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<br />N <br />ca <br />C,[) <br />I- -, <br /> <br /> <br />Table 8-118. Effective value. 01 .oil .aturation <br />extract conductivities lor levels 01 <br />.oJAnit1/ to be expected in the ble1lded <br />water 01 the Roo.eveU Irrigation Dis- <br />trict as the .alinit1/ 01 Centrat A....01Ia <br />Project UNlter increase. to 1400 mull <br />(based on an allDtmeot 0140, ()()() ac ft 01 <br />Ceotrat A....01Ia Project UNlter). <br /> <br />TDS of <br />Roosevelt <br />Irrigation <br />District. <br />Central <br />Arizona <br />Project <br />Blend <br /> <br />1169 <br /> <br />1200 <br /> <br />1225 <br /> <br />1250 <br /> <br />1275 <br /> <br />1300 <br /> <br />1325 <br /> <br />Irrigation <br />Number <br /> <br />16 <br />22 <br />29 <br />35 <br />Sprinkler <br /> <br />16 <br />22 <br />29 <br />35 <br />Sprinkler <br /> <br />16 <br />22 <br />29 <br />35 <br />Sprinkler <br /> <br />16 <br />22 <br />29 <br />35 <br />Sprinkler <br /> <br />16 <br />22 <br />29 <br />35 <br />Sprinkler <br /> <br />16 <br />22 <br />29 <br />35 <br />Sprinkler <br /> <br />16 <br />22 <br />29 <br />35 <br />Sprinkler <br /> <br />Drainage Classification <br /> <br />Well Moderate Poor <br /> <br />J.J <br />J.J <br />J.J <br />J.J <br />0.0 <br /> <br />1.2 <br />1.2 <br />1.2 <br />1.2 <br />0.0 <br /> <br />1.3 <br />1.3 <br />1.3 <br />1.3 <br />0.1 <br /> <br />1.4 <br />1.4 <br />1.4 <br />1.4 <br />0.1 <br /> <br />1.4 <br />1.4 <br />1.4 <br />1.4 <br />0.2 <br /> <br />1.5 <br />1.5 <br />1.5 <br />1.5 <br />0.2 <br /> <br />1.6 <br />1.6 <br />1.6 <br />1.6 <br />0.3 <br /> <br />3.2 <br />2.3 <br />2.0 <br />1.4 <br />0.7 <br /> <br />3.3 <br />2.4 <br />2.1 <br />1.5 <br />0.8 <br /> <br />3.4 <br />2.5 <br />2.2 <br />1.6 <br />0.9 <br /> <br />3.6 <br />2.6 <br />2.3 <br />1.7 <br />1.0 <br /> <br />3.7 <br />2.7 <br />2.4 <br />1.7 <br />J.J <br /> <br />3.8 <br />2.8 <br />2.5 <br />1.8 <br />1.2 <br /> <br />3.9 <br />2.9 <br />2.6 <br />1.9 <br />1.3 <br /> <br />6.1 <br />5.2 <br />4.9 <br />4.3 <br />3.6 <br /> <br />6.3 <br />5.4 <br />5.1 <br />4.5 <br />3.8 <br /> <br />6.5 <br />5.6 <br />5.3 <br />4.7 <br />4.0 <br /> <br />6.7 <br />5.8 <br />5.4 <br />4.8 <br />4.1 <br /> <br />6.8 <br />5.9 <br />5.6 <br />5.0 <br />4.3 <br /> <br />7.0 <br />6.1 <br />5.7 <br />5.1 <br />4.4 <br /> <br />7.2 <br />6.3 <br />5.9 <br />5.2 <br />4.6 <br /> <br />the observed data and the corresponding fitted <br />damage function. In the functional notation of Y = <br />bernx as defined earlier, b = 0.7983, e = 2.718281828, <br />m = 0.6537, and x = any level of TDS within the <br />confines of the appropriate interval. The fitted curve <br />has an RZ of 0.91. <br /> <br />A summary of the findings for the RID is <br />presented in Table 3-118. Even though annual total <br />damages are listed as $5,409, the net contribution <br />from this District is considered zero due to the TDS <br />level of present water supplies of the RID as compared <br /> <br />to present and projected salinity levels of Colorado <br />River water in the CAP system. <br /> <br />SAN CARLOS PROJECT <br /> <br />The San Carlos Project is located in the lower <br />Santa Cruz River Basin, between Florence and Casa <br />Grande, Arizona, and includes 100,000 acres of Indian <br />and non-Indian land. All project facilities are operated <br />jointly. They include: 1) Coolridge Dam and San <br />Carlos Reservoir with a capacity of 948,584 ac ft at <br />spillway level; 2) Ashurst-Hayden Diversion Dam on <br />the mainstream of the Gila River 10 miles east of <br />Florence; 3) Picacho Reservoir with a capacity of <br />18,000 ac ft used to store and regulate the delivery of <br />water; 4) Florence-Casa Grande Canal, Pima Lateral, <br />and sublaterals which serve both Indian and non- <br />Indian lands; and 5) drainage and pumping works with <br />110 producing wells. <br /> <br />Over the last 5 years the water supply has <br />consisted of approximately 70 percent surface water <br />and 30 percent groundwater. The surface water comes <br />from the natural flow of the Gila River and releases <br />from the San Carlos Reservoir, plus the erratic flows <br />of the San Pedro River. The groundwater is pumped <br />into the system from wells scattered throughout the <br />project area. During the last 20 years, pumping for <br />both project and nonproject lands has resulted in a <br />progressive lowering of the water table at an average <br />rate of 8 feet per year to its present level of <br />approximately 236 feet (Babcock, 1973). <br /> <br />Since 1934 the project has pumped an average of <br />89,000 ac ft per year, but for the last 10 years the <br />average has been approximately 75,000 ac ft per year <br />(Records of the San Carlos Irrigation Project). <br />However, the rapidly lowering water table indicates <br />that this rate of pumping cannot be maintained. In <br />addition, yearly diversions of surface water from the <br />river at the Ashurst-Hayden Dam have averaged <br />190,000 ae ft and are a reasonable expectation for the <br />future. <br /> <br />There has been no decision on how much CAP <br />water the project will receive. They have requested <br />240,000 ac ft which would enable the district to <br />irrigate the entire 100,000 acres of land with a <br />minimum of 4.0 ac ft per acre after a110wing for losses, <br />which are expected to be minimized by lining a11 canals <br />and laterals. For the purposes of this study, it seems <br />reasonable to assume an allotment of no more than <br />150,000 ac ft to the San Carlos Project. Water sources <br />for the project would then bc 150,000 ac ft, Colorado <br />River water, 190,000 ac ft Gila River water, and <br />possibly 50,000 ac ft of groundwater. <br /> <br />The salinity of the Gila River ranges from 510 <br />mg/l to around 1000 mg/l "mean annual" TDS (Water <br />Resources Data for Arizona), or an average 775 mg/l. <br />Salinity of the groundwater ranges from around 500 <br />mg/l TDS for the best wells to a high of 3,957 mg/l. <br />Records on 64 wells are summarized in Table 3-119. <br />The average of these 64 wells is 1510 mg/l TDS. If we <br />assume 50,000 ae ft of groundwater with 1500 mg/l <br /> <br />193 <br />