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<br />. <br /> <br />. <br /> <br />. <br /> <br />000386 <br /> <br />PART XL COMPARISON OF VIRGIN AND mSTORlC STREAMFLOW <br />AT GAGE NEAR mGHWAY 666 <br /> <br />Tables 27 and 28, respectively, are summaries of the estimated virgin <br /> <br /> <br />and historic streamflow at the gage near Highway 666. The table of historic <br /> <br /> <br />streamflow has been corrected by adding 1,400 acre-feet to the gage records <br /> <br /> <br />each year to compensate for the irrigation diversions during May through <br /> <br /> <br />September that historically bypassed the gage. The difference between the <br /> <br /> <br />virgin and historic streamflow is attributable to the activities of man in the <br /> <br /> <br />drainage basin upstream of the gage. Although municipal and domestic water <br /> <br /> <br />use have had a negligible effect on streamflow, diversions for irrigation on <br /> <br /> <br />up to 11,500 acres have had a significant impact. The effect of irrigation on <br /> <br /> <br />the flow of the Mancos River is expressed by the following relationship: <br /> <br />(6) Historic Streamflow = Virgin Streamflow - hrigation Depletions <br /> <br />The difference between virgin and historical stream flows is summarized <br /> <br /> <br />in Table 29, and varies from 4,700 to 30,300 acre-feet per year, with an average <br /> <br />of 19,100 acre-feet. As described in Part V of this report, it is estimated that <br /> <br /> <br />overall historic irrigation depletions have averaged about 18,800 acre-feet per <br /> <br /> <br />year. Thus, it is concluded that the virgin streamflow estimates for the Mancos <br /> <br /> <br />River are accurate within the limits of the available data. <br /> <br />As shown in Table 29, irrigation in the Mancos River basin has resulted <br /> <br /> <br />in large depletions to the Mancos River flows from April through July during <br /> <br /> <br />the spring runoff period when large amounts of streamflow was available for <br /> <br /> <br />storage and irrigation use. Since groundwater return flows from irrigation reach <br /> <br />the river on a lagged basis, the return flows typically resulted in a net accretion <br /> <br /> <br />to the river in November through March as indicated by the negative numbers <br /> <br />in Table 29. <br /> <br />-40- <br /> <br />,~, <br />