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constituents in. the alluvial water would see similar increases. None of the increases <br />would be enough to impair the use of alluvial water. <br />Compliance with Colorado Water Quality Control Commission's Regulation No. 41, <br />Basic Standards for Ground Water. Alluvial ground water monitoring at the Eagle <br />Mines has not: detected a negative impact to water quality. The F coal seam, downdip <br />from the bond release area, is the stratigraphic unit most likely to be negatively impacted <br />by mining in the bond release area. No water quality data has been collected for the F- <br />seam in the area downdip from the workings. Baseline TDS in groundwater in the E coal <br />seam at the rriine was 778 mg/1 (permit application Table 111- l Og). TDS of migrating <br />mine water (l~eachate) is expected to be at least 1,000 mg/1, and possibly significantly <br />higher. Assuming the F seam premining water quality was similar to the E seam, the <br />migrating leachate from the F seam could degrade native ground water in its path. This <br />migration path would extend downdip from the downdip edge of the mining workings, at <br />a depth of 800 feet below the ground surface. Seepage from the workings into the <br />bedrock expo:;ed in the workings would occur at a rate on the order of less than 100 feet <br />per year based on a calculation ground water flow velocity using the Darcy equation <br />(Table 1 in the hydrology evaluation memorandum). Dispersion would limit the areal <br />extent of degradation along the migration path. The slow seepage velocity, combined <br />with the dispE:rsion, supports a conclusion that the Basic Standards for Ground Water <br />probably have not been exceeded in the vicinity of the bond release area. <br />Compliance with requirement to minimize ground water hydrologic impacts inside the <br />permit area [CDRMS regulation 4.05.1(2)J. The approved post-mining land use in the <br />permit area i s rangeland/wildlife habitat, pastureland, and cropland. As previously <br />discussed, ground water quality in bedrock and alluvial aquifers has not been adversely <br />impacted by mining and reclamation operations at the Eagle Mines. The approved <br />post-mining land uses have not been impaired by the changes to the ground water <br />hydrologic balance caused by mining operations. Aquifers probably have been partially <br />dewatered inside the bond release area. These changes are the minimum that can be <br />expected from. an underground mining operation. <br />Surface Water Impacts: <br />Compliance with Instream Numeric Standards (Colorado Water Quality Control <br />Commission .Regulation 3.3.0). The Eagle Mines are on Segment 13b of the Lower <br />Yampa/Green River Sub-basin of the Lower Colorado River Basin. CWQCC Regulation <br />3.7.0 lists numeric standards for Segment 13b. The permittee monitors water in the <br />Williams Forl: River at a site that is upstream from Eagle's mining (WF-1), and a site <br />downstream from mining (WF-2). Data from the upstream site indicate the Williams <br />Fork River naturally exceeds the iron numeric standard frequently, and the lead and <br />manganese standards occasionally. The operator also monitors underground mine water <br />quality where it is discharged into the Williams Fork River at NPDES outfalls 003 and <br />024. There have been no exceedances of discharge limitations at either outfall for at least <br />10 years. (They operation has been in temporary cessation since December 3, 1995.) The <br />discharge lirriitations applicable to the outfalls were based on which chemical <br />