HomeMy WebLinkAboutDRC-2012-002050 - 0901a068803141f5. f
State of Utah
GARY R. HERBERT
Governor
GREG BELL
Lieutenant Governor
Department of
Environmental Quality
Amanda Smith
Executive Director
DIVISION OF RADIATION CONTROL
Rusty Lundberg
Director
DRC-/e|12-002050
September 20,2012
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cr a Jo Ann Tischler, Director, Compliance and Permittmg a
Energy Fuels Resources (USA) Inc. ^
225 Umon Boulevard, Suite 600
Lakewood,CO 80228 —
U.S. Postal Service ri
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City, State, 2
Jo Ann Tischler
Energy Fuels Resources (USA) Inc
225 Union Boulevard, Suite 600
Lakewood, CO 80228
PS Form 3100, August 2006 See Reverse for Instructions
Subject: Energy Fuels Resources (USA) Inc. ''''Revised Report on the Hydrogeology of
the Perched Groundwater Zone in the Area Southwest of the Tailings Cells,
White Mesa Uranium Mill Site'': DRC Review Summary, Request for
Information and Conclusions
Dear Ms. Tischler:
The Utah Division of Radiation Control ("DRC") has reviewed the Energy Fuels Resources
(USA) Inc. ("EFR") July 13,2012 Response to May 30, 2012 NOED and RFI Southwest
Hydrogeology Investigation Report ("EFR Response Letter") and, the August 3,2012 EFR
Cover Letter and attached Document titled "Revised Report on the Hydrogeology of the
Perched Groundwater Zone in the Area Southwest of the Tailings Cells, White Mesa Uranium
Mill Site" ("Revised Report") prepared by Hydro Geo Chem, Inc ("HOC").
Summarv
The Report was revised from the January 12, 2012 Report on the Hydrogeology of the Perched
Groundwater Zone in the Area Southwest of the Tailings Cells ("Onginal Report") based on
telephone conferences between EFR and DRC staff on May 23,2012 and July 2,2012, as well
as a DRC Notice of Enforcement Discretion and Request for Information Letter dated May 30,
2012 ("DRC Letter")
Per these documents/discussions EFR responded to the identified issues (and modified the
Report as applicable) as follows:'
• In response to the May 30, 2012 DRC Letter regarding EFR abandonment of study
bonngs with a saturated thickness greater than five feet [violation of the White Mesa
195 North 1950 West • Salt Lake City, UT
Maihng Address P O Box 144850 • Salt Lake City, UT 84114-4850
Telephone (801) 536-4250 • Fax (801) 533-4097 'TDD (801) 536-4414
www deq Utah gov
Printed on 100% recycled paper
Jo Ann Tischler
Page 2
Uranium Mill Ground Water Discharge Permit, UGW370004 (Permit) Part IH 6 a 2],
EFR disagrees with the basis of the violation, specifically per the EFR Response Letter
"At the outset, and as discussed with DRC staff, it should be noted that Denison
disagrees that the abandonment of three borings, which had a saturated thickness of 5-
feet or more, constitutes a violation of the Permit Part IH6a 2 The Permit does not
specify how many borings are required or where the bonngs were to be located The
Permit merely requires that the charactenzation/definition of the subsurface shall be
based on either dry wells, to delineate dry areas, or wet wells to delineate areas that
are not dry, in an effort to define the dry zones It further states that in order to qualify
as a wet well, the well must have a saturated thickness of at least 5 feet The Permit
does not state that all bonngs drilled need to be retained It merely states that enough
dry and wet bonngs must be drilled in order to define the dry area Denison and its
experts determined that the three borings in question were not required in order to
define the dry area, so they were abandoned."
DRC Response: DRC disagrees that the only intention of the Permit requurement was
to define dry areas Per the Permit Part I H.6. "The purpose of this investigation is to
define, demonstrate, and characterize 1) Hydraulic connection and local groundwater
flow directions between the area near Tailings Cell 4B, and the western margin of
White Mesa, including Westwater, Cottonwood Seeps, and Ruin Spnng, and 2) the full
physical extent of unsaturated area between former well MW'16, MW-33 and the
western margin of White Mesa, as defined above " Part I H.6.a of the Permit requnes
that bonngs and/or momtonng wells are installed to achieve both of these goals, not
just the delineation of area unsaturated ("dry") zones.
In preparation of the groundwater level and groundwater contour maps included with
the Report, water level data at wells, with at least 5 feet of saturated thickness, are the
cntical tool to develop the contours and groundwater flow directions. In particular, the
decision to abandon well DR-02 and to discount the water levels at that well and not
perform hydraulic tests biased the data west of the tailmgs cells by eliminating
important information relevant to the study Per the DRC Letter request for information
item one "the Report data shows relatively significant saturated thickness, >10 ft,
measured at piezometer DR-05 and boring DR-02 (pnor to abandonment), but does not
provide field data to determine how far west the zone of saturation extends or to
provide hydraulic evaluation of that zone." Information relevant to abandoned well
DR-02 was needed to help charactenze the flow directions m that area, additionally; the
information for all **wet wells" was needed m order to define and support the Report
ground water elevation contours and anticipated flow paths. It is the DRC contention
tiiat the abandonment of the 'Vet wells" was m violation of the Permit Part IH 6.a.2
which requires EFR to completely enclose and define the shallow aquifer and to
complete piezometers that encounter a saturated thickness of five feet or more as
specified, m order to achieve the purposes of the study
Jo Ann Tischler
Page 3
• In response to the DRC Letter request for information item number one, EFR has
included a potential flow path fi"om the tailings cells to Cottonwood Seep, and included
travel tune calculations This action is required based on the lack of field data and
study to predict flow directions west of the tailings cells in the area piezometer DR-05
and abandoned bonng DR-02. The HGC conclusion in the Onginal Report that a flow
divide is present m this area is not supported by the current field data. EFR has
mcluded figures m the Revised Report to depict a potential flow path fi-om the tailmgs
cells to Cottonwood Seep. DRC and EFR agreed that Cottonwood Seep may be
recharged m part by the Dakota/Burro Canyon aquifer (Perched Aquifer)
• In response to the DRC Letter request for information item number two, EFR has
committed to repeat slug tests at piezometer DR-08 and recalculate average hydraulic
properties (K and Ss) as discussed m the request for information section of this letter
below.
