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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />;'(, .-:",(" .-:~ <br />':'J;,; v ',' <br /> <br />SECTION III OPERATIONAL STUDY ASSUMPTIONS <br /> <br />STREAM TRANSIT LOSS <br /> <br />, <br />When reservoir, transbasin, or exchanged water is transported in a natural <br />stream to a point of use, the State Engineer normally calculates a stream <br />loss transportation charge. Due to the lack of stream loss data, the <br />magnitude of the charge is often estimated. From Ruedi Reservoir to <br />Battlement Mesa, it is estimated that a five percent charge is reasonable. <br />If, however, the State Engineer were to determine a different stream transit <br />loss estimate, this estimate would be used. <br /> <br />RIVER WATER CALLS <br />A thirty-year period of study from 1941 to 1970 was used to establish the <br />pattern and dependability of the Battlement Mesa diversion. It was <br />concluded that the Dow Pumping Plant and Pipeline water right will not be <br />directly affected by the Colorado River Basin Compact. <br /> <br />To determine when the Battlement Mesa water right would be in priority, the <br />Colorado River Simulation Program (CORSIM II) river basin operation <br />simulation program and its associated data bank were used. This simulation <br />model and data bank have been developed by the David E. Fleming Company. <br />The modified Future Base Problem File utilized for the CORSIM II simulation <br />of the Colorado River is referred to as the "Colony Model." This data base <br />included future average depletions from the basin of about 820,000 acre feet <br />per year above present levels of water use, including 225 cfs of continuous <br />demand for oil shale developments. In addition, the Grand Junction - <br />Colorado River Pipeline diversion capacity was increased from 91.5 to 120 <br />cfs, and the Cities Service Pipeline diversion capacity was increased from <br />35 to 55 cfs. In the CORSIM II model, the level of development was <br />estimated for year 2005 conditions under virgin flow and climatological <br />conditions similar to the historic period of 1941 through 1970. <br /> <br />(7) <br />