CHARACTERIZATION  OF  OIL  SHALE  MINE  WATERS
      CENTRAL  PICEANCE BASIN,  COLORADO

                     by
                 K.  E. Kelly
               J.  0.  Dederick

                 Kaman Tempo
           Denver,  Colorado 80222

         Contract  No.  EPA  68-03-2449

               Project Officer
               Edward  R.  Bates
Industrial  Environmental  Research Laboratory
           Cincinnati, Ohio 45268

INDUSTRIAL  ENVIRONMENTAL  RESEARCH LABORATORY
     OFFICE OF RESEARCH AND DEVELOPMENT
    U.S.  ENVIRONMENTAL PROTECTION AGENCY
           CINCINNATI", OHIO 45268

                  MAY, 1984

-------
                                   NOTICE


    This document has been reviewed in accordance with U.S. Environmental
Protection Agency policy and approved for publication.  Mention of trade
names or commercial products does not constitute endorsement or recommenda-
tion for use.
                                    ii

-------
                             FORWARD

     When energy and material resources are extracted, processed,
converted  and  used,   the  related  pollution  impacts  on  our
environment  and  even on our health often require that  new  and
increasingly  more  efficient pollution control methods be  used.
The   Industrial  Environmental  Research   Laboratory-Cincinnati
(lERL-Ci)  assists  in  developing  and  demonstrating  new   and
improved   methodologies   that  will, meet  these   needs   both
efficiently and economically.

     This  report  provides  data characterizing oil  shale  mine
waters  from  the central part of the Piceance Basin  in  western
Colorado  and  assesses the effectivness of  retention  ponds  to
treat  these  waters.   The results should assist developers  and
permit writers in selecting appropriate controls for,the handling
'of excess mine waters.
                    David G. Stephan,  Director
                    Industrial Environmental Research  Laboratory
                    Cincinnati
                                i i i

-------
                            ABSTRACT'


     A  study  was conducted to 'character!ze  the  oil   shale   mine
waters  in  the  Piceance Basin.   The  study  sites   were   Federal
Prototype Lease Tracts C-a and C-b,   located  in the  central   por-
tion  of the basin.   The objective  was  to  collect water   quality
data  in order to characterize the mine  waters and to  assess   the
effectiveness  of treatment systems  located at these   facilities.
These  treatment systems involve  in-series  retention   ponds.    In
addition,  the effectiveness of a one-pond  versus two-pond  system
was investigated.

     The  sources of the water routed through the retention ponds
were  water pumped from the on-site  aquifers  that were  dewatered
during  mining activities and the water  pumped directly from   the
underground mines.  Water samples were  taken  from both the  inflow
and  outflow points for both the Tract  C-a  and C-b   pond   systems
and  were analyzed for a fairly detailed  suite of selected  water
quality constituents.  This suite included  total  suspended  solids
(TSS) and total dissolved solids (TDS),   pH,  the  major species  of
cations  and  anions,   and  dissolved   trace  elements   such   as
selenium,  lead,  and  arsenic.   The   inflow samples  were   then
compared  to  the outflow samples to  determine changes  in  water
quality and, therefore, the effectiveness  of  the  retention  ponds.
An  additional  part  to  this study  was   an  assessment   of   the
effectiveness  of  using a flocculent and  sulfuric acid   for   the
treatment  of  excess waters encountered  during aotive mining   on
Tract  C-b.   The  flocculent was added  to  reduce : the  suspended
solids  concentrations  during periods  of  active  mining   and   the
acid was used to reduce the somewhat  high  pH  values.             ;

     The water quality changes observed  during this  study,   when
comparing  the  inflow  waters  to   the   outflow  waters   of   the
respective  pond  systems,  were  found  to  be  generally   small.
Fluccuations  in  some  constituents  may  have been   due   to   such
phenomena as pH changes,  aeration,   evaporation,  and oxidation-.
reduction  changes  associated  with  the   transformation   of   the
groundwater  from an underground (aquifer)  environment to  a   sur-
face (retention pond) environment.    The  retention time,   as  well
as  inherent  laboratory  technique   variations,  may  also   help
explain the small fluctuations.

     The  overall conclusion with respect  to the  effectiveness  of
the  retention  pond systems in maintaining  or   improving  water
quality  is that they appear to make .negligible difference  unless
chemicals  are  added .   The addition of  the flocculent   in   the
Tract  C-b pond system during periods of  active mining  was   very
effective in reducing the suspended  sediment concentrations.    In
addition,  the sulfuric acid treatment reduced the, pH  at  Tract  C-
b.   Concerning  the  general  water  quality,  such as  the  trace
elements,  cations and anions,  and  other  pertinent constituents,
there  was  not  a significant increase  or  decrease  due   to   the
chemical  additives.    In addition,   the  effectiveness  of  the  one-
pond and two-pond systems are very similar  upon comparison.

                             -iv-

-------
                            CONTENTS-:


Forward                                                     iii
Abstract                                                     iv
Contents                                                      v
Figures                                                      vi
Tables                                                      vii
Acknowledgments                                           viii

Section                                                   .  Pagi

   1      Introduction and Background                         1
            Purpose and Objective of Study                    1
            Location and Description of Study Area            1
            Overview of Tract C-a and C-b                    17
               Development Activities

   2      Study Approach                                     22
            Constituents Selected for Analysis               22
            Sample Collection Points                         22
            Sampling and Analytical Procedures               25

   3      Data Discussion                                    27
            Water Quality Data for Tract C-a                 27
              and C-b
            Conclusions                                      40

   4      Quality Assurance Programs                         42
            Field Sampling Program Quality Control           42
            Laboratories Quality Assurance Programs          46

References                                                   49

Appendix

     A    Analytical and Field Data for the                  51
          Sampling Sites on Tract C-a

     8    Analytical and Field Data for the                  64
          Sampling Sites on Tract C-b
                              _ v -

-------
                             FIGURES


Dumber                                                    Page.

  1       Location of Tracts C-a and C-b   '                 2
            Study Area in the Piceance Basin

  2       Geologic Section of the Piceance Basin            3
            Along a North-South Line Between
            Tracts C-a and C-b

  3       Concentration of Dissolved Solids in              5
            the Lower Aquifer, May-September 1973

  4       Trilinear Diagram of Water Quality Data          12
            for the Upper and Lower Aquifers,
            Tract C-a

  5       Trilinear Diagram Presenting Groundwater         13
            Quality Data for Tract C-b

  6       Concentration of Dissolved Solids in the         14
            Upper Aquifer, May-September 1973

  7       Trilinear Diagram for the Geffrey Pond           29
            Inflow, Tract C-a

  8       Trilinear Diagram for West Retention Pond        30
            Inflow, Tract C-a

  9       Trilinear Diagram for West Retention Pond        31
            Outflow, Tract C-a

  10       Trilinear Diagram for the Pond A  Inflow,         35
            Tract C-b

  11       Trilinear Diagram for the Pond B  Outflow,        36
            Tract C-b

-------
                             TABLES


Number                                                    P age

  1        Lower and Upper Aquifer Baseline Water            7
            Quality Data on Tract C-a

  2      .  Lower Aquifer Baseline Water Quality             10
            Data Collected on Tract C-b

  3        Upper Aquifer Baseline Water Quality             15
            Data Collected on Tract C-b

  4        Surface Water Baseline Water Quality             18
            Data for Water Year 1975

  5        List of Constituents/Methods Selected            23
            for Chemical Analysis

  6        Tract C-a Water Quality Data                     28

  7        Comparison of Tract C-a Groundwater           .   33
            Baseline Data and Federal Drinking
            Water Standards With Holding Pond Data
            Collected During This Study

  8        Tract C-b Water Quality Data           ';         37

  9        Comparison of Tract C-b Groundwater              39
            Baseline Data, Surface Water Baseline
            Data, and Federal Drinking Water
            Quality Standards With Holding Pond
            Data Collected During This Study

 10        U.S. EPA Recommended Sample Preservatives,       43
            Volume Requirements, Containers, and
            Holding Times
                             - vii  -

-------
                         ACKNOWLEDGMENTS


     Dr.   Guenton  C.  Slawson,  Jr.  was  a  principal   initial
contributor  to the report.   Dr.  Slawson's involvement with the
report ceased when he joined the Rio Blanco Oil Shale Company  as
Manager  of Environmental Affairs.   His continued support toward
the  study after joining Rio Blanco Oil Shale Cornpany is   greatly
appreciated.

     In  addition,  Kaman  Tempo would like  to  acknowledge  the
support and cooperative interaction of Mr. E.B. Baker,  as  well as
others, of Cathedral Bluffs Shale Oil Company.
                              -  vi11  -

-------
                            CHAPTER 1

                   INTRODUCTION -AND BACKGROUND

PURPOSE AND OBJECTIVE OF STUDY                                  :

     The  objective  of  this  study was to  provide  a  detailed
characterization  of  the  mine water and  assess  the  treatment
systems  used  on  Federal Prototype Le-ase Tracts  C-a  and  C-b,
located  in  the  Piceance  Basin,  Colorado.  , These  data  were
collected to assist other' oil shale developers and permit writers
in selecting appropriate controls for the handling of excess mine
waters.   The treatment facilities at both sites consisted of two
in-series  retention ponds.   To characterize  these  facilities,
samples  were  collected  for determining the  quality  of  water
derived  from  mine  pumpage and  aquifer  dewatering  activities
previous to treatment,  as well as the treated water derived from
the  outflow of the in-series retention  ponds.   Presently,  the
treated  water is disposed of by reinjection into the groundwater
system, utilized for on-site activities, or discharged to surface
water  systems.   The data collection  procedures,  results,  and
quality assurance programs are discussed in Chapters 2, 3, and 4,
respectively.

LOCATION AND DESCRIPTION OF STUDY AREA

     Lease  Tracts C-a and C-b are located in the Piceance  Basin
of Rio Blanco County,  Colorado (Figure 1).   The ^climate of  the
Piceance Basin is considered to be semiarid montane.  The average
annual  precipitation  in  the central portion of  the  basin  is
generally  on  the order of 12 inches,  most of which  occurs  as
snowfall.   High  summer  temperatures coupled with low  humidity
create a high evaporation rate.

     The  Piceance  Basin is drained by  two  perennial  streams,
Yellow  Creek and Piceance Creek,  both of which are tributary to
the  White River.   The White River flows into the  Green  River,
which  is  a tributary to the Colorado River.   The base flow  of
Yellow  and  Piceance  Creeks is  provided  by  numerous  springs
throughout the basin.                                           :

     The  regional stratigraphy of the basin is comprised of  the
following Eocene units,  in ascending order:   Wasatch Formation,
Green River Formation, and the Uinta Formation.  In addition, the
Green  River Formation is comprised of the following members,  in
ascending order:   Douglas Creek, Garden Gulch, Anvil Points, and
Parachute  Creek.   The oil shale to be mined is located  in  the
Mahogany  Zone  of  the Parachute Creek  member.   A  generalized
geologic  cross-section  through the Piceance Basin is  shown  in
Figure 2.

     The  area  contains two important bedrock  aquifer  systems:
the  Upper  Aquifer and the Lower  Aquifer.   The  Lower  Aquifer
occurs  in  the Parachute Creek Member below the  ,Mahogany  Zone.
The  Upper Aquifer is located in the upper Parachute Creek Member

-------
o
CO
01
 o
 CO
oo
CO

 0)
 a
 c:
 
-------
                                                                                           O
                                                                                           oo
                                                                                            i
                                                                                           S-
                                                                                           o
                                                                                           O5
 in
 «
03

 O)
 O

 §
 O)
 u
•i—
Q_
                                                                                               res
                                                                                               CD
                                                                                           cno

                                                                                              -O
                                                                                           S-

                                                                                           -C
                                                                                               (O
                                                                                               fO
                                                                                           C  I
                                                                                           O O
                                                                                           O 4-5
                                                                                           0)  O
                                                                                           OO  ra
                                                                                            I   i-
                                                                                           o  c
                                                                                           S-  CU
                                                                                           •r-  
-------
and  the Uinta Formation above the Mahogany Zone.    The   Mahogany
Zone  acts  as  a  leaky aquitard between  the   Upper   and   Lower
Aquifers.

     Recharge  for the Upper Aquifer  dominately  occurs  along   the
rim  of  the  Piceance  Basin where   the  Green  River  Formation
outcrops,  although  downward infiltration of snow melt   probably
also contributes.   The downward potential difference between  the
Upper  Aquifer  and  Lower Aquifer indicates  that   most  ' of   the
recharge  for  the  Lower Aquifer occurs as leakage  through   the
Mahogany Zone from the Upper Aquifer.  The water in  both  aquifers
flows  toward  the center of the basin and,  in  some   locations,
discharges into Piceance and Yellow Creeks.

     In regard to water use within the Piceance  Basin,  there   is
no  extensive  use  of water from the  bedrock   aquifers  beneath
Tracts C-a and C-b.   This is probably due to groundwater quality
and depth considerations,  as well as the availability  of surface
water   sources.    In   addition,    there  is   rather   limited
agricultural, livestock, industrial,  and municipal development  in
the area.

     The  agricultural  development which does occur  within   the
basin  consists  of 5100 acres of irrigated hay  an:d  pastureland.
The  irrigation water for these activities is derived   domi-nately
from the Piceance Creek watershed during the months  of April   and
May.   In addition to the irrigated acreage in the Piceance Creek
watershed,  approximately 200 acres of irrigated land are present
in the Yellow Creek watershed.  This  land is irrigated with water
derived from Yellow Creek.

     The   existing  water  quality   within  the  basin   will   be
discussed separately as Upper Aquifer, Lower Aquifer, and surface
water.   The major source of baseline water quality  data  are   the
Tract  C-a and C-b operators due to the environmental  monitoring
requirements  associated  with the  Federal  leases.   Additional
sources  of  baseline  data,   particularly  for  surface  water,
includes  the  Bureau  of Land Management (B.L.M.) and  the  U.S.
Geological Survey (U.S.G.S.).

Lower Aquifer

     The  total dissolved solids (TDS) content for Lower  Aquifer
water ranges from about 500 milligrams per liter (mg/1) to nearly
40,000 mg/1 (Figure 3),  with the average 9400 mg/1.   Using   the
classification developed by Robinove,  et al.  (1958), this water
is classified as moderately saline,   although it can be briney  in
some locations.  Obviously, these high salinity  values render  the
Lower   Aquifer  unsuitable  for  many  uses  in  many  locations
throughout the basin.                                            :

     The  water is of fairly pure sodium-bicarbonate  type,  with
chloride as the only other major ion.   Calcium  and magnesium  are
very  low,  partly because of the minerals dissolved  are  sodium
salts,  dominatly nacholite.   Chloride is significant because  of

-------
                                            EXPLANATION
                            •     WELL
                        	1000	 LINE OF EQUAL DISSOLVED-SOLIDS CONCENTRATION
                                    Interval, in milligrams per litre, is variable
                                                              108°
       Base from US Geological Survey
       State base map, 1969
                            0
                                       10    15 KILOMETRES
Figure 3.   Concentration  of dissolved solids in  the Lower Aquifer,
             May-September  1973 (Weeks et  al., 1974).

-------
the  presence of -significant quantities of halite in the aquifer.
Trace  elements  in  the aquifer which  can  attain  rather  high
concentrations include barium, boron, fluoride, and lithium.  For
instance, even in regions of lower salinity, the fluoride content
is over 10 mg/1 , with extremes as high as 60 mg/1 common.   In the
high-salinity  region,  barium concentrations of 13  mg/1,  boron
concentrations of 120 mg/1,  and lithium concentrations of  6 mg/1
have  been  measure.    Baseline  water  quality  values  for  an
extensive  suite  of constituents measured for samples  collected
from the Lower Aquifer on Tracts C-a and C-b are shown in   Tables
1  and 2,  respectively.  This data has been tabulated to show the
minimum, maximum, and mean, as well as the standard deviation for
the  period  of collection.   In addition,  Figures 4 and   5  are
trilinear  diagrams  for  the  Upper Aquifer  and  Lower  Aquifer
baseline data .on Tract C-a and C-b, respectively.  These diagrams
provide a useful means for characterizing the groundwater quality
data.

      Aquifer                                                   ;

     The Upper Aquifer water quality does not exhibit the extreme
salinities or trace element concentrations of the Lower  Aquifer.
The water- quality for the Upper Aquifer in the basin does show an
increase  in  total  dissolved  solids from  350  mg/1  near  the
recharge  areas to over 2000 mg/1 in the basin center (Figure 6).
However,  this  increase in TDS is not accompanied by high  trace
element concentrations.   The water is of a similar type to  that
of  the  Lower Aquifer,  with a sodium-bicarbonate, character  and
moderately chloride.  However, unlike the Lower Aquifer, fluoride
and other trace elements have very low concentrations.   Baseline
water  quality data for the Upper Aquifer collected on Tracts C-a
and C-b are shown in Tables 1 and 3, respectively.  This data has
been tabulated to show the minimum,  maximum,  mean, and standard
deviation for the period of collection.

Surface Water

     As previously mentioned,  Yellow and Piceance Creeks are the
primary surface waters in Piceance Basin.  The location of  Tracts
C-a  and  C-b in relation,to these creeks are shown in Figure  1.
Baseline water quality data for four U.S.6.S.   stations  located
along  Piceance  Creek  and  a  tributary  to -Yellow  Creek  are
presented in Table 4.   These data represent the October, 1974 to
September,  1975,  water  year.   The description•of the U.S.G.S.
stations are as follows:

U.S.G.S. STATION                             LOCATION

   09306007                        Piceance Creek below Rio
                                   Blanco, Colorado; in SE1/4,
                                   SE1/4, Sec. 32, T2S, R96W,
                                   above Tract C-b.

   09306061                        Piceance Creek above Hunter
                                   Creek, in SE1/4, NE1/2,

-------





c
en
r— i
o
CO
o
CO
0£.
03
1
O
S
a:
^p.
O
a
j^.
i— .
i — i
	 i
:D
C3*

rv^
LU
3
UJ
h-H
LU
CO

co a
i






X
(0

c
ta

C ra

J_3 ("i
Conductivil
Total Dissi


to O
•* 0
•3- 00

LO en
CM •*






OO O
•si- to
CO CM
CM

LO •
to co
CO


tO CM
to i —


•* <*
CM »
OO f"»*




•Cf- r-l
en
r- « "St"

CD CD
LO CO
CM en


CO CM
LO CO
CM


O CO
co to








£>
'c S
la o
i — 03
«=C 0


to
OO
<— fl

00






r— 1

OO
*
en
LO


CM


"*.




t— 4
e
CM

r-l


CM
co"
CO


co
to








Magnesium


CM O
tO CM
CO tO

0 0
CM CM
r-l CM






0 0
1 — tO
i— i r— -
r-l CM

CO •*
r— 1 [^*
o
CO

CM CM
r-. r-.


co r-.
oo to
r-l CM •




to o
CO r-.
r— 4

O 0
CM CO
oo en
r-l CM


^i" en
co en
CM LO


r-. CM
to to







d)
Sodium
Bicarbonat


=f *=T
OO r-l
r— 1

r-l. O
0
« r— 1






to en
to 
tO LO








Nitrate
Sulfate


o
*

r-l






0
00

o
*
OO


CM
r-.


