
(£>
r—o
Q_ CM
CO
o
00.
o
•
o
o
o
0.00
0.02
I i ] i I
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) .
o
LU
X
£ VERY
3 HIGH
CC
o
a.
-------
0_
Q_
-------
o
o.
*
(M
O
ID
n
Q_ c\J.
ho
O
CO
o
00.
o
•
o
o
o
68.9 cm Hydraulic Loading
KEY
D 1981
O 1983
0.00
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
o.
KEY
o
CO
IT0
Q_ CM.
ro IT
t-o O
o
o
00.
o
o
o
D 1981
O 1983
—, , , . , j
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
-------
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
-------
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
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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
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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
-------
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
-------
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
-------
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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22. EPA. Operation and Maintenance Considerations for Land Treatment
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24. Ferrara, R.A. and AVci, C.B. Nitrogen dynamics in waste stabilizations.
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26. Gerba, C.P., Wallis, C., and Melnick, J.L. Fate of Wastewater Bac-
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Brown Co., Publishers. Dubuque, Iowa. 1972. 504 pp.
29. Hinsely, T.D., Thomas, R.E., and Stevens, R.G. Environmental Changes
from Long-term Land Application of Municipal Effluents. U.S. EPA
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30. Holford, I.C.R. and Mattingly, G.E. The high- and low- energy
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31. Hook, J.E. and Kardos, L.T. Nitrate leaching during long-term spray
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32. Hook, J.E., Kardos, L.T., and Sopper, W.E. "Effect of Land Disposal
of Wastewaters on Soil Phosphorus Relations". In: Recycling Treated
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33. Hunt, P.G., Peters, R.E., Sturgis, T.C. and Lee, C.R. Reliability
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34. Inter-American Labs. Scientific Services for Agriculture. 1976.
35. Iskandar, I.K., and Wright, E.A. Land Treatment Research and Develop-
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36. Johnson, D.E., Camann, D.E., Register, J.W., Thomas, R.E., Sorber,
C.A., Guentzel, M.N., Taylor, J.M., and Harding, H.J. The evaluation
of microbiological aerosols associated with the application of waste-
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40. Lubbock Christian College Institute of Water Research. Lubbock Land
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41. Majeti, V.A. and Clark, C.S. Health Risks of Organics and Land Appli-
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42. McNabb, J.F.., Dunlap, W.J. and Keeley, J.W. Nutrient, Bacterial and
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278
-------
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
-------
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
-------
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
-------
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
-------
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
"i.1?
Us.
Tv
i^.
_3&.QQ.
_aooQ
X/X^SL
K)
VO
VJ1
^35.
-3020
n
y**$
tUcL
•_&d
O l
13
sM.
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
!•
19
ao
at
as
as
24
29
MONTH . ^.JtiA.irh — J _^=Wi .1 R U_w> / CLX"^v^ ^\
s
PCMCON ON
COMPANY
neccivco FROM
ITCH DESCRIPTION
• HOW UB3 BU TONS
NUMBER, ETC
TOTALS
1
TOTAL CASH
RECEIVED
7/fi2fl
1
3
cattle
f*ON FARM
3
COTTON
VJ399
^7
A
7C^
Op
7
3%?
CO
WHEAT AND
BARLEY
Sow
00
OAI TAX
^pmoSIjA-I1
12*11
10
-
OEblTOKQir
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
a
1 AXES
20&J
on
6
ANO
6,RL,t
nn
7
CAS OIL
a CREASE
tUCEPT IN
PERSONAL.
AUTO
iJlJ~J'
no
e
IRRIGATION
EXPENSE
rutL. REPAIR
OIL.
/9 ^09
oo
• CCD
ANO
if^Va-
W)
IO
CHEMICALS
POISON a
SPRAYING
CO
IVP.'
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.-
CLU
;l
j
_
PAID TO
^u.
^A V-*JQ u^vt"
o
Se9-L.
OdtoUcx-
.*A)ooe.t*«.tjftr
^eceu~Jt>a*-
IT€M Of SCHIPTION
SHOW LBS BU TON
NUMBCn ETC
TOTALS
*OTAL CASH
EXPENDITURE
19 .IV
,33O(»
/753
2532^
4931
6,593
•4.2/0
•yzis
'
12,388
754,0
383
^vD3&
358W
43
^
93
^3
^
34
94.
