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GENERAL47047
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Last modified
8/24/2016 8:21:44 PM
Creation date
11/23/2007 3:05:36 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1984065
IBM Index Class Name
General Documents
Doc Date
1/1/1985
Doc Name
PROPOSED DECISION and FINDINGS OF COMPLIANCE
Permit Index Doc Type
FINDINGS
Media Type
D
Archive
No
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- 18 - <br />There is the potential for some seepage from the embankment reaching the <br />alluvial valley floor just downstream from the embankment by short-circuiting <br />around the sediment pond. <br />Table 1 gives a comparison of mean water quality of ground water at the mine <br />site. OW-9 is located within the drainage proposed for location of the refuse <br />embankment. The existing water quality is very poor, with a mean conductivity <br />of 5105 umhos/cm and a sulfate level of 3084 mg/1. This is characteristic of <br />water draining from the Mancos Shale. Due to the existing poor water quality, <br />it is not expected that seepage from the refuse embankment will decrease water <br />quality in the downstream colluvial material beyond that present. <br />OW-11 is an existing water well present in the alluvial material downstream of <br />the proposed refuse site. This welt has an extremely high sodium absorption <br />ratio (SAR) of 23.1. The water quality of this well varies greatly from the <br />expected quality of alluvial water for the area and suggests that <br />contamination is occuring possibly due to casing or completion technique. The <br />applicant has committed to drilling another well for alluvial monitoring at <br />the mine site. This well will be drilled in adequate time to collect a year <br />of baseline before construction begins at the refuse disposal site. This well <br />will be placed to detect impact, if any, to"the alluvium from seepage at the <br />disposal site. <br />The alluvium present in the vicinity of the Coal Ridge No. 1 Mine and adjacent <br />to the Colorado River is recharged by the Colorado River surface water and by <br />surface runoff from the upland area. The subcrop of the Wheeler seam is <br />located approximately 55 feet above the alluvium and dips, steeply away from <br />the alluvial body. Undermining of the alluvial body will not occur during the <br />life-of-mine. Therefore, dewatering of the Wheeler seam due to mining is not <br />expected to impact the alluvium or surface water system of the Colorado <br />River, <br />Hydraulic mining requires large quantities of water for operations such as <br />cutting of the coal and in the slurry line transporting fine refuse to the <br />waste site. The operation has facilities designed to process and recirculate <br />the majority of water required for the operation. The water circulation is <br />designed as a closed-system, with the major water loss occurring through <br />evaporation, adhesion to the coal and refuse, and by seepage underground <br />during mining, The application projects that water loss through these <br />processes will require a makeup of approximately 600 acre feet of water <br />annually to the system. The Coal Ridge No. 1 Mine has acquired water rights <br />more than sufficient to augment their annual projected water loss. <br />
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