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~J ~ UI~il <br />-za- <br />The predicted mine inflow for the fifth year (1988) to the Eagle No.S Mine is <br />1460 gallons per minute (gpm) and the predicted inflow to the Eagle No. 9 Mine <br />is 960 gpm, (Table II-20d). These predictions are made with the assumption <br />that mine inflows from faults and subsidence will not increase from present <br />levels. (Also, calculated seepage inflow rates from Table III-20, page <br />III-72a were doubled to Come up with the maximum projected inflows.) These <br />projections may be low, given the significance of faults to mine inflows <br />currently observed in the two Eagle Mines in mine areas located below <br />stream/alluvial systems. Also, subsidence fracturing could significantly <br />increase inflow rates beneath stream/alluvial systems. Given the <br />unpredictability of the occurrence of faults subcropping beneath the <br />stream/alluvial systems; and given the present state of the art of subsidence <br />projections; the companies projections are reasonable. The actual impacts of <br />mining (empiric data) on the quantity of surface and ground waters will be <br />obtained through the inflow monitoring required by the Division and through <br />mine inspections conducted by the Division staff. <br />The total inflow rate per affected acre is greater in the Eagle No. 9 Mine <br />than in the Eagle No. 5 Mine. This may be due to the greater piezometric head <br />and hydrostatic pressures in strata affected by the Eagle No. 9 Mine. The <br />Eagle No. 9 Mine is a relatively young mine in comparison to the Eagle No. 5 <br />Mine. The drawdowns caused by the mine workings in affected aquifers would <br />not be as extensive. The pietometric head difference and ground water <br />gradient would be greater around the Eagle No. 9 Mine. This would increase <br />the ground water flow rates towards the mine workings. The Eagle No. 9 Mine <br />is also located near the axis of the Big Bottom Synclinal Basin where there <br />are higher hydrostatic heads in water bearing strata (aquifers). This would <br />also increase the quantity and the rate of ground water flow towards the mine <br />workings. All inflows to the Eagle No. 9 Mine are from areas of partial <br />extraction. No areas have been pillared, whereas, in the Eagle No. 5 Mine, <br />areas have been pillared. Therefore, subsidence is presently not considered a <br />source of mine inflows in the Eagle No. 9 Mine and was not used in predicting <br />mine inflows. The projections of subsidence due to the development mains and <br />the extractlon of room and pillar panels upon advance for the Eagle No. 9 Mine <br />have been made using extrapolated data. Empiric data on subsidence will be <br />obtained through stipulated subsidence monitoring in sections VII and XX of <br />this permit document. If subsidence were to occur, there would be an <br />increased communication between overlying rock aquifers and the Yampa <br />River/Big Bottom stream/alluvial system and inflows would be expected to <br />increase. <br />Empire Energy Corporation has shown that the mine inflows at the Eagle No. <br />and No. 9 Mines have lowered water level in overlying aquifers (Figures <br />III-l7a through III-llc and III-17e through III-17g in the permit <br />application). The company has also shown that the mines have dewatered the <br />"f" and "P" coal seams and have lowered the ground water level in the coals <br />(Appendices III-8b and III-ec of the permit application). <br />