^V
^
TO
R3
72
22
2
/6.2>
70
?
/3o
259?
-297i
n?
R7
pO
//
78
V3
3
L'BOB
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1771
frffi
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(flail
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V9
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03
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50
4
WITHHELD
?
/33;
/s
9
Si
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V^
(WV5
Vft
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O(n
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OR
02
A
TIMES *ND
TO
MACHINERY
AND
FA«M AUTOS
yV9
/35"
83
a&5
/73
3.^1*
A-Jft
-470
-5AA
' 73
/(OO
/9«r
26^0
3P.
Vfr
•^P,
rP 1
?3
0?
DO
83
35"
75
ff?
7o
95"
T
CAS OIL
« CRCASE
EXCEPT N
FEWSONAL
97
ffl
p/fe
&
611
584
Ptf
/»/
Ba3
/?o
iV
,5ft?
•Vo89
0|
5"P
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35
67
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e
IHNlCATION
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rucL «tp*m
loll
•30
25/p
30U
/L3a
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(etc?>
ll^oS
^loS,
1(07
fi-73
3273.1
K
TO
B,5
93
0^
H
4>3
07
5<«
PR
/o
80
•
• •CD
AND
LnTILIZEM
mi
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/020
^553
58*
50
5?
oo
3*T
/8
10
CHEMICALS
POISON A
SPRAYING
^tfi
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Urt
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^
pp
90
2^
oo
1 1
HOEING
AKIO
HCMICAL
ONTilOL.
3tfc
Hal
/7fi
<^3
ISO
9/8
o
r?(0
,50
oc
Oo
to
CO
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
70.8
( 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
10731
10932
AT
SD
S
3D
AT
50
5
xn
AV
SD
S
•ID
AT
SD
S
no
AT
SD
S
no
0.218
(0.141)
<-0.26>
0.209
0.206
(0.151)
< 0.51>
n. iB4
J.BOO
(0.0 )
< 0.0 >
*****
9.180
(0.0 )
< 0.0 >
• ••*•
6.060
(0.0 )
< 0.0 >
»••••
0.007
(0.004)
< 1.50>
0.005
0.006
(0.003)
< 1.50>
0.005
O.OOS
(0.0 )
< 0.0 >
*****
0.005
(0.0 1
< 0.0 >
*****
0.007
(0.0 )
< 0.0 >
*****
0.042
(0.019)
<-0.37>
0.043
0.067
(0.033)
< 0.53>
0.05X
0. J5«
(0.0 )
< 0.0 >
*****
0.369
(0.0 »
< 0.0 )
*****
0.121
(0.0 )
< 0.0 >
*****
0.538
(0.683)
< 0.69>
0.188
0.488
(0.513)
< 0.71>
n. 1911
0.0
(0.0 )
< o.o >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
38.9
1 12.7)
< 0.26>
41.
25.5
I 7.1)
21.
