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<br />Table 2.2-Comparison of Salinity Levels to the Numeric Criteria for the Existing (1991) Level <br />of Development and Salinity Control <br /> <br />w <br />(D <br />()l <br />o <br /> <br />Station <br /> <br />Nu mericCriteria Adjusted Observed Salinity <br /> (mglL) Salinity (mglL) <br /> (mglL) <br /> 723 no 634 <br /> 747 747 635 <br /> 819 864 753 <br /> <br />Colondo River below Hoover Dam <br /> <br />Colorado River below Parter Pam <br /> <br />Colorado Ri\'er at Imperial Dam <br /> <br />. Reflects salinity dial would occur from long~tenn mean water supplY'8 computed by CRSS. Observed <br />1991 aalinity levels were lower due to unuBUAlly high runoff in earlier years and storage ufibel water in <br />the reservoir .ystem. <br /> <br />PRO.IECTlONS <br /> <br />Future Water Depletions <br /> <br />One of the significant factors affecting salinity concentrations is water use. Estimates of <br />projected water use through the year 2015 for each of the seven states were developed jointly <br />by the states and Reclamation. <br /> <br />Table 2.3 presents a summary of estimated water depletions in the Upper Colorado River <br />Basin, and from the main stem of the Lower Colorado River. <br /> <br />Table 2.3 <br />SlImmary of Projected Water Deoletions in the <br />Colorado River Basinli. ~I <br /> <br />(1,000 acre-feet) <br /> <br /> 1995 2 000 2005 2010 2015 <br />Upper Basin:!! 3,776 3,945 4,094 4,280 4,390 <br />Lower Basin~1 7,500 7,500 7,500 7,500 7,500 <br />Total 11,276 1 1,445 11 ,594 11,780 11 ,890 <br /> <br />I/Source: Table prepared from primary depletion projections utilized by Reclamation for CRSS salinity runs. <br /> <br />lIDoes not include deliveries to Mexico. <br /> <br />liDepletions at point of use. Does not include Colorado River Storage Project reservoir evaporations estimated by <br />Reclamation to average 520,000 acre-feet per year under full development. <br /> <br />~/Lower main stem only. Diversions from the main stem less returns. Does not include main stem reservoir evaporation <br />and stream losses. <br /> <br />2-9 <br />