(PART II)
By
Glenn Catchpole, Project Manager,
OPI-Western Joint Venture
Roger Garling, Operations Superintendent (Former),
UNC Teton Exploration Drilling, Inc.
Mike Neumann, Senior Licensing Specialist,
Rocky Mountain Energy
INTRODUCTION
In the first issue of this two part article (see The Mining Claim, June 1984) an introduction to uranium solution mining was presented along with a review of the various groundwater restoration methods and the regulatory requirements that apply to groundwater clean-up. By way of review, solution mining is the process of recovering uranium from a water-saturated, underground orebody in a manner which leaves overlying rock strata and the land surface intact. The process involves the installation of a series of wells through which a chemical solution (lixiviant) is injected into the uranium-bearing formation, passed through the formation, and pumped back to the surface. From the recovery or production well, the uranium-bearing solution is piped to a surface plant where a series of conventional chemical processes extract uranium from the solution. The resulting solution, now barren of uranium, is then refortified with leach chemicals and reinjected into the orebody (See Figure 1). Typically, the leach chemicals consist of nothing more sophisticated (or non-toxic) than sodium bicarbonate (baking soda) and, oxygen.
Once all uranium has essentially been recovered from the orebody, groundwater affected by the leaching solution must be "cleaned up" to a condition which allows appropriate future use of the resource. Generally, regulatory agencies require that groundwater be returned to a quality as close to premining (baseline) conditions as can practically be achieved. The State of Wyoming requires that, at a minimum, groundwater be returned to a condition compatible with the premining use or potential use of the water.
The second part. of this two part series will focus on the groundwater restoration results from three Research and Development (R&D) uranium solution mining operations conducted in the late 70s and early 80s at three geographically separated sites in Wyoming. The water quality data from the three sites demonstrate that groundwater affected by solution mining activities can be restored to acceptable conditions. For background information the reader is encouraged to read Part I of this article.
REVIEW OF RESTORATION TECHNIQUES
To achieve restoration, constituents added to the groundwater for mining and
those mobilized during the mining process must be removed or rendered nonmobile.
In some cases, it may also be necessary to chemically treat the geologic formation
in order to reverse or inhibit reactions initiated during the mining phase.
The optimum restoration technique for a given site will be largely determined
by inherent geologic and hydrologic conditions of that site, and observations
made during the initial R&D phase. In general, however, combinations of
two basic approaches have been used most extensively within the industry in
Wyoming.
The first, and simplest of these techniques, is referred to as "groundwater
sweep" in which both chemical constituents and groundwater are removed from
the affected area by pumping selected wells. Although this technique has been
successfully employed at the R&D level, several considerations may preclude
total reliance on the groundwater sweep method for commercial- scale operations.
Disadvantages of the sweeping method include consumptive use of large volumes
of groundwater and extensive waste water storage facilities or evaporation ponds
which, in turn, require large surface disturbances.
A more accepted technique utilizes treatment equipment to remove chemical constituents
from the groundwater which renders the resulting water fit for reinjection into
the aquifer. Several processes exist for continuous water treatment. Those processes
most common to ISL restoration are reverse osmosis, electrodialysis, and ion
exchange. The advantages of utilizing continuous water treatment systems in
aquifer restoration, or a combination of groundwater sweeping followed by treatment
and reinjection, include:
· Reduction in groundwater consumption and waste generation by up to
90 percent;
Provides a means to direct groundwater flow in the aquifer through selective
well pumping and reinjection; and
Provides a means of introducing chemicals to the formation to reverse or inhibit continuing chemical reactions.
SUCCESSFUL CASE HISTORIES
A. Bison Basin Mine
The Bison Basin in-situ leach uranium mining project, located
in southern Fremont County, Wyo., is a joint venture between Ogle Petroleum
Inc. of Calif., the operator, and Western Fuel Inc., a subsidiary of the Duke
Power Company. In the summer and fall of 1979 the OPI-Western Joint Venture
conducted an R&D pilot scale uranium solution mining test to assess both
the amenability of the orebody to in-situ mining, and the technical and economic
practicality of restoration of the groundwater quality following mining.
