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REP30848
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REP30848
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Entry Properties
Last modified
8/25/2016 12:01:21 AM
Creation date
11/27/2007 5:45:00 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981044
IBM Index Class Name
Report
Doc Date
12/11/2001
Doc Name
2000 AHR Text
Permit Index Doc Type
hydrology Report 2000
Media Type
D
Archive
No
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RAG, Empire Corporation 2000 AHR <br />.• HYDROLOGIC IMPACTS <br />No significant unpredicted adverse impacts were detected during 2000. The continued <br />drawdown in the Middle Sandstone unit is determined to be the most significant impact related <br />to mining operations associated with Mines 5 and 6. Drawdov`m effects in the Twentymile <br />Sandstone unit were evident in the 2000 data as well. The Probable Hydrologic Consequences <br />section of the Permit predicted drawdown in the Middle Sandstone unit associated with mining <br />the F and E coal seams at Mines 5 and 6, although the extent and magnitude of the drawdown <br />were not quantified. A worst-case evaluation was, however, prepared for the overlying <br />Twentymile Sandstone. The drawdowrl in Middle Sandstone Well TR-4 attributable to the <br />longwall mining in the E and F seams at a distance of approximately one mile has historically <br />been determined to be between 50 and 60 fee[. This is comparable to the 60-foot drawdowns <br />projected in the PHC for the overlying Twentymile Sandstone at a distance of one mile from the <br />location of mine subsidence. The impacts observed in the Middle Sandstone are comparable to <br />the worst case projectiuus developed for the Twengmiile Sandstone. The increased TDS in the <br />7 North Angle Discharge seen in 1991 has decreased to approximately 1150 mg/L. The <br />increase in TDS was due to the accumulation of water in the North Angle Sump location that <br />was able to equilibrate with oxidized rock within old workings and rubbleized rock within <br />subsidence panels. The maximum concentrations of 1474 mg/I probably represent this <br />equilibrium concentration. Flow from the #] Strip Pit spring discharge was within the range <br />observed during ] 982 through 1986. Flow from this spring is influenced by both snowmelt and <br />ditch seepage associated with the 7 North Angle discharge. Flows from the 5 mine workings <br />were somewhat lower than previous years. <br />• <br />I:\Environmenlal\E~1PIRE\AFIR\2000\Tezl\Empve2000AHR.doc Page 8 <br />
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