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<br />~") <br /> <br />-... ___. <br />~ <br />to <br />~ <br /> <br />~ <br /> <br />.<, <br /> <br />and were determined by subtracting the amounts in columns 3 and 4 <br /> <br />from the amounts in column 2. Excess depletions in column 9 and <br /> <br />depletion shortages in column 10 were determined by comparing the <br /> <br />state credit at the Catlin headgate with the historic consumptive <br /> <br />use, which was obtained from table 4. <br /> <br />It can be seen in table 5 that the total of depletion short- <br /> <br />ages is greater than the total of excess depletions. Excess deple- <br /> <br />tions occur during the years when a larger water supply is available, <br /> <br />and depletion shortages occur during the dryer years. During all <br /> <br />_ years except the flood year of 1965, the amounts left in the river <br /> <br />were greater than the excess depletions. Thus, the vested rights <br /> <br />of other water users are not only protected by this plan but actually <br /> <br />improved by making additional water available during the dryer years. <br /> <br />The amounts of water that were available in the simulation for <br /> <br />evaporation replacement at John Martin reservoir are shown in <br /> <br />column 7 on table 5. They were determined by deducting the trans- <br /> <br />mission losses (5.5 percent) from the state credit at the Catlin <br /> <br />headgate. The state's storage decrees in the transfer plan are <br /> <br />6.383 percent (6.755% x 0.945 = 6.383%) of the amounts of the <br /> <br />original Catlin decrees. The annual " amounts range from a low of <br /> <br />1,640 acre-feet in 1954 to 4,808 acre-feet during seven of the <br /> <br />24 years and average 3,789 acre-feet; they will provide a satisfac- <br /> <br />tory permanent pool operation. <br /> <br />--- --- <br />------------- <br />Figure 2 is a circle graph, wh-ich depTcts the disYiinuEi6n of _u_ <br /> <br />11 <br />