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<br />. <br /> <br />o <br />o <br />tv <br />W <br /> <br />. <br /> <br />. <br /> <br />CHAPTER 2 - SALINITY OF THE RIVER <br /> <br />Overview <br /> <br />The Colorado River drains 246,000 square miles (approximately 157 million acres) of the <br />western United States and a small portion of northern Mexico. Its waters serve some 5,5 million <br />people within the United States' portion of the Colorado River Basin, and through export provides <br />full or supplemental water supply to another 22.3 million people outside the Basin, The regional <br />economy is based on irrigated agriculture, livestock grazing, mining, forestry, manufacturing, oil and <br />gas production, recreation and tourism, About 3.5 million acres are irrigated within the Colorado <br />River Basin and hundreds of thousands of additional acres are irrigated by waters exported from the <br />Basin, Hydroelectric power facilities along the Colorado River and its tributaries generate <br />approximately 12 billion kilowatt-hours annually which is used both inside and outside of the Basin, <br />The Colorado River also serves about 2.3 million people and 500,000 irrigated acres in Mexico, <br /> <br />Salinity has long been recognized as one of the major problems ofthe river. The Colorado, <br />like most western rivers, increases in salinity from its headwaters to its mouth, carrying an average <br />salt load of approximately nine million tons annually past Hoover Dam, the uppermost location at <br />which numeric criteria have been established, In addition to total salt load which measures the total <br />mass of salt carried in the River (tons/year), this report also examines salinity in terms of <br />concentration as expressed in milligrams per liter (mg/L), <br /> <br />The salts in the Colorado River system are indigenous and pervasive, Many of the saline <br />sediments of the Basin were deposited in prehistoric marine environments, Salts deposited with the <br />sedimentary rocks are easily eroded, dissolved, and transported into the river system, The Colorado <br />River Basin Salinity Conn:.~l Program is designed to prevent a portion ofthis abundant salt supply <br />from moving into the river system, <br /> <br />In a 1971 study!, the EPA analyzed salt loading in the Colorado River Basin and divided it <br />into two categories, naturally occurring and human-caused, The EP A concluded that about half (47 <br />percent) of the salinity concentration measured in water arriving at Hoover Dam is from natural <br />causes including salt contributions from saline springs, ground water discharge into the river system <br />(excluding irrigation return flows), erosion and dissolution of sediments, and the concentrating <br />effects of evaporation and transpiration, The natural causes category also included salt contributions <br />from nonpoint (excluding irrigated agriculture) or unidentified sources or from the vast, <br />sparsely-populated regions of the drainage, much of which is administered by the BLM or other <br />governmental agencies, Gfthe land within the Colorado River Basin, about 75 percent is owned and <br />adrninistered by the Federal Government or held in trust for Indian tribes. The greatest portion of <br />the naturally-occurring salt load originates on these federally-owned and adrninistered lands, Human <br /> <br />'The Mineral Qualitv Problem in the Colorado River, Surrunary Report, Environmental Protection <br />Agency, Regions VIII and IX, 65 pp" 1971. <br /> <br />2-1 <br />