150.3
( 0.0)
< 0.0 >
• «*»
138.0
I 0.0)
< 0.0 )
• ***
I
63.0
( 0.0)
< 0.0 >
****
0.000
(0.0 )
< 0.0 )
0.000
0.001
(0.000)
< 1.50>
o.ooo
U.001
(0.0 )
< 0.0 >
*****
0.001
(0.0 )
< 0.0 >
*****
0.000
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0. 005
O.U06
(0.0 )
< 0.0 >
*****
0.006
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 )
*****
0.005
(0.0 1
< 0.0 >
0.005
0.005
(0.0 >•
< 0.0 >
0.005
0.005
(0.0 1
< 0.0 >
*****
0.006
(0.0 1
< 0.0 >
*****
0.031
(0.0 )•
< 0.0 >
*****
0.047
(0.086)
< 1.48>
0.006
0.009
(0.006)
< 0.51>
0 005
0.090
(0.0 )
< 0.0 >
*****
0.027
(0.0 )
< 0.0 >
*****
0.032
(0.0 )
< 0.0 >
*****
0.518
(0.635)
< 0.75>
0. 141
0.775
(0.908)
< 0.39>
Q. 190
2.227
(0.0 )
< 0.0 >
*****
4.688
(0.0 )
< 0.0 >
*••«•
3.258
(0.0 )
< 0.0 >
*****
0.002
(0.001)
< 1.50>
0.002
0.002
(0.000)
< 1.00>
o.ooi
o.ol I
(0.0 )
< 0.0 >
*****
0.011
(0.0 )
< 0.0 >
*****
0.003
(0.0 )
< 0.0 •>
*****
N)
HELL
• 1 1 • •$
10112
10211
10521
10542
10931
> *• • <
AT
SD
S
no
AT
SD
S
SD
AT
SD
S
HO
AT
SD
S
SD
AT
SD
S
SD
!IG
>4|t9Atfrt49£4
39.7
(11.2)
< 1.07>
36.5
36.3
(10.4)
< 0.71>
33.0
21.4
( 7.4)
<-0.03>
22.0
27.8
( 6.5)
29.0
37.3
(11.2)
< 0.99>
35.0
nil
i^####*$##fc*
0.052
(0.040)
< 0.49>
0.038
0.002
(0.049)
< 0.71>
0.012
0.192
(0.179)
< 0.28>
0.121
0.322
(0.414)
< 1.00>
0.102
0.074
(0.096)
< 0.97>
0.035
RG
0.000
(0.0 )
< 0.0 >
0.000
0.000
(0.0 )
< 0.0 5
0.000
0.000
(0.0 )
< 0.0 >
*****
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
no
0.007
(0.003)
< 0.33>
0.006
0.006
(0.003)
< 0.59>
0.006
0.011
(0.007)
<-0. 34>
0.015
0.014
(0.006)
< 0.82>
0.013
0.058
(0.011)
<-0.08>
0.060
HI
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.000)
< 1.79>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.162
(0.214)
< 1.08>
0.090
0.009
(0.008)
< 1.50>
0.005
K
7.9
( 1.3)
< 0.61>
7.5
7.8
( 1-2)
<-0. 14>
7.9
7.0
( 2.2)
< 0.36>
7.0
8.6
( 1-5)
<-0.54>
8.5
10.4
( 1-8)
<-0.26>
11.0
SE
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)
< 1.50>
0.005
0.007
(0.003)
< 0.41>
0.005
AG
• • t 4 • t# *# • fc (
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
(0.000)
< 1.50>
0.005
• A
72.0
( 6.9)
<-0.73>
72.5
87.0
( 15.9)
< 0.63>
87.0
47.4
I «1.5)
< 0.04>
44.0
120.2
( 36.0)
< 0.39>
99.0
103.0
( 13.5)
< 0.24>
102.0
Tt
0.007
(0.006)
< 1.79>
O.OOS
0.005
(0.0 )
< 0.0 >
O.OOS
0.008
(0.006)
< 1.50>
O.OOS
0.005
(0.0 >
< 0.0 >
O.OOS
0.005
(0.0 )
< 0.0 >
O.OOS
ZN
0.043
(0.026)
< 0.60>
0.034
0.097
(0.092)
< 0.62>
0.055
0.084
(0.116)
< 1.45>
0.037
0.176
(0.317)
< 1. 48>
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
S
no
AT
SD
S
no
AT
SD
S
SD
AT
SD
S
no
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
no
AT
SD
S
no
AT
SD
S
HD
AT
SD
S
HD
AT
SD
S
HD
41.1
< 1.46>
39.0
63.5
(15.9)
< 0.27>
62.0
70.1
(17.0)
< 0.20>
67.0
59.5
(12.8)
< 0.44>
56.0
55.0
(12.9)
< 0.1 0>
57. 0
51.3
(10.9)
< 1.20>
49.0
50.8
(17.1)
< 0.43>
49.0
33.1
( 5.4)
<-1.09>
35.0
62.0
( 0.0)
< 0.0 >
*****
38.0
( 0.0)
< 0.0 )
*****
33.0
( 0.0)
< 0.0 5
*****
0.012
(0.014)
< 0. 55>
0.004
0.059
(0.040)
<-0.04>
0.061
0.063
(0.047)
< 0.47>
0.061
0.190
(0.174)
< O.R9>
0.098
0.036
(0.022)
< 1.21>
0.032
u.038
(0.042)
< 0.66>
0.019
0.019
(0.009)
<-0.36>
0.021
0.028
(0.022)
< 0. 17>
0.024
0.465
(0.0 )
< 0.0 >
*****
0.650
(0.0 )
< 0.0 >
*****
0.231
(0.0 )
< 0.0 >
*****
0.0
(0.0 )
< 0.0 >
0.0
0.000
(0.0 )
< 0.0 >
*****
0.002
(0.0 )
< 0.0 >
*****
0.000
(0.000)
< 0.0 >
0.000
0.0
(0.0 )
< 0.0 >
0.0
0.001
(0.000)
< 0.00>
0.001
