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<br />N. <br />~ <br />~ <br />~, <br /> <br />adopt salinity standards and an implementation <br />plan to limit further increases in salinity that <br />are discussed later in chapters 5 and 6, <br /> <br /> <br />Chapter 3 <br /> <br />Causes and Impacts of Salinity <br /> <br />CAUSES OF SALINITY <br /> <br />Nearly half of the salinity in the Colorado River <br />system is from natural sources, Saline springs, <br />erosion of saline geologic formations, and runoff <br />all contribute to this background salinity, <br />Irrigation, reservoir evaporation, and municipal <br />and industrial (M&I) sources make up the <br />balance of the salinity problem in the Basin, <br />Figure 2 shows the relative amounts each source <br />contributes to the salinity problem, The EPA[I] <br />estimated the natural salinity at Hoover Dam <br />was 334 mgIL, In 1991, the salinity at Hoover <br />Dam was reported to be 634 mg/L, a 300 mgIL <br />increase. <br /> <br />Ifrigalion (37%) <br /> <br /> <br />Natural (47%) <br /> <br />Reservoir (12%) <br />Evaporation <br /> <br />Figure 2,-Sources of salinity, <br /> <br />The natural or background salinity of the <br />Colorado River has been increased by the <br />development of water resources in two major <br />ways: (1) the addition of salts from water use <br />and (2) the consumption (depletion) of water, <br /> <br />The combined effects of water use and <br />consumption have had a significant impact on <br />salinity in the Colorado River Basin, Concern <br />over the damaging levels of salinity prompted <br />the Basin States and the Federal Government to <br /> <br />Agricultural Sources of Salinity <br /> <br />Irrigated agriculture is the largest user of water <br />in the Colorado River Basin and a major <br />contributor to the salinity of the system, <br />lorns[2] found that irrigated lands in the Upper <br />Colorado River Basin contribute about <br />3.4 million tons of salt per year (37 percent of <br />the salinity ofthe river), Irrigation increases <br />salinity (figure 3) by consuming water and by <br />dissolving salts found in the underlying saline <br />soils and geologic formations, usually marine <br />shales, <br /> <br />Deep percolation mobilizes the salts found <br />naturally in the soils, especially if the lands are <br />overirrigated, Through salinity control <br />practices, these contributions to the river system <br />eM be dramatically limited, ensuring the future <br />beneficial uses of the river, <br /> <br />Irrigation development in the Upper Basin took <br />place gradually from the beginning of settlement <br />in about 1860 but was hastened by the purchase <br />ofland from the Indians in 1873, About <br />800,000 acres were being irrigated by 1905, <br />Between 1905 and 1920, the development of <br />irrigated land increased at a rapid rate, and by <br />1920, nearly 1.4 million acres were being <br />irrigated, The Upper Colorado Region <br />Comprehensive Framework Study, June 1971 <br />reported that over 1,6 million acres were in <br />irrigation in 1965, Since that time, development <br />has leveled off and decreased somewhat because <br />of physical, environmental, and economic <br />limitations, About 1.4 million acres are <br />currently being irrigated, <br /> <br />Irrigation development in the Lower Basin <br />began at about the same time as in the Upper <br />