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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 />ZORICH, SPRONK a ASSOCIATES, INC. <br /> <br />Page 7 <br /> <br />I <br /> <br />.-' <br />w <br /> <br />of the Compact. The lines, and the slope indicated for each <br />line segment, were calculated by applying the least squares <br />method to the data contained in Table 1. <br />Figure 1 is a mass diagram of the Combined District 67 di- <br />versions. The slope of the post-Compact line segment is less <br />than that for the pre-Compact line segment, indicating that the <br />long-term trend has been a reduction of 10,500 acre-feet per <br />year ((159,32 - l48.82)x 1000)) in average District 67 diversions <br />since the Compact was adopted. <br />Figure 2 is a mass diagram of the Fort Lyon Canal diversions. <br />The slope of the post-Compact line segment is greater than the <br />slope of the pre-Compact line segment, indicating that the long- <br />term trend has been an increase of 10,820 acre-feet per year <br />((228.56 - 2l7.74)x 1000)) in average Fort Lyon diversions since <br />the Compact was adopted, <br />Figure 3 is a double mass diagram showing the relationship <br />between annual Fort Lyon and District 67 diversions. The slope <br />of the two line segments indicate that the average annual Fort <br />Lyon diversions were 1,37 times greater than the average Dis- <br />trict 67 diversions prior to adoption of the Compact, and 1.52 <br />times greater thereafter. The long-term trends reflect a re- <br />duction of approximately 10 perc€nt in the annual average <br />District 67 diversions (relative to the Fort Lyon Canal diversions <br />made before adoption of the Compact) during the time period after <br />the Compact was adopted, <br />An analysis of the relationship between the Arkansas River <br />flows at the upstream and downstream ends of Districts 14 and 17 <br /> <br />N <br />C,Q <br />~ <br />= <br />