The Bison Basin R&D project utilized sodium carbonate/bicarbonate as the
lixiviant and oxygen as the oxidant. Due to the high sodium levels in the groundwater
(400-500 mg/ 1) it was felt that sodium carbonate/bicarbonate would be an excellent
choice of lixiviant from both a mining and restoration standpoint. The R&D
wellfield consisted of four injection wells and three recovery wells arranged
in a line-drive configuration, and operated at a flow rate of about 25 gallons
per minute. Wells were completed within the mineralized zone of the Laney member
of the Green River formation, which is of lower Eocene age.
The mining phase of the pilot operation lasted three months during which the
amenability of the orebody to solution mining was adequately demonstrated. Target
values for total number of pounds recovered, product purity, and quantity of
uranium in solution (head grade) were achieved.
As part of the planning and procedures for the aquifer restoration phase of
the project, the OPI-Western Joint Venture followed a step-by-step program designed
to terminate each leaching reaction in the proper sequence. Following the sequential
mining termination process, the restoration activity of circulating clean, surface
treated water through the orebody aquifer was initiated. The surface water treatment
system consisted of a reverse osmosis (R.O.) unit rated at 30,000 gallons per
day (21 gpm).
TABLE I
BISON BASIN MINE
R & D RESTORATION
DATA
(units: mg/l unless
otherwise indicated)
| Parameter | Average Baseline Concentration | Post Restoration Concentration | DEQ Restoration Requirement |
| pH | 9.8 | 8.3 | 10.8 |
| TDS | 1500 | 1325 | 1650 |
| Ammonia (as N) | 0.72 | -0.10 (2) | 0.79 |
| Nitrate (as N) | 0.11 | 0.03 | 0.12 |
| Bicarbonate | 71.8 | 152.5 | 500 |
| Carbonate | 29.5 | 12.1 | (3) |
| Calcium | 36.1 | 53.8 | 500 |
| Chloride | 34.1 | 36.5 | 250 |
| Boron | -1.0 | -1.0 | -1.0 |
| Fluoride | 0.95 | 0.79 | 1.04 |
| Magnesium | 4.5 | 8.2 | 5.0 |
| Potassium | 9.75 | 6.8 | 10.7 |
| Sodium | 442 | 390 | 486 |
| Sulfate | 906 | 773 | 997 |
| Aluminum | -0.05 | -0.05 | -0.05 |
| Arsenic | -0.01 | -0.01 | -0.01 |
| Barium | -0.05 | -0.05 | 1.0 |
| Cadmium | -0.002 | -0.002 | -0.002 |
| Chromium | -0.01 | -0.01 | -0.01 |
| Copper | -0.01 | -0.01 | -0.01 |
| Iron | -0.03 | 0.02 | 0.03 |
| Lead | -0.05 | -0.05 | -0.05 |
| Manganese | -0.01 | 0.04 | -0.01 (4) |
| Mercury | -0.001 | -0.001 | -0.001 |
| Nickel | -0.04 | -0.04 | -0.04 |
| Selenium | -0.01 | -0.01 | -0.01 |
| Zinc | -0.01 | 0.03 | 5.0 |
| Molybdenum | -0.05 | -0.05 | -0.05 |
| Vanadium | -0.05 | -0.05 | -0.05 |
| Uranium | 0.002 | 0.17 | 5.0 |
| Radium-226 (pCi/l) | 94.5 | 97.9 | 104 |
NOTES
(1) The majority of the restoration requirements
are baseline plus
ten percent.
(2) "-" means not detected at level indicated.
(3) The restoration requirement for total carbonate
(carbonate plus
bicarbonate is
500 mg/l.
