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<br />Causes and Impacts of Salinity <br /> <br />population increase, M&I sources will be increasing salinity by approximately 133,000 tons per <br />year by the year 2010. However, most municipal wastes are relatively low in salt concentration in <br />comparison with natural, industrial, and agricultural sources. Complete elimination of such waste <br />discharges would be expensive when compared to other salinity control methods. <br /> <br />Consumptive Use of Water IRcreases Salinity <br /> <br />Addition of salts to the river system is not the only cause of increased salinity in the Colorado <br />River Basin. The consumption (depletion) of water reduces the dilution of saline inflows to the <br />river system, increasing the concentration of salinity. Water use is evaluated as part of <br />Reclamation's responsibilities in managing the river system. The Colorado River Basin, <br />Consumptive Uses and Losses Report[4] summarizes water use in the Basin. Table 2 summarizes <br />the Basin uses for 1981-85, including tributaries to the Colorado River in the Lower Basin. Work <br />is underway to update these estimates. <br /> <br />Table 2.-Water use in the Colorado River Basin (1981-85 average) <br /> <br />Total <br /> <br />Upper Basin use Lower Basin use <br />(1,000 af/yr)' (1,000 af/yr) <br />812 1,255 <br />2,312 5,101 <br />203 841 <br />0 30 <br />669 4,063 <br />3,996 11,290 <br /> <br />Type of use <br /> <br />Reservoir evaporation and channel losses <br />Agriculture (within basin) <br />M&I <br /> <br />Fish, wildlife, and recreational <br />Transbasin exports <br /> <br />1 Acre-feet per year. <br /> <br />With the exception of the Central Arizona Project, the Lower Basin has already developed most of <br />its water supply. CAP is the last major development to deplete water from the Lower Colorado <br />River (approximately 1.5 million acre-feet per year). Agriculture use is the single largest source of <br />depletions to the Colorado River. Exports, reservoir evaporation, and M&I uses also account for <br />lesser but significant depletions. <br /> <br />Most of the exports from the Upper Basin are made at higher elevations where the salinity <br />concentrations are very low. This loss of high quality water results in the remaining flows <br />downstream becoming more concentrated. Water exported from the Upper Basin during the period <br />1941-72 averaged about 360,000 acre-feet per year. Completion of such large projects as the <br />Colorado-Big Thompson, Duchesne Tunnel, Roberts Tunnel, and more recent projects increased <br />exports to about 669,000 acre-feet per year. <br /> <br />11 <br />