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REP26901
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REP26901
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Entry Properties
Last modified
8/24/2016 11:57:58 PM
Creation date
11/27/2007 4:36:42 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980005
IBM Index Class Name
Report
Doc Date
4/8/1986
Doc Name
SENECA II 1985 ANNUAL HYDROLOGIC REPORT FILE C-80-005
From
MLRD
To
STEVE RENNER
Permit Index Doc Type
HYDROLOGY REPORT
Media Type
D
Archive
No
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Richard D. Lamm <br />Governor <br />DATE <br />TO <br />r <br /> <br />DEPARTMENT OF NATURAL RESOURCES <br />Dared H. Getcnes, Executive Director <br />MINED LAND RECLAMATION DI\ <br />DAVIDC. SHELTON, Director <br />April 1, 1986 <br />Seneca II File <br />FROM: Steve Renner <br />RE: 1985 ANNUAL HYDROLOGY REPORT: GROUND WATER REVIEW <br />Enclosed are my comments after reviewing the ground water section (including <br />spoil springs) of the 1985 AHR. <br />In general, water levels at most wells decreased during the 1985 reporting <br />period. This is due to a general decrease in precipitation at the mine site. <br />Note, however, that even though precipitation decreased, it was still an above <br />average water year. Runoff in 1985 was about one month earlier than usual, <br />the peak being somewhat less then 1984. <br />Most wells exhibit a decrease in head due to the lower amount of available <br />water. Also, recorded was the seasonal variability of water levels, <br />especially in the near surface completions. <br />Water quality has not significantly changed in 1985, however, some wells do <br />exhibit elevated TDS levels. This is probably due to a high concentration of <br />"salts" in the surrounding strata, which is less diluted than in previously <br />high water years. <br />The well of most interest, GW-546, is completed in the alluvium of the unnamed <br />ephemeral tributary (aka Cow Camp Creek) to Fish Creek, below the 004 pond. <br />This well exhibited the normal seasonal fluctuations expected in an alluvial <br />completion. The water in this well is a magnesium/sulfate type, and exhibits <br />an average TDS concentration of 2444 mg/1 (versus 2068 mg/1 previous to <br />mining, and 1529 mg/1 at the 004 pond discharge). This is apparently due to <br />natural conditions of the alluvial material rather than being a direct result <br />of mining activities (004 pond should intercept surface as well as underflow <br />from the backfilled Wadge Pit). <br />The Lennox-Wadge interburden completion GW-S44P2, as well as Lennox overburden <br />completion GW-S44P1, and Wadge Coal completion GW-S44 exhibit decreasing head <br />as mining progresses toward these wells. <br />In the Wolf Creek mining area, the following wells have been losing head as <br />mining progresses: GW-S360, (Wolf Creek overburden/Wadge underburden <br />completion. Wells GW-S8 and GW-S8P1, also completed as GW-S360, have lost <br />head, it is postulated that this may be due to Wadge mining operations, <br />continued careful monitoring at these sites, as well as more thought, is <br />warranted at this time. . <br />423 Centennial Building, 1313 Sherman Street Denver, Colorado 80203 Tel. (303) 866-3567 <br />
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