(4) The 0.04 mg/ I manganese value was not considered
a significant
factor in the overall restoration results as 4 of the
5 restoration sampling wells had final restoration values
of -0.01 mg/l for manganese
Groundwater restoration values acceptable to both the NRC and the DEQ were
met in a little over one month of restoration after circulating about six pore
volumes of R.O. treated water through the aquifer. A pore volume is simply an
estimate of the quantity of groundwater contained within a specific volume of
formation material. A total of nine pore volumes during a two month time period
were eventually circulated through the aquifer to collect additional data on
the slope of the restoration curves, and to obtain cost-benefit information.
Table I presents the baseline and restoration water quality data at the Bison
Basin R&D project.>
The two main regulatory agencies concerned with solution mining in Wyoming,
the NRC and DEQ, both found the results of the OPI-Western Joint Venture aquifer
restoration test acceptable which led to their respective approvals of a commercial
scale license for the Bison Basin project. The DEQ expressed their approval
of the restoration results in correspondence dated April 9, 1980 and May 5,
1980. The NRC expressed their approval of the restoration results in the Final
Environmental Statement (FES) on the commercial scale license application (NUREG-0687).
B. Reno Creek Project
The Reno Creek R&D in-situ leach project is a joint venture
between Rocky Mountain Energy Company (RME), Halliburton Company, and Mono Power,
a subsidiary of Southern California Edison Company. RME operates the project
which is located in southern Campbell County, approximately nine miles southwest
of Wright, Wyo. Uranium in this portion of the Powder River Basin is found within
the Wasatch Formation of Tertiary Age, as a typical roll front deposit.
Testing to evaluate the amenability of the ore deposit to solution mining with
a sodium carbonate/bicarbonate lixiviant began in October of 1980. The wellfield
consisted of two recovery wells ringed by four injection wells and an outer
ring of monitor wells. This well configuration is known as a modified "five-spot
pattern," illustrated in Figure 2.
Leaching operations were conducted over a 10-week period during which the feasibility
of recovering uranium using a sodium carbonate/bicarbonate lixiviant was confirmed.
Groundwater restoration began in December 1980 by pumping production fluid from
the wellfield through the surface plant facilities where an ion exchange (IX)
process was used to remove undesirable constituents. This process continued
for a one-month period and was followed by a groundwater sweep which also continued
for about one month.
At the close of the restoration program, all groundwater constituents, except
uranium, were restored to levels below or within baseline ranges. Uranium was
reduced to less than five parts per million which is the standard for drinking
water in Wyoming. This was accomplished through the circulation of about seven
pore volumes of groundwater through the aquifer. Total groundwater consumption
during restoration was equivalent to 5 pore volumes or 1.3 million gallons.
A representative comparison of premining and restored groundwater quality is
shown on Table 2.
Groundwater restoration and stabilization monitoring data were thoroughly evaluated
by the Land and Water Quality Divisions of the DEQ and by the NRC. Both agencies
concluded that the goal of restoring groundwater to premining baseline conditions
was achieved for all parameters except uranium which met WDEQ's water use class
standards. Further, the NRC and DEQ acknowledged that restoration results would
be suitable to support commercial-scale operations at Reno Creek. See copies
of DEQ and NRC correspondence approving the restoration results pages 18 and
19.
C. Leuenberger Project
The Leuenberger site is located approximately seven miles northeast of Glenrock
in the southern portion of the Powder River Basin. The R & D project was
originally a joint venture between NEDCO and UNC Teton, operator, designed to
evaluate the feasibility of solution mining within the Fort Union Formation
of Paleocene Age.
UNC Teton began test operations in April 1979 also using a sodium bicarbonate/carbonate
lixiviant. Uranium mineralization within this portion of the Fort Union Formation
frequently occurs as "stacked" or layered zones in different sand units so two
separate test patterns were constructed at different depths. Both wellfield
configurations were typical five-spot patterns consisting of four injection
wells surrounding a central recovery well (see Figure 2).
