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<br />. <br /> <br />. <br />STATE OF COLORADO <br /> <br />, <br /> <br />MEMORANDUM <br /> <br />RECEIVED <br />JAN 1 2 1998 <br /> <br /> <br />. <br /> <br />OFFICE OF THE STATE ENGINEER <br />Division of Water Resources <br />Department of Natural Resources <br />131 3 Sherman Street, Room 818 <br />Denver, Colorado 80203 <br />Phone (303) 866-3581 <br />FAX (303) 866-3589 <br /> <br />January 12, 1998 <br /> <br />FROM: <br /> <br />Hal Simpson <br />Glenn Graham J6 D /} <br /> <br />Colorado Water <br />Conservation Board <br /> <br />Roy Romer <br />Governor <br />James s. loch head <br />Executive Director <br />Hal D. Simpson <br />State Engineer <br /> <br />TO: <br /> <br />SUBJECT: <br /> <br />Denver Museum of Natural History Denver Basin Project Proposal <br /> <br />I have reviewed the museum's proposal to the National Science Foundation in order to identify <br />components of the project that would directly benefit the Division of Water Resources. The <br />benefits I see are described below. There may be others that are not apparent at this time. <br /> <br />. <br /> <br />The proposed well would provide data point in a part of the Denver Basin where little <br />hydrogeologic information is available. Most of the aquifer parameters (e.g. specific yield, <br />transmissivity, and determination of thickness of saturated aquifer material) and the assumptions <br />which we use to administer the Denver Basin Aquifers and quantify the resource were based on <br />cores and geophysical logs obtained from the Castle Pines well. With the possible exception of <br />the Dawson Aquifer, the part of the Denver Basin Aquifers having hydrogeologic properties <br />similar to those found at the Castle Pines site contains only a fraction of the ground water stored <br />in the Denver Basin. A larger amount of water is contained in aquifer materials more closely <br />resembling the rocks likely to be present at the proposed museum project site. <br /> <br />The aquifer material at the Castle Pines site, being closer to the sediment source, consists <br />mostly of coarse-grained material. The proposed project site, at a greater distance from the <br />mountain front, is characterized by the deposition of fine-grained sediments. The hydrogeologic <br />data to be obtained from the museum project core and well will provide aquifer data more <br />representative of the material comprising the majority of the Denver Basin Aquifers. The project <br />provides an opportunity to relate hydraulic conductivity and specific yield data generated from <br />laboratory analysis of the core to a suite of geophysical logs from the same well. Our ability to <br />quantify ground water and predict effects of well pumping in a large part of the Denver Basin will <br />be greatly enhanced. <br /> <br />, <br /> <br />High precision temperature logging to be provided by New Mexico Tech will provide data with <br />regard to the movement of ground water through the aquifers, both horizontally and vertically. <br /> <br />Finally, while I have not seen it, it is my understanding that Stan Robson of the U.S.G.S has <br />written a letter to Mike Serlet, which identifies, from his perspective, the benefits of the proposed <br />project. <br /> <br />cc: Mike Serlet <br /> <br />. <br />