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<br /> <br />SUMMARY <br /> <br />N <br />.&:0. . <br />.&:0. <br />CO <br /> <br />The purpose of the Grand Valley Unit of the Colorado River Basin <br />Salinity, Control Project is to decrease salt loading to the Colorado <br />River. ;The unit was authorized for construction by the Colorado River <br />Basin S4linity Control Act of June 24, 1974 (Public Law 93-320). The <br />Grand V4lley Unit area is located along the Colorado River in western <br />Mesa Coubty in west-central Colorado. The area includes mostly the irri- <br />gated pqrtion of the Grand Valley, consisting of approximately 70,000 <br />acres a~dinvolving about 200 miles of canals and about 500 miles of <br />laterals~ <br /> <br />The: Colorado River at its headwaters in the mountains of north- <br />central cj:olorado has a salinity concentration of about 50 milligrams per <br />liter (mg/L). The concentration progressively increases downstream as a <br />result o~ water diversions and salt contributions from a variety of <br />sources. : In 1983, the total dissolved solid concentration averaged ahout <br />710 mg/L:at Imperial Dam, the last major diversion point of the Colorado <br />River in;the United States. In 20 of the last 23 years, average annual <br />total diSsolved solids exceeded 800 mg/L with a maximum of 896 mg/L in <br />, . <br />1970. Uj:lless control measures are undertaken, the concentrations are <br />expected :to increase as the Colorado River Basin States continue to de- <br />velop the~r compact-apportioned waters.l/ . <br /> <br />,~ <br /> <br />The ~alt loading to the Colorado River from the unit area is esti- <br />mated at:approximately 580,000 tons annually, which is 7.0 percent of <br />the avera~e annual load at Imperial Dam. The salt loading is attributed <br />to the Mapcos Formation which underlies the Grand Valley and consists of <br />a sequenc~ of thick beds of gray calcareous marine shale that contains <br />a high percentage of salt. At the land surface, the Mancos Formation <br />exhibits ~ thin, weathered, and fractured zone that acts as an aquifer <br />which. alll>ws water from conveyance system seepage and irrigation deep <br />percolati&n to dissolve salts from the shale and convey them to natural <br />drainages 'and ultimately the Colorado River. <br /> <br />". <br />Deve~opment of the Grand Valley Unit waS planned in stages. Stage <br />One, encompassing about 10 percent of the unit area and completed in <br />April 1983, consisted of the concrete lining of 6.8 miles of canal, con- <br />solidatin~ 34.2 miles of open laterals into 29.7 miles of pipe, and in- <br />stalling ~n automated moss and debris removal structure. The Stage One <br />area is designated by the cross hatching on the Frontispiece Map. The <br />Stage Two area involves most of the remainder of the valley outside the <br />Stage One area. <br /> <br />",,,, . <br /> <br />,.,-- <br /> <br />1/ TIle waters of the' Colorado River are divided by the Colorado <br />River-ComP4ct of 1922, agreed on by the seven Colorado River Basin States <br />(Arizona, California, Colorado, Nevada, New Mexico, Utah, and Wyoming). <br /> <br />S-l <br /> <br />i <br /> <br />-j:.[ <br />- <br />