CM
0
to




LO
O


CM
00


LO
OO
*
to


I— (
to








Fluoride



-a
OJ

o







































-------





























































T3
(!)
3
C

4J
£1
O

- --

,—1
UJ
	 1
ca
«=c













s-
£
•r-
3
CT
cC
S-
CU
Q.
O.
=

















^
O)
<1-
•^—
3
CT


S-
CU

o



























S=
-o o
S- T-
tO •!->
T3 lO
d -f—
to >
4-> 0}
oo a

c
•r~
*—






x
(O


e

cu
S
•z.

•a s=
S- 0
tO -i-
-a +J
e to
(O *^™ '

OO  kO











CU
+J
lO (O
c CL c:
Jco O
0 i-

a. ca




00

p-».



^







co
LO


CO

OJ
CO
OJ
r~-



CO
«
LO



i— 1
e





OJ
CO





co
o
t_4


co
VO














o
•^
^~
•^
CO




en
a
^f



LO
0







co
c-H


CO
*
IO

OJ
I—.



t^*
en
a
OJ


LO
0





OJ
«
<£>
^^



LO
•
CO


I —
IJD















C
o
i.
I—"




VO
a
LO



t-H







LO
CO


OJ
•
o
<— i
LO
LO



.—1
OJ
e
i —


o

CO




t*^.
CO





co
1— t
r— t


OJ
LO
c
o
i-
(O

o
•^
^3
(0
01
0

HC3
CU

"o
CO
CO
•r-
Q




rH
0




0
V






•51-
o


<— 1
0


OJ
r-»


















-^•^
<-H
O
•
V
a
ca



!^,
«3













o
*^~
c
cu
CO
i_
«C


















«^™^
.-H
O
V
	 1
Q
CO


OJ
!*••


















^•^
r-H
C3
•
V
_J
O
ca



co
U3












gs
3
•1™
CU

*«
CO


















*•- ^ *~^
CO - — *• «~"1
O t— I • — • C3
V V V V
_J _1 _1 _l
Q a Q Q
ca ca ca ca


OJ i-l OJ OJ
r*^ ^~^ r*^* r*^









,








^~* *—** *~~*
r— 1 1— 1 r—4
00 — 0
• • l-H •
V V V V
_J _l _1 — J
Q a o o.
ca ca ca ca



co co co co
CD « — ' *«o ^o












E

^ cz E E
3-1- 33

S. 3 C -O
cu i — to to
^" gf PQ C_3




*— "^
-o
cu
3
sc
+3
o
c_>

















co
O) '
CO
cu
JH
4^
C
a>
a.
c
"r"

•o
cu
i %
(0
4^
(/)

+J
•i^
E

• —
sr
o
•r™
4->
O
CU
•a
«
CO
£
c
o
^J
o
cu
+J
cu
•o
5
o
[—
cu
ca

• *
— i
<"^
ca

-------











































^ 	 s
•o
CO
3
'|~l
C
O
o

^~i
UJ
CO
•a:







s_
<£
3

•O ro
E -r-
res >
4-> CO
t/5 Q
•r-
s





X
res


£=
re
CO

•y


-a c
S- 0
ro T-
•a •(-»
C ro
res -f
t/0 O>
o


c
s:

X
(O
^-
2.



c
ro
CO



Z





"£f
CO
33
>r-
in
O
^™^




t^O ^3 «—•*
o co t— t
• » •


-j _J -J -J
O Q Q Q
CQ CQ CQ CQ

r^ ^~l *1^ ^"^
o o o o
V V* V° V


CVJ CO LO CO
CD r-- i —
CVJ


i — 1 CTV LO P*^
o o oo i— i


1—1 cvj cvj cvj


CVJ «=J- LO LO
O O LO O



,— t <— 1 ^H 1— 1
o o o o


LO CVJ tD LO





I— 1 CO O rH
O O <0
• • *



CO t-» VO CO
10 <0 10 VO








CO
E to
3 CO
.? i- c
E CO re
O Q. T3 C35
S- Q. re C
j= 0 CO «
o o — is:


<— 1
0
*


Q
ca
,_!
o
V


o
o


cvj
o


co
<0

LO
o



0
o


en





CVJ
0
*



oo
10










r—
CO
o
•I—
•z.


CVI
*



Q
ca
^
o
V


LO
LO


oo
LO


co
10

o
LO



i-H
0


LO
LO




10
"



10











o
c
•p-



















•
to
CO
to
CO
c;
rO
CL

E
^
CO
ro
to
to

]s
r_

c:
o
o
CO
CO
-o
to
+j
'i
•r-
O
•r—
O
CO
-t->
CO
•o
o
CO
CO

a •
_J
a
ca







* •

0
•r—
Q.
CO
O
X
CO
05
•r™
S
o
CO
-C
4~>

g™

s_
co
p—
s_ .
CO --^
Q. tn
t/) *f*~
CO 3

cn a:
•p- n.
M^ 3=
E o-
r^" e A

"~ s_
co co
S- •)->
ra CO
E
tO T-
CO "I-3
3 ^Z
r— CO
re U
s_
E CO
3 Q.
•i- to
c: o
•i— .c:
-S !
c o
rS 'g
»-_^
E
S •+•>
X >
o
«> 3
c -o
re c:
CO O
S O
*

-------









-i
r*.
en
2
1
_,
O

LLJ
— J
-T-
to

•^
ii
•=>
U
U
1
UJ
h-
U
LU

g
1

_J
i
C£
LU

LU
5
«C
CO
ce
LU
LL.
g.
ee.
1
«J


CSJ
s













•a c
S- 0
re-^
•o -u
c re
re i-
K|



I

X
£


c




14-
0 1
re tn
M 


0)
5

IB 4-9
SE VI
O C
5 s
K-
z -o c
UJ &- O
o re •»•
z -o -M
o e re
*j >
t/> Ol
-a

e
re
01

X
re




£


O 1
s_ > tn
HI


_j_*
g
s



=
o




o




CO
o

CO

1— 1
g

0
V




U)





HI


•o
o

0
s
jj


o

CM

o
o

s"



to



en



^
•J


u
3
•d
c
o
u

CO






eo
0

eo

LO
0
o
V





en







c
o

"9-
G5
O


n^

00

CO
en




eo



en











a.

to co ~*
O CM CSJ .

O



CO O 1-1
O —" t-i
o

^- en o
o •-*

CO 0 LO
§•
•-< i— i

o





r- p» en



S

3 In

•a -c =
re •*-» en
o> *^ re
-j — i s:

§CO 0
eo to
!— 4


O CO tO
en CM **


o o o
o to en
C3 ^T CO
CM


to O O
LO
CO



en co co

•o
01

"o re
tn ^1 re
tn Q. e *•> c:
t- i—O 01 0
•a re i- ^ i-
tn 4J *J
*— -o tn re tn re
re '^ in •?- tn •»-
•u i— o-o o -a
o o t. re s- re
h- in cs s- cs t.

en p*.
o o
• o
0 0 •
CJ


^^ o
d 8
o

to r»
• CsJ
0 8.
o
CSJ CO
8 |

O O
<— ^
V



00 ' «•



01
01 >>
c &.
re 3
en u
c s-
« _«

—• CO
^-< CO



O CO
*-t CM


O LO
i— 1

•

»-4 CM




CM CM

re
u en
c o
re
i- 01
o >
C i— C
•— o o o
re ja tn ja
*-> s- tn s.
o re -^ re
h- u o u


o

O



^
o
0

CM
0


8

O
V




CM



f
01
•o


i

o



CO'

o

CM




CM
8

o

LO









^

<




; a



^^
0

g
O

i-4
8

o
V




o






o>

u
z

CO



r*



8
CSI



«— *
0



CO






re

c


<




o



vo
0

**•>

CSI

cp
V





en




a>

re
s.
•t—

i
i



i
i
t

0
•



a




^






c


4-»
c
4

O' 16
^™l CO

. o



Cft ^^
« CSI
o
' V

. r** o
• CSI
' o —i

^H t-H
O
o





!
en co



(U £
i re i-
£ C/l
CX tf)
t/i re
O 4->
S £

CO f-
C
v • •"*
O



CM 03
O •
0
O

CM CO
O



^H CM
8 °-
• o
0

eo P~






u

c: 3
01 1-
tn &.
I- re

-------
"2 §
tO -F-
c to
tO **-

"$

e
to
£

X
£



c

O 1
ro (/>
i. > C
 •«->
3.O 10 '
Z O >



•£
3


«O +•»
z in
H™ f_ *
g
1 11
Z •§ 4J
o =_ra
^j >
bO O)
•o



C
(O

^^

X
(O

s£


**-
O) W C
"H Si '?
— ^-g*1
1
.=
c
o

CM 3
UJ »f—
s 1

CM
O




O
O

°l
o



o
o



^
^






E
3

•5
IX

i
i
i






i
i



§
o
o



CO
«— 1






E
3
1

§ I

ej o


i i
0 O

o o

0 O


o o
o o
3 9



n» co
"3- CM






§E
3

•5 c
c a>
fO F—
U 0)
to to

o o
o o
in





o vo
0 CO

^>

*
to
CM
o vo
o o
VB


5 S





s
to
c
o
j3
i- C
(O O
U S-
••- o
CO CO

•*•




2


CO




CM




en
^




0)
X
0
"5


T*

c
CO

i 1

«•


t o
1 O
i in
CM

CM O
O 0
0
O •

^*
Z §




en en
^«









CD 3
> •*•
f— "a
« CO

i






i »— i
t



•-• O
• CM
O CM

a CM



«r en






g g
•S ^
CO ro
r_> O

K^
CM




CO


O
I-H




O




en







^


1
to

o
en
•cr






o
CM
CM



|
CM
-



5






S
(O
c
0
-e
ra
O

CM 1
en i
i




ro i
i


o — «
in o
CO O

o
,v
CM CO




en -*
^







a> £

£ IT
~- o
to r—

co o
o' S
CM





CM 0
O
O CM

|Mt

0- O
o
CO
tt
en
g -
o
V

ic en






E 1
5 e3
C/l 1^
U -C
CJ U

CM 1
• I
O I




«-4 1
c 1
O I


i-< in
o

o


o
o



r~ co
*T »— t




•

E C
3 O)

C U>
ro O
4-> C
£ |2

I 1
0 O





en 10
o o
o o

o o
V
3 I

CM ^H
O O
O O
ep o
V

5 3






E
I 1
O O

! CM
I O
1 •
o



1 »— «
1 0
o

o •

^3


S 8
°



O r--







g
E 3

"E: ra
ro C
= 5

0- 0
r— t t— t
o






O CM
o


en co
O ^

CO •»
8
o


10 en







33
•o
c
o
U


tn
o
a.
a>
u
X
01

01
•§
"o
1
i.
OJ

*^
s_
Sl-d

-------
                                                        TRACT C-A


                                                        LEGEND

                                                          ° LOWER AQUIFER
                                                          • UPPER AQUIFER
Figure 4.  Trilinear diagram of water quality data  for Upper and Lower
           Aquifers, Tract C-a (data from RBOSP,  1977).
                                    12

-------
                                                       TRACT C-B
                                                        « UPPER AQUIFER
                                                        9 LOWER AQUIFER
                                                        ° SEEPS AND SPRINGS
                                                        • ALLUVIAL WELLS
Figure  5.   Trilinear  diagram presenting groundwater quality data for
            Tract C-b  (data from  C-b Shale Oil  Venture,  1977).
                                     13
                                                                            v

-------
                                                EXPLANATION
                                •    WELL

                                <»»   SPRING

                           • - 507 - LINE OF EQUAL DISSOLVED-SOLIDS CONCENTRATION
                                        Interval 500 milligrams per litre
                                                                 108 •
       40°
        Bue from US. Geological Survey
        State base map, 1969
                              0
                                       5
                                     i  I
                                        10    15 KILOMETRES
Figure  6.  Concentration of dissolved  solids  in the  Upper Aquifer,
            May-September 1973  (Weeks et al.,  1974).
                                           14

-------








-
CV
LU
^~
z
UJ
_1

o
LU
_l

LO
J2
0,
ja
i
u
H-
U
s
z

o
LU
H-
a
«i
— j
0

o
>-
^™
g
at
UJ

_j
LU
cC
ea
ce
LU
u.
1
os
3
• 0
CO
LU
—I
OQ

•o

c
i
x


c
£



O 1
s-SS




=

*•>
4-9

o
u
"z
o
£ -1
Oi "O 4^
LU 4J ">
O C/l 

tfl
C
O
o
0





s
0
CO
o
o

o
o
o
V



to
•3-








£
•5
o



g
p^



o
-"
1


o
o
CO





CM
LO




4^


^
u
3
•o
c
o
CM
*-*




LO
O
-


°
C3
V




t»J
LO









g




CM
O



to
CO
oi


1-H
CO





CO
LO









3:
Q.
O
o




^^
o
o
o
o

CM
g
o
V



CM
L
o
V)
Ul
•5
Ul
i"^ ^3
o "o
! § S §
0 S

o


i CM .— «r
t «r • o
g
o
1— 4 O tO •— '
• LA • *O
CO i-H O O
0
o
1 CM CM 0
a' 1

o
V


«M m rn ov
in if) to «•





§0)
in

•^ OJ (O 3
=c c: cn u
^ en c s-
•**• CO A3 
«J E S £


in co CM i
i



to co co •
1
f— « f) O> 1
CM CO 1


00-|
1





S 5 S :

u
*c
u o*
ra co
-.= __« «


+J 4-> C ^- C
(Am en « p— o oo
(/> i— Wl I"" CO .O Vi ijQ
O "D O*O •*-» 1- on i-
C5 S- C5&. H- O O U
CM
0
o




CM
o
o
o


O
O




r^
^T





s
3
C

i->
,2*




0



ro

«»•


§
O




•a-







§
^
E
3
<
CO
0
0




CM
O
0
o
o

^
0
o
V



0
L£)








"a;
"o




2



CM

cn
!**.


*
o





LO







(0
"c
|
LO
0




p-1
^"
o
CM


CM
O




CM
IA







4J
a
i




i
i



1
i
S
0


Z





t-4







c
_E
•M
«
s
o




en
O
?:
O:


.1




•— <
LA





OJ

J=
a.
0




S
o



t— i
o
g
0


o
o
o
V



LO







u
"c
tt)
Ul
cC
to
CO





„

g
*-<


«— «




CO
^r





s

"ui
Ul
2




0



— .
o
to
o


I
o




LO








g
'C
CD
^~
3

^
O
u




















































15

-------


































































1
e
c
— •


S

•o c
s- o
10 1-
•o +»
c re
(O 1—

««



C
re
E

X

c
^


o >

s- > c
OJ S- O

z o >




—
c
0)
I
c
o
o
10.
•— -O C
t— s. o

e: -o -w
i— c re
Z 101-
UJ -*J >
O (/) O)
o
C_!
c
1



X



c

5



O 1
10
w > tf>




z o


4->
01

*J
v»
c
o
u

•—a
O
o






CM
O
0

in
0
O

I
{£
v



o
in








S
•a
P





i
i
i



i
t



o
o
o

C5








«— i







E
3

0)
ffi

OJ 10
§CM
0
0 0





tn vo
8 S
O 0

o o
o- °'

o o
o o
o o
V V



in co








s e
1 1
03 f—
O U
C/3 G1



LO (O
CM •
LD CM



O ^
Ct •
r^> «— *



o *-<
.— i
CM

O ^"<

PO •






in tn






OJ







• I • I O O ill
o o •
o

«iexi-««)i«o,oi
OimCMOCMlOO--! " 1
• 1 • 1 O • III
0 0 • 0
o



~ g o * ~ e « - « g g g -

? " = o- o- V

UJOOCJOLL.CDC3IC





cu
o.
<«
^
H
u
o
u
5
1
to
•o
u)
4J
C
3
J=
Q.
Ic.
.0

0)
"S
5
c
OJ
u
s-
(U
a.
en
O
1
u
E



•<->


«
3
1
8
c
o
^
a.

-------
                                   Sec. 27, T2S, R97W, below
                                   Tract C-b.

   09306235                        Corral Gulch near Rangely,
                                   Colorado in SE1/4, NW1/4,
                                   Sec.5, T2S, R99VI, a trib-
                                   utary to Yellow Creek above
                                   Tract C-a.

   09306242                        Corral Gulch near Rangely,
                                   Colorado in SE1/4, NW1/4,
                                   Sec. 25, T1S, R99W, a
                                   tributary to Yellow Creek
                                   below Tract C-a.

     The total dissolved solids concentration for Yellow Creek in
the  area  of Tract C-a ranges from 664 to  1140  mg/1,  with  an
average  of  735  mg/1  upstream  from Tract  C-a  and  851  mg/1
downstream  from Tract C-a.   The major cations of  the  baseline
water  quality for Yellow Creek consist of sodium,  calcium,  and
magnesium, whereas the major anion is bicarbonate.  There are not
any trace elements present which obtain appreciable  values.   In
general,  the  water quality of Yellow Creek can be characterized
as magnesium-calcium-sodium bicarbonate type, very, similar to the
type  found  in the Upper Aquifer,  which provides, base  flow  to
Yellow  Creek.   In addition,  the water quality of Yellow  Creek
degrades  downstream,  as  indicated  by the  increase  in  total
di ssolved solids.

     The  baseline  water  quality for  Piceance  Creek  is  very
similar  to  Yellow  Creek.   Total  dissolved  solids  range  in
concentration from 502 to 1050 mg/1,  with an average of 698 mg/1
upstream  from  Tract C-b and an average of 893  mg/1  downstream
from  Tract C-b.   The major cations of Piceance Creek consist of
sodium,  calcium,  arid magnesium;  whereas the dominant anion  is
bicarbonate.    In  regard  to  trace  elements,  none  are  very
important.   The  water  quality of Piceance Creek1 is  also  very
similar to the Upper Aquifer water quality.   In addition,  there
is  a  general  degradation  of water  quality  in1  a  downstream
direction, as indicated by the increase in total dissolved solids
from an average of 698 mg/1 to 893 mg/1.

OVERVIEW OF TRACT C-A AND C-B DEVELOPMENT ACTIVITIES

     Kaman   Tempo's   sampling   activities   occurred   between
September,  1981  and March,  1983.   The specific dates for each
sampling effort were September,  1981;  May, June, September, and
November,   1982;   and  January  and  March,  1983.   To  better
understand and interpret the analytical data,  the activities  of
the operators for Tracts C-b and C-a will be discussed below.

