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Last modified
7/14/2009 5:02:28 PM
Creation date
5/22/2009 7:12:05 PM
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UCREFRP
UCREFRP Catalog Number
2002
Author
U.S. Bureau of Reclamation.
Title
Final Environmental Impact Statement
USFW Year
1986.
USFW - Doc Type
Grand Valley Unit, Stage Two, Colorado River Basin Salinity Control Project, Mesa County, Colorado.
Copyright Material
NO
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• <br />SUMMARY <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 Salinity Control Act of June 24, 1974 (Public Law 93-320). The <br />Grand Valley Unit area is located along the Colorado River in western <br />Mesa County in west-central Colorado. The area includes mostly the irri- <br />gated portion of the Grand Valley, consisting of approximately 70,000 <br />acres and involving about 200 miles of canals and about 500 miles of <br />laterals. <br />The Colorado River at its headwaters in the mountains of north- <br />centraT Colorado has a salinity concentration of about 50 milligrams per <br />liter (mg/L). The concentration progressively increases downstream as a <br />result of water diversions and salt contributions from a variety of <br />sources. In 1983, the total dissolved solid concentration averaged about <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 />1970. Unless control measures are undertaken, the concentrations are <br />expected to increase as the Colorado River Basin States continue to de- <br />velop their compact-apportioned waters.l/ <br />The salt 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 average annual load at Imperial Dam. The salt loading is attributed <br />to the Mancos Formation which underlies the Grand Valley and consists of <br />a sequence 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 a thin, weathered, and fractured zone that acts as an aquifer <br />which allows water from conveyance system seepage and irrigation deep <br />percolation to dissolve salts from the shale and convey them to natural <br />drainages and ultimately the Colorado River. <br />Development 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 />solidating 34.2 miles of open laterals into 29.7 miles of pipe, and in- <br />stalling an 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 />1/ The waters of the Colorado River are divided by the Colorado <br />River Compact of 1922, agreed on by the seven Colorado River Basin States <br />(Arizona, California, Colorado, Nevada, New Mexico, Utah, and Wyoming). <br />S-1 <br />
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