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0. 0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.031
(0.050)
< 1.49>
0.010
0.007
(0.003)
< 0.12>
0.007
0.005
(0.003)
< 0.42>
0.004
0.012
(0.008)
<-0.23>
0.013
0.009
(0.007)
< 0.91>
0.007
0.012
(0.007)
< 0.23>
0.012
0.008
(0.004)
<-0.33>
0.010
0.010
(0.005)
< 0.40>
0.009
0.006
(0.0 )
< 0.0 >
*****
0.004
(0.0 )
< 0.0 >
*****
0.009
(0.0 )
< 0.0 >
*****
0.020
(0.034)
< 1.50>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.029
(0.060)
< 1.79>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.034
(0.065)
< 1.50>
0.005
0.001
(0.0 I
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.016
(0.024)
< 1.50>
0.005
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 |
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
9.1
( 2.1)
<-0. 54 >
10.3
13.1
( 3,0)
<-0.48>
13.0
12.8
( 3.7)
< 0.17>
13.0
13.3
( 2.5)
<-0.96>
13.5
10.6
( 2.5)
<-0. 41 >
12.0
10.6
( 2.5)
<-0.64>
11.8
10.7
( 1.7)
<-0.24>
10.8
9.8
( 2.1)
<-0. 14>
10.1
13.5
( 0.0)
< 0.0 >
**»*
10.5
( 0.0)
< 0.0 >
****
19.1
( 0.0)
< 0.0 )
• **•
0.008
(0.006)
< 1.50>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.008
(0.004)
< 0.92>
0.006
0.006
(0.002)
< 1 . 12>
0.005
0.009
(0.006)
< 0.42>
0.005
0.005
(0.000)
< 1.50>
0.005
0.011
(0.011)
< 1.36>
0.005
0.005
(0.0 )
< 0.0 >
0.005
0.005
(0.0 )
< 0.0 >
*****
0.006
(0.0 )
< 0.0 >
*****
0.005
(0.0 )
< 0.0 >
*****
0.005
(0.0 1
< 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 l<
< 0.0 >
0.005
0.005
(0.0 n
< 0.0 >
0.005
0.005
(0.0 1
< 0.0 >
0.005
0.005
(0.0 I
< 0.0 >
0.005
0.005
(0.0 i>
< 0.0 >
0.005
0.0
(0.0 I
< 0.0 )
0.0
0.0
(0.0 )
< 0.0 >
0.0
0.005
(0.0 |
< 0.0 >
*****
81.4
( 36.0)
< 0.37>
69.0
145.6
( 80.5)
< 1.37>
122.0
105.5
( 24.3)
< 0.60>
105.5
96.0
( 34.8)
< 1.45>
84.0
123.0
( 43.5)
< 0.49>
110.0
54.0
( 36.6)
< 1.72>
39.0
145.2
( 55.2)
< 0.67>
124.0
113.4
( 34.6)
< 0.34>
98.0
56.0
I 0.0)
< 0.0 )
*****
30.0
( 0.0)
< 0.0 >
*****
75.0
( 0.0)
< 0.0 >
*****
0.005
(0.0 I
< 0.0 >
0.005
0.005
(0.0 I
< 0.0 >
0.005
0.005
(0.0 1
< 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 )
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)
-------
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
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00
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.6)
0 >
00
.0
.6)
0 >
00
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0 >
00
(
< 1
1
(
1.7
0.5)
.»5>
.60
1.1
0.1)
. 15>
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1.0
0.0)
. 15>
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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
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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
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< 0.0 >
••*»•*
16.9
( 0.0)
< 0.0 >
**»«•«
*••••
( 0.0)
< 0.0 >
2.0
( 0.0|
< 0.0 >
******
2.0
( 0.0)
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»•••**
2.0
< 0.0)
< 0.0 >
******
2.0
( 0.0)
< 0.0 >
*»*•••
2.0
( 0.0)
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2.0
C 0.0t
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2.Q
t 0.0)
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•*•»••
2.0
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*«••*•
2.0
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< 0.0 >
*•••*•
2.0
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< 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)
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»••**•