Tract C-b

     The  principal activities associated with the development of
Tract  C-b during the sampling project were the continuation  and


                              17

-------
                                        LOCM'd-COtOOCnO.'—'LOCO
                                        ID    to    cn  '    •    CM          «a-    o      •    CM      •
                                        •^                       -3-          co    CM    co      -
                                                                              CO    O
                                                                              tO    CM
                                                                              to    co
J§
                                         CM    CM
                                         CO    ^O
                                                     r-t    LO    CM
                                 • LO    LOLOCnLOLOLOLOLOLOOLO
                                  CMCMCMCMCMCMCMCMCMCMCMCM
                CM    CO
                o    *-*
                                                     OtOCOO^OtOtOCO
                                                     CM     •    «-*          CM    *-*     •      •      •
                                                     .-i    1-4    LO          «a-    co    cn    •—'
                                                                              CO    CO    (*«.
                                                            cn    cn    en    cn    cn    cn
                o    co    CM    o    cn    to    o
                  .i-lO          LO    tO    O
                                   —«   co    co
                                                            o    co    cn
                                                 ^-    o    to    cn    cn

                                                 LO    CO
                 CM    o    ^*    to    P*»    cn    co
                   .      .    o    o     •      •    T=r
                 ^o    r**      •           co    to    «—«
                              r-s.    CM    to    CM    cn    LO    cn

                              co"    LO    «—<    «a-    CM    co
                 CM    CU    CM    CM    CM    CM    CM
                 (-tCMO^*«3>'*LO<::l'OOOOOS.LOLOi—iococncncMCO

                 ^   S    5    S    °i   ~    *    ^    S    "J    r>j    S
                 CVi           .      .cOtOLOCOLO'-i<3-'-1
                 to    r-»    co
sKgsassasssss
                  a;
                  £"
                                                 on     S
                                                 a>     3

                                                 cn   TD
                                                 ID     O
                                                 S    t«
                                4J.   U
                                O    -i-
                                o.    ca
                                      c    •*-»••-
                                      o     «     z
                                      J3     =    ••-
                                      1.     0    r—
                                            ja     .a
                                             i-    ^:
                                                        i—    i—    •t-'     3
                                                                     18

-------
                           O>    O    O    Ol    O    «
                           o    
-------
                                                  —-*   o   o
                                                  1-1   O   O
                                                   V   CM   CM
2
P*»    O


CM    CM
                                            UD


                                            CM
§    ":    «
O    CO    CO
                                            LO    CO    CO    t-H    CO    LO
         O    O   O   O   LO
                                                        o    o
                                                        o    o
                                                        CO    CM
        CM   •-(   CO
                                                  ca    o    o    LO    r*-
                                                        o    o     -   • .
                                                        CO    CM    CO    CO
                                CMc\JcncM«-it-HCMcn
        CM    vo    co    ca    r*«»    ca    «—i

        CM    i—i    r-          en
                                                           O    «*

                                                           CM    LO
        CM    CM    CM    CM

                                                                                         £
                                                                                         (Q
                                                                                         a.
        o    o    o
                                                        o    o

                                                        CO
                    Ol    —l«T—JOOCOCOC3LO
                     •    o     -a     *cao     »co      «
                    O%    CD    O    CD    f—I          ^o   vO         sO
                                                                                        ^
                                                                                        o
                                                                                        CJ
                                     l—    01   r—
                                                             20

-------
completion  of  three  major  shafts.    In   addition,   the   water
management program to treat and dispose  of  waters Associated  with
the  mine  dewatering  activities  was   expanded.    This  program
consists  of  pumping  the excess mine   water   derived  from   the
dewatering  of two of the shafts  into two retention  ponds   (i.e.,,
Ponds A and B) which are in-series.   The retention  ponds outflow
water  is then discharged to Piceance Creek, . reinjected  into  the
groundwater system, or utilized for on-site  sprinkler  irrigation.
These  activities did not vary over the  duration of  the   sampling
project.

     The  mining  activities associated  with the  development   of
Tract C-b were rather sporatic during the project.   For instance,
mining  activities were not very  active  during  the first  half   of
1982, and virtually non-existent  after September, 1982.   However,
activities were fairly brisk during 1981.

Tract C-a

     At  the end of 1981,  Rio Blanco Oil Shale  Company  (RBOSC)
nearly  completed the 4-1/2 year  development program designed   to
determine the technical,  economical, and environmental viability
of  the  modified in-situ (MIS) recovery process.    This  program
resulted  in the ignition of Retort 1 on June,  1981.   Retort   1
burned through December of 1981,  at which time  it was  shut-in  and
is presently cooling down.  Due to the retort activities, aquifer
and surface water quality data collected after  June  of  1981,   are
not considered to represent baseline conditions (RJ30SC, 1983).

     The next phase of development was intended to determine   the
viability   of   Lurgi  surface   retorting   activities.    This
demonstration was temporarily suspended  on August 1, 1982.

     The dewatering operations during the initial sampling  effort
(September,  1981)  consisted of  two upgradient dewatering  wells
and mine sumps.   In November of  1981,   the  use of the  dewatering
wells  was  discontinued,  although pumping  from the   mine  sumps
continued  to  dewater the mine.   The water from the   dewatering
operations is treated by two retention ponds which are  in-series.
The  treated  water is then reinjected into  the  Upper   Aquifer.
There are no surface discharges.  In addition,  water derived from
the   Retort  1  burn  is  pumped  to  another  treatment   system
consisting of non-discharging evaporation ponds  and,   therefore,
was not sampled during this project.                             ,
                              21

-------
                            CHAPTER 2

                         STUDY APPROACH                         ;

               CONSTITUENTS SELECTED FOR ANALYSIS

     To  best  characterize the water derived from the  mine  and
dewatering  activities,  as well as the treated water,  a  fairly
extensive suite of constituents was selected for analysis.   Many
of  these  constituents  have also been identified  as  potential
pollutants    from    studies   conducted   on    the    chemical
characterization  of  simulated and observed  in-situ  oil  shale
process water (e.g.,  Fox et al.,  1978;  Slawson,  -1979; Pfeffer,
1974; Stuber and Leenheer, 1978; LBL, 1978).

     The constituents selected for analysis during this study are
shown in Table 5.   In addition, the methods of analysis for each
constituent   are  also  shown  in  Table  5.    This  suite   of
constituents  was  divided  into  a comprehensive  group  and  an
abbreviated  group.   Analysis  for  the  abbreviated  group  was
conducted during the months of September,  1981; September, 1982;
and  November,  1982.   Analysis for the comprehensive  group  of
constituents,  which  also included analysis for the  abbreviated
group,  was conducted during the months of May, 1982; July, 1982;
January,  1983;  and March,  1983.  The analytical and field data
collected  during this study for Tract C-a and C-b are  presented
in Appendices A and B, respectively.

SAMPLE COLLECTION POINTS

     An overview of the development activities on both Tracts C-a
and  C-b  was previously discussed in Chapter  1.   This  section
identifies the sample collection points on each tract, as well as
discusses the mine dewatering and water treatment activities.   '.

Tract C-a

     The  water from the mine on Tract C-a is pumped from  levels
within the mine and the mine shaft to the Jeffrey Pond,  which is
the  primary retention pond.   After preliminary treatment in the
Jeffrey Pond,  the water is discharged to the West Retention Pond
for  secondary treatment.   The West Retention Pond is  in-series
with the Jeffrey Pond.   The treated water derived from the  West
Retention Pond is then reinjected into the Upper Aquifer.       :

     The   sampling  points  on  Tract  C-a  consisted  of  three
locations:   (1) the mine outflow into the Jeffrey Pond,  (2) the
Jeffrey  Pond outflow into the West Retention Pond,  and (3)  the
West   Retention  Pond  outflow.    This  approach  allowed   the
evaluation of the total treatment system.   For example, sampling
both the inflow and outflow of the primary retention pond  (i.e.,
Jeffrey  Pond)  provides an indication of the effectiveness of  a
single retention pond.   In addition, sampling the outflow of the
secondary  pond  (i.e.,  West Retention  Pond)  demonstrates  the
effectiveness of the treatment system as a whole.               '.


                               22

-------
                             TABLE 5               '   .'•

  LIST OF CONSTITUENTS/METHODS1  SELECTED FOR CHEMICAL ANALYSIS

Abbreviated Analysis

    CONSTITUENTMethod
CONSTITUENT
Method
pH                         Field-
Temperature                Field
Conductivity               Field
Dissolved Oxygen           Field
Ammonia                    350.3
Arsenic2                   301A.VII
Bicarbonate                310.1
Boron                      212.3
Carbonate                  310.1
Calcium2                   301A.II
Chloride                   325.3
Fluoride                   340.2
Iron2                      301A.II
Magnesium                  242.1
Mercury                    245.1
Molybdenum                 246.1
Nitrate                    352.1
Nitrogen                   351.1
Potassium                  258.1
Selenium                   270.3
Silica                     370.1
Silver                     272.1
Sodium                     ---3
Sulfate                    375.3
V an ad i urn                   ___ 3
Dissolved Organic Carbon   .--7
Total Dissolved Solids     160.1
Total Volatile Solids      160.4
Total Suspended Solids     160.2
Total Solids               160.3
Settleable Matter          160.5
Bari urn
Beryllium
Cadmi urn2
Chromi unr
Cobalt2
Copper2
Cyan i de
Fractionated DOC

Lead2
Lithium
Manganese
Nickel2
Orthophosphorus
Phenols
Phosphorus
Silver2
Strontium    EPA
Sulfide
Thallium
Thiosulfate
Tin
Titanium
Tub i di ty
Uranium      EPA
Zinc
208. 1
210.1-
301A.III
301A.III
219.1
301A.II
355.2
USGS
Report4
301A.II
AA8
243. 1
301A.II
365.1
420.2
365.4
301A.II
Report 5
376.1
279,2
NSM9
282. 1
283.1
180.1    '
Report6
301A.II
                           (continued)
                               23

-------
 TABLE  5

                            (continued)
   11   methods   are  from  U.S.   EPA,   1979.    Methods   of   Chemical
       Analysis   of   Water  and   Wastes,   EPA-600/4-79-620;   unless
       otherwise  denoted.

2Methods  from American Public  Health  Association,  1976.   Standard
       Methods for the Examination  of  Water  and  Waste  Water.   14th
       Ed.

3Method   from U.S.   EPA,   The  Inductively Coupled  Plasma   Optical
       Emission  Spectrometric Method  (Method  200.7).

^Analyzed  according  to method  stated  in:    U.S.  Geolog.   Survey,
       1979.   Analytical   Method   for   Dissolved   Organic   Carbon
       Fractionation.  USGS/WRI-79-4.
5                                                                :
 Analyzed   according to  method  stated   in:   U.S.  Environmental
       Protection Agency,  1975.  Interim  Radiochemical  Methodology
       for  Drinking  Water.   EPA-600/7-760-093.

 Analyzed   according  to  method stated   in:   U.S.  Environmental
       Protection  Agency,    1979.   Radiometric  Method   for   the
       Determination  of Uranium  in  Water.  EPA-600A7-79-093.

 Analyzed  on a Coulmetric  Carbon Analyzer.
o
 Analyzed  with Atomic Absorption.
g
 No standard method.
                               24

-------
Iract C-b                                                       :

     As with the treatment facilities  on Tract C-a,  the Tract  C-b
facilities  consist  of two retention  ponds  which  are   in-seri.es.
The water from the mine production  and service shafts   dewatering
operations are pumped  into the primary retention pond  (i.e., Pond
A).   After  retention  in  Pond  A,   the water  is   treated  with
sulfuric acid and a magnifloc cationic flocculent  to  lower the  pH
and settle the suspended solids,  respectively.    This  water then
flows into Pond B via  gravity for additional retention.   The acid
and  flocculent  treatment was discontinued  in   September,   1982,
when the mining activities terminated.   After this   date,   chem-
icals  were not used in the treatment.   The treated  waters  were
then  subject  to one  of the following modes  of   disposal:    (1)
discharge to Piceance  Creek, (2) on-site sprinkler  irrigation,  or
(3) reinjection into the Upper Aquifer.

     The   sampling  points  on  Tracts  C-b  consisted   of    two
locations:   (1) the inflow into Pond  A,  which  is  water  derived
from  the dewatering of the shafts  previous  to treatment  and   (2)
the treated water discharge from Pond  B.  The discharge from Pond
A  was  not sampled since the effectiveness  of treatment  with  a
single  pond was evaluated on Tract C-a.   By sampling  the inflow
and  outflow  of  the  entire  treatment  system   on   Tract  C-b,
comprehensive  analytical  data  for   the  effectiveness  of   the
treatment system as a  whole were collected.

SAMPLING AND ANALYTICAL PROCEDURES

     Grab  samples  were  collected in the field   from  the  dis-
charging water at the  various sample collection  points  previously
discussed.   Immediately  upon sample  collection,   the  following
constituents  were  measured in'the field with   portable  instru-
ments:   pH,  specific conductance, dissolved oxygen,  and temper-
ature.   Samples  which were sent to the laboratory  for   analysis
and  required filtering were also filtered in the  field through a
standard  .45   micron  (ym) membrane  filter  with   a   Skougstand
filter apparatus.   A  Gilman stainless steel filtering  apparatus
was used to filter dissolved organic carbon  samples  through  a  .45
ym silver membrane filter.   After  filtration,   the  samples  were
preserved  and  cooled  with ice according to  U.S.   EPA  (1979a)
recommended procedures and placed in ice chest for  shipment.   The
samples  were  shipped via commercial  bus to  both   the   Colorado
State  University (CSU) laboratory  in  Fort Collins,   Colorado  and
CORE laboratories in Denver, Colorado.  Every shipment  during  the
course  of  the study  was received  within 24 hours   by  the  lab-
oratories,  except for the samples  collected July  20,  1982,  whic.h
did not arrive at the  CSU laboratory until 36 hours  after collec-
tion.

     Th.e  analytical laboratories performed  the  analyses  of   the
selected  constituents  in  Table   5.   These  constituents  were
analyzed  according  to the methods presented in   Table   5.    The
quality  assurance  program for the analytical   laboratories,   as


                              25

-------
well as the field sampling, is presented in Chapter 4.   It  should
be  noted  that  values for ammonia and  nitrate  reflect   abrupt
changes  that  are  not  characteristic  of  historical   trends.
Therefore, the data on ammonia and nitrate are suspect.
                              26

-------
                            CHAPTER 3

                         DATA DISCUSSION
     The  results  of the sampling program are discussed in  this
chapter.  The effects of changes in operational procedures on th.e
water  quality trends at each sampling point are also  discussed.
The  data  for  each tract is  discussed  separately  under  each
section below.

WATER QUALITY DATA FOR TRACT C-A and C-B

Tract C-a                                                       :

     As  previously  discussed  in Chapter 2,  there  were  three
sampling  points on Tract C-a.   These included the  mine  inflow
into the primary retention pond (i.e.,  Jeffrey Pond), the inflow
to the secondary retention pond (i.e.,  West Retention Pond) from
the  primary  retention pond,  and the outflow of  the  secondary
retention  pond.   The data collected during this sampling effort
are shown in Appendix A.   In addition,  the following statistics
have been summarized on the major constituents and are  presented
in Table 6:    number of samples,  mean,  high,  low, and standard
deviation.   In  addition  to  the  data presented  in  Table  6,
trilinear  diagrams  were  prepared  to  characterize  the  water
quality at each sampling point over the duration of the  project.
The  trilinear  diagrams  for  the  Jeffrey  Pond, inflow,   West
Retention Pond inflow,  and West Retention Pond outflow are shown
in Figures 7, 8 „ and 9, respectively.

     Inspection  of  the trilinear diagrams for all three of  the
sampling points indicates that the quality can be classified as a
non-dominant  type water.   The major cations and anions  consist
of:    magnesium,   sodium,   sulfate,   and  bicarbonate.    The
percentages   of  total  anion or cation  concentration  for  each
constituent   at  each  sampling point over the  duration  of  the
project were:
Sampling Point
Jeffrey Pond
   Inf1ow
West Retention
   Pond Inflow
West Retention
   Pond Outflow
Magnes ium  Sodi urn  Bicarbon ate  Sulfate

  39.0%     49.4%     50.9%      46.7%

  39.4%     48.6%     50.4%    •  47.0%

  39.2%     48.7%     50.5%      46.8%
     The  operational procedures on Tract C-a did  change  during
the course of the study.   In November of 1981, the Upper Aquifer
dewatering  system  was discontinued.   Previous to this  period,
dewatering  wells 6S-D6U and 6S-D8U were used for this  activity.
The  water  derived  from these wells  was  discharged  into  the
Jeffrey  Pond.   In addition,  the water from the mine sumps  was
also discharged into the Jeffrey Pond.   This composite water was
then  treated  in  the two ponds and reinjected  into  the  Upper
                             27

-------

























gj
&•"
£
^
3


OS
IS
«c
s

I
CJ

u
1
1
to"

cc

£•"


































t!
cl
§
s
s
1

f"
i§:

1
3t






g
S
5'
i
S,
2:
o
bl

S
&*•

OS
E»


3


L



i

i

t

g

ii

ta
-3
Q


§
tl4
Z
1-4











Is




g
H

X
a
X

z

I



1
i
Is
en c


§'



1






z

2;



S
i
1



2! >
we








Z

S




g
=


ce
z

e-
z
a:
i— i
1
8
z;
p-
«••. to
CO

~* ®
" V CO
— to
CO
« j
" cqco
in
in


CM
p-

in



0 CO
Oi


o
CO
in
CO
CM O
CO O
O CO
V «3-
— m



CM
CM -J
flQ in
CO
in


p~ p*



CM
—4 CO
in
CM



^
p-
CM
in
CO
t— 0
^ o
V Oi

m


o
' S in
in
in




til

«s o o
1-1 *"* S
0 § <
I: to cj
£ ce >-.
«s «s cs
OI CO
CM CM 00 —<



m co co
-« o o m
" « — I r-


o r-
to rr in if
~* CO OI
^ vO





co o o ^a*
r*- — * co




r* r- r-



o in o
^^ CO CO CO
CM r-




CM TT
-* O « P»
— « CM r-
PO

— . O> Csj
^p o P*- in
O> CO CO




^^ CO 10
*
£1
g m£
zlis§

Q «C < 1C O
a u o o u

Oi
^3*



o
CM
CO
—
in
r-



Oi
0

•"^



CO
in


g
s
^^

o



(— 4



•Q9


^

r*





CO
o
CO



o
o .



o

CM
CM


o
in
^JJ



^

0 c
§s
IS
-S
r^ co ^ co co
^ Oi


^4 ^H i— i in to

CM CO -H V CO V
.r-
ooocoSoiSP5
CO 00 -4 " O " " -4
o


COCOCMOJCOCMCOCO
co in I-H c*j
CO




>O 00 O 00 CO CO
— « CO CO


CO CO \O
Ot M O —* O <-* CO
PO in •-* ^a« V o


o* o* ^r
in r* m o* co in tM
tr GO "— • oo co *"H
o>





in r- co -*< —* co r*
(*)«—* Csj — *
CO



p*O.p»P*r*.r-P*.[*.



i-^ O f>J CO >O
i^cocMcoooeoco
*-« — ^ CO




~H CO -V
O «-* O CO O ^H ~H
(M CO ^H V (N V V
V (^

— t *-t CM O
p^cor~-oo^-*ocM
^3" O ^H ^H in CM HH




m o> «o co -x
i°"
ti2 Ci£

iii
M Q£ l-i
5- a: z
E- O< Cz3
HI E -I
M M M
' E- OT
r— co
' r~ eo
^*
m
o
O 0
-J r- CM v
^H C— O —
—4 CO
00 _J
CM 00 Ol O
-H o> "a"


to
-- CM r-

»-4 CO



«r c*
W oi r**
CO
in
o
Ol O
o o m v
—1 CO

J
CM 00 >-4 03
CM O> IT





CM
CO 0 CM

t— 4 f)







m CM
^* GO •— i
CO

^^
in
g
— T CO V
—4 CO



CO O O
CM 03 CO
CM *T


oi _:
CO -H CM 03
^H Ol CD








CM
— to
-H P*
m

CO
CO Ol
CM « to
CO
to
Oi Oi
rr o co
r—

r*
m >o
CO Ot rv*

"



CO
-< r-
(—4 t— 4
•^

CM
in a
CM CM r*
•
• *o
*g
« **
O J
1 •
•^ «
n ^
•« j
|g
0 0
W M
to Q>
.3 o

» o
«a,
CT 11

* i
28

-------


ce
LU
i-
_, 3
 H—
i- 0)










(T3
1
CJ

O
fO
s_



LEGEND



CO
a
2
o
L DISSOLVED S
<
t
2



1500-1750 mg/l
O'





1250-1500 mg/l






1000-1250 mg/l






750-1000 mg/l


O



500-750 mg/l


*



-ING DATES
£
S
«



flO
r*"
a.
Ul
C/9

*~



CM
I
R"
>•
2

~



I S i s
s s e *;.
5 ^ >
3 gJ § <
'

m v \o 
S

"
                                             LLJ
                                             o;
                                             CD
                                             )—t
                                             U_
29

-------


cc
Ul
1
_J ~*
2 £
0°-
l-CO
U.Z
og
PERCENT
EQUIVAL
Ij
S-
o
4- 13
E o ce
n} 0- 1
S- 0
05 C
(X3 ^^ •I™'
•r— -i— CJ
Q •)-> ro
S. 
-------
                                                       o
                                                      Q.
                                                    S  O  I
                                                    «3 -i- O
                                                    s_ 4->
                                                    en c: +J
                                                    to  cu  u
                                                           (O
                                                           s_
                                                       01
                                                      CK
                                                   CD  W
                                                   ED
                                                   •r-  S_ +J
                                                   S-  O 3
                                                   H-«J= O
                                                   LU
                                                   ce.
                                                  en
31

-------
Aquifer.   After  the discontinuation of  the  dewatering  wells   in
November of 1981,  the dewatering of the  mine  via  sumps  continued
throughout the duration of the project.

