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<br />. <br /> <br />ru <br />~ <br />~ The river below Lake Powell was divided into distinct reaches <br />~ <br />. to determine future salinity levels. Future estimates of water use <br /> <br />and salt loading for each appropriate reach of the river below Lake <br /> <br />Powell and the accumulative effect above Powell were superimposed <br /> <br />. <br /> <br />upon historical conditions for each year of the study. The changes <br />were routed downstream with the accumulated impact reflected at <br /> <br />downstream stations. <br /> <br />. <br /> <br />The studies were made on a monthly basis using a range of water <br />supply conditions and future depletion rates. <br /> <br />. <br /> <br />Projections of Future Water Use <br />The use of Colorado River water by the Upper Basin States in <br />1973 was 2,976,000 acre-feet. A number of water development projects <br />are either now under construction or have been completed and water use <br />. is building up to project capacities. Several other projects have <br /> <br />been authorized for construction. In addition, studies are being made <br />of numerous in-basin projects that would develop water for irrigated <br /> <br />. agriculture, oil shale, thermal-electric generation, and municipal <br /> <br /> <br />and industrial purposes. Some of the projected future developments <br /> <br />will provide for increasing transmountain diversions to the eastern <br /> <br />. <br /> <br />slopes of the Rocky Mountains in Colorado, to the Bonneville Basin <br />in Utah, and to the Rio Grande Basin in New Mexico; there also may <br />be new trans basin diversions in Wyoming. Actual depletions by year <br />1990 in the Upper Basin, exclusive of main stem reservoir evaporation, <br />will be dependent on many variables, including physical and legal <br />restraints. In the studies to estimate future salinity levels, <br />three possible rates of 1990 water usage were projected. These <br /> <br />. <br /> <br />. <br /> <br />-25- <br /> <br />. <br />