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<br />in the aquifer for natural recharge that occurs principally during <br />periods of snowmelt. Pumping in excess of the annually replenishable <br />supply (mining) is a feasible alternative whereby a critical water <br />supply can be obtained over a specified period of time with con- <br />sequential effect on the environment and the surface water component <br />of the hydrologic system. Large-scale dewatering operations <br />for open-pit and subsurface mines would, in effect, be considered <br />local mining of ground water if the amount pumped exceeds the annual <br />recharge rate. In the Piceance Creek Basin, the lessees of Colorado <br />prototype oil shale lease tracts C-a and C-b have estimated the water <br />demand for processing and disposal of oil shale to be 11,500 and <br />10,000 acre-feet per year, respectively. Both lessees propose to <br />supply this demand entirely by ground water obtained from the mine <br />dewatering operations. <br /> <br />Water quality considerations are significant in utilization of <br />water developed by mine dewatering. The range of water quality <br />that can be anticipated is reflected in Table 10, Depending on <br />the process for which the water is to be used, some desalination <br />process or blending of saline ground water with better quality <br />surface water should be considered. <br /> <br />To summarize, a tremendous quantity of ground water is stored in <br />aquifers throughout the Upper Colorado River Basin--many times the <br />amount that can be stored in existing and planned surface reservoirs. <br />A significant percentage of this quantity can be pumped for energy <br />related purposes on a time-limited basis, provided that tradeoffs <br />with regard to depleted streamflow, water quality factors, and other <br />environmental effects are acceptable to the user and to the public. <br />Specific quantities that are in storage or that can be feasibly <br />developed cannot be determined from presently available information. <br />Detailed studies, such as those currently under way in the Piceance <br />Creek Basin are prerequisite to realistic determination of these <br />quantities, the stresses of various ground water development patterns, <br />and the impacts of the development. <br /> <br />36 <br />