     In  regard  to water quality trends  at each  sampling   point,
none  were  observed  over the course of  the   study.    In   fact,
inspection  of  the trilinear 'diagrams for  each   sampling   point
(i.e.,  Figures 7,  8,  and 9) indicates  that  the  analytical data
are very consistent.  The analytical data for  all  of  the sampling
dates are very similar for each sampling  point, and consequently,
result  in very good grouping of points on the  trilinear diagram.
In  addition,  a variation in the water quality was not  observed
after  the  discontinuation  of  the  dewatering  ^program.   This
indicates  that the quality of water derived  from  the mine   sumps
is  very  similar to the quality, of water derived  from   the  once
operating  Upper Aquifer dewatering program.    Comparison of   the
trilinear  diagrams  for  the data collected   during  this   study
correlates quite nicely with the Upper Aquifer  data presented   in
Figure 4,  a trilinear diagram of the water quality baseline data
for the Upper and Lower Aquifers on Tract C-a.   Therefore,  it  is
reasonable  to  assume  that water derived  from   the  dewatering
activities on Tract C-a is predominately  from  the  Upper  Aquifer.
                                 i
     The  changes  in  water quality between  the   three  sampling
points is somewhat variable.   A comparison between the  untreated
water  flowing into Jeffrey Pond with the treated  water  flowing
out of the West Retention Pond shows an increase  in concentration
of  many  constituents.   For  example,   the  mean .values  of   the
following  constituents  show  slight  increases   when   the  data
collected  for the Jeffrey Pond inflow is compared with  the  data
of  the  West  Retention Pond  outflow  (see   Table   6):    boron,
carbonate,    calcium,   dissolved   oxygen,    iron,   magnesium,
molybdenum,  potassium, total solids, and total dissolved solids.
None  of these increases are very significant  and  can probably  be
related to pH changes,  aeration,  evaporation,  and  reduction
oxidation  changes  associated  with the  transformation  of   the
groundwater   from  an  underground  environment   to  a   sur'face
environment,  as  well  as the associated retention time  in   th.e
ponds.   In addition,  some of the changes may  be  attributable  to
laboratory variations.

     Groundwater  quality  data for Tract C-a  are  available   for
both  the Upper and Lower Aquifers.   These data,  as wel1-a.s  the
data  collected during this study to characterize  the   treatment
system,  are  presented in Table 7.   In  addition,  corresponding
Federal  Drinking  Water Quality Standards are  also   included   in
Table 7.  It should be noted that this comparison  is  not meant  to
imply  that the discharges from the treatment  system  should  meet
these standards, these are only included  for  reference purposes.

     Comparison  of  the water quality data   collected   from   the
outflow  of the West Retention Pond with  the  baseline groundwater
quality, data indicates that several constituents  exceed baseline
conditions upon discharge from the West Retention  Pond.  Specific
water  quality constituents in which the  mean  values  exceed   the


                             32                   '           •   <

-------
oo
o
1
LU

|


CD
Z
t—i
i«i

c—i

a


3:
LU
U_
Q
a oo

UJ OO
LU
OO CD

LU O
z: o
=3 LU
O —I
Q£ _l
CD O
O
I— o
   a.
u_
o CD
o o
oo _i
>-> o
Q. a:
O i-i
o 3
co
«=c






h-
«£
o
IT)

OS
I—

'

US
(O
GJ
|
h-
<
i
UJ
z
_J
UJ
•
^
as «t
UJ =5
0 0
UJ

0 2
*- < o
t— _J
Z U-
uj h-
UJ O
°=0
H- Z
uj a.
2
Z
Si
Z — 1
UJ U.
t— 5C
UJ •— <
as
Ca
h- Z
CO O
3!

ol
H- OL
IS
_J UJ
(j_ u_
Z u.
t— 1 UJ
r-a
OS
UJ
u.
3
O
<
CC
UJ
.2
UJ _)
h-
<
Z
3
0
SOS
UJ
=
o
<
OS
UJ
o_
3


en
^
co »—
>-
OS H-
2S
1°-
C_> OS
UJ U~
CO CJ
o
^>
••*•
CM ^
>-l—
OS OS
< <
ZQ.
t— »
OS OS
O.U.
O
O
-<*
LU
O_l
•-•<
Z >
UJ
Z=3
£g
UJ
S3
a= >
UJ
Z =
ss
UJ
O _l
= 5
UJ
Z3
ig
UJ
S3
re =»
UJ
S3
IS
UJ
^ 3
tD _l
S§
UJ
< -J
S5
CONSTITUENT*

un
CO
0 O
to m t
esj CM
LTJ
10
in
CNJ
U» CM r—
O ' « O
. 1
O O 0
O r—
CM
CO U^
CM O O I*- CM-*r**f^O» ^- C3iO
^•o cn^- ^- coocoioo^cai*.^- r— oco oo» cy»
OOOOOOCMOt trt CnCO<— OOOOi— CM^-ij->Lf>OOOC\JaDOlO'«l-OCO
v«> r-vo r* o cnVcy>CMVoaVr-o^^^V r-
10 ^T »— « CO CM r- ^- ^J-
^ co 10 ^r a* co er» ^- r-
CM CO tft «f <3> COOOCMCMCOCMCOaO 9itO UO U3
^r— *r cs ao r-ooococ3^ea^a»i— .esco
CO Irt ^- ^-QQr-r-OQOQf— COflQ^
CO fcO
CM o o r- cytef*** *^ oo*
cooco^*u*i*r trt r— tn CT> co urs CM ^- o oo^o
o o ao o >— co o» o ••raaf— ocnocor- voovocMocococMeor— O"*«*PC»
V*** r-»O r— C7* ^r— *rinVCMVCMO**^V r*-
ui u*» ^*»-CM r— *r «*•
CM •* O* tfJ «J- CO UD CO lO «d
CM cooo^- uiocor— or— cor- co in CM co<0
aco «r co co eoir»cy»csr— car— 
vo» ^r min en mvoc\jVr-vcMocov o
in ' CM CM r— CM CM C\J *T ITi
CM »— r—
O r— CO U3 incniACOCM
co CM co oo o mocor-r— oui*o cocn r- r*
ca B
OO CD CD CM O O CM
CM O O O *** O3 *d O r-ICMtOO'CMI Ol 1 1 1 IOCMOOI t O O
VCOCMCOCT»O>C3COCOr— CO lO VCOCMO «!• r-
O1 vO r— CO CO lO IT)
CM" co" co t— eu
u*> ^ in in in r—
CO CM CM CM CM CO CO ^ CM «T , CD , ^*
Oi— cn^i-^cocr> co r— i *0 co co i o i voi i i i t _j o *r o i i co r-
_i cr» CM ^ m r— co r- ca r— co in in
OLD CM en CO CM CM in
CO
co o co co o m o oo
•-^ CP o *r «J3 o en o in i r— co in i ^r i 01 i < i locooot icoco
i0 U3 U3 U3 p— CO r— in C7» Vmr— O •*
r*CM*o ^- r* ^-er»co
CM" CM" CM ^- CM
r* r— in co r— o co
eoor-cnincn cMCOcocoin coco r-
o o ^*- o CD co y» CM otoiocntoi r-i t i • i I_JCM^-«TI i^-us
*? co r— o i — m u9 co eo o r- m
r— r- CM co co ^f vo
ce
UJ
^~
^ O C3 h- — •
3tt UJ UJ UJ UU «t CJ
o o =» ca _j zo
CO >- _1 Z GO "-« '—
>- -^ OS X O UJ O t— UJ
uj h- E < o oo o. »-* -a; _i uj
t— »-H u o 3C oo GO _j _i ca or >- -^
 h- tn
Z H- UJt-iVtUJOUJUJ 3Z =GOeSGOGO=»UJl— 3C K !-*-*-»
^ tj C3 <^CSH-°;»i— *^C3 t— i UJ UJ i— • UJ __J < Z3 UJ Z3 >- ^ -—
<->>-4CO 2==3»— — >-Hh- i-«C;
SEZoxzoi-iceo Eooz^^cx«C'-tK-H-^-t— ^o-uji—«-*u.^e3^ —
Zoo(jasee_i_Jz^w>o£co3otD-JH-^ coooooujZ— i-jea_izi— t *t
aice«-«o
l_ O t—
 o
CO — •
3! U">
f~- cn
aien r—
c ^ cn
J^ a
c ^r -
— CM cn
^ r—
t
*» ja ^~
a» E =>
a> l
r— TO
3 -13
J= 
(O 4) V) ^
J= 3 E 3
O ftj -4-*
in * t- «O
•o e o a*
ra i_ a.
*» u. a. E
m cn  i_ t- x cn
«-» 0) D> (B i—
•a c -M a> £
a> *- w as -
-4-> •— U- >)
m ^» cnr— o c
u o a> m «o
•- z ce «-  L. ej
-i^ l_ U_  c a> >  e j=
,_ P- M- at GO
a> a> i j=t _i i~
•*-» C (U (U C -*-> --
o QJ i—  O
VI <*- O> <*- U Q. O
r- l_ ^ UJ -M O) m
C 0 0» h- •—
3  **- >»C3 CO
C t— C
i — V> UJ r— jt O O
•NH 03 ro O «-
cn >» k. f— -M os
E -o <— o>  f— "d CO 01 ••
C T3 (O 0» T3 O>
jf w- I- U. II C (J
•» > (O QJ L.
Vt O "O •*-• 	 1 CX. 3
O) W V O O O> O
a o. u. z co ea GO
(O

                                                               33

-------
mean  values  for  baseline conditions in some or  all   instances
include carbonate,  flouride,  magnesium, and pH.  However,  it  is
evident  from  reviewing  Table  7,  that  these  increases  over
baseline  conditions  are  minimal  and,   consequently,  do  not
constitutesignificant increases.

Tract C-b                                                        '-

     There were two sampling points on Tract C-b.   These  points
consisted  of (1) The inflow to the primary retention pond (i.e.,
Pond  A)  and  (2) The outflow of the  secondary  retention  pond
(i.e..   Pond  B).   The  data collected on Tract C-b  during  the
sampling period are presented in Appendix B.

     In addition,  the following statistics have been  summarized
for the major constituents and are presented in Table 8:   number
of samples, mean, high, low, and standard deviation.  In order  to
characterize the water quality,  trilinear diagrams were prepared
for  both the inflow to Pond A and the outflow of Pond B.    These
diagrams are presented in Figures 10 and 11, respectively.       ;

     The  trilinear  diagrams  presented in Figures  10  and  11,
indicate that the dominant cation and anion present in the   water
sodium and bicarbonate, respectively.  The average percentages  of
total  -anion or cation concentration for each constituent at each
sampling point over the duration of the project were:

     Samp ling Point      Sodi urn         B icarbonat-e
     Pond A Inflow        96.8%            90.356
     Pond B Outflow       96.9%            88.3%.

Therefore,  the water of the Tract C-b system is classified  as   a
sodium-bicarbonate type.

     In  regard  to water quality trends at each sampling  point,
none  were observed during the sampling program (Table   8).   The
sampling dates plotted'on the trilinear diagrams (Figures 1-0  and
11)  for  the sampling points show a very good grouping  of  data
points.  However,  a small deviation is noted for Sample 1,  which
represents  the  sample  collected  during  acid  .and  flocculent
treatment.   In general,  the remaining data points indicate that
there is very little variability in the water quality.   In regard
to  Tract  C-b  operational procedures,  the  dewatering  of  the
production  and service shafts continued throughout the  sampling
period without variation.

     The  trilinear diagrams for the data collected on Tract  C-b
during  this  sampling program correlates fairly  well   with  the
Lower Aquifer data presented in Figure 5,  a trilinear diagram  of
the  baseline water quality data for the Upper and Lower Aquifers
on  Tract  C-b.   This indicates the water  from  Jthe  dewatering
activities  is-  primarily  derived  from Lower  Aq'uifer  sources.
However,  the  stratigraphic interval from which  the  dewatering
occurs  is located in the zone designated as Upper Aquifer.   One
explanation  for  this  discrepancy may be  that  the  dewatering

                             34

-------
                                                                    cu
                                                             00     as
                                                             en     eu
                                                             i—  CO  S-
 re o
                                                                    
-------
                                                                     •M

                                                                     O)
                                                              co     ic
                                                              en     CLI
                                                              r— 'W1  S_
                                                       M—   *»VO QJ -Q


                                                       SO    QJ  o
                                                       res i—  o i.  to
                                                       f- 1- +J O.
                                                       CD+-> CL aj TJ
                                                       US  3 0) J_  E
                                                       •r- O 00     «3
                                                       O    >._< Q
                                                          03    +J +J

                                                       S-     -Q (d  E

                                                       O)  C C_) "° ,2f

                                                       CO    <1)  3
                                                       •r- Q. -M r^  /)
                                                                 trt M-
                                                      LU
                                                      QC
                                                      U_
36

-------
en
to
:c
on


Q


Q
LJJ


O
O
O
•=c
a
 ;=C
 p

 O
 13.

 es
 ;z
 i— ^
 a
 — i
 o
 CXD





t—
as
UJ
H=
<
ec
4
C.
3
3
CJ




H-
2
C
CJ
C
c.
u
»—
ffl
L
<


?s
va ea
3
0
_l
CD
ea
o
Q.
£i
OS i— i
u_ 3:
i
u-
^->
=)
°s
UJ
aC
Q£
UJ

o •
H- UJ
(/> O
|
«c
a
ST
5s
1
_j
Z
u
O£
UJ
3
3C
O
OS
20
O 3
_j o
u_ a.
i
o
h— <
11
_> 0
u. a.
z
HH
t
P
*•"•
1—
I
1
o ~
2SS*''0 § r- V V OV«-a> i- CM P~
e\j f— o e\j en ir» ^
^T cl ^ i-T . i-
CM« ^- 0 —.1-0
«o CMOI— oor^.«r— coeor* o r- owi cnoca evj
V9)9te tf» uoir> cotoa»«*veovr*03C3V«3OOi
— S°"fl'~ S " g35S~cv<~Kin-2:
« * • • •
,_ <\j f— i— ^
« f*r- ^rcxjcocjcn « 2 .-,
co o» co a> cr> co r* ^ u^ co r- *o in to ea o> irt
gSSS10-0 S * ««§'-§ s~g «
A * * * *
•—CM c— •— *—

m irt^p— oocoir»co ^*r^S«**
?- or*r*co »— r* co o u» *i- co •— «r co ^- o» o co
r^.*— m^-co ^^o>^coc\»co *o co r— r»
S r- cv f— r- *r to «*•
j^ CO ^m p"" *^
r- ^ COO* r— O CO O tf> ^^ w
cvi r*,— !—,— o*— ocoora*o •— •— o* «o o
ifi •«*• *J- ID C3 C\J*J-f— VCOVr— r— CM<^OOCOVU3 ^O »— O CM to 03
S ~ • S v " 5vSeo S- P .
So r* o **• •—  oa f— i— *—
f^, r— in o cnocom^ co co— »
co r*. r— r* r- eor*inomcocnm o •— co co en a» co
SCM ^ e\j co^ co m ca o
„ o • • *
e— fSJ <— »— r"

S5?oS~ cnocoSS^-inP- r^5. «! °°
,-! V en *r-^^>coo co cnui " ^ v ^ * ^*o"cnV"^V*co5^V''vcSr*
QV S *~ In»nca'~"incocr»
,_r CM i^ ^
t~~
**
eno cocococo r* ocoo5r-caco ^^^ "? ^"^
'vLn'dr^co'jn ^ « IA W V ^ ^ SS2S^2?c3°SV*1V "
p.. e\j comcnco inr—
r-^ CM 1-^ i-^
O£
UJ
^ ^ ea es H- •-*
C3 UJ UJ UJ UJ h- CJ
03 CS > Q _I«CO
>. ^ >- _J ^ CO *-• Z ^-«
i— i « x o uj ca H-
... i— — ej o tfl O- t-t •< uj uj
lr r-^e ac «4fl_j_i_io£ >- — • ,
5 uj >  z => w ea oo co XH- ac ac ^ -^»
«t ej S 5aco>— '"^z^ea »-* uj uj i— • uj uj«c=» uui=i>-z-^*
2 ^ S z=3Scjo2S-jS coaf— W3_i— J— i_j_JO£i-Kaci— •-•>— —.e
55S^oi^o:Sj=ocJoa: Luco
QSScelmtJOoEoocEOOOZZ>-o:<»-«f— t— >— H- H- o.uji-t^-tu-«ce*t —
§wSSor_j3zv30w = oS!ji— t— coooooujac-i-jo-jzi-*^
55ttSoS^zo^.*-tt-i_jci;«cc3v-ioujH-t— »— I— ooLLjujt-io=)««c_j«J3:
5SSca555S— S ou7SzeaczQ.a:i i i i II-WCOWCOXC-CQ.









v>
0
J=
^*
C
o>
«
ex
c
(/I
•+*
•her wise Indicated.
on Limits, with detection Urr
0 -'
u
Ut O)

O OJ
p- ca
= |
r-*dj
^s. CO
Ol
E
CO
«— 1 -J
•K OO
                                                            37

-------
activities have reversed the gradient between the Upper 'and Lower
Aquifers  to such an extent, that the Lower Aquifer is  recharging
the Upper Aquifer through the semi-permeable Mahogany zone.

     A comparison of the inflow and the outflow of the Tract  C-b
treatment  system  indicated  no significant changes  except  for
reductions  in total suspended solids and pH when flocculent  and
sulfuric acid were added.   (see Table 8).   This relationship  is
true  for  the samples collected during the  period  of  chemical
treatment  (i.e.,  flocculent and sulfuric acid) and the  periods
without chemical treatment.   Once again, this aspect is probably
due  to  the  exposure of the groundwaters  to  atmospheric  con-
ditions.   The  fact  that  many of  the  constituents  increased
slightly  after  residence in the retention ponds Vindicates  that
this  type of treatment method may not be totally  effective  for
groundwaters.

