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WSP00180
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Last modified
1/26/2010 12:13:07 PM
Creation date
10/11/2006 9:34:06 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8271.300
Description
Colorado River Basin Salinity Control Program - General Information and Publications-Reports
Basin
Colorado Mainstem
Water Division
5
Date
3/1/1981
Title
Feasibility of Financial Incentives to Reuse Low Quality Waters in the Colorado River Basin
Water Supply Pro - Doc Type
Report/Study
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<br />. <br /> <br />. <br /> <br />w <br />en <br />N <br />W <br /> <br />CHAPTER I. INTRODUCTION <br /> <br />The Colorado River Basin <br /> <br />The research described in this report deals with aspects of <br />water management, policy and specific planned reuses of water in the <br />244,000 square mile area of the Colorado River Basin (CRB). The pur- <br />pose and scope of this study are strongly shaped by the unusual geo- <br />graphic, climatic, and political characteristics of the Colorado River <br />Basin. <br /> <br />Earlier studies have described in detail the need for salinity <br />control and the consequent incentives for water reusel in terms of Ba- <br />sin physical characteristics, demands on water supplies, and predicted <br />development. Those parameters remain in effect as the demands of ener- <br />gy development begin to strain already scarce water resources. <br /> <br />Physical characteristics of the CRB. The Colorado River <br />stretches 1,400 miles through portions of seven states and northern <br />Mexico before emptying into the Gulf of California. Its drainage basin <br />includes the five driest states in the nation (Nevada, Arizona, Utah, <br />Wyoming, and New Mexico), the seventh driest (Colorado), and the desert <br />portions of California. The. climate of the Basin extends from the semi- <br />arid Rockies and high plains of Wyoming and Colorado to the arid desert <br />of Arizona, <br /> <br />Water supply in the CRB, The mean annual precipitation in the <br />Basin ranges from nine to 17 inches (excluding the non-basin portion of <br />the seven states). Most of the water in the river comes from high moun- <br />tain snowmelt supplemented by occasional summer rains and by natural <br />springs, In the Lower Basin (see Figure '1) evaporation and transpira- <br />tion can exceed rainfall by more than 600,000 af/yr.2 <br /> <br />ISee, for example: Richard L, Perrine, et al., Institutional <br />Barriers to Waste Water Reuse in Southern California (Washington, D.C.: <br />U.S, Department of the Interior, Office of Water Research and Technology, <br />1979); A. Bruce Bishop, et al., Evaluating Water Reuse Alternatives in <br />Water Resource Planning (Washington, D.C.: U.S. Department of the Inte- <br />rior, Office of Water Research and Technology, 1974); the entire January <br />1975 issue of Natural Resources Journal, 15:1, University of New Mexico <br />School of Law; U.S. Department of the Interior, Critical Water Problems <br />Facing the Eleven Western States (Washington, D.C.: Government Print- <br />ing Office, 1975). <br /> <br />2Water Resources Council, The Nation's Water Resources, Part IV: <br />Water Supply and Water Quality Considerations (Washington, D.C.: Govern- <br />ment Printing Office, 1979), pp. 108-109. <br /> <br />1 <br />
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