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<br />eGGS <br /> <br />Water Requirements <br /> <br />Service Area <br /> <br />Lands considered to be served by the ground-water recharge program <br />were the areas within the Lower South Platte Water Conservancy District <br />(LSPWCD) overlying the alluvial aquifer. Lands within the North Sterling <br />Irrigation District do not overlie the alluvial aquifer, These lands, <br />amounting 'to 46,100 acres, cannot be served directly from ground water. <br />Therefore, lands considered for recharge amount to 120,300 acres, <br /> <br />Farm Delivery Requirements <br /> <br />Water service from the Narrows Reservoir is contracted to the Central <br />Colorado Water Conservancy District (CCWCD) and the Lower South Platte <br />Water Conservancy District (LSPWCD). Detailed water requirement studies <br />were conducted for 23 ditch systems within the LSPWCD as a part of the <br />Narrows Unit feasibility studies (USBR, 1966). These studies resulted <br />in an estimated average annual river diversion requirement for supple- <br />mental surface water of 178,000 acre-feet during the period 1947-1961. <br /> <br />The recharge service area, which excludes lands served by the North <br />Sterling Irrigation District, was estimated to have an average annual <br />river diversion requirement for supplemental surface water of 84,000 <br />acre-feet. Annual conveyance losses for the existing distribution <br />system have been estimated to be approximately 38 percent of the river <br />diversions. The estimated annual farm-headgate demand for supplemental <br />water on the 120,300 acres overlying the alluvial aquifer is estimated <br />to average 52,100 acre-feet. It ranged from 20,300 acre-feet in 1951, <br />to 109,100 acre-feet in 1972 (see exhibit 6). <br /> <br />River Diversion Requirements <br /> <br />The bulk of the water will be recharged early in the irrigation season, <br />but will be pumped at a varying rate throughout the irrigation season <br />with maximum pumpage anticipated to occur in July and August, Due to <br />this lag time, drain-out of a portion of the recharged water will <br />occur. Assuming homogeneous and isotropic aquifer characteristics <br />between the recharge area and the stream, the amount of drain-out <br />occurring in a given time frame depends largely upon the distance <br />between the stream and the recharge ponds. <br /> <br />40 <br />