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REP49531
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REP49531
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Entry Properties
Last modified
8/25/2016 12:53:29 AM
Creation date
11/27/2007 12:36:34 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981010
IBM Index Class Name
Report
Doc Date
7/18/2005
Doc Name
2004 AHR Review Memo
From
Tom Kaldenbach
To
Janet Binns
Annual Report Year
2004
Permit Index Doc Type
Hydrology Report
Media Type
D
Archive
No
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<br /> <br />Requirement <br />Require-ment <br /> <br />citation Require- <br />ment <br />complied <br />with ? <br />es / no <br /> <br />Comment i <br /> Potential aquifers. The post-mining uses of ground water in <br /> the permit area will be irrigation and livestock uses. Only <br /> the massive sandstone aquifers within the upper Williams <br /> Fork Formation at Trapper could reasonably be expected to <br /> yield enough high quality water to serve as a local supply <br /> source. These aquifers are the Twenty Mile sandstone, 2"a <br /> White sandstone, and 3`a White sandstone. Coal aquifers in <br /> the area possess neither the deliverability nor water quality to <br /> be considered for reliable water supplies. <br /> Twentymile Sandstone. The Twentymile Sandstone is the <br /> only regionally extensive aquifer in the vicinity of the <br /> Trapper Mine. tt is several hundred feet deeper than the <br /> deepest mining at Trapper and has shown no effect from <br /> Trapper's mining based on monitoring data from well GF-1 <br /> (and previously GD-1(2)). <br /> 2"a White Sandstone (well P-5) and 3'a White Sandstones <br /> (well P-8). The 2"a and 3`a White Sandstones overlie the <br />U. Prevention of stratigraphic sequence being mined at Trapper. The 3'a <br />impacts to White has been cut by Trapper's pits; the 2"a White crops out <br />ground water CDMG down-slope from the pits. TDS concentrations in both of the <br />that adversely regulations White Sandstones have increased over the past several years <br />impact the 4.05.1(2) and yes in the two Trapper wells (P-5 and P-8) that monitor these <br />postmining land 4.05.11 aquifers in East Pyeatt Gulch. <br />use within the <br />permit area Suitability for postmining use of water from wells P-5 <br /> and P-8. Prior to mining, high TDS levels caused <br /> electroconductivity values of water in both wells to exceed <br /> DMG's guidelines for irrigation water of 1.0 mmhos/cm. <br /> Water from both wells, though, remains suitable for the <br /> lower level use of livestock and wildlife watering based on <br /> comparison with water quality suitability standards for <br /> domestic livestock issued by the State of Wyoming <br /> Department of Environmental Quality. (The Wyoming <br /> standards are used for comparison because Colorado has not <br /> issued suitability standards specifically for livestock or <br /> wildlife.) Trapper believes the TDS (and <br /> electroconductivity) will eventually subside, possibly <br /> hundreds of years after mining and reclamation, as discussed <br /> under Probable Hydrologic Consequences, Section 4.8.3 of <br /> the mining and reclamation permit. The suitability of <br /> Trapper's ground water for livestock and wildlife is expected <br /> to continue into the future based on long-term trends in <br /> Trapper's water quality data. <br />Page 6 <br />
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