• In response to the DRC Letter request for information item number three, EFR has
removed language and figures in the Revised Report which related to a hydrauhc
corinection between Westwater Creek and Cottonwood Seep. The statements that such
a connection is "likely** are not supported by the investigation data & were not withm
the scope of the mvestigation
Request for Information
Per the DRC Letter, the request for mformation item number two specifically requested*
"The Report, Table 3, lists slug test results (K and Ss) for the investigation completed
piezometers DRC notes that the slug test results for piezometer DR-08 differ by an order of
magnitude between the automatically logged data and the hand collected data DRC
additionally notes that Table 3 lists, "Not Interpretable " as the K value at DR-08 by the
Bouwer-Rice Method using the Hand Collected data Slug tests at piezometer DR-08 need to
be repeated in order to validate the reported hydraulic conductivity values, and to substantiate
the inclusion of these results in the hydraulic conductivity averages."
In the EFR Response Letter regarding this request EFR "agrees to repeat slug tests at
piezometer DR-08 as requested."
DRC noted that no timelme was included m the EFR Response Letter regardmg when EFR will
conduct/complete the pump test and recalculate the average hydraulic conductivity used m the
Revised Report. Per a telephone conversation between EFR Representative (Jo Ann Tischler)
and DRC Staff (Tom Rushmg) on September 18,2012 (2.15 P M.), EFR will submit the results
of the repeated slug tests, as well as the recalculated hydrauhc parameters and travel time
calculations (if necessary) on or before November 9,2012
DRC appreciates that any calculated travel times in the Revised Report are estimations only
and have been represented as such These calculations mclude a potentially large margin of
Jo Ann Tischler
Page 4
error based on the hydraulic testmg method used (fallmg head slug tests). Per literature review
it IS noted that such aquifer tests cannot account for formation amsotropy, may underestimate
hydraulic conductivity due to the development of a low permeable well skin, and provide a
weighted average for the entire wetted length of the boring/well screen (does not account for
formation heterogeneities).^ The calculations submitted with the Revised Report provide
usefiil information as an estimate of travel times for the anticipated ground water paths in this
context, and comphes with the Permit Parts I H.6.a.2 and IH 6 e.6
Conclusions
Based on review of the Report, DRC agrees with the Report Section 2 4, Part 3 and
Conclusions that "an as yet unidentified connection may exist" between the Burro Canyon
perched zone and Cottonwood Seep. Per discussions between DRC and EFR, the contmued
investigation of preferred ground water flow path lines and potential hydraulic connections
between the Burro Canyon Member and the Brushy Basin Member will not be reqmred at this
time due to the EFR recogmtion that Cottonwood Seep may be recharged m part by the
Dakota/Burro Canyon Aquifer (Perched Zone).
Additionally, DRC recogmzes that Report language and figures (postulated source area) of the
Ongmal Report which inferred that the "the likely source" of water discharged at Cottonwood
Seep is Westwater Creek, via coarser gramed materials in the Brushy Basin Member and
Westwater Canyon Member, has been removed smce such claims are unsubstantiated (see the
DRC May 30, 2012 Letter for additional detail).
DRC appreciates that HGC has better reflected the available ground water head data by
removmg suspect ground water path Imes from the Ongmal Report which were based on an
assumed hydrauhc divide in the area of piezometer DR-05. Per the DRC Letter, the postulated
hydraulic divide on which those path lines were based is not supported by the field data. DRC
acknowledges that additional study to charactenze the saturated zone and flow west of DR-05
and DR-02, in order to substantiate or refiite the claims m the Onginal Report, will not be
required at this time based on the EFR acknowledgement that Cottonwood Seep may be
recharged in part by the Dakota/Burro Canyon Aqmfer (Perched Zone)
Therefore, per DRC mterpretation of the Revised Report, contmued ground water momtonng
and analysis from Westwater Seep, Cottonwood Seep and Rum Spnng is warranted since they
are potential pomts of exposure for discharges from the White Mesa Uramum Mill Tailings
Impoundments.
DRC appreciates the effort by EFR to prepare the Report and Revised Report This
information is valuable regardmg mterpretation of ground water momtonng results from the
White Mesa Mill momtonng network, a better understandmg of local geology/hydrogeology,
as well as identification of long term momtonng needs.
' Binkhorst, Gordon K and Robbins, Gary A, February, 1994, A Review and Assessment of Factors Affecting
Hydraulic Conductivity Values Determined from Slug Tests, EPA/600/R-93/202
Jo Ann Tischler
Pages
If you have any questions regardme th,^ I.H. I
Rusty Lundber^Director ^
RL:TR.tr
""•^ ^es..«a.™yAug„,. 3.20.2 Revse. HOC R M™.