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WSP06497
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Last modified
1/26/2010 2:23:02 PM
Creation date
10/12/2006 1:40:42 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8270.100
Description
Colorado River Basin Water Quality/Salinity -- Misc Water Quality
Basin
Colorado Mainstem
Water Division
5
Date
1/1/1974
Author
USDOI
Title
Colorado River Water Quality Improvement Program - Status Report
Water Supply Pro - Doc Type
Report/Study
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<br />increases would be in excess of $40 million a year by <br />the turn of the century. <br /> <br />QUALITY OF WATER-COLORADO <br />RIVER BASIN (USDI) <br /> <br />Biennial Progress Reports on the "Quality of <br />Water-Colorado River Basin" are prepared by the <br />Department of the Interior. The initial report was <br />issued in 1963 and the latest report is dated 1973. The <br />1973 report displays the past, present modified, and <br />estimated future quality of the Colorado River at 17 <br />gaging stations for the period of 1941-1970. The future <br />quality condition as used in that report is an estimate <br />of the situation after the presently authorized <br />developments, projects proposed for authorization, and <br />private developments are placed in operation. The <br />re port estimates the present modified average <br />concentration below Hoover Dam to be 745 mg/I and <br />with future known developments, 971 mg/1. At <br />Imperial Dam the comparable estimates are 851 and <br />1,200 mg/l, respectively, under the same conditions. <br /> <br />COMPUTER SIMULATION OF THE HYDRO. <br />LOGIC SALINITY FLOW SYSTEM WITHIN <br />THE UPPER COLORADO RIVER <br />BASIN (USU) <br /> <br />Salinity conditions were investigated by Utah State <br />University. In 1970, the university issued a report <br />entitled "Computer Simulation of the <br />Hydrologic-Salinity Flow System Within the Upper <br />Colorado River Basin." This study employed an <br />electronic analog computer in developing a simulation <br />model of the hydrologic and salinity flow systems of <br />the Upper Colorado River Basin. Estimates were <br />derived based on the 1931-1960 period and reflect <br />cropping and riverflow regulation conditions as of <br />1960. The estimated salt load at Lees Ferry was 8.6 <br />million tons per year of which approximately 4.3 <br />million tons originated from natural sources, 1.5 <br />million tons from within the agricultural system, and <br />2.8 million tons from other inputs to the system; thus, <br />natural sources are thought to contribute 50 percent of <br />the salt load, agricultural sources 17 percent, and <br />unidentified sources 33 percent. The report states that <br />the agricultural salt load and cropland consumptive use <br />increase the total dissolved solids concentration within <br />the Upper Basin by 104 and 113 mg/l, respectively. <br />The model was designed to predict the effects of <br />various possible water resource management <br />alternatives. <br /> <br />SALINITY OF SURFACE WATER IN THE <br />LOWER COLORADO RIVER-SALTON SEA <br />AREA (USGS) <br /> <br />U.S. Geological Survey Professional Paper No. 486-E, <br />entitled "Salinity of Surface Water in the Lower <br />Colorado River-Salton Sea Area," was published in <br />1971. The report shows that during the period <br />1926-1962, the chemical regimen of the Colorado <br />River at Grand Canyon and upstream, although <br />probably somewhat different from. the virgin regimen, <br />was relatively stable. There may, however, have been <br />small increases in average mineral concentrations, <br />particularly toward the end of the period, caused by <br />co~struction of reservoirs, increased irrigation, and <br />out-of-basin diversions. The research also found that <br />most of the mineral burden of the Colorado River, like <br />most of its flow, originates in the Upper Basin. The <br />largest individual increment to the mineral burden of <br />the Colorado River below the Lees Ferry compact <br />point and above Imperial Dam was found to be the <br />Blue Springs located near the mouth of the Little <br />Colorado River. The report further shows that a <br />principal increase in salinity in the lower reach is <br />derived from irrigated land in the Parker and Palo <br />Verde valleys. <br /> <br />~.I <br /> <br />THE MINERAL QUALITY PROBLEM IN THE <br />COLORADO RIVER BASIN (EPA) <br /> <br />In 1971, the EPA released its report entitled "The <br />Mineral Quality Problem in the Colorado River Basin." <br />In this report, salinity and streamflow data for the <br />1942-1961 period of record were used as a basis for <br />estimating average salinity concentrations under <br />various conditions of water development and use. <br />Under these conditions, concentrations at Hoover Dam <br />were estimated to average about 700 and 760 mg/l in <br />1960 and 1970, and 880 and 990 mg/I in 1980 and <br />2010, respectively. At Imperial Dam, the report <br />estimates 760 and 870 mg/I for 1960 and 1970, and <br />1,060 and 1,220 mg/l for 1980 and 2010 conditions. <br />The findings of the study with respect to salinity <br />sources were that natural sources accounted for 47 <br />percent of the salinity concentrations at Hoover Dam. <br />The remainder was accounted for by irrigation (37 <br />percent), reservoir evaporation (12 percent), <br />out-of-basin exports (3 percent), and M&I uses (1 <br />percent) . <br /> <br />The present annual economic detriments of salinity <br />were estimated to total $16 million. The report further <br />advises that if no salinity controls are implemented, it <br /> <br />18 <br />
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