2.0
{ 0.0)
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0.0)
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2.00
2.0
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0.0 5
2.0
0.0)
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2.00
2.0
0.0)
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2.0
( 0.0)
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2.00
2.0
( 0.0)
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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)
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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)
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2.00
2.0
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2.00
X2
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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)
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0.0
0.0
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< o.o •>
0.0
0.0
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0.0
0.0
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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)
< 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
1.6
( 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)
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•••*•*
2.0
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< 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
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< 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)
< 0. 15>
2.70
2.5
( 1-7)
< 0.«6>
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
0.9
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
*¥
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
(
<
(
<
(
<
(
<
(
<
(
<
(
PBEIOt
5.5
( 6.4)
< 0.0 >
5.50
«.o
( 5.2)
< 0.71>
1.00
5.5
( 5.1)
<-0.00>
5.60
5.5
( 5.2)
< 0.0 >
5.50
«.7
( 4.5)
< 0.26>
3.85
1.5
0.5)
•0. 24>
1.60
1.7
0.8)
0.33>
1.50
1.3
0.6)
0.71>
1.00
1.3
0.6)
0.71>
1.00
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
( 4.6)
< 0.0 >
6.00
8.0
( 4.0)
<-1. 15>
10.00
1.3
( 0.6)
< 0. 71>
1.00
1.3
( 0.5)
< 1. 15>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0.71>
1,00
1.3
( 0.5)
< 1.1 5>
1.00
1.3
( 0.5)
< 1. 15>
1.00
1.*
( 0.*5)
t'.OO
I-TBHPIBBOL
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
1.3
( 0.5)
< 1.15>
1.00
3.0
( 1.7)
< 0.71>
2.00
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. 15>
2.00
2.8
( 1.5)
< 1.15>
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)
< 0.0 )
1.00
2.9
( 3.2)
< 1. 10>
1.»5
«
(
<
(
<•
(
<-
(
<
i
<
i
<
TOLOEVB
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
3.0
1.2) (
0.46> <
2.70
2.2
1.8) (
0.9O <
1.50
2.0
1.0) C
-0.06> <
2.00
1.8
0.8) (
-0.38> <
2.00
2.3
1.2) (
0.3*> <
2.20
3.*
1*8) (
1.0«> <
2.70
2.5
0.5) (
0.«7> <
2.50
TIICRLOlOETflllB
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 >
5.00
5.0
( 0.0)
< 0. 0 >
•»»**•
u.a
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
0.9
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
£
£
$
u
6
CO
.C
1
•o
a
u
*J
s
t> &
"* £ £
It N N
t- C C
-p E C
•ICC
o
£
1
^H
3
J
4
-e
•rl
t->
o
1
i
u
g
•e
(C
c
•H
-^
&
0
o
u
0*
&
£
-8
o
X
u
1
o
,0
.c
*o
i
&
&
•g
1
0.
£
U
-8
0)
4J
4->
O
o
•6
1
OJ
tc
CD
4-1
1
*>.
.0
•r«
flj
C
s
h
2
^
M"
,
aj
S
a.
0)
03
X
4-)
£1
4^
O
en
•H
O
OJ
CD
X
X
0.
>>
u
o
(U
£
1
X
UJ
Cv
1 1
-c t
4-1 CC
n X
1 ^
"C
0
-1
I
c
c
X
0.
_J
g
1
0)
I
-1
X
0*
0.
la
i
T)
X
flJ
^
X
_0>
4.
