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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />'I <br />II <br /> <br />by utility records for these years. Power coefficients are simply the amount of electrical <br />energy used in pumping one acre-foot of water; a power coefficient of 135 kwh/ac-ft for a <br />particular well, for example, indicates that it takes 135 kilowatt-hours to pump one acre-foot <br />of water through that well. Since the remaining wells were equipped with totalizing flow <br />meters in 1994, only incomplete data were available for them. The pumping from these <br />metered wells was estimated at 11.11 percent of the pumping from the power coefficient <br />wells, based on the data that were available for 1994. Obviously, the separation between the <br />wells in the main stem area and the wells out of the main stem area was based on well <br />location. <br /> <br />During water years 1986-94, the irrigation pumping averaged 62,206 acre-feet <br />annually, and ranged from 23,194 acre-feet in 1987 to 91,328 acre-feet in 1991. An average <br />of 60,547 acre-feet annually, or 97.33 percent of the total occurred in the main stem area. <br />Table 2 shows the breakdown of the main stem irrigation pumping between supplemental and <br />sole-source water. The supplemental water averaged 44,586 acre-feet annually or 73.64 <br />percent of the total main stem irrigation pumping, and ranged from 14,387 acre-feet in 1987 <br />to 68,027 acre-feet in 1991. The sole source water averaged .15,962 acre-feet annually, and <br />ranged from 8,188 acre-feet in 1987 to 24,385 acre-feet in 1994. The pumping in individual <br />years shows considerable variation, most of which was caused by climatic and hydrologic <br />factors. The amount of surface water available to the ditches and reservoirs was probably <br />the single most important factor in determining the amount of supplemental pumping. <br /> <br />Water years 1990-94 were selected as a representative analysis period in this study. <br />The pumping during this period is judged as larger than normal in that it includes two years <br />of relatively high pumping (1991 and 1994) and no years of low pumping. Studies prepared <br />for the Colorado Division of Water Resources for use in Kansas v. Colorado indicate that <br />pumping by LAWMA's membership was probably larger during the extreme drought conditions <br />of the 1970's; however, several institutional factors have changed since then that will reduce <br />pumping, even during a repeat of those drought conditions. Included among these <br />institutional factors are the implementation of the 1980 Operating Plan at John Martin <br />Reservoir, the implementation of the Pueblo Reservoir Winter Storage Program2.J , and more <br /> <br />2.J The Pueblo Reservoir winter storage program affects the operation of the ditches and reservoirs <br />that divert upstream from John Martin Reservoir during November 15 through March 15. Water that <br />historically was used for irrigation is stored in Pueblo Reservoir and the private off-channel reservoirs, <br /> <br />9 <br />