The first of the patterns to undergo active groundwater restoration was the
N sand which is the shallower sand unit. The test pattern was successfully restored
using a groundwater sweep method initiated June 1980 and completed in November
1980. Following a 14-month groundwater stability monitoring period, DEQ agreed
that the aquifer restoration had been effective and met license requirements.
Although restoration was successful, groundwater consumption was high due to
the sweep method.
Leaching operations within the lower ore zone, or M sand, were terminated in
February 1981 after confirming the viability of uranium recovery using the sodium
bicarbonate/carbonate lixiviant. The restoration program was designed to recapture
all groundwater affected by leaching constituents while minimizing the consumptive
use of groundwater. This was accomplished through the use of electrodialysis
(ED) treatment which is basically a water purification process. The ED concentrates
undesirable groundwater constituents into an effluent or brine for disposal
and produces "clean" water which can be reinjected into the wellfield.
By the end of the restoration program, approximately half (46 percent) of the
affected groundwater recovered from the pattern was sent to the ED unit for
treatment. Of this amount, approximately 8 percent was disposed of in an evaporation
pond. The ED product, or "clean" water was then mixed with untreated groundwater
from the pattern and reinjected to improve overall groundwater quality. The
total restoration process resulted in the consumption of 1.7 million gallons
of groundwater which represents a 90 percent improvement in water conservation
compared to the groundwater sweep method.
Restoration was terminated in December 1981 when water quality in all pattern
wells was at or below restoration goals contained in the R & D permit. Comparison
of baseline and post restoration water quality indicated that all parameters
except radium were restored to specified levels or well within baseline water
quality ranges. Radium levels were reduced to an average of 350 pCi/l compared
to a baseline average of 185 pCi/I. Wyoming DEQ standards for Class I (Domestic),
Class II (Agricultural), and Class III (Livestock) groundwaters are 5 pCi/ 1.
Therefore, post restoration radium levels did not impair groundwater use suitability.
The Final Environmental Statement (FES) prepared by the NRC for the commercial-scale license application concluded that " . . . the applicant has demonstrated that restoration of the ore zone aquifers to their original potential use condition is achievable."
Reno Creek
Pattern 2 Production Wells
Restoration Data
| Parameter (1) | Baseline Range | Well P-10
4/1/82 NML ------- CDM |
Well P-11
4/1/82 NML ------ CDM |
| Field | |||
| pH | 8.2 - 8.9 | 7.6 ------ 8.1 | 7.7 ------ 8.0 |
| Conductivity | 1890 - 2234 | 2000 ------ 2500 | 1990 ------2400 |
| Major Constituents | |||
| Bicarbonate (HCO3) | 89 - 1780 | 187 ------ 160 | 159 ------ 130 |
| Carbonate (CO3) | 0 - 14 | 0 ------ 0 | 0 ------ 0 |
| Alkalinity (as CaCO eq) | 73 - 146 | 153 ------130 | 130 ------110 |
| Calcium | 108 - 153 | 118 ------ 110 | 92 ------ 105 |
| Chloride | 7.0 - 18.8 | 18 ------ 11 | 16 ------ 12 |
| Magnesium | 19 - 33 | 17 ------ 25 | 16 ------ 22 |
| Potassium | 5.8 - 9.5 | 7.5 ------ 8.1 | 6.8 ------ 7.3 |
| Sodium | 287 - 360 | 295 ------ 350 | 282 ------ 330 |
| Sulfate | 818 - 1002 | 783 ------ 960 | 644 ------ 910 |
| TDS | 1340 - 1580 | 1330 ------ 1510 | 1160 ------ 1410 |
| Anion/Cation Balance | - | 101 ------ 99 | 105 ------ 101 |
| Minor Constituents | |||
| Ammonia (as N) | <0.2 | <0.2 | <0.2 |
| Nitrate (as N) | <0.05 | <0.05 | <0.05 |
| Nitrate (as N) | <0.05 | <0.05 | <0.05 |
| Aluminum | <0.2 | <0.5 | <0.5 |
| Arsenic | 0.001 - 0.016 | 0.006 | 0.007 |
| Barium | 0.08 - 0.40 | <0.2 | <0.2 |
| Boron | <0.1 | <0.1 | <0.1 |
| Cadmium | 0.01 - 0.02 | 0.012 | 0.009 |
| Chromium | 0.02 - 0.11 | <0.005 | <0.005 |
