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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 />I <br /> <br />19 <br /> <br />.~~~ <br /> <br />r <br />The increase in flows of the Arkansas Riv r at Las Animas for the <br /> <br /> <br />period of 1974-1984 may be the result of ransmountain return <br /> <br /> <br />flows which also increased during this per'od. These return flows <br /> <br /> <br />may be masking depletions of flow above John Martin Reservoir. <br /> <br /> <br />which otherwise would have been apparent if the transmountain re- <br /> <br /> <br />turn flows were not available. It is also likely that some deple- <br /> <br /> <br />tions to usable stateline flows have been masked by the existence <br /> <br /> <br />of transmountain return flows in the river. <br /> <br />The continued existence of these return flows in the Arkansas <br /> <br />River is not guaranteed since users of transmountain water are <br /> <br />entitled under Colorado water law to reuse and completely consume <br /> <br />transmountain diversions, If transmountain return flows are not <br /> <br />maintained, the future available supply for downstream users on <br /> <br />the Arkansas River would decrease, This decrease in supply may <br />reduce the quantities available for conservation storage in John <br /> <br />Martin Reservoir and usable stateline flows. <br /> <br />~QN~1Q~IQN~ <br />The data and mass diagrams indicate that post-compact depletions <br />of usable stateline flows have occurred as evidenced by changes in <br />slope on the post-compact portions of the curves, The breaks in <br /> <br /> <br />slope generally occur in 1949 and 1974. Analyses of the slopes of <br /> <br /> <br />the curves indicate that usable stateline flows have been depleted <br /> <br /> <br />by approximately 40,000 to 50,000 acre-feet per year for the <br />