C
Oi
CC
X
&
c
-c"
1
1
o
1
a
X
Oi
E
1
f-4
O
£
D.
X
1
1
-3
£
CD
4-1
2
g
OJ
CD
C
(U
C
"o S
£ &
X (-.
2_ CL
g
!
^
0)
c
"g-
OJ
1
a
i
I
^
I
-u
0
£ "*
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
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( 0.0)
< 0.0 >
< 2.00
(
2.9
2.U
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( 0.0)
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2.5
1-2)
1.79>
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< 2.0
( 0.0)
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( 0.0)
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0.0)
1.79>
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I 0.0)
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( 0.0)
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( 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 >
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1.2
( 0-»)
< 1.79>
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( 0.0)
< 0.0 >
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I 0.0)
< o.o •>
< 1.00
< i.o
( 0.0)
< 0.0 >
< 1.00
< 1.0
( 0.0)
< 0.0 >
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< 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)
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( 0.0)
< 0.0 1
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C O. 0)
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( 0.0)
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J 0.0)
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( 0.0)
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( 0.0)
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1.00
( 0.0)
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( 0.0)
< 0.0 )
< 1.00
< 1.0
( 0.0)
< 0.0 )
< 1.00
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( 0.0)
< 0.0 )
< 1.00
< 1.0
( 0.0)
< o.o •>
<1.00
< 1.0
( 0.0)
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( 0.0)
< 0.0 >
< 1.00
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( 0.0)
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< 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>
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I 0.0)
< 0.0 >
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( 0.0)
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( 0.0)
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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)
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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
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( 0.0)
< 0.0 >
< 2.00
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( 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
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( 0.0)
< 0.0 >
<2.00
5.5
( 8.7)
< 1.79>
<2.00
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( 0.0)
< 0.0 >
<2.00
6.4
( 7.0)
< 0.83>
<2.00
<10.0
( 0.0)
< 0.0 >
< 10.00
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( 0.0)
< 0.0 >
<10.00
2. 3-DICHLOROAIILIIE
• ••499A^*A**A ** •* * ** "
(
<
(
(
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6.2)
1.68>
5.00
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6.6)
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5.00
5.0
0.0)
0.0 >
5.00
7.8
6.2)
1.50>
5.00
6.0
2.2)
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5.00
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1.50>
5.00
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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
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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)
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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)
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0.0
25.6
( 0.0)
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• •*•**
111.0
( 0.0)
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0.0
( 0.0)
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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
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<2.00
(
2.3
0.6)
< 2.00
4.7
( 6-1)
< 1.50>
< 2.00
2.0
0.0)
0.0 >
2.00
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0.0)
0.0 >
<2-0
( 0.0)
< 0.0 )
< 2.00
< 2.0
( 0.0)
< 0.0 >
< 2.00
<2.0
( 0.0)
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<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
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IV
so
S
no
IV
so
S
•0
IV
SD
S
BD
IV
SD
S
(ID
IV
SO
S
BD
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SD
S
BD
IV
SD
S
BD
IV
SD
S
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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)
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1.00
1.0
( 0.0)
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1.00
1.0
( 0.0)
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1.00
1.0
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1.00
1.0
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1.00
1.0
( 0.0)
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1.00
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1.00
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2.00
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2.00
2.0
( 0.0)
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0.9)
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2.00
3.7
3.7)
1.74>
2.00
( 3.5)
< 1. 17>
2.95
2.0
( 0.0)
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2.00
2.9
( 2.4)
< 2.04>
2.00
2.0
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2.00
2.0
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2.00
2.0
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2.00
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0.0)
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1.79>
2.00
2.5
( 1-1)
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2.00
3.0
( 2.1)
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2.00
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{ 0.0)
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2.3
0.5)
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2.8
2.2)
2.04>
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2.0
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2.00
2.3
< 0.5)
< 1.15>
2.00
2.0
I 0.0)
< 0.0 >
2.00
3«.3
( 0.0)
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0.0
( 0.0)
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0.0
0.0
( 0.0)
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0.0
0.0
1 0.0)
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0.0
0.0
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0.0
0.0
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0.0
0.0
( 0.0)
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0.0
50.7
( 0.0)
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••••*•
0.0