| Copper | 0.01 - 0.02 | <0.005 | <0.005 |
| Fluoride | 0.09 - 0.15 | 0.1 | <0.1 |
| Iron | 0.03 - 0.61 | 0.08 ------ 0.13 | 0.03 ------ 0.08 |
| Lead | 0.03 - 0.11 | <0.005 | <0.005 |
| Manganese | 0.01 - 0.14 | 0.068 | 0.071 |
| Mercury | <0.0001 | 0.001 | 0.0001 |
| Molybdenum | 0.01 - 0.11 | 0.008 | 0.011 |
| Nickel | 0.01 - 1.10 | 0.02 | <0.02 |
| Selenium | 0.009 - 0.017 | <0.005 | <0.005 |
| Vanadium | 0.05 - 0.34 | 0.39 | 0.43 |
| Zinc | 0.01 - 0.09 | <0.005 | <0.005 |
| Radiochemistry | |||
| Uranium (1) | 0.012 - 0.287 | 3.51 ------ 3.5 | 2.11 ------ 2.3 |
| Radium-226 | 106 - 768 | 320 | 250 |
| Thorium-230 | 0 - 1.9 | 6.1 | 31 |
All values expressed as mg/I except pH (standard units), conductivity
(umhos/cm), radium and thorium (pCi/1).
Baseline range is for all pattern production zone wells
following outlier
removal.
NML values are U308; CDM values are U nat.
Conclusion
In-situ leaching of uranium is a mining method undergoing rapid technological
development. Experience to date confirms that this method can compete favorably
with traditional open pit or underground mine operations from an economical
standpoint. An advantage of solution mining is that surface facilities and disturbances
are significantly less extensive than those associated with open pit or other
surface mining methods. Consequently, protection of groundwater resources is
of greatest environmental concern, particularly the restoration of affected
groundwater to premining conditions. At least three different operators in Wyoming
have demonstrated, in different geographical and geological settings, that groundwater
restoration to the original use suitability can be achieved.
Domestic marketplace requirements for uranium are currently quite depressed
as imported uranium is readily available and utilities are deferring construction
on existing and proposed power plants. When market demand increases, however,
the domestic industry is expected to rely heavily on in-situ mining as an economical
means of production. As documented in this article, the mining industry has
shown that in-situ mining can be done in an environmentally acceptable manner
which protects land and water resources for future use.
Final Environmental Statement
related to the operation of
Bison Basin Project
Docket No. 40-8745
Ogle Petroleum, Inc.
U.S. Nuclear Regulatory
Commission
Office of Nuclear Material Safety and Safeguards
April 1981
(This is one page of the above titled document.)
Restoration baseline for each parameter shown in Table 3.22 shall be the highest value
obtained from three rounds of
samples (four rounds, at NRC option, if significant variation has occurred) collected from all of
the restoration
baseline monitoring wells in each well-field unit, except that baseline for radium-226 shall be
established on a
well-by-well basis following the same sampling procedure. In comparing restoration determination
values with
baseline values, the average of each parameter for each round of samples from the restoration
monitoring wells must
be equal to or less than the baseline value.
In the event that significant variation in water quality is indicated during baseline sampling or
during restoration
determination sampling, the NRC reserves the option to require well-by-well restoration
determination.
4.3.2 Applicant's restoration test
Starting August 5, 1979, approximately one nominal pore volume was pumped from the pilot
well field to the
evaporation pond. This operation, completed on August 9, 1979, represented the lixiviant that
would be transferred to
a new well field during commercial operation. From August 10 through September 14, 1979,
fluids from the
recovery wells were routed to a reverse osmosis (RO) unit. The clean water from the RO unit was
reinjected into the
pilot well field, and the concentrated brine from the RO unit was discharged to the evaporation
pond, as would be the
case for commercial-scale wellfield restoration.