     Baseline  water  quality information is also  available  for
Tract C-b.  These data include locations above and below Tract  C-
b  on  Piceance Creek,  as well as groundwater data for both  the
Upper and Lower Aquifers.   This information is included in Table
9.   In addition,  both the quality data for the treatment system
on Tract C-b collected during this study and the Federal Drinking
Water Standards are also included in Table' 9.                   '••

     An inspection of Table 9 indicates that the mean values  for
some constituents in the discharge from Pond B exceeded,  in some
cases,  the mean values in the Upper Aquifer baseline groundwater
quality concentrations.  These constituents include  bicarbonate,
carbonate,  conductivity,  flouride,  molybdenum,  (except during
sulferic acid and flocculent treatment) nitrate,  potassium, TDS1,
and  sodium.   However,  these increases were fairly minimal and,
therefore,  not large enough to insinuate significant degradation
in the quality of groundwater derived from Tract C-b.

     The mean values of the following constituents upon discharge
from  Pond  B  exceeded baseline conditions for the  mean  values
along  Piceance Creek at the site below Tract C-b (see Table  9):
ammonia,  bicarbonate,  boron, carbonate, conductivity, dissolved
oxygen (lower concentration),  TDS, temperature, sodium, alkalin-
ity,  and pH.   One obvious reason for the elevated values of the
above  constituents  relative  to  the  baseline  conditions    of
Piceance  Creek is the fact that the water discharged from Pond B
is  derived  entirely from the groundwater system,  which  is   of
poorer quality than Piceance Creek.
                             38

-------
oo
Q
Di
a
-<
II 1
_l

<=c






%

C-b HOLDIN
1








S
i
i
1
CD










2
1

i
|


a
1
r^
X
O



Oi
S
|
VI


*s
I








DRINKING .
y STANDARDS'
11
a
i
1C

ii
go.

u. m
^

||


|«
"S
^ffi

u U
J U
Ii
i
3
ee
i
oe
g:







ll





u
z =


ss
Is
= =
53
=c3
is
53

Is
ll
sis
II
33


1
u



ad
i
~
O 0 CO S
ey d o o
<•».— en O*M un o —
:• ~- :- :-~ "" -
So oooocojo r-o eo oS r— CM eo in o a in CM
2 - R - SiSSS - ~S^ VZ
SS <. =0 S
oocnocooca o o r-en oinoui in ca in en -voeoor-co a p « ocn
vm<0p- es P- enco^vtMvr-mVcn
co in co »CM m P-
eo CD fMr» *IMCOCM o t i i tp-ooooo i •» en
f- co ao •— us f— oo m CM CM CD co •*•
«o in o P- eo in
eo 91 r- CM
o<— Stnr.jrt r> to o en o co r- — ei o co
OCMCMOP-COCO •» t en O o in o o e*i m t t i ienor— cocno ICMCD
In l*"~ eo "** S *~*S 5
CO "°«0 ^ "
O eo r~  in CM r—
O eo ov o oi—

CMO •— en O o (—
r-^oocDiooo o i lor^cpeacMp- o i i i t IOCMOOO i i en
CM *T (O r—
i— CM P- o a
eno ^ m o «r CM o o 10
en CM r» CM r-. r— » o r— eo CM
<— to P- coeM
— ' —
xx eso ni— •
•* uj »wtaoo C^'X — = a o « 5 H^CT
Z 1— LU « -s. uj *- i uj UJ =3 Z =3 V> O M VI ^ ^ ^ ^ C i-.**
Xc^t-ioecx^.^^ c/aov>^o«a— IP- p- ^
III § .
1 PllfS
" £SSS2°r;
g- •% s = S I-™?:
• -lsa=fs
^ ^'^^"•Saiaj
nj


39

-------
CONCLUSIONS


     This  discussion  is divided into two sections.   The  first
section  addresses the effectiveness,  of a one-pond or  two-pond
system without chemical treatment (i.e.,  flocculent and sulfuric
acid).   The  second section presents conclusions concerning  the
effectiveness of adding a flocculent to decrease total  suspended
solids concentrations and adding sulfuric acid to decrease the pH
in the treatment system.  It should be noted that the discussions
of the respective pond systems with respect to water quality data
and  the  resultant  changes are presented using mean  values  of
respective water quality constituents.

Effect i veness of System Without Chemi cal Treatment

     The  one-pond  system addressed here consisted of  the  West
Retention Pond on Tract C-a.   With respect to Jeffrey  Pond,  it
was  not included as part of the assessment due to  its  extremely
small  size and corresponding short retention time.   It was felt
that even though the water passed through Jeffrey Pond before  it
entered  the West Retention Pond,  the holding time was so  small
that  effects  on  water quality were believed to   be  negligible
compared to the West Retention Pond.

     The  overall  quality remained essentially unchanged as  the
water  passes through the West Retention Pond.   The decrease  in
total  suspended  solids concentrations from 6.3  -mg/1  to  below
detection limits is not significant.

     The two-pond system assessed during this study is located on
Tract ' C-b and consisted of the primary retention pond  (Pond  A)
and  the secondary retention pond (Pond B),  which  are in-series.
Samples  were collected for the inflow to Pond A and the  outflow
from  Pond  B on six occassions.   In addition,  one  sample  was
collected when flocculent and sulfuric acid were added,  as  dis-
cussed below.   Similar to the one-pond system,  fluctuations for
most of the water quality constituents were insignificantly small
(less than 10%).   Total suspended solids concentrations remained
unchanged  (less  than 10 mg/1).   Concentrations of  other  con-
stituents varied slightly but not significantly.  In summary, the
general water quality did not improve nor was it degraded,  after
treatment in the two ponds (without chemical treatment).

Treatment with F1occulent and Sulfuric Ac i d

     A  magnifloc cationic flocculent designed to precipitate out
suspended solids concentrations was added to the two-pond  system
on  Tract  C-b.   This was done at a time when mining  activities
were occurring and large increases in total suspended solids were
expected to be observed in the two ponds.

     Water  quality samples were taken on September 16,  1981  at
the  inflow to Pond A and the outflow from Pond B to  assess  the
effectiveness of the flocculent.   The concentration of suspended


                              40

-------
solids at the  inflow to the  system  was  found  to  be  565  mg/1,  with
the  concentration  reduced   to  6.0 mg/1  at  the   outflow   of   the
system.   These  data  clearly  indicate  the  effectiveness  of   the
flocculent,  as the suspended solids  concentration  was  reduced  by
about 99%.   At the, same time,  the  silica  concentration  increased
(from 23 mg/1  to 35 mg/1) and the total  dissolved solids   concen-
tration  increased  (from 1,354  mg/1  to   1,517   mg/1).    However,
these  increases did not significantly  degrade the  water  quality,.

     At  the same time as the flocculent  was  added  (during  mining
activities),  'sulfuric acid  was  also  added  in order  to  reduce  th.e
pH  of  the  water  be.fore it  was  discharged  from   the   two-pond
system.   The  water sampled  at  the inflow  point  had  a  pH  of  9.2,
compared to a  value of 7.8 at the outflow  point,  which   reflects
the addition of sulfuric acid.   At the  same  time,  alkalinity  was
reduced  from  1147  mg/1 to 926  mg/1 (a  decrease   of   19%),  while
acidity  remained stable at  <5  mg/1.    The  one apparent effect  of
adding sulferic acid was an  increase  in  sulfate  from  186  mg/1   to
311 mg/1 (an increase of 77%).   However-,  this increase  in  sulfate
did not seriously degrade the water quality.

     The  overall   conclusion regarding  the  effectiveness  of   the
one- and  two-pond  systems is the same.    The wate:r  quality  con-
stituents  analyzed  for  in  this  study   were   not  appreciably
affected  by the respective  pond systems.    With  respect   to   the
addition  of flocculent and  sulfuric  acid,   both  additives  appear
to  adequately treat specific constituents.   The flocculent   was
very  effective in  reducing  suspended solids  concentrations   and
the sulfuric acid reduced the pH.  These changes  occurred  without
significant degradations of  the  general  water quality.
                             41

-------
                            CHAPTER 4

                   QUALITY ASSURANCE PROGRAMS

FIELD SAMPLING PROGRAM QUALITY CONTROL

     Grab  samples were collected in 5-gallon carboys at each  of
the sampling points.   Previous to sample collection, the carboys
were  thoroughly rinsed with a deionized water to prevent  cross-
contamination.   In addition,  samples were collected as close tp
the   discharge  point  as  possible  in  an  effort  to   obtain
representative samples.   Immediately upon sample collection, the
following  constituents were measured with portable  instruments:
pH,  temperature, dissolved oxygen, and specific conductance.  In
order  to obtain accurate measurements the samples were  analyzed
for  a  period  of  at  least  20  minutes,   which  allowed  the
instruments to equilibrate.   In addition, all of the instruments
were calibrated previous to sample measurement.   The instruments
were thoroughly cleaned with deionized water after each sample.

     Samples  which  required filtering were filtered  with  high
purity  nitrogen  in  a Skougstad-type  filter  apparatus.   This
apparatus  is'  composed  of a polyethylene material  and  can  be
pressurized to force the sample through a 0.45 micron filter into
the sample container.   The dissolved organic carbon samples were
filtered  with a stainless steel apparatus through a 0.45  micron
silver  membrane filter to prevent the introductio,n of  organics.
Previous to the introduction of another sample into the filtering
units,  the units were disassembled and thoroughly decontaminated
with deionized water.   In addition,  a new filter was  installed
into each unit previous to the filtration of another sample.

     Following  filtration,   preservatives  were  added  to  the
sample,  if necessary.   In addition,  the samples were placed in
ice  chests and cooled to 4 degrees Celsius with ice.   The  U.S.
EPA  (1979a)  recommended  procedures were  utilized  for  sample
preservation.   In  addition,  the U.S.  EPA  recommended  sample
volume requirements,  containers,  and holding times were used as
guidelines during this study.   All of these aspects are shown in
Table 10.

     Samples  were shipped from Rifle,  Colorado to the  Colorado
State University laboratory in Fort Collins and Core laboratories
in  Denver.   Commercial  buslines  were used  for  these  sample
shipments  due  to  the  overnight  services  provided  by  these
buslines.   This  arrangement  worked  very well  throughout  the
duration of the project and,  in every case except one,  the sam-
ples  were  received  by the laboratory within 18  hours  of  the
sampling  effort.   The exception was during the July  20.,  1982,
sampling  effort  in which the samples were not received  by  the
Colorado  State  University laboratory until 36 hours  after  the
samples were collected.

                              42

-------
                  TABLE  1O
     U.S. EPA RECOMMENDED  SAMPLE PRESERVATIVES,
VOLUME REQUIREMENTS, CONTAINERS, AND HOLDING TIMES
             (U.S. EPA.  1979)1
Constituent
RESIDUE
Filterable
Non-
Filterable
Total
Volatile
Settleable"
Matter
Turbidity
METALS
Dissolved
Suspended
Total
Mercury
Dissolved


Total


Req.
(ml)

100
100
100
100

1000
100

200
200
100
100


100


2
Container Preservative

P, G Cool, 4°C
P, G Cool, 4°C
P, G Cool, 4°C
P, G Cool, 4°C

P, • G None Req.
P, G Cool, 4°

P, G HN03 to pH<2
Cool, 4°C
P, G HNO3 to pH<2
P, G HNO3 to pH<2


P, G HN03 to PH<2


Holding
Time
-
7 Days
7 Days
7 Days
7 Days

24 Hrs.
7 Days

6 Mos . ( 4 }
6 Mos . ( 4 5
6 Mos . ( 4 }
38 Days
(Glass )
13 Days
(Hard
Plastic)
38 Days
(Glass)
13 Days
(Hard
Plastic)
                    (continued)
                       43

-------
Constituent
INORGANICS ,
Non-Metallic
Acidity
Alkalinity
Bromide
Chloride
Cyanides

Fluoride
Nitrogen
Ammonia

Nitrate
Phosphorus
Ortho-
phosphate,
Dissolved
Total

Silica
Sulfate
Sulfide

Vol.
Req.
(ml)


100
100
100
50
500

300

400

100



50
50

50
50
500

TABLE 1O
(Continued)
2
Container Preservative


P, G
P, G
P, G
P, G
P, G

P, G

P, G

P, G



P, G
P, G

P only
P, G
P, G



None Req.
Cool, 4°C
Cool, 4°C
None Req.
Cool, 4°C
NaOH to pH 12
None Req.

Cool, 4°C
H2SO. to pH<2
Cool, 4°C



Cool, 4°C
Cool, 4°C
H-SO. to pH<2
Cool, 4°C
Cool, 4°C
2 ml. zinc
acetate
Holding
Time^


24 Hrs.
24 Hrs.
24 Hrs.
7 Days
24 Hrs.

7 Days

24 Hrs.

24 Hrs.

.

24 Hrs.
24 Hrs.

7 Days
7 Days
24 Hrs.

Organic carbon   25
P, G
Cool, 4 C
H2S04 or
 HC1 to pH<2
                                                          (6)
24 Hrs.
                         (continued)
                              44

-------
                           TABLE 1O

                          (continued)
1.   More   specific   instructions   for   preservation  and
     sampling  are  found with  each procedure  as  detailed  in
     this  manual.   A  general  discussion on  sampling water
     and   industrial   wastewater  may   be   found  in  &STM,
     Part 31, p. 72-82 (1976) Method D-3370.     '

2.   Plastic  (P)  or   Glass  (G) .   For  metals,  polyethylene
     with a polypropylene cap (no liner)  is preferred.

3.   It  should  be pointed  out that  holding  times   listed
     above  are  recommended  for  properly  preserved   samples
     based  on  currently  available  data.  It  is recognized
     that  for some sample  types,  extension  of , these times
     may be  possible  while for  other  types,  these times may
     be  too  long.   Where shipping regulations  present the
     use of  the  proper preservation technique or the  holding
     time  is  is  exceeded,  such  as  the  case of  a   24-hour
     composite,  the final  reported  data for  these   samples
     should indicate the specific variance.

4.   Where   HNO,   cannot   be   used  because   of   shipping
     restriction's,   the  sample  may  be  initially preserved  by
     icing and  immediately shipped  to  the laboratory.  Upon
     receipt  in  the laboratory,  the sample must;be acidified
     to  a  pH<2 with  HNO,  (normally  3 ml.   1:1 HNC>3/liter
     is  sufficient).   At  the  time  of  analysis,  the   sample
     container  should  be  thoroughly  rinsed  with 1:1 HNO,
     and the  washings  added  to the sample  (volume correction
     may be required).

5.   Data  obtained from National  Enforcement Investigations
     Center-Denver,  Colorado,   support  a .four-week   holding
     time   for   this   parameter   in   Sewerage   Systems.
     (SIC 4952).
                              45

-------
LABORATORIES QUALITY ASSURANCE PROGRAMS

     Two laboratories were utilized during this sampling project.
They  consisted of the University of Colorado laboratory and CORE
laboratories.   The  quality assurance programs for each will  be
individually discussed below.

CORE Laboratories

     I.   Instrument Quality Control
          A.   Calibrations and Standardizations
               (1)   Instruments are checked daily for
                     temperature consistency, weighing
                     accuracy, etc. prior to sample
                     introduction to assure proper
                     operation.
               (2)   Detection limits and linear working
                     range data are verified by using
                     sample blanks, standards, standard
                     additions, sample  spiking, etc.
          B.   Service
               Instruments receive periodic servicing to
               assure proper functioning within specif-
               ications.  Special care is taken to  insure
               precise and accurate operation of all
               analytical balances, being the initial
               source of  laboratory accuracy.  Files
               are maintained on all major analytipal
               .instruments to document servicing.

     II.  Laboratory Supplies and Reagents
          A.   Water
               (1)   Tap water - used as  a preliminary
                     wash  for glassware daily.
               (2)   Deionized water -  obtained by
                     passing through Cation-Anion ion
                     exchange columns.  This water meets
                     all specifications set forth by the
                     U.S.  Environmental Protection Agency.
          B.   Reagents - all A.C.S./analytical grade
          C.   Solvents - all A.C.S./analytical grade            ;
          D.   Volumetric Glassware -  all glassware              •
               used  for this purpose meets Class A
               requirements as set forth by the National         '
               Bureau of  Standards.  This glassware
               includes volumetric flasks and pipets
               •which are  always used for standard
               preparation and measurement of sample
               volumes, as well as for other purposes.

     III. Internal Quality Control/Precision and Accuracy

               To  assure  that data be  both precise  and   accurate,
          duplicate   samples,    spiked  samples,   and   internal
          unknowns   are run on a  routine basis within  the   Aurora


                              46

-------
     Lab,   as  well  as  within  the  entire   CORE   laboratories
     network for comparative purposes.

           In addition,   the data base  is  evaluated  on  CORE'S
     computer   system   prior   to   report   finalization   for
     statistically  known  correlations.    These   correlations
     include  sodium  conductivity,  anion/cation   balances,
     cation/anion sums,   total  dissolved  solids, maximum  oil
     and grease, maximum  BOD,  and  nitrogen  relationships.

           Ultimately,   a  data  base which  has had  individual
     data   point   pairs   compared    against   themselves,
     individual sample  inter-relationships  compared  against
     themselves   and   sample   interrelationships   compared
     against  other samples within  the  same area or  project
     wi11  be provi ded.

          .This  detailed  procedure  performed .on  a continuing
     basis  results   in   water  quality  data  that  is  both
     precise and accurate.

IV.  Sample Tracking

           Sample  bottles with  the  appropriate preservatives
     added . are  supplied by the .laboratory for  use  in   the
     field.   Records   are maintained which indicate   bottle
     groupings,  client   name,  client  location,  and  total
     bottles  shipped.    This   information  is   then   cross-
     referenced upon  sample receipt.

V.   Analysis Reporting

           Raw  data   is handled a single time  when  entered
     into  the  in-house  PDP-11  computer  for  calculation,
     storage,   and   reporting.    The  data  base  analyses
     previously  mentioned is then performed !and appropriate
     analyses   are   re-checked  and  re-entered  into    the
     computer.     Subsequent   data    manipulation,   i.e.,
     additional  reports,  transfer of  data base  to   client
     computers,  storage, etc.   are handled electronically to
     insure integrity of  the data.

Colorado State University

     Colorado State University  laboratory has a quality con-
trol program in the following areas:    sample  preservation,
sample  analysis,  and data handling.  These programs are per-
formed   according  to the  criteria of the  U.S.  EPA (1979b).
Each of these items are discussed further below.

    The sample analysis quality control involves the use  of
blanks  and duplicates.   For example, both a blank and  dup-
licate  sample are  analyzed per   sample set.  In  addition,   a
standard curve consisting of four or more  values is   estab-
lished  and compared to the analytical   results.   The   sample


                        47

-------
analysis quality control also involves  analyzing  the  U.S.
EPA  Reference Standard and  biannual  participation  in  the
U.S.. EPA performance study.

    In regard to the data handling, records are  kept of the
correlation  coefficient,  slope, and the  intercept  of  the
standard curve.  These records are used to insure  linearity
and acceptability of standards.  In  addition,  quality con-
trol charts are kept to provide criteria for, accepting data1.

Kaman Tempo Qua!ity Control

    Kaman  Tempo also  performed  internal  quality   control
measures  for the data received by the laboratories.   These
measures consisted of calculating the  cation-anion   balance
for the data set and the evaluation of general water  quality
trends at each sampling point.  The  ions  utilized   for the
cat ion/an ion balance calculation consisted of calcium,  mag-
nesium, sodium, potassium,  carbonate, bicarbonate, sulfate,
and chloride.  The data was considered to be fairly accurate
if the difference  between the  cations  and  anions  did not
exceed ten percent.

