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<br />0131 <br /> <br />. <br /> <br />7 <br />The permanent pool was assumed to contain 10,000 acre-feet (1.2xlO <br /> <br />m3) of water at the start of the simulation and, hence, the initial <br /> <br />- <br /> <br />'1 <br /> <br />volume in John Martin Reservoir was increased by a like amount. The <br /> <br />permanent pool was limited to 15,000 acre-feet (1.9xI07 m3), but was not <br /> <br />allowed to invade the flood-control pool by more than 10,000 acre-feet <br />7 3 <br />(1.2xlO m). Neither of these limitations was encountered in the <br /> <br />simulation, but the latter condition may be a consideration during times <br /> <br />of major flooding. <br /> <br />Once the Division of Wildlife's water is stored in John Martin <br /> <br />- <br /> <br />Reservoir, it begins to suffer evaporation losses. Evaporation losses <br /> <br />are calculated each month on the basis of the total volume of water in <br /> <br />the reservoir. This evaporation is then charged against the permanent <br /> <br />. <br /> <br />pool and other water in the reservoir on the basis of their respective <br /> <br />- <br /> <br />volumes. During a month in ~hich the water is being transferred to John <br /> <br />Martin Reservoir, the evaporation charge is one-half of what the charge <br /> <br />would be had the water already been in the reservoir. <br /> <br />. <br /> <br />.,' <br />. <br /> <br />13 <br />