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chemistry. Production of acid may occur in very local settings and is probably most prevalent iii <br />the coal which will be mined. Calculations indicate that neutralization of they acid will occur <br />rapidly with mixing of water, or with movement of acidic water into calcite-bearing rocks. Also, <br />the analysis conducted indicates that chemical changes are not likely to occur. _ <br />Effects of mining on the local geomorphologk Impacts from mining on the local <br />geomorphology will be long term, but appear to be of minimal significance. The reestablished <br />reach of the drainage which will be mined will result in a shorter, slightly steeper stream channel. <br />The potential for increased sediment loads in the drainage (once pond 007 is removed) should <br />be offset by the stable banksides and the relatively small change in overall gradient. The <br />increased runoff and consequent erosion potential on disturbed basins in the mining area due to <br />the temporary loss of topsoil stricture should be of minimal significance. Contour ripping, <br />mulching and revegetation have been demonstrated to minimize soil erosion and will be used tc <br />mitigate the increased runoff potential until the topsoil structure is developed. <br />Effects of sediment ponds on channel characteristics and downstream users. Potential <br />impacts of sediment pond 007 on downstream users will involve possible reductions in flow due <br />to impounded water. The water augmentation plan discusses the available ~roater which will be <br />used should impacts be identified. WFC currently has rights to a sufficient quantity of water to <br />supply all users associated with the mining activities, plus an additional quantity of water that can <br />be used to mitigate any impact io downstream users. <br />Effects of sediment pond discharge on surtace water quality, The effects of sediment pond <br />diversions on surface water quality will be negligible because the structure has been designed to <br />minimize imp<rcts to the hydrologic balance. The diversion involves such minor areas of <br />disturbance that chemical and sediment changes in the flows will be unmeasurable. <br />Effects of runoff from reclaimed areas on the quality of streamflow. Due to the relatively <br />small area of disturbance in the New Horizon 2 mining area, any reductions in runoff will have . <br />only a minimal impact on streamflow quantity, as flow in Calamity Draw is dominated by irrigatior <br />return flow. Decreased sediment loads predicated by SEDCAD+ indicate that reclamation effort;. <br />conducted in the mining area will ensure that additional contributions of suspended sediment in <br />runoff from reclaimed areas will not occur. Effects of runoff from reclaimed areas on the quality <br />of streamflow. Based on past operating history at the Nucla Mine, no significant trend toward <br />higher concen4rations of the selected parameters have been detected. In addition, the pond <br />discharge will be monitored in accordance with NPDES discharge limitations and any potential <br />impact will be identified. Therefore, runoff from the reclaimed area should have no significant <br />impact over time on the quality of receiving stream water quality. As a result, post mining land <br />uses which currently occur in the area should not be affected due to the mine plan which has <br />been approved. <br />Summary. The discussion presented herein of the probable hydrologic consequences of the <br />revised mine plan approved by WFC identifies the potential effects of mining. Table 2.05.6(3)-1 <br />summarizes the discussion by listing the probable hydrologic consequences and the results of <br />the analysis of each. As can be seen, all of the probable impacts have been determined to be of <br />a short term nature, of minimal significance, or a plan has been presented to mitigate those <br />determined to have some significance. As a result, mining and post mining affects to current <br />land uses should be negligible. <br /> <br />