    These quality control measures  resulted in  identifying
some potential problems with the  analytical  data  received
from the Colorado State University laboratory.  For instance.
some data sets had a cation-anion balance off by as much  as
45 percent.  However, by the  time the  data , was  received^
many of the constituents were beyond the recommended  holding
periods and, therefore, a reanalysis would probably not have
resulted in more accurate data.

    An additional problem associated with the Colorado State
University data were the analytical results for some  fairly
volatile constituents.  For example, ammonia and nitrate are
very inconsistent and, in some cases,  reflect very   abrupt
increases which are not characteristic with historic  trends.
                        48

-------
                       REFERENCES CITED


American  Public Health Association,  1975.   Stndard Methods for
     the  Examination  of Water  and  Wastewater,  14th  Edition,
     1193p.

C-b  Shale Oil Venture,  1977.   Environmental Baseline  Program,
     November 1974 - October 1976.  Final Report.

Fox,  J.P.,  D.S.  Farrier,  and R.E.  Paulsen,  1978.   Chemical
     characterization  and  analytical considerations .for an  in-
     situ oil shale process water.   LETC/RI -78/7, Laramie Energy
     Technology Center.

Hem,  J.D.,  1971.   Study  and  Interpretation of  the  Chemical
     Characteristics of Natural Water.   U.S. Geol. Survey Water-
     Supply Paper 1473, 363 p.

Lawrence Berkley Labs (LBL), 1978.  Diffuse source effects on in-
     situ oil shale development on water quality.  Draft report.

McKee,  J.E.,  and  H.W.  Wolf,  1963.   Water Quality  Criteria:
     California State Water Quality Control  Board'.   Publication
     3-A, 548p.

Pfeffer,  P.M.,  1974.  Pollution Problems and Research Needs for
     an  Oil Shale Industry.   Environmental Development on Water
     Quality.  Draft Report.                                     :

Rio Blanco Oil Shale Company, 1977.  Final Environmental Baseline
     Report for Tract C-a and Vicinity.  Volume 2.

Rio  Blanco  Oil Shale  Company,  1983.   Scope  of  Work,  Lease
     Suspension   Period,   Environmental   Monitoring   Program.
     Submitted to Area Oil Shale Office.

Slawson,  6.C.,  Jr. (ed .), 1979.  Groundwater Quality Monitoring
     and  Western  Oil  Shale  Development:   Identification  and
     Priority Ranking of Potential Pollution Sources,  EPA-600/7-
     79-023, U.S., Environmental Protection Agency.

Sla.wson,  G.C., Jr. (ed.), 1980.  Monitoring Groundwater Qualitys
     Th-e Impact of In-Situ Oil Shale Retoring.  EPA-600/7-80-132:,
     U.S. Environmental Protection Agency.

Stuber,  H.A., and J.A. Leenheer, 1978.  Fractionation of Organic
     Solutes  in  Oil  Shale  Wastes  for  Sorption  Studies   on
     Processed Shale.   U.S. Geol. Survey, paper presented at ACS
     Fuel Sciences Division Symposium.

U.S.  Environmental  Protection  Agency,  1979(a).   Methods  for
     Chemical  Analysis of Water and  Wastes.   EPA-600/4-79-020,
     Environmental Monitoring and Support Laboratory, Cincinnati,
     Ohio.
                              49

-------
U.S.   Environmental  Protection  Agency,  1979(b). Handbook  for
     Analytical   Quality   Control  in  Water   and   Wastewater
     Laboratories.  EPA-600/4-79-019.

U.S.  Geological Survey, 1977.  Water  Resources Data for Colorado
     Water Year,  1975,  Volume 2.    Colorado .River Basin.  Water
     Resources Division, Report No. USGS/WRD/HD-77/005.

Weeks,  J.B.,   6.H.  Lewesley, F.A.  Welder, and G.J. Saulnier, Jr.
     1974.   Simulated  Effects  of Oil Shale Development on  the
     Hydrology  of Piceance  Basin,  Colorado.   U.S.   Geological
     Survey Professional Paper 908.
                             50

-------
                         APPENDIX A





ANALYTICAL AND FIELD DATA FOR THE SAMPLING  SITES  ON  TRACT-C-a
                           51

-------
           TABLE A-l:  ANALYTICAL AND FIELD DATA FOR THE MINE INFLOW TO JEFFREY POND

Constituents*
ABBREVIATED MONITORING
Ammonia (NH,-N)
Arsenic
Bicarbonate
Carbonate
Calcium
Chloride
Fluoride
Iron
Magnesium
Mercury (ug/1)
.Molybdenum
Nitrate (N03-N)
Potassium
Selenium
Silica
Sodium
Sulfate
Vanadium
Acidity (As CaCOj)
Alkalinity (As CaCOj)
9/17/81

0.11
<0.01
532
<1
36
'8.34
1.71
0.06
83
<0.3
<0.1
<0.1
0.35
<0.01
23
200
430
<0.5
<5
469
5/27/82

.28
<0.005
548
5.1
32
7.9
1.1
.017
78.9
<.001
<0.05
.09
.8
<.02
11
190
388

5.6
458
Sampling Date
7/20/82 9/23/82 11/17/82

.467
<.003
577
6.06
44.1
8.23
1.51
.15
77.1
<.001
<.05
<1.0
.531
.<.002
" 12.3
191
343

5.25
483

.333
.003
527
7.59
46.3
8.52
1.4
1.00
95
<-001
<.03
<1.0
1.26
<.002

174
438
<0.1
3.51
445


<.005
599
9.09
48.7
7.74
1.2
<.01
77.5

.052
.245
.666
<.002
12.7
193
414

3.79
506
1/7/83

.354
<.005
- 554
9.44
32.6
7.89
1.32
.085
76.2
.001
<.03
.231
.615
<.01
12.1
195
400
<.005
3.13
470
3/9/83

.253
<.005
548
3.02
31.9
7.89
1.21
<.01
72.8
<.001
.107
2.02
.136
<.01
12.0
195
400
<.U05
9.45
454

*In mg/1, unless otherwise  indicated.
                                                 52

-------
                                     TABLE A-l (Continued)

Constituents*
Conductivity (field,
ijmhos/cm)
DOC -
pH (field, units)
Dissolved Oxygen
(field, ppm)
Boron
Fractionated OOC
-Hydrophobics (Total)
-Bases
• -Acids
-Neutral
-Hydrophilics (Total)
-Bases
-Acids
-Neutrals
Residues
-TDS •
-TS.S
-Total Solids
-Total Volatile
-Settleable Matter
Temperature (field, °C)
9/17/81
2250
3.1
9.2
3
0.41

1.5
0.2
1.1
0.2
2.4
0.7
1.6
0.1

1033
<4
1036
226
<0.1
14
5/27/82
1400
4.7
8.35
3.2
.21

3.6
0.0
0.2
3.4
1.1
0.0
• 1.1
0.0

992
<4
992

.
-------
                                        TABLE A-l  (Continued)

Constituents* 9/17/81
COMPREHENSIVE MONITORING*
Aluminum
Barium
.Beryl! ium
Cadmium
Chromium
Cobalt
Copper
Cyanide
Lead
Lithium
Manganese
Nickel
Phenols
Phosphorus
-Ortho
-Total
Silver
Strontium
Sulfide
Thallium
Thiosulfate
Tin
5/27/82

<.02
.083
<.0005
<.001
<.005

-------
                                      TABLE A-l (Continued)

Constituents*
Titanium
Zinc
Turbidity
Uranium-234 (pci/1)
Uranium-235 (pci/1)
Uranium-238 (pci/1)
9/17/81 5/27/82
<0.5
.005
.6
1.3 ± 1.1
.2 ± 0.5
0.9 ± 1.0
Sampling Date
7/20/82 9/23/82 11/17/82
<.05
.007
4.5
0.3
0.0
0.3

.122
7.5
± .3
± .2
± .3
1/7/83 3/9/83

: .075 .033





*In rng/1, unless otherwise indicated.
                                               55

-------
           TABLE A-2:  ANALYTICAL AND FIELD DATA FOR THE JEFFREY POND  DISCHARGE  INTO THE WEST
                      RETENTION POND.

Constituents*
ABBREVIATED MONITORING
Ammonia (NHj-N)
Arsenic
Bicarbonate
Carbonate
Calcium
Chloride
Fluoride
Iron
Magnesium
Mercury (vig/1)
Molybdenum
Nitrate (NOj-N)
Potassium
Selenium
Silica
Sodium
Sulfate
Vanadium
Acidity (As CaCOj)
Alkalinity (As CaCOj)
9/17/81

0.10
<0.01
531
1.08
, 37
9.47
1.70
0.05
83
<0.3
<0.1
0.1
0.36
<0.01
22
190
382
<0.5
<5
474
5/27/82

.11
<.005
540
5.7
31
8.1
1.2
.026
79.4
<.001
<0.05
.008
.9
<.02
11
187
392

4.9
452
Sampling Date
7/20/82 9/23/82 11/17/82

.317
.003
546
11.4
44.1
7.90
1.22
.049
78.1
<.001
<.OS
<1.0
.369
<.002
10.9
197
345

2.52
467

.238
<-003
523
8.01
47.5
8.94
1.43
.59
98.9
<.001
<.03
<1.0
1.24
<.003

170
427
<0.1
3.28
442


<.005
525
10.5
63.5
8.67
1.28
.282
84

.038
.245
.817
<.002
12.7
196
441

2.53
448
.1/7/83

.306
<.005
533
7.21
32.4
7.58
' 1.21
" .164
74.1
• <.001
<.03
.219
.636
<.01
11.9
198
412
<-005
3.78
449
3/9/83

.243
<.005
548
5.76
31.7
8.14
1.31
.124
76.5
<-001
.3
8.59
1.02
<.01
'10.9
192
364
<.005
4.99
459

*In mg/1, unless otherwise  indicated.
                                               56

-------
                                       TABLE A-2 (Continued)

Constituents*
Conductivity (field,
pmhos/cm)
DOC
pH (field, units)
Dissolved Oxygen
(field, ppm)
Boron
Fractionated DOC
-Hydrophobics (Total)
-Bases
-Acids
-Neutral
-Hydrophilics (Total)
-Bases
-Acids
-Neutrals
Residues
-TDS
-TSS
-Total Solids
-Total Volatile
-Settleable Hatter
Temperature (field, °C)
9/17/81
1425
3.9
8.2
7.0
.39

1.5
0.2
1.1
0.2
2.4
0.7
1.6
0.1

1053
<4
1054
214
<0.1
15.5
5/27/82
1400
3.2
8.35
7.4
.22

2.4
0.0
0.9
1.5
1.3
0.2
1.1
0.0

988
4
1016
N/M
<1
16
Sampling Date
7/20/82 9/23/82
1400 1510
<3' 4.0
8.96 7.0
8.5 6.2
.8 <3.0

1.8
0.1
1.2
0.6
2.2
0.0
1.5
0.7

1018 1188
6 10
1061 1244
235 230
.3 <0.1
23 16
11/17/82
1400
4.0
8.7
5.9
.15










1220
<4
1228
252
<0.1
10
1/7/83
1390
3.6
7.8
5.9


1.5
0.0
1.2
0.3
2.1
1.1
0.7
0.3

1446
,<4
1446
74
<.l
10
3/9/83
1510
3
7.45
6.2
.183










1023
5
1028
184
<.l
11

*In mg/1, unless otherwise indicated.
                                              57

-------
                                      TABLE A-2 (Continued)

Constituents* 9/17/81
COMPREHENSIVE MONITORING*
Aluminum
Barium
Beryllium
Cadmium
Chromium
Cobalt
Copper
Cyanide
Lead
Lithium
Manganese
Nickel
Phenols
Phosphorus
-Ortho
-Total
Silver
Strontium
Sulfide
Thallium
Thiosulfate
Tin
5/27/82

<.02
.081
<.0005
<.001
<.005
<.005
<.001
<0.005
<.01
.091
<.002
<.005
<.005

<.01
.4
<.001
8.2
<.l
<.005
5
<.05
Sampling Date
7/20/82 9/23/82 11/17/82

.06
1.05
<.005
.005
<.005
<.005
<.001

<.01
.077
<.002
<.001


<.4
<.05
<.001
8.5





<1.0 .042
<1.0
<.01
.005 <.004
.024
<.05
<.005
<0.5
<.01
.074
.042 .056
<.05 .01
<.05

<.4
.141
<.001
9.19 7.16
<.l

<.05
<0.01
1/7/83

.175
.074
.493
<.004
<.05
N.05
<.005
<.l
<.025
.085
.007
<.01
<.05

<.0l'
.144
<.01
8.31
.06
1 .012
<.05

3/9/83

.242
.069
<.0005
<.004
<.05
' <.05
<.005
<.l
<.025
.085
<.005
. <.01


.257
.299
<,01
7.24

.004



*In mg/1,  unless otherwise indicated.
                                               58

-------
                                       TABLE A-2 (Continued)

Constituents*
Titanium
Zinc
Turbidity
Uranium-234 (pci/1)
Uraniura-235 (pci/1)
Uranium-238 (pci/1)
Sampling Date
9/17/81 5/27/82 7/20/82 9/23/82 11/17/82
<-5 -<.05
.009 .032 .077
1.4 3.2 4.9
.1 ± .4 0.4 ± 0.4
0 ± .1 0.0 ± 0.1
1.4 ± 1.5 0.3 ± 0.3
1/7/83 3/9/83

.062 .026


:"


*In rag/1, unless  otherwise  indicated.
                                             59

-------
          TABLE A-3:   ANALYTICAL  AND FIELD DATA FOR THE WEST RETENTION POND DISCHARGE.

Constituents*
ABBREVIATED MONITORING
Ammonia (NH,-N)
Arsenic
Bicarbonate
Carbonate
Calcium
Chloride
Fluoride
Iron
Magnesium
Mercury (vg/1)
Molybdenum
Nitrate (NO-j-N)
Potassium
Selenium
Silica
Sodium
Sulfate
Vanadium
Acidity (As CaCOj)
Alkalinity (As CaCOj)
9/17/81

0.22
<0.01
535
<1
37
9.47
1.25
0.26
83
<0.3
<0.1
0.2
0.36
<0.01
20
190
348
<0.5
<5
469
5/27/82

.16
<.005
541
6.8
32
8.0
1.2
.018
77.4
<-001
<.05
.05
.7
<.02
11
194
391

4.1
455
Sampling Date
7/20/82 9/23/82 11/17/82

.424
<.003
558
5.99
44.5
7.8
1.2
.069
77.5
<.001
<.05
<1.0
.466
<.002
11.6
194
350

4.96
467

.163
<.003
368
5.58
47.5
5.73
1.11
.283
100.9
<.001
<.03
<1.0
1.34
<.002

177
302
<0.1
2.33
311


<.005
524
10.4
62
8.56
1.26
.44
84.6

.24
.769
.858
<.002
12.8
195
449

2.53
447
1/7/83

, : .317
<.005
,- 553
10.1
34.6
8.02
1.32
.644
73.1
<-001
<.03
.516
.632
<.01
11.7
198
398
! <.005
2.92
470
3/9/G3

.185
<.005
1541
6.09
32.4
8.14
1.31
<.01
78.7
<.002
.232
.407
1.49
<,01
11.1
198
402
<.005
4.6
454

*In mg/1,  unless otherwise indicated.
                                              60

-------
                                           TABLE A-3 (Continued)

Constituents*
Conductivity (field,
umhos/cm)
DOC
pH .(field, units)
Dissolved Oxygen
(field, ppm)
Boron
Fractionated DOC
-Hydrophobics (Total)
-Bases
-Acids
-Neutral
-Hydrophilics (Total)
-Bases
-Acids
-Neutrals
Residues
-TDS
-TSS
-Total Solids
-Total Volatile
-Settleable Matter
Temperature (field, »C)
9/17/81
1475
3.3
8.1
8.0
.37

1.6
0.0
1.1
0.5
1.7
0.2
1.4
0.1

1003
4
1007
205
<0.1
15
5/27/82
1400
3.7
8.4
6.6
.21

2.0
0.0
0.9
1.1
1.2
0.1
1.1
0.0

1390
<4
1395

<1
16
Samp!
7/20/82
1400
3
8.9
6.4
.9










980
<4
1023
225
<1
20
ing Date
9/23/82
1400
3.8
6.9
3.9
<3

1.5
0.0
1.0
0.5
2.3
0.1
1.7
0.5

1198
<4
1193
207
<.l
16
11/17/82
1420
3
7.9
4.2
.16










1250
<4
1254
236
<0.1
10
1/7/83
1450
4.6
8.1
5.8
.175

1.6
0.0
1.0
0.6
2.0
0.6
1.1
0.2

1392
<4
1392
86
.<.!
9.5
3/9/83
1320
2
7.6
5.6
.173










1028
<4
1028
162
<.!
11

*In ing/1, unless otherwise indicated.
                                              61

-------
                                     TABLE A-3 (Continued)

Constituents* 9/17/81
COMPREHENSIVE MONITORING*
Aluminum
Barium
Beryllium
Cadmi urn
Chromium
Cobalt
Copper
Cyanide
Lead
Lithium
Manganese
Nickel
Phenols
Phosphorus
-Ortho
-Total
Silver
Strontium
Sulfide
Thallium
Thiosulfate
Tin
5/27/82

.04
.082
<.0005
<.001
<.005
<.005
<.001
<0.005
<.01
.09
<.002
<.005
<.005

<.01
.4
<.001
8.4
<.l
<.005
<5
<.05
Sampling Date
7/20/82 9/23/82 11/17/82

.27
1.05
<.0005
<.005
<.005
<.005
<.001

<.01
.077
<.002
<.001


<.4
<.05
<.001
7.2





<1.0 .089
<1.0
<.01
.005 <.004
.024
<.05
<.005
<0.5
<.01
.079
.042 .063
<.05 .01
<.05

<.4
.087
<.001
9.19 7.49
<.l

<.05
<0.01
1/7/83

] .158
.075
1.103
<.004
<-05
<.05
.021
<.l
.025
.085
.022
<.01
<.05

<.01
.166
<.01
8.1
.06
.011
<.05

3/9/83

.115
.07
.946
<.004
<-05
<.05
<.005
8.72
.025
.079
<.OOS
<:.01


<.01
.379
<.01
7.14

.005



*In mg/1, unless otherwise indicated.
                                            62

-------
                                       TABLE A-3 (Continued)

Constituents*
Titanium
Zinc
Turbidity
Uranium-234 (pci/1)
Uranium-235 (pci/1)
Uranium-238 (pci/1)
9/17/81 5/27/82
<.5
. 006
1.2
.5 ± .9
0 ± .1
.5 ± .9
Sampling Date
7/20/82 9/23/82 11/17/82
<.05
.007 : ..068
1.7 5.2
0.2 ± 0.2
0.0 ± 0.1
0.3 ± 0.3
1/7/83 3/9/83

.08 .013





*In mg/1, unless otherwise indicated.
                                              63

-------
                        APPENDIX B





ANALYTICAL AND FIELD DATA FOR THE SAMPLING SITES ON TRACT C-b
                          64

-------
               TABLE B-l:-  ANALYTICAL AND FIELD DATA FOR THE MINE DISCHARGE TO POND A.

