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~. <br />-I9- <br />VI. Hydrologic Balance: Ground water - Rules 2.04.5, 2.04.7, 2.05.3(4), <br />2.05.6(3) and 4.05 <br />For a description of the ground water hydrology of the mine area and a discussion <br />of the impacts of mining on ground water, please refer to the Regional Geology and <br />Cround Water Hydrology portion of Section IX, Probable Hydrologic Consequences and <br />Cumulative Impact Assessment of this document. <br />The ground water sections, found on pages 30-34 and 44-47-1a of the application for <br />the Bear No. 1 and No. 2 mines, and on pages 2.04-29 - 2.04-32, 2.05-55, and 4.05-8 <br />through 4.05-11 of the Bear No. 3 mine application, have been reviewed by the Division <br />for compliance. <br />The following problems were identified in the P.A.R. of May ZS, 1981 and have been <br />fully resolved: <br />First, the Division noted that page 42 of the original application stated that water <br />was pumped from the mine to maintain the competency of floor shales for safety <br />reasons. The Division requested that the applicant provide data on the rate of <br />mine inflows and a description of the method of disposal of the water. In their <br />responses, the applicant explained that any water accumulation in the mine is a <br />result of the dust suppression system or water used with the continuous miner. The <br />applicant states that the Bear No. 1 and No. 2 mines have not experienced mine inflows <br />and that there have been no discharges. To insure the competency of floor shales, <br />water which accumulates in small depressions on the floor of the active mining areas <br />is pumped or drained to inactive areas of the mine. <br />Second, the Division requested additional information regarding water table extent <br />and storage capacity above the "F" seam (the Barren Member). The applicant provided <br />data collected by ARCO on the permit and adjacent area, including results of pump <br />tests run on wells in the Barren Member and the "F" seam, a Barren Member water <br />level map and water level tables. <br />Third, the Division requested that the applicant document the low permeability of <br />the Mesa Verde Sandstones, stated on~page 45 of the application. The applicant <br />responded that pump tests completed by RRCO, included in the application, indicate <br />that perrreabilities within the sandstones may vary from a fraction of one millidarcy <br />to as much as IO millidarcies. <br />There is some question as to the accuracy of the ARCO data provided at that time <br />regarding the aquifer characteristics of the Barren Member Sandstones. However, <br />the C seam is separated from the Barren Member by over 300 feet of sedimentary <br />strata. Only minor inflows have resulted from previous mining of the C seam in <br />the Bear No. 1 and No. 2. As stated in Section XXII Subsidence of this document, <br />the proposed mining within the Bear No. 3 is considered, by the Division, to <br />represent no potential threat to the Barren Member aquifers or the coal seams <br />overlying the C seam. The additional information requested in the P.A.R. concerning <br />aquifer characteristics of the Barren Member is not considered, by the Division, <br />to be critical to the determination of the probable hydrologic consequences of <br />the Bear mine. <br />