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<br />2359 <br /> <br />The amounts tabulated for years 1968 and 1969 were estimated <br />using data from less frequent measurements than are made under the <br />ISSP program, and have a lower confidence level. However, they are <br />judged to be adequate for this preliminary analysis. <br />Figure 3 shows the quantities of diversion water and return flow <br />for each year of record, their salinity in milligrams per liter, their <br />salt content in tons, and the net salt discharge in tons. <br />An attempt was made to evaluate the reasons for the variation in <br />net salt discharge as shown on the preceding page. It was found <br />that the years with the three relative highs were years of relatively <br />low per acre water use, apparently involving interruptions of irriga- <br />tion operations. In 1976 a tropical storm caused unusually heavy late <br />summer rain, which apparently caused more of a reduction in diver- <br />sions than drainage. Higher than average rainfall also occurred in <br />1970 and 1972 and the timing of rainfall may have interfered with <br />irrigation deliveries, but this correlation is not strong. The varia- <br />tions are discussed further in a following section of this chapter. <br />The Boyle Engineering Corporation was retained by the Bureau <br />of Reclamation in 1975 to gather data on irrigation efficiency and <br />agricultural drainage, and to make a preliminary evaluation of whether <br />water system improvements would reduce salt discharge to the river. <br />The results of the study were presented in a report entitled "Salinity <br />Control and Irrigation System Analysis, Colorado River Indian <br />Reservation," August 1976. [2] <br />Using primarily data from 1974 operations, Boyle Engineering <br />concluded that the Reservation received 779,036 tons of salt and <br />discharged 647,608 tons. The difference of 131,428 tons was retained <br />on the Reservation. The various components of the water and salt <br />budgets are on Table 1, which shows that a substantial amount of <br />water and salt enters the Reservation in addition to Colorado River <br />diversions. <br />The Boyle estimate can be reconciled with the Bureau of <br />Reclamation estimate for 1974 if certain unmeasured inflows are added <br />to the latter. The Bureau of Reclamation ISSP data include only <br />diversions at Headgate Rock Dam and discharges in the three drains <br /> <br />12 <br />