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2010-08-02_REVISION - M1977300 (36)
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2010-08-02_REVISION - M1977300 (36)
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Last modified
6/15/2021 3:06:16 PM
Creation date
8/4/2010 8:44:58 AM
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Template:
DRMS Permit Index
Permit No
M1977300
IBM Index Class Name
REVISION
Doc Date
8/2/2010
Doc Name
New Amend.- EPP- Mitigation Options and Construction Schedule.
From
Cotter Corp.
To
DRMS
Type & Sequence
AM2
Media Type
D
Archive
No
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Environmental Protection Plan, Schwartzwalder Mine 15-3 <br />• (ii) Thickness and Extent of Alluvium <br />Alluvium along Ralston Creek ranges in thickness from 5 feet to over 30 feet in the vicinity of the mine. In <br />general, the alluvium is confined to the valley floor along Ralston Creek and pinches out near the property <br />boundary, where a natural constriction in the valley occurs. This "choke point" occurs where the valley <br />narrows and its walls rise steeply from the creek bed. Bedrock is exposed along the width of the valley <br />floor and groundwater previously flowing in the alluvium is forced to the surface where it enters Ralston <br />Creek. Alluvium thickens again downstream from the choke point. Monitoring Well MW8 is installed in <br />the alluvium on the downstream side of the choke point and has always been dry. Alluvial monitoring well <br />MW4 was also frequently dry as a result of its distal location on the southwestern fringe of the alluvial <br />system3o <br />(iii)Potential Pathways for Alluvial Groundwater <br />The alluvial aquifer near the mine is of limited areal extent and is not directly connected with alluvium <br />below the choke point, except via Ralston Creek. At present, the only potential contaminant pathway to <br />receptors from the alluvial aquifer is limited to releases into surface waters of Ralston Creek. For this <br />reason, mitigation strategies logically focus on removing source term material in the alluvial fill, or on <br />treating alluvial groundwater before it reaches Ralston Creek and/or isolating the creek from the alluvial <br />fill, thus breaking this exposure pathway. <br />No drinking water wells are installed within impacted aquifers at the site, so at present, there is no direct <br />pathway for human health risk from drinking alluvial groundwater. If targeted source term removal is not <br />successful at meeting groundwater standards in the affected portions of alluvial fill near the mine, <br />institutional controls may be required to ensure that water wells are not installed in those areas. <br />Alternatively, additional remedial measures may be considered to meet surface water quality standards in <br />• Ralston Creek. <br />A detailed human health risk assessment can be conducted to determine whether any other potential <br />pathways for human exposure to impacted alluvial groundwater exist. If no potential for exposure exists, <br />alternative concentration limits (ACLs) that are not based on human health drinking water standards may <br />apply to the alluvial aquifer. The Operator's goal and commitment is to ensure that all potential exposure <br />pathways from impacted alluvial groundwater are mitigated or managed to the extent that water quality <br />standards in Ralston Creek are met and that public health and the environment are fully and permanently <br />protected under any potential future uses of the site. <br />(iv) Effect of Alluvial Water Quality on Ralston Creek <br />Ralston Creek above the mine site generally has uranium concentrations below the 0.03 mg/L stream water <br />standard, but concentrations increase as it flows past the mine and interacts with groundwater in the <br />alluvium. The waste rock dumps have had no discernable effect on water quality in Ralston Creek. <br />Uranium concentrations at surface water stations above (SW-AWD) and below (SW-A001) the waste rock <br />dumps are consistently low (Figure 14-1). However, uranium concentrations in Ralston Creek increase as <br />the creek flows past the mine site downstream from SW-A001, then decrease past the property boundary <br />(Figure 11-6) as sorption and precipitation processes remove uranium from solution. <br />Uranium concentrations in Ralston Creek spiked after the alluvial sumps were turned off 2002, and spiked <br />a second time after Sump 1 recirculation was discontinued in 2008. In 2002-2003, reactive surfaces on <br />alluvium and fill had been exposed to subaerial weathering for over a decade while the sumps were in <br />operation. The "first flush" caused uranium concentrations to spike and then decrease in later sampling <br />events. A similar spike occurred in 2008, several months after the cessation of Sump 1 recirculation. Since <br />the spike in 2008, uranium concentrations have fluctuated seasonally, meeting water quality standards <br />• so Monitoring well MW-4 was damaged and removed during site reclamation activities in 2005. <br />4109C.100731 Whetstone Associates
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