( 0.0)
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0.0
0.0
I 0.0)
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0.0
0.0
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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
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I 0.0)
< 0.0 >
<2.00
< 2.0
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< 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>
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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>
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( 0.01
< 0.0 >
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I 0.0)
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<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
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3D
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if
SD
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if
SD
S
(ID
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
< 0.0 >
1.00
1.0
( 0.0)
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1.00
1.0
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1.00
1.0
( 0.0)
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t.oo
1-HBTHTI.IiPHTlU.llI
Ftg)t9ftf999t944t£tt4t9
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2.00
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2.0
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2.00
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2.00
2.0
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2.00
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2.00
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2.6
( 1.3)
< 1.50>
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41.4
( 48.8)
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41.40
44.2
( 0.0)
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( 0.0)
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(
3.7
3.4)
<2.00
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( 0.0)
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( 0.0)
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<2.00
< 2-0
( 0.0)
< 0.0 >
<2.00
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( 0.0)
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llPHTHiLIIB 4-MOIILPUaOL OCTiDICilB
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2.00 0.0 <2.00
2.0
( 0.0)
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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)
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0.0
0.0
( 0.0)
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0.0
4.4
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2.00
0.0
( 0.0)
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0.0
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0. 0
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( 0.0)
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< 0.0 >
<2 nn
-------
Table C.27. continued
ho
0\
06864 *T
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a
no
06870 IT
SD
3
HO
06B80 IV
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3
HO
06681 IF
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06882 1*
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06887 IT
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S
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06889 AT
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0.0)
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2.00
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2.00
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2.00
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2.00
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2.00
2.3
( 0.7)
< 1.79>
2.00
2. a
{ 0.0)
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2.00
2.0
( 0.0)
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2.00
2.0
( 0.0)
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2.00
2.0
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2.00
2.0
( 0.0)
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2.00
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1.7)
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2.00
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2.00
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5.00
( 1.2)
5.00
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s.oo
5.0
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5.00
5.0
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S. 00
2.0
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2.9
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< 2.00
-------
Table C.27, continued
N5
06890
06891
06892
06893
06894
06896
BILL
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068*8
068*9
06852
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06855
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PBOP1ZIBB
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<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
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<-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
06856 AT
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 >
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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
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< 0.0 >
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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)
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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
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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)
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0.0
3.0
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3.00
2.7
( 0.6)
<-0.71>
3.00
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3.00
2.5
( 0.6)
< 0.0 >
2.50
2.7
( 0.6)
<-0.71>
3.00
2.5
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2.50
2.5
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2.50
2.7
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<-0.71>
3.00
2.7
( 0.6)
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3.00
2.7
( 0.6)
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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
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5.10
29.7
( «3.5)
< 1.01>
11.65
2.0
( 0.0)
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2.00
175.0
0.70>
31.90
11.4
( 1«-3)
< 0.71>
2.00
95.2
(129.5)
< 0.60
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862. 1
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< 0.71>
6.40
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( »2.8)
< O.«0>
33.70
0.0
( 0.0)
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0.0
18.6
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••*•••
