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<br />. <br /> <br />b <br /> <br />... <br /> <br />... <br /> <br />.0. <br /><, <br /> <br />" <br /> <br />I .~. , <br /> <br />- .. <br />.' ..,' <br /> <br />~ <br />1',) <br />(JI <br />CO <br /> <br />, <br /> <br />the laterals and only 20 percent of the canals should be linecl. The cost- <br />effective canal lining program is limited to Mancos Shale soil types. The <br />total canal lining program can be found in Table D-2 in Appenclix D. It should <br />be mentionecl that the Ironstone ancl M q D Canals were subjectecl to a partial <br />Level D analysis for the Mancos ancl nonMancos shale areas. <br /> <br />The optimal salinity control program for the Uncompahgre Valley portion <br />of the Lower Gunnison is included (Figure 25). At the present time, this is <br />the only portion of the area which is being consiclered for improvement by the <br />Water ancl Power Resources Service. PL 93-320 specifiecl the Lower Gunnison as <br />a potential salinity control project; however, the WPRS has apparently re- <br />strictecl their investigation to only the Uncompahgra River area. Stoppage of <br />the winter water in this case also greatly c1iminishes the importance of canal <br />, lining for control in this area. ' ,.., <br /> <br />. '1J'intah Basin <br /> <br />....... <br /> <br />'. <br /> <br />Figure 26 presents the optimal salinity control strategy for the Uintah <br />.aii"s'in inclucling the Ashley Creek and Brush Creek drainages. The canal lining <br />which is inclicated on the graph and in Table 10 is basically the canal lining <br />to be done unller the Central Utah Project and little more needs to be done. <br />Most of the rS1llSinin.~ canal lining will be in the Ashley Valley. This analy- <br />sis did not consider the consolidation of several of the canals in the Ashley. <br />Valley near Vernal, Utah, which is being proposed by the Water ancl Power <br />Resources Service. The optimal canlll lining program for the area can be found <br />in Table D-3 in Appenclix D. <br /> <br />'. , .: ", ',:> - <br />The Uintah Basin is expected to lose a cons.iderable amount of its water <br />to energy ancl relatecl development in the area because of its proximity to oil <br />shale, coal and tar sancls c1eposits. The effect or the quality of this c1eple- <br />tion cannot be determined at this time. <br /> <br />Price-San Rafael-Mucldy Creek Draina~es <br /> <br />Figure 27 illustrates the optimal cost-effective salinity control program <br />for this area. The crescent-shapecl band of irrigation development is located <br />almost entirely in Mancos Shales and has operation ancl irrigation characteris- <br />tics similar to the Lower Gunnison of Colorado. The canals in this region are. <br />also usecl for winter livestock water ancl elimination of this practice. will ' <br />recluce an estimated 30,000 Mgm of salt per Year to the Colorsdo River. <br />Table D-4 in Appenclix D tabulates the total optimal canal lining for this <br />area. <br /> <br />It is expectecl that much of the area's agricultural water rights will be <br />transferracl to energy relatecl users. Some transfers have already taken place <br />to supply cooling water for fossil fuel thermal-electric generation facili- <br />ties. In allclition, there is a large coal slurry pipeline proposed for the <br />Muclcly Creek drainage which will require substantial amount:s of water. <br /> <br />Table 11 presents the data which have been plotted in Figure 27. One <br />hunclred percent of laterals in the area should be linecl uncler existing condi- <br />tions. The on-farm program inclucles the improvement of existing surface <br /> <br />81 <br /> <br />..' <br /> <br />i.~ <br /> <br />"" <br /> <br />.,.. ~ <br /> <br />. , ~ ~. <br /> <br />..,'-. <br /> <br />,'.,> <br /> <br />"_J>,-' <br />