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<br />36 <br /> <br />The average reduction in deep percolation returning to the river <br />with the USDA program is 6 inches. The average reduction in salt <br />~) loading of returnflow is 1,30 tons per acre foot. This <br />en translates into an average salt load reduction of ,65 tons per <br />~ irrigated acre treated, The USDA program will reduce onfarm salt <br />QQ loading about 50 percent, <br /> <br />Several aspects of the salt and water budgets for the Uintah are <br />different than the Colorado units. The first and most <br />significant attribute is the short water supply, This makes <br />defining an average year more difficult, During wet years excess <br />water is applied and there is a lot of deep percolation, and in <br />drought years there still may be excess water added in the <br />spring, but irrigators run out of water in the summer, When new <br />and improved systems are installed the first increment of <br />conserved water may go to reduce water shortages, However, <br />irrigators may still run out of water in the summer. <br /> <br />The second attribute in the uintah Basin is the large acreage of <br />wetlands and phreatophetic vegetation, which uses deep <br />percolating and seepage water. This reduces the water returning <br />to the river and salt pickup. Over half of the deep percolating <br />water is used by wetland vegetation, and their is some reuse for <br />irrigation, with improvements in the delivery system and onfarm <br />systems less water will be used by wetland vegetation and will <br />add to instream flow for fisheries, <br /> <br />ANALYSIS of USGS WATER QUALITY DATA <br /> <br />A trend analysis was used to identify a decrease in the salt load <br />of the Duchesne River before it enters the Green River due to the <br />USDA salinity control program. Water quality data was obtained <br />from analysis of water samples collected on the Duchesne River <br />near Randlett monitoring station by the U.S.Geological survey. <br />Trend analysis is a statistical procedure used to detect changes <br />in stream water quality at a monitoring station over time. SCS <br />used a linear regression analysis, The regression shows a <br />decrease in the salt load since the USDA program started in 1981. <br /> <br />A regression analysis was performed on the 1941-1980 pre-project <br />years and the 1981 to 1992 project years, Figure 1 displays the <br />results. The slopes of these regressions are different, which <br />points to an effect on the salt loading of the Duchesne River. <br /> <br />USGS publishe~a f~ep~rt intitled "National Water Summary 1990-91- <br />-Stream wateriQuality: Utah", USGS Water Supply Paper 2400, The <br />results of there independent study confirms the conclusions of <br />the SCS water quality trend analysis, Water quality data were <br />analyzed for trends by using the seasonal Kendall test, A <br />downward trend in sulfate concentration, chloride concentration, <br />and dissolved solids at site 8 on the Duchesne River in the Upper <br />Colorado River Basin has been identified in the paper as probably <br />the result of improvements in irrigation water management. <br />