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2010-06-04_PERMIT FILE - C1982056A (10)
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2010-06-04_PERMIT FILE - C1982056A (10)
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Last modified
8/24/2016 4:12:47 PM
Creation date
10/14/2010 10:11:32 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1982056A
IBM Index Class Name
Permit File
Doc Date
6/4/2010
Doc Name
Pages 2.05-123 to 2.05-197.3
Section_Exhibit Name
2.05.5 Postmining Land Uses
Media Type
D
Archive
Yes
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GROUND WATER SYSTEM <br />•A detailed discussion of ground water hydrology is presented under Rule 2.04.7(1). The proposed life -of -mine <br />area for the Foidel Creek Mine is located within the Twentymile Park ground water basin. The Twentymile Park <br />Basin is an enclosed ground water basin. Therefore, any mining related impacts on the ground water hydrologic <br />system should be confined within the basin. <br />Potential Mining Related Impacts on Ground Water Quantity and Quality <br />The mining and related operations have the potential to locally affect the water levels, and the water chemistry of <br />the ground water contained in the Wadge overburden unit, the Twentymile Sandstone aquifer and the Trout Creek <br />Sandstone aquifer. The Wadge overburden unit will be directly affected due to removal of the Wadge Coal Seam, <br />which is at the bottom of the unit. The Twentymile Sandstone and the Trout Creek Sandstone aquifers may be <br />affected if significant hydrologic communication is established with the underground workings. This is not likely <br />to occur except in the vicinity of major fault zones or if greater than predicted subsidence results, due to the <br />existence of thick, intervening bedrock sequences of very low permeability as described in the general description <br />of geology and hydrology (sections 2.04.5, 2.04.6 and 2.04.7). To date, June 1999, no significant hydrologic <br />communications have been encountered with these two aquifers. <br />During the mining operation, the major ground water effects will be on water quantities in the immediate <br />overburden. Ground water inflows from the overburden sequence into the mine workings will cause dewatering of <br />the sequence near the mine and will cause drawdown of potentiometric levels at some distance from the mine. If <br />significant hydrologic communication is established with the Twentymile Sandstone or the Trout Creek Sandstone <br />then drawdown of potentiometric levels in these units will also occur. Discharge of these bedrock aquifers to <br />surface streams may be reduced as a result of these drawdowns. The extent of these effects is examined in more <br />• detail under Rule 2.05.6(3)(b)(iii), Probable Hydrologic Consequences, of this revision application. <br />No water quality effects in these units are anticipated during the mining operation, as flows will be from the units <br />to the workings. Mine inflows will be collected in sump areas within the mine and pumped to the surface where <br />they will be treated and discharged to surface streams. The effects of this operation on surface water flows and <br />quality are discussed under Rule 2.05.6(3)(b)(iii), Surface Water Probable Hydrologic Consequences. After <br />mining operations at the Foidel Creek Mine have been completed and the mine workings are allowed to flood, <br />there is the potential for water quality effects on units that are in communication with the workings. The increased <br />surface area of rock material that has been exposed to weathering is more susceptible to leaching by the ground <br />water in the flooded workings. This may lead to increased solute concentrations and changes in water chemistry <br />characteristics. As pre- mining potentiometric levels and ground water, flows are re- established, discharge of this <br />lower quality water to other units and to surface streams is occurring. The effects of this occurrence are discussed <br />under Rule 2.05.6(3)(b)(iii), Probable Hydrologic Consequences Ground Water System Effects on Ground Water <br />Quality of Aquifers. <br />Leaching of waste rock material in disposal areas upgradient from the underground mining operation, and of caved <br />and fractured material in and above the mined workings is unavoidable and will result in increased TDS levels in <br />affected Wadge Overburden ground water unit. Once leaching has occurred, there is no practical technology <br />currently available to treat the water to decrease TDS concentrations. Decreases in TDS levels will occur after <br />sufficient water has percolated through the newly exposed material; however, this may take several hundred years <br />under existing hydrologic conditions. The only method to minimize the impacts of mine - related leaching on <br />ground water quality is to minimize the amount of water, which can pass through these materials. The effects of <br />this leaching are discussed in Effects on Ground Water Quality of Aquifers and Surface Water Systems Impacts of <br />Mine Discharge below. <br />It should be noted that despite some unavoidable increase in TDS concentrations or change in ion balance, the <br />overall ground water impacts are limited to this relatively unimportant overburden unit. Water supply wells in the <br />PR 99 -05 2.05 -133 APPROVED JUN 2 8 2000 328/00 <br />
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