The results for the major ionic constituents from production well P-22 are shown in Fig. 4.2.
The restoration test
demonstrated that staff objectives for restoration could be realized. Bicarbonate and chloride
exceed baseline as shown
in Fig. 4.2, because neither is at levels unacceptable for any water use. (For public drinking water,
the chloride
maximum is 250 mg/liter, and no standard exists or is needed for bicarbonate.)
Conductivity, a reasonable measure for total ionic content, was restored to baseline after a
nominal five pore volumes
of RO treatment.
None of the minor constituents or trace elements exceeded drinking water standards after
restoration.
Monitoring through March 18, 1980, showed either no increase or an insignificant increase
for the constituents in
monitored wells (Fig. 4.1). Radium-226 exceeded applicable standards both before and during
mining.
The applicant calculated the nominal pore volumes of 437 in' (115,000 gal), using only 0.6 to 0.76 in (2 to 2.5 ft) for lixiviant penetration from the well bore external to the well-field dimensions. From a cursory material balance for sulfate, chloride, and sodium ions over the restoration phase, the staff estimates that at least twice this pore volume was affected by the lixiviant during mining. The staff conclusion is that fewer treated pore volumes will be needed for restoration than appears necessary from Fig. 4.2 because the percentage volume affected external to the injection well perimeters decreases radically with an increase in well-field area. The applicant was able to reinject only 62% of the RO unit input. An estimated improvement to 90% reinjection would further reduce the treatment pore volumes required.
4.3.3 Staff conclusions
In the opinion of the staff, the applicant has demonstrated that restoration of the aquifer to its
original potential use
condition is achievable. The staff believes that the applicant can improve RO unit performance to
achieve 90%
reinjection; this improvement would reduce the water consumption for restoration as well as the
evaporation pond
volume and surface requirements. The staff considers it necessary for the applicant to mine
sequentially, commencing
restoration of each mined-out area as mining begins on the next mine area or as soon as feasible.
Sequential mining
will be a condition of the license.
The staff's conclusion is that this proposed operation is state-of-the-art and, with monitoring
and proposed mitigating
measures, will pose no major risk to the environment.
MEMORANDUM
TO FILE: License to Explore No.
38
FROM: Ed Francis, District III Engineer
DATE: April 9, 1980 (Finalized May 5, 1980)
SUBJECT: Restoration Report Response. Refer to Ogle's Final
Restoration Report of May 2, 1980.
COMMENT:*
Radiological results from Land Quality Division sampling are not available at this date. This report will be finalized upon receipt of radiologic data.
See Hereford memo of April 11, which comes to similar conclusions through mathematical and
graphic analyses.
SUMMARY
Upon Ogle's request for a Land Quality Division decision concerning satisfaction of Ogle's
groundwater restoration,
District III undertook a three- fold analysis of the restoration situation:
1. Statistical analysis of restoration sampling results versus baseline results.
a. Evaluation of specific values for individual species.
b. Analysis of mean value comparisons.
2. Value by value comparison between final round and baseline means.
3. Analysis of environmental implications of those species determined to be more than 10% out of
range of baseline
conditions.
The conclusions from the above studies are that Ogle Petroleum, Inc., has demonstrated
capability to restore
groundwater to an acceptable quality of original use following sodium bicarbonate leaching.
Technology used was
reverse osmosis and reintroduction of treated water into the aquifer. Declaration of capability has
no relevance to bond
release (which is not sought) because this declaration has nothing to do with surface reclamation,
which is not
intended at this time.
*Radiological data was obtained by phone on 5-5-80. LQD results served to confirm (even enhance) the Ogle data. As a result of this confirmation, this report stands as the final report documenting restoration capability.