Constituents*
ABBREVIATED MONITORING
Ammonia (NH3-N)
Arsenic
Bicarbonate
Carbonate
Calcium
Chloride
Fluoride
Iron
Magnesium
Mercury (yg/1 )
Molybdenum
Nitrate (N03-N)
Potassium
Selenium
Silica
Sodium
Sulfate
Vanadium
Acidity (As CaCOj)
Alkalinity (As CaC03)
9/16/81

.90
<.01
1135
10.8
7.30
8.34
15.3
.08
4.40
<.3
<.l
1.2
4.3
<.01
23
540
176
<.5
< 5
1147
5/27/82

.24
< .005
1245
28.6
7.0 '
• 7.2
19.2
.063
4.0
<.001
<.05
4.0
2.9
.02
6.7
530
16.8

5.2
1068
Sampling Date
7/20/82 9/23/82 11/17/82

.688
<.003
1300
46.1
4.78
6.61
19.8
.210
5.38
<.001
.14
1.2
2.29
<.002
7.3
578
13.6

3.57
1140

.208
.003
896
24.1
5.5
5.79
17.0
<.l
4.31
<.001
<.03
1.34
1.81
<.002 -

391
10.9
<.l
3.24
775


<.005
1190
53.3
6.08
7.47
11.1
<.01
5.0

.125
3.12
1.65
<.002
7.23
525
22.6

2.63
1065
1/7/83

.342
<.005
-1320
46.9
5.62
7.4
18.9
-.079
4.52
<.001
<.03
4.12
1.92
<.01
7.06
551
14.6
<.005
3.63
1160
3/9/B3

.396
<,005
1350
33.2
5.52
8.14
19.04
.026
3.S
<.001
.883
3.91
4.67
-:.01
6. 1C
545
17
<.005
5.3
1160

*In mg/1, unless otherwise  indicated.
                                                65

-------
                                           TABLE 8-1 (Continued)

Constituents*
Conductivity (field,
umhos/cm)
DOC
pH (field, units)
Dissolved Oxygen
(field, ppm)
Boron
Fractionated DOC
-Hydrophobics (Total )
-Bases
-Acids
-Neutral
-Hydrophilics (Total)
-Bases
-Acids
-Neutrals
Residues
-TDS
-TSS
-Total Solids
-Total Volatile
-Settleable Matter (ral/1)
Temperature (field, °C)
•• - •
9/16/81

2275
4.7
9.2

4.0
.86

3.9
0.2
0.9
2.8
0.8
0.2
0.3
0.3

1354
565
1919
320
4.5
13
Sampling Date
5/27/82 7/20/82 9/23/82 11/17/82

2430 2500 1620 1925
3.0 <3 2.8 5
8-4 8.8 8.6 8.2

4-3 5.7 5.4 4.3
•87 -77 <3 .756

2-2 1.8
0.0 o.l
0-8 0.6
1-3 ' 1.2
0.8 o.9
o.i o.o
0-4 0.6
0-3 0.3

1280 1312 912 1361
8 <4 <4 <4
1296 1424 958 1372
194 117 88
<1 <.i 1
21 23.5 22 16
1/7/83 .

2100
4.3 ,
8

4.6
.739

2.3
o.i t
1.0
1.2
2.0
0.9
0.6
.0.5

1380
<4
1380
172
< 1
16
3/9/H3

2100
<2
(5.3

4.0
.73U










1366
6
1372
136
<
17
	 	 	 	 — • 	
*In mg/1,  unless  otherwise indicated.
                                                       66

-------
                                         TABLE 8-1  (Continued)

Constituents* 9/16/81
COMPREHENSIVE MONITORING*
Aluminum
Barium
Beryllium
Cadmium
Chromium
Cobalt
Copper
Cyanide
Lead
Lithium
Manganese
Nickel
Phenols
-Ortho
-Total
Silver
Strontium
Sulfide
Thai! ium
Thiosulfate
Tin
5/27/82

.1
.92
<.0005
<.001
<.005
<.005
<.001
<.005
<.01
.043
<.002
<.005
<.005
<.01
.8
<.001
2.0
<.l
<.005
< 5
<.05
Sampling Date
7/20/82 9/23/82 11/17/82

.31
1.05
<.0005
.016 <
<.005
<.OOS
.001 <

<.01
.028
.063
<.001

<.4
.34
.001 <
1.1





<1 .036
1.05
<.01
.005 .004
<.02
<.05
.005
<.05
<.01
.062
.004 .65
<.05 .01
<.05
<.4 <.01
.043
.001
1.73 1.15
< .1

<.05
<.01
1/7/83

.181
.742
.647
<.004
<.05
<.OS
.119
<.l
.025
.04
.007
<.01
<.5

.244
<.01
1.31
.06
.026
<.05

3/9/C3

.414
.751
4.24
<.004
<.05
<.QS
<.005
<.l
<.C25
.037
<.005
<.01

.212
l.OS
<.01
1.P4

.QCS



"In Kig/1,  unless otherwise indicated.
                                                   67

-------
                                       TABLE B-l  (Continued)

Constituents*
Ti tanium
Zinc
Turbidity (NTU)
Uranium-234 (pci/1)
Uranium-235 (pci/1)
Uranium-238. (pci/1)
9/16/81 5/27/82
<.5
.007
2.8
1.6 ± 1.4
0.0 ± .1
2.3 ± 1.9
Sampling Date
7/20/82 9/23/82 11/17/82
"=•5
.007 .001
.8 1.9
0.0 ± .2
0.0 ± .3
0.4 ± .5
1/7/83 3/9/H3

.02 .001





*In mg/1, unless otherwise indicated.
                                                 68

-------
                  TABLE  B-2:  ANALYTICAL AND FIELD DATA FOR THE DISCHARGE OF POND B.

Constituents*
ABBREVIATED MONITORING
Ammonia (NH3-N)
Arsenic
Bicarbonate
Carbonate
Calcium
Chloride
Fluoride
Iron
Magnesium
Mercury (mg/1)
Molybdenum
Nitrate (NO-j-N)
Potassium
Selenium
Silica
Sodium
Sulfate
Vanadium
Acidity (As CaC03)
Alkalinity (As CaCOj)
9/16/81

1.33
<-01
1069
<1.0
6.50
8.12
15.10
.05
4.60
<.3
<.l
1.5
4.1
<.01
35
540
311
<.5
<5
926
5/28/82

.28
<.005
1295
25.9
10
7.2
19,7
.048
5.7
<.001
<.05
2.45
2.7
<.02
6.6
550
50.3

6.2
1104
Sampling Date
7/20/82 9/23/82 11/17/82

.326
<.003'
1210
48.2
4.78
6.09
18.2
.311
4.64
<.001
.11
<1.0
2.2
<.002
7.5
541
16.2
<.l
2.97
1070

.346
.004
1359
45.7
5.99
6.13
18.7
<.l
4.07
<.001
<.03
< 1.0
2.56
<.002

578
5.98

3.94
1190


<.005
1274
47.5
5.67
7.25
12.2
<.01
3.94

.063
5.82
1.66
<.002
5.61
522
14.4

3.36
1124
1/7/83

.342
<.005
-1287
63.2
5.43
6.98
18.1
.126,
4.61
.002
<.03
2.5
1.7
<.01
6.75
555
15.7
<.005
2.6
1160
3/9/83

.372
' <.005
1340
38.6
6.04
8.14
19.23
.065
4.13
.002
.804
12.1
4.94
<.01
5.98
545
17.5
<.005
4.5
1160

*In mg/1,  unless otherwise indicated.
                                                   69

-------
                                       TABLE  B-2  (Continued)

Constituents*
Conductivity (field,
umhos/cm)
DOC
pH (field, units)
Dissolved Oxygen
(field, ppm)
Boron
Fractionated DOC
-Hydrophobics (Total)
-Bases
-Acids
-Neutral
-Hydrophilics (Total)
-Bases
-Acids
-Neutrals
Residues
•-TDS
-TSS
-Total Solids
-Total Volatile
-•Settleable Matter
Temperature (field, °C)
9/16/81
2200
3.9
7.8
9 ,
.79

2.1
0.3
1.7
0.2
1.5
0.1
1.0
0.3

1517
6
1523
297
<.l
15.5
5/28/82
2000
3.7
8.5
7.0
.990

3.0
0.1
1.1
1.8
0.7
0.2
0.3
0.3

1390
<4
1395
N/M
<1
20
Sampling Date
7/20/82 9/23/82 11/17/82
2100
<3
9.2
6.3
.83










1206
<4
1342
244
<.l
23
2500 2150
3.6 2
8.5 9.0
4.3 4.5
<3 .648

2.3
0.1
1.2
1.0
1.3
0.1
0.6
0.7

1380 1354
5 <4
1439 1358
125 120
<.l <.l
22 15
1/7/83
2100
4.2
8.2
4.7
.718

3.0
0.1
- 1..1
1.9
1.2
0.5
0.0
:o.7

1398
<4
1398
180
<.l
13
3/9/83
2050
6
8.3
5.1
.736










1352
<4
1356
96
<.l
12

"In mg/1,  unless  otherwise  indicated.
                                                   70

-------
                                        TABLE B-2 (Continued)

Constituents* 9/16/81
COMPREHENSIVE MONITORING*
Al umi num
Barium
Beryllium
Cadmium
Chromium
Cobalt
Copper
Cyanide
Lead
Lithium
Manganese
Nickel
Phenols
Phosphorus
-Ortho
-Total
Silver
Strontium
Sulfide
Thallium
Thiosulfate
Tin
5/28/82

.2
.83
<.0005
<.001
<.005
<.005
.002
<.005
<.01
.042
<.002
<.005
. <.005

<.01
1.0
<.001
1.8
<.l
<.005
<5
<.05
Sampling Date
7/20/82 9/23/82 11/17/82

.3
1.34
<.0005
<.005
<.005
<.005
<.001

.04
.028
.012
<.001


<.4
<.05
<.001
1.0





<1 <.02
1.34
<.01
.008 <.004
<.02
.<.05
<.005
<.05
<.01
.056
.004 1.47
<.05 .01
<.OS

<-4
.224
<.001
1.73 .977
<.l

<.OS
<.01
1/7/83

.235
.735
.166
<.004
<.05
<.05
<.005
<.l
<.025
.043
<.005
<.01
<.05

<.01
.202
<.01
1.29
.06
.033
<.5

3/9/83

.586
.748
6.35
<.004
<.OS
<.05
<.005
1.06
<.025
.037
<.005
<.01


.166
1.03
<.01
1.76

.026



*In mg/1, unless otherwise  indicated.
                                                71

-------
                                     TABLE B-2 (Continued)

Constituents*
Titanium
Zinc
Turbidity
Uranium-234 (pci/1)
Uranium-235 (pci/1)
Uranium-238 (pci/1)
9/16/81 5/28/82
<.05
.008
1.2
.5 ± .9
0.0 i .1
.5 t .9
Sampling Date
7/20/82 9/23/82 11/17/82
<.5
.013 .007
1.9 1.2
0.0 ± .2
0.0 ± .2
0.1 ± .2
1/7/83 . 3/9/83

.02 .007





*In  rag/1,  unless otherwise indicated.
                                                72

-------
TECHNICAL REPORT DATA
(Please read Instructions on the reverse before completing)
1. REPORT NO.
2.
4. TITLE AND SUBTITLE
Characterization of Oil Shale Mine Waters,
Central Piceance Basin, Colorado
7. AUTHOR(S)
K. E. Kelly
J. D. Dedrick
9. PERFORMING ORGANIZATION NAME AN
Kaman Tempo
600 South Cherry Street
Denver, Colorado 80222
D ADDRESS
12. SPONSORING AGENCY NAME AND ADDRESS
Industrial Environmental Research Laboratory
US EPA
Cincinnati, Ohio 45268

3. RECIPIENT'S ACCESSION NO.
5' 'larch ?A7§4
6. PERFORMING ORGANIZATION CODE
8. PERFORMING ORGANIZATION REPORT NO.
10. PROGRAM ELEMENT NO.
N104 Multimedia Energy
1 1 . CONTRACT/GRANT NO.
Contract 68-03-2449
13. TYPE OF REPORT AND PERIOD COVERED
Final
14. SPONSORING AGENCY CODE
15. SUPPLEMENTARY NOTES
16. ABSTRACT
A study was conducted to characterize the oil shale mine waters in the
Piceance Basin. The study sites were Federal Prototype Lease Tracts C-a and C-b ,
located in the central portion of the basin. The objective was to collect water
quality data in order to characterize the mine waters and to assess the effective-
ness of treatment systems located at these facilities. These treatment systems
involve in-series retention ponds . :
The overall conclusion with respect to the effectiveness of the retention
pond systems in maintaining or improving water quality is that they appear to
make negligible difference unless chemicals are added. The addition of the ;
flocculent during periods of active mining was very effective in reducing the
suspended sediment concentrations. In addition, sulfuric acid treatment reduced
the pH. — - - .- - -
Concerning the general water quality, such as the trace elements, cations :
,__and anions, and other pertinent constituents, there was not a significant increase
or decrease due to the chemical additives. In addition, the effectiveness of the
one-pond and two-pond systems are very similiar. '.
17.
2 DESCRIPTORS
Synthetic Fuels
Oil Shale
Minewaters
Wastewater treatment
18 DISTRIBUTION STATEMENT
'
jxexease unlimited
KEY WORDS AND DOCUMENT ANALYSIS
b. IDENTIFIERS/OPEN ENDED TERMS
Colorado
Mining
Piceance
19. SECURITY CLASS /This Reoor!)
|
20. SECURITY CLASS ,This page I

c. COSATI Held/Group
68D
05C
21. NO. OF PAGES :
22. PRICE
EPA FOTTT 2220 —I  (Rev. 4 — 77)    PREVIOUS EDITION is OBSOLETE

-------
                          PROJECT  SUMMARY          ;
             CHARACTERIZATION  OF OIL  SHALE  MINE  WATERS
                 CENTRAL  PICEANCE'  BASIN, COLORADO
                                by
                KEVIN  E.  KELLY  AND JIM  D.  DEDERICK
     A  study   was conducted  to  characterize  the  oil   shale   mine
waters  in the  Piceance  Basin.    The  study  sites  were  the  Federal
Prototype  Lease  Tracts  C-a  and  C-b,   located   in  the   central
portion of the  basin.  The  objective  was  to collect  water  quality
data  in order  to characterize the mine  waters and to  assess   the
effectiveness   of  the  treatment  systems   located    at    these
facilities.   These treatment  systems  involve  in-series retention
ponds.  Additionally, the effectiveness  of  a  one-pond  versus  two-
pond system was investigated.                     ;

     The  sources of the water routed  through  the retention  ponds
were  water pumped from the on-site aquifers  that were  dewatered
during  mining  activities and  the  water  pumped directly from   the
underground mines.  Water samples  were taken  from .both  the inflow
and  outflow points for both the Tract C-a  and C-b   pond   systems
and  were analyzed for a fairly 'detailed  suite of selected   water
quality  parameters.   This suite  included  total  suspended solids
(TSS) and total dissolved solids (TDS),   pH,  the  major  species of
cations  and  anions,   and  dissolved   trace  elements  such  as
selenium,   lead,  and  arsenic.   The  inflow  samples   were   then
compared  to  the outflow samples to  determine changes  in   water
quality and, therefore, the effectiveness of the  retention ponds.
An  additional  part  to this study was   the   assessment   of   the

-------
effectiveness  of  using a flocculent and sulfuric acid  for  the
treatment  of excess waters encountered during active  mining  on
Tract  C-b.   The  flocculent was added to reduce  the  suspended
solids  concentrations  and  the  acid was  used  to  reduce  the
somewhat high pH values.

     The  water quality changes observed during this study,  when
comparing  the  inflow  waters  to  the  outflow  waters  of  the
respective  pond  systems,  were  found to  be  generally  small.
Fluctuations  may have been due to such phenomena as pH  changes,
aeration, evaporation, and oxidation-reduction changes associated
with  the transformation of the groundwater from  an  underground
(aquifer)  environment to a surface (retention pond) 'environment.
The  retention  time,  as well as inherent  laboratory  technique
variations, may also help explain the small fluctuations.

     The overall conclusion with respect to the effectiveness  of
the  retention  pond  systems in maintaining or  improving  water
quality  is  that they appear to make no  significant  difference
unless  chemicals are added.   The addition of the flocculent  in
the Tract C-b pond system was effective in reducing the suspended
sediment  concentrations.    In  addition,   the  sulfuric   acid
treatment  effectively  reduced the pH  values.   Concerning  the
general  water quality,  such as the trace elements,  cations and
anions,  and other pertinent parameters,  there was no noticeable
increase or decrease.

-------
                          INTRODUCTION


     The  objective  of  this study was  to  provide  a  detailed
characterization of the mine waters and treatment systems used on
Federal  Prototype  Lease  Tracts C-a and  C/-b,  located  in  the
Piceance Basin,  Colorado (Figure 1).   These data were collected
to  assist  other  oil  shale developers and  permit  writers  in
selecting  appropriate controls for the handling of  excess  mine
waters.

     The  treatment facilities for the excess mine waters at both
sites   consisted   of  two  in-series   retention   ponds.    To
characterize  these  facilities,   samples  were  collected   for
determining  the chemistry of water derived from mine pumpage and
aquifer   dewatering  activities  previous  to   treatment.    In
addition,  samples were derived from the outflow of the in-series
retention ponds to characterize the  treatment.   Presently,  the
treated  water is disposed of by rei-njection into the groundwater
system,  is utilized for on-site activities,  or is discharged to
surface water systems.  The approach, data collection procedures,
and results are discussed below.

                            APPROACH

     The  procedures utilized for obtaining these  data  involved
collecting  grab samples of five sampling points.   On Tract C-a,
the  sample  collection included sampling the mine  water  inflow
into  the primary retention pond (Geffrey Pond),  rthe outflow  of
the  primary  retention pond into the  secondary  retention  pond

-------
o
00
cr>
 o
 in

 to
 in
 03
CO


 
 o
 03
 £=
 o
 (T3
 O
 O
 a>

-------
(West Retention Pond),  and the discharge from the secondary pond
previous  to disposal.   It was felt that Jeffrey Pond was fairly
inconsequential with respect to the total treatment  system due to
the  very short residence time of the mine waters in  this  pond.
Therefore,  the  above described sampling scheme would adequately
assess the effectiveness of treating the excess mine waters  with
a one-pond system, namely the West Retention Pond.

     In regard to Tract C-b, samples of untreated mine water were
collected at the inflow point of the primary retention pond (Pond
A).   In  addition,  samples of the treated water were  collected
from  the  discharge  of the secondary retention pond  (Pond  B),
which is in-series with Pond A.   During periods of  active mining
on Tract C-b,  sulfuric acid and a magnifloc catibnic  flocculent
were  added  to  the  ponds in order to treat the  pH  and  total
suspended  solids (TSS),  respectively.   This sampling  strategy
assessed  the effectiveness of treatment consisting  of two  ponds
which are in series.   In addition,  the samp!ing .program allowed
for  an evaluation of chemical treatment  (i.e.,  flocculent  and
suIf uric acid).

