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<br />. <br /> <br />PART 11/ <br /> <br />CAUSES OF SALiNITY <br /> <br />J. Municipal and Industrial Sources of Salinity <br /> <br />,-. <br />oJ' <br />o <br />~ <br /> <br />Salt loads contributed to the Colorado River systpm by munlCi- <br />pal and industrial sources are generally minor, total iog about percent <br />of the basin salt load. Future increases in salt loads from these <br />sources are expected to be smal t relative to the total basin salt burden <br />and will have only a minor effect on salinity levels. <br /> <br />.... <br /> <br />Most municipal and industrial ....astes are relatively low in <br />total salt load in comparison ....ith natural and agricultural sources, and <br />complete elimination of such waste discharges ....ould have little effect on <br />salinity concentrations in the main riv~r system. Since these wastes are <br />point sources of salinity, control could be achieved if salinity levels <br />in the waste beinK discharged (i.e., industrial brines) warrant such <br />control. <br /> <br />The energy shortage has caused an Increase of inter<"st for <br />construction of large energy producing industries within the Colorado <br />River Basin. With emphasis placo'!d on improving the water quality in the <br />basin, these industries have been under pressure by State and Federal <br />agencies to prevent the return of salts to the river by consuming all <br />water diverted for use. <br /> <br />. <br /> <br />Development of oil and gas, oil shale, and mineral resources in <br />the basin also has the potential to increase salt loading. !1any saline <br />ground water aquifers are static (very little .....Her movement) until they <br />are disturbed by drilling or mining activities. An example of Where this <br />has happened is the Meeker Dome Salinity Control Unit described in Part <br />VIII Which came about as the result of deep ground water, high in di.s- <br />solved salts, flowing back to the surface through abandoned oil wells. <br /> <br />B. Increased Concentration from Water Depletions <br /> <br />Addition of salts to the river system is not the only cause of <br />increased sal inity concentrat ions. The dt>plet ion of water of better <br />quality than in downstream reaches produces a concentrating effect on the <br />waters of the downstream reaches. This concentrating effect occurs to a <br />greater degree when the diverted salts return to the river than when they <br />are depleted along with the water. <br /> <br />1. In-basin Depletons <br /> <br />. <br /> <br />Consumptive use of water for irrigation within the basin is <br />responsible for the largest depletions while municipal and industrial <br />us~s account for a lesser depl~tion. Evaporation from r~serVOlr and <br />stream surfaces also produces large depletions. Phreatophytes cause <br />significant water losses by evapotranspiration, especially in the Lower <br />Basin below Hoover Dam. In most cas~s where in-basin deplet ions occur, <br />the diverted salts return to the river system, adding significantly to <br />the increase in concentration. Only in the case of large industri~s such <br />as steam powerplants are the salts depleted along with the water. <br /> <br />12 <br />