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<br />PART III <br /> <br />CAUSES AND IMPACTS OF SALINITY <br /> <br />r--< <br />tv <br />c.-1 <br />v'; <br /> <br />Assuming a yield of 5.8 million acre-feet for the Upper Basin, this <br />leaves approximately 1.8 million acre-feet to be developed. <br /> <br />Consumptive use of water for irrigation within the basin and ex- <br />ports from the basin were responsible for the largest depletions of <br />the Colorado River, while reservoir evaporation and municipal and indus- <br />trial uses account for a lesser depletion. <br /> <br />Average water'use of the Colorado <br />for 1976-80[1] <br />(Unit--l,OOO) <br /> <br />River <br /> <br />Type of use <br />Reservoir evaporation <br />Irrigated agriculture <br />Municipal and industrial <br />Fish, wildlife~ and recreation <br />Transbasin exports <br />Deliveries to Mexico <br />Total <br /> <br />Ac re- fee t <br />2,114 <br />3,473 <br />271 <br />50 <br />3,525 <br />2,847 <br />12,280 <br /> <br />. <br /> <br />The major part of the transbasin depletions in the Upper Basin is <br />made at higher elevat ions where the sali ni ty concentrat ions are very <br />low. This removal of high quality water results in the remaining flows <br />downstream becoming more concentrated even though some salts are removed <br />by the water delivered to another basin. Many transbasin diversions <br />have been made over the years and an additional number will occur in <br />the future. <br /> <br />Water exported from the Upper Basin during the period 1941-72 aver- <br />aged about 360,000 acre-feet per year. Completion of such large proj- <br />ects as the Colorado-Big Thompson, Duchesne Tunnel, and Roberts Tunnel <br />and more recent projects such as the San Juan-Chama, Fryingpan-Arkansas, <br />and Homestake resulted in increased exports to about 726,000 acre-feet <br />per year for 1976-80, with a peak in 1978 of 852,000 acre-feet. <br /> <br />C. Effects of Water Quality on Water Users <br /> <br />1. Recreation, Esthetics, and Fisheries <br /> <br />The major instream uses in the Colorado River include hydro- <br />electric power, propagation of fish and aquatic life, recreation (in- <br />cluding swimming, water skiing, boating, rafting, etc.), and esthetics. <br />A number of conflicts between water uses have become prominent issues in <br />recent years. <br /> <br />. <br /> <br />There can be many tradeoffs in water quality, eutrophication, <br />and esthetics both in the reservoir and downstream, depending on the <br />depth of reservoir withdrawal and the flushing rate. The depth of with- <br />drawal impacts the temperature and nutrient releases from a reservoir. <br />These releases can now be controlled by the use of selective withdrawal <br />structures; however, the optimum temperatures for cold water sport <br /> <br />14 <br />