     The  following  constituents  were  measured  in  the  field
immediately   upon   sample   withdrawal:     pH,    temperature,
conductivity,  and  dissolved  oxygen.   The  samples  were  then
filtered  (if necessary) and preserved according to  the U.S.  EPA
(1979) recommended procedures.   The samples were then shipped to
the laboratories located at the Colorado State University in Fort
Collins, Colorado, and Core Laboratories 'in Denver,  Colorado.  In

-------
mbstjcases,  the U.S.  EPA  (1979)  recommended  holding  times   were
observed.   The  holding  times  for  a  few   constituents   of   the
samples  collected on July,   1982  were   exceeded.    However,   the
analytical  results  were generally  in  agreement with   those   for
other  sampling periods.    Exceptions to  this  include  nitrate  and
ammonia, which were higher  in concentration  than historic  trends.
Seven  samples  were collected at  each   sample  collection  point
between September, 1981 and March, 1983.

     A  fairly  detailed suite of  constituents was   selected   for
analysis during this study.   This suite  of  constituents  involved
two groups, an abbreviated  group and  a  comprehensive group (Table
1).   Analysis  for  the  abbreviated group  of  constituents   was
conducted during the months of September,  1981; September, 1982;
and  November,  1982.   Analysis for  the  comprehensive  group  of
constituents, which included  the abbreviaxed group,  was conducted
during the months of May,   1982;   July,   1982; January, 1983;  and
March,  1983.  These constituents  were  selected after  a review of
the baseline water quality  data collected by the Tract C-a and C-
b operators,  as well as the  chemical characterization studies of
simulated and observed in-situ oil shale  process waters conducted
by various researchers (e.g.,   Fox et al.,   1978;   Slawson, 1979;
Pfeffer,  1974, Stuber and Leenheer, 1978; LBL, 1978).

                         DATA DISCUSSION                        ;

     The   analytical   results  for  the data collected during  this
study  on  Tracts C-a and C-b are  presented  in Tables  2  and  3,
respectively.   In  order to  provide a perspective for evaluating
                              6

-------
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0



Acidity
Alkal inity
Ammon i a
Arsenic
Bicarbonate
Boron
Carbonate
Calcium
Chlori de
Conductivity
Dissolved Org

Alumi num
Bar i um
Beryl 1 i um
Cadmi um
Chromium
Cobalt
Copper
Cyan i de
Fractionated
DOC
LIST


0
0
0
0
0
0
0
0
0

an ic

0
0
0
0
0

0
0
0

OF PARAMETERS FOR
AND COMPREHENSIVE
ABBREVIATE
Dissolved Oxygen
Fluori de
Iron
Magnes i um
Mercury
Molybdenum
Nitrate
PH
Potassi um
•
Carbon (DOC)
COMPREHENSI
Lead
Lithium
Manganese
Nickel
Phosphorus
(total and ortho
Silver
Strontium
Sulf ide

A
D











VE





)




                               TABLE 1
                                         ABBREVIATED
                                        ANALYSIS
o
o
0
0
0
0
0
0
0
0

0
0
Residues
(Total, total
  dissolved,
  total , suspended,
  settleable,
  and volatile)
 Silica
Sodium
Sulfate
Temperature
Thallium
Thiosulfate
Tin
Titani urn
Turbidity
Urani urn
(234, 235,
Vanadi urn
Zinc
238)
NOTE:  Comprehensive list includes all parameters in the
       abbreviated list.

-------
I
Ol
1

§
:TENTION POND OUTF
a
1



—I
1
RETKNTION
5-
|
i
P
JEKFRKY f
z
hi



Is

s
X
z

i
c: •
ca a

z
<
S
or
1
Sgi
ca c
=

ce
1
e
E-
u
3
en
2§
V
" 03


O>
O
o
m
eM O
en o
o
V
evj -J
'§

2

m
p* a
KP O


•e u
z z
O ci:
IS
< *C
cy\ en P"* en *«^ co PO
O4 CM CO —» CO^OCM— *OO4^
o en •-* ~* i-4 in o
— < p* oo*— »o*-*ooen
co ~i ro tn o CM en ~« v en v
4
fS
f*icncoc3 moen-H— «c3in*o
in tococo cs en^*-^ o
in en o\ co
in in
-H
™ ^9 S° s
z e- tiit-,**v^t_d;ci; ^z zjco
o ciEOt-g^z^c: — Lg M — cti
HzoSceB-goSoa: ScSccc
<:o£L3Oa E5oa:coozz>-a£
, DISSOLVED
cC

o in
r- in
r- \o
o 03
o
?m m
»— m CN
M in r-
CO CO
r-4

0
rsj o in
-H
«» >o *r
v -H r-
o
t~4
0 3 co o<
o
"" 2 m

T P-
m
o o in
— t r- -v
*^ en
rsj co -H
rM
PO O P*3
— < cn

in 01
^* CO «-^
en
~~ ^3* n
^i r- ^
— « en
eN o en
en — « evi
— < o o

CJ 3 ft
— Si
•— O =
CO CO CO
2
m
o en
V 
en

en
r-t
in
o es
o in
v  .»
                                                                        o u
                                                                          (D
                                                                        U i.
                                                                        U 0)
                                                                        0) Q
                                                                        Si

-------
OO
o


UJ
h-

LU
—I

O


eC
o-

1=1

o
a.

CJ3

t—i
a
	i
o
-Q
 I
00


UJ
—I
CO




p—
Z
UJ
ae
S
UJ
0 CHEMICAL 1



Z
UJ
CJ
CO
z
t— 1
CJ
CJ
OS
u.
=1
CO





co e=
CO
ca
o
a.
Ssc
to
OS •-<
u_ 3:
o
u_
o z
UJ
ac
UJ
CO
a:
=3
Z
0 -
P— UJ
co ca
|
 CO CM CO CO i— tO C3 r~ m O CO 10 O CO CO
CO 10 CO ^ p— 10 i—
p— CM r— p— p—
CO CM p— CM CO f— CO U1 CO O
p— CM p— p— p— '
CO p— en CO CM U1O P—
i0V co p— t— CMCT»P— co«fp— VCM
o CM to 10 CM LOCO en
p- CM p— r—
en o GO co co co r» ocoo^i-p— CMCO IOCOP— to »CM
COp— r*- p— UT)i0t— CMp— VCM^r-*V
p— CM cotncnco iop—
p— CM p— P—
UJ
Z'Z a ea i— — •
co us > ca _j «a:o
>• os>> -j z to *-* a: — '
»-• «C X O ua CO r—
uj p— * cj co co a. i— i «£ uj uj
i— »-» E ac co co _j _i _j as >- — -
< uj =» o co cj co a: =1 ac •-* ^ co o co 3 P-M
 z >ea ^ uj uu •-< uj uj < = uj = >- z *-
ZZO=ZOHHCt= = J=OCSOa= UJCO
Ul -*->
p— ca
c
"S,"
f
c ca
* CO

-------
the  mine  water data,  the analytical  results  were   compared   to
groundwater and surface water baseline  data,  as  well  as   Federal
Drinking Water Standards.   This comparison'is  not.meant  to  imply
that the discharges should meet these standards.   The  comparisons
for  the Tract C-a and C-b data are presented in  Tables 4  and.  5,
respecti vely.

     The  Tract C-a system involved treating the  water  in  a   one;-
pond  system  and reinjecting all of the treated  water  back   into
the  groundwater  system.   Concerning  the effectiveness   of   th:e
treatment  of the mine waters,  the following   constituents   were
found   to  generally  exceed  baseline  groundwater   conditions:
carbonate,  calcium,  conductivity, fluoride, magnesium,  nitrate,
TDS,   sulfate,   and  pH.    However,   the  increase  in   these
constituents above groundwater baseline conditions- were small.

     The  following  constituents exceeded the  Federal   Drinking
Water  Quality  Standards  in the discharge from   the  Tract   C-a
system:   iron, TDS, sulfate, and pH.  However,  these constituents
also exceeded standards in the groundwater analyzed to  determin-e
baseline  water quality conditions.   Therefore,   this aspect  may
not be a problem if the water is reinjected.

     In   regard  to the Tract C-b in-series  two   pond  treatment
system,   the  following  constituents in the  discharge  exceeded
baseline   groundwater  quality   concentrations:    bicarbonate.,
carbonate,    conductivity,    fluoride,   molybdenum,   nitrate,
potassium,  TDS,   silica,  sodium,  and pH.  However,  none of  the
increases were very great.  In addition, during periods of active
                              10

-------
 CO



 a


 I
 CO
CD
a:
a
LU
u_
O


«=C
O  CO


UJ  
UJ O
a
•
O
ce.
   «c
I— Q
   Q
I— O
   a.
O C£J
O Q
CO _l
1-1 O
O
O
03
•a:



























«s


t
CJ
I—
as
p-











10
—
•?
CJ

h—

"*"
£
g
UJ
Z
-J
UJ
CO
eo
















as

taTc/J

02
11
Z 1—
t-t CO
as
ca >•
j—
3- *~
as <
ea 5
UJ
u.

z
2i
r- _
Z u.
LU 1—
p- SD
LUO
02
ea
(— Z
UJ Q_
3
Z
2 3:

UJ U.
(•— 2
UJ t— 1
OS
r- Z
UJ O_






Z
o o
r— a.
IE >-
-J LU
U. U.
1— t LU
1-3

LU
U_
O
^
OS
UJ
OS O
LU _J
r-
<
O
z
las
tS LU

O
«£
LU
a.













CO
CO r-
li
•x. a.
o
CJ OS
UJ U_
C/) CJ
o
±
—
*
CM
OS OS
E CU
l_4
as as
O. '.!_
CJ
O
LU
3; — >







LU
Z 3
£5
UJ
*-« «C
31 >



LU
«C _1





UJ
1-4 <


UJ
li
UJ
C3 _I



UJ
uj «e



UJ
55
3= >


LU
< —I






•k
£
Z
LU
t—
CO


in
0 «
0
OOCOOOCMen to COCOr— OOOOi— CM^mLOOOOCMCOCnO^OCO
m ^ r— COCOCM *"" i— «*• £?





CM co to ^ en co co CM CM co CM co co en <0 tn <0
SS » J • qg^-g-g-SRg 5
co to
CM CD o f^- "enen^ r— o en
co o co «* m «r LO r» tn en co in CM r— o o en ca
oocoor-cocn o ^cor— o co o co ^- wao^DCMOcoocacoi— o^r^rcn


F- r- »—

CM COOO"* LOOCO*— Or— COP-- CO to CM 00(0
O — J to O r* f— CO ^- CO r— OCMO^O <*u9COCO«J<>_JCOOCM_]CO(0ph>
eaco ^ co co cotocncar— ear— cn^-eaun
COtn <• r— r— r— CO CQ (— COCO^"

r- r— r—
co r* uo
p^ o r— en c\j f^ o CM ic> r— o in
^*O ^OP^UO f^COP*-OOF-OCM r— O O^T CM
o o en o en co co oo*r\0i— .— toocMr— CM«rco>0ocnocoooocnt0en
Vcn «a- into en tnvofMVr—vcMocovo
mCMCM r— CM CM CM*fm

CM r— ,_
co CM co co C3 in o co r— f— o m >0 co en i— r~-
o «i m o t0 co co o co *^ i— o o o o o *f ^ «~~ r*> _j ^ ^ co r— CM _j in en r^
cam co en co encar— cncs*— cs»— cnoovo
coun to en co o r- co co i— ^ca«s>
O O O O CM O O CM
CM o o o ^*- co UD ea P— i CM ^o o i CM i 01 i i i IOCMOOI (oca
en i0 r— co co 10 to
CM CO CO r-^ CM*

m " ^ in to in p».
CO CM CM CM CM CO CO «T CM <^ CO i—
Car- Cnr-r-COCn CO r— I «0 CO CO 1 O 1 101 1 1 1 1 _l O <• O 1 ICOP-^
— i en » CM p— to r— co P— ear— com in
o to CM en eo CM CM to
CO »
r~

CO O CO CO O to O CO
i — oca^uaocn o intr— co r— CO r— tO en V tO P^ C3 ^*
p*>c\t»0 r— p— r-enco
CM CM CM r— CM

p- p— in co P- o co
co o i— • en m en CMCOCOCOLO coco p-
oo^*oocov0*CM o i o 10 en i o i f— ' i > i i -j CM •— «r t i<-v0
^ co i — .Or— in (0 OCOOP— m
p* P— CM co co «r >0

f— r-
as

Z o ea i— —
Z LU UJ LU LU < tj
ea tD ^ ea _..' z o
ca >• _j z co i-* —
^ "w" as x o LU ea H- uj
UJ t— S < O CO O_ t— i ^ _J UJ
t— *-i^cj a: crt oo _j _j ca or >-— »
z t— tu i— i g tu cj uj uj =) z ^coeacoco^ujr-ac z i-« -j
i— » »-H ea ^^*->

tt) S*3
CJ OJ ^O
E u


3 -T3
O >i w»
J= (T3 t-
V> -O 3
O> OJ H— — -
cn <= M
J= 3 S 3
 " L> (Q
•r- Wl W t.
TO g O O
-i-* fc. a. E
_e; es f— «*•*
o- -»-> t-
^ i_ 5 *~
tcu
*-• < >»
•r- (O Cl_ r-
IE LU •*—
o m
-*-» E
a> *- irt os *
 0>
U) «- T3 1 -u ^ r-
Tj CLU- V E _g
 1 JO _) i_
JC O  «—
O 0> r- u O 03 O
(_ J5 t- «r- l_
M 0) «J O -*^ OJ O
(/) **• OJ **- u Q. U
r— t_ t. LU -i-» a) *a
C O 0) t— r—
3 to tk. >»ea ea
r- in LU f— 3 O O
"N. rg (O O •—
o> >» u. *— -*-> as
E T3 r— O* OJ C
 ••
C T3 (TS 
"~ "> 0> "" " S "
trt O -O -M ,J o. 3
Of t. oj o ea o> o
3 o. u. z co ca co
rt3
* r- CM CO ^- tn «0
                                                                   11

-------
00
o
Q

3
00
QC
LU

i
 LU
O —J
a: _i
o o
O
=C
a:
   2
o CD
O Q
00 _l
>-> o
CQ





<
g
s
a
g
.0
O
|







JS
B
§
£
5
.









UJ
|
3
1
VI


1
^
X



?
^


LU
i

LJ





Ji
|i
11
"s
5
|
||

si
i°"

•L. ea
||
d

g<
II


XI—
S3
n
ill
£§
O£
UJ
OS
3

OS
1
£




SECONDARY
(40CFR PART 143)
~£S
££
S|




l!
z =
SS

li
S3
£ 5
==
^
2i
«:=»
= =
ta _
S5
=s
£S
i§
3=»
5 =
^5

Si
IU
IS-
ITUENTS*
»
A
ul
„  ^ ' »«
So SeMO^ o O !*•« r» o eor-. o r— o S m c"> o CM  ^ ^ ea •* CM e= d
oatM ^- n co ^- m oa in ea <—
01 c3 r- o^ ^ as r— 10 o r— too co vo o co CD
vuiui eg r- cBcvir\jvr>c\iv>0
co in co •» !— in i—
^. (M ^- ,» ^_
O«— i— tpmr- eo m*r- -r tsttM en r- O r- Ven_ jiaoiA_jcor-ce
ai^ ^ *~ S co_* *~ea Si *~ S e§
So S oat^oor^o •— o o CM
Oinaaocnr-to o i 10 o o CM o O wt o i i i t •— o O o o o t «r «?>
ia "~ i« ^ O »— co in
CO 0t r- CM
fu co » o en • o o
ocvrviOf— coco v loiooviaoco co i i i icnor-cocno t CM co
s^-ss * £ -;=CM£
2o S «« |S Sir-
O in CM o CM ^taoocn CM i i i ICNJOCDOO^I^TCD
oeoi--c\i^ ^ m ^<0 evi^tncnvcTi
>C » 1— r- r- ^
*• en oo f^ i— to S
o^ F— (n o* m e7> «n o CM o eo <•» r- o » eo
CM vo i— m «r CT» f— •—  i t t i i o" as ei o O i i en
LO cC en" .n ~ r."
o eo SS o S • • i^
r~OO^5O*-C= O CO i^C9^-«3e3»- O 1 t 1 1 l O* CO O CO O 1 1 eo
O CM CM CM r— \ft '
^ i— r»  o7<= lijieo*
^ 5S oSoP^uT
S« S?oo« a:= = 2ie3SSI t^
-tjl 5a=sS^§S§ca 2§uj2S3°^W*Sei= uj = » S ^
>-»-*e3 z = «-.<_)0_K_it- vaeii— to = «i_j«j_j_ttu— «:KI— — t— — e
§3=a£Zoi- t_> ae ae _j _i ;c */i o to ;s o o — 1 1— H- v» cs o O o LU uj _i _j o_i ^ »-« ^
« — o«3So :t— — -toe^oi-ouj^t-i-f-wjt-iu^ejsxtjjz












.15
s*a
?o"-
2*1
1_ O *—
^s!
l~v
li^
•— ta
w> ^ »
i- T) " V
•g3^ 2
X-Tfe 2
'132 |
Its ^
5s^ *
E — < >.
""52; ^
2£ , 5
•aSt L. e
i-Sef °g -
** 01^ o r^
o ai n en
- *ffl  r^
g. *£ g'g g §-^21
x "• oUJ'St2:ert .
« fo u- **ea v*
^ s^ijfSs
| llf^lss
~ i-g!n j !.§ s
« t-
-------
mining  on Tract C-b,  flocculent and sulfuric  acid  were  added  to
the system to settle suspended solids and  lower the  pH,   previous
to the discharge to Piceance Creek.  This.treatment  was effective
and  should be utilized if suspended solids and pH are  areas   of
concern.

     The  quality  of the discharge from Tract  C-b also   exceeded
many  constituents in the Federal Drinking  Water  Standards,   as
well as the baseline water quality data for Piceance Creek.   For
example,  iron,  TDS,  and  sulfate  exceed  the  Drinking  Water
Standards.   In addition, ammonia, bicarbonate, boron, carbonate,
conductivity,  fluoride,  iron,  molybdenum,  nitrate, potassium,
TDS, ' temperature, silica, sodium, alkalinity, and pH all  exceeded
the   baseline  water  quality  conditions  of  Piceance   Creek.
However,   all  of  these  constituents  were   within  reasonable
agreement with baseline groundwater quality,  which  is considered
poor.    Furthermore,  the  water  discharged  to  Piceance  Creek
appears to be adequate for livestock and irrigation  use.

     The   water  quality  changes  observed  in  the  data  when
comparing  inflow  and  outflow of  the  treatment   systems  were
generally  insignificant.   These changes can probably be related
to pH  changes,  aeration,  evaporation,  and  reduction-oxidation
                                                  i
changes  associated  with the transformation of  the  groundwater
from an underground environment to a surface environment, as well
as the associated retention time in the ponds.  In addition, some
of the variations may be attributable to laboratory  procedures.

                              13

-------
                           CONCLUSION

     The  effectiveness of the treatment systems with respect   to
improving  water quality without use of chemicals appeared to   be
negligible.   For'the one-pond treatment system on Tract C--a,  the
overall  quality,  with the exception of total suspended  solids,
remained  essentially  unchanged during  treatment.   The  slight
decrease  in total  suspended solids concentrations from 6.3  mg/1
to  below  detection  limits is not  significant.   The  two-pon'd
treatment  system on Tract C-b is very similar in results to   the
one-pond system on  Tract C-a.   The general water quality did  not
improve or degrade after treatment.   However,  the addition of  a
flocculent  and  sulfuric acid was effective   in  reducing  total
suspended solids by nearly 99% and adjusting  pH to desired value.
                               14

-------