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)
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0.0
2.0
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< 0.0 >
******
2.0
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•*«»•*
2.0
0.0)
0.0 >
2.00
2.0
0.0)
0.0 >
• »*•**
2.0
( 0.0)
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2.00
5.8
I 5.3)
< 0.0 >
5.75
2.0
0.0)
0.0 >
• •••*•
2.0
( 0.0)
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••• »**
2.0
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2.0
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0.0
0.0
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o.c
I 0.0
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0.0
0.0
( 0.0)
< O.J >
0.0
2.0
0.0)
0.0 >
0.0
( 0.0)
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0.0
0.0
( 0.0)
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0.0
0.0
( 0.0)
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0.0
0.0
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< 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)
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0.0
0.0
( 0.0)
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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 >
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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)
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3.0
0.0
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< 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
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••••••
2.0
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*• • *•*
0.0
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0.0
0.0
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0.0
0.0
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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)
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2.00
2.0
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2.00
2.0
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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)
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2.00
2.0
( 0.0)
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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
(
<
{
<-
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<-
(
<
(
<-
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(
<-
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<-
(
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(
<-
2.0
0.0)
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2.00
1.7
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2.00
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0.6)
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2.00
1.0
( 0.0)
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1.00
1.0
( 0.0)
< 0.0 >
1.00
1.3
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1.00
1.3
( 0.6)
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1.00
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0.6)
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1.00
1.5
( 0.6)
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1.50
1.5
( 0.6)
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1.50
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
< 0.71>
1.00
1.3
( 0.6)
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1.00
1.3
( 0.6)
< 0.71>
1.00
2.0
( 0.0)
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0.0
( 0.0)
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0.0
2.0
( 0.0)
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2.0
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2.0
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2.00
{
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2.00
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0.0)
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2.00
2.0
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•••**•
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0.0)
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2.00
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0.0
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0.0
0.0
( 0.0)
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0.0
0.0
{ 0-0)
< 0.0 >
0.0
0.0
( 0.0)
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0.0
0.0
( 0.0)
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0.0
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
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< 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
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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)
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2.00
2.0
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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
o
(M
O
»-<_
•
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
-------
Ol 1 O
34. 2
*_, Q 1 "7
Jl . /
cc
UJ
H
> oc o
-------
i
QC
LJJ
1-
1
o
H
X
t" QI q
j^ Oi . J
LU
Q
on o
d^:. J
+2.1
-2.
r
-
_^^— -^"
~
•^
—
w^
I
M
5
1
/x ^^
MEAN
H;
i
Nl
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
-------
3 7 «
UJ
CO
Z
UJ
z
o
o
cc
UJ
i
ULJ
O
<
oc
Ui
o
H
CC
UJ
CO
CD
O
LL
O
Q.
UJ
O
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.
o
H
cc
liJ
co
o
LL
O
z
H
Q.
UJ
a
SONDJFMAMJJASO
TIME (MONTHS)
Water Content as Indicated by Neutron Probe #TTU 4
535
-------
UJ
CD
z
UJ
I-
z
o
o
cc
UJ
H
5
7
4.3
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
31 "
31
30
29
28.9
29.0
28.4
.+ 2%
.8
3
2
7
J" 29.1
3 29.0
< 29.2
ffi 28.6
27.1
27.5
27.0
26.6
26.2
25.9
25.6
25.0
24.6
23.7
23.2
23.8
25.3
0.33
0.49
0.66
0.82
0.98
15
31
48
64
80
97
13
30
46
62
SONDJFMAMJJASO
TIME (MONTHS)
O
P
>
CC
UJ
OQ
O
LL
O
X
I-
o.
UJ
o
Figure D.16. Water Content as Indicated by Neutron Probe #TTU 5
536
-------
UJ
-J
o
13.4
20.5
20.7
19.1
17.6
18.4
19.2
19.9
20.8
21.6
.5
.0
.9
26.9
.2
U
O
O
cc
UJ
<
.3
.9
27.
.0
.8
.7
.8
.9
ni *- *•
£25.0
325.8
tt 27.0
UJ 27.4
> 27.4
< 26.0
24.2
24.3
25.8
k5.5
25.5
25.9
26.0
25.6
25.2
E+2% /Vv^
c — 2% /»s. •••*»»
E ^->^-A^ VW.
F •~-^r^>_J^>l™r'J ^
F *~~»~-^/ "
F "-»— ^^ "* "
F "~-^-d-^"^ •••---»
F '^-^A^'V^'*""'"*
F '-^-r^^*",-^^***^
F — «— »s/T '
p — — -_. J ^ J-
P — -, ^K-/ "-••—
F — ^V**- T^ ~~ "
F yv^^v'V^VwJ"'
' . ^ ..*"****""*
E x V ' '""*•
F — n_ j»i*--rv-
E -- -^ '-^- »*
£ . r .-r ^JT.-n»»4V'K
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1 Lift
1 . 4O
i en
1 . D4
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D . <1
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<^
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CL
UJ
SONDJFMAMJJA SO
TIME (MONTHS)
Figure D.17. Water Content as Indicated by Neutron Probe LCCIWR # 8
537
-------
O
p
>
CC
UJ
03
O
IL
O
Q.
UJ
0
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
------- |