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<br /> <br />. <br /> <br />'7.') <br /> <br />~- <br />~ <br />Q) <br />-...I <br /> <br />1,360,000 acre-feet delivered to Mexico upstream of Morelos Dam have <br />an annual average salinity of no more than 115 ppm plus or minus 30 <br />ppm over the annual average salinity of Colorado River waters which <br />arrive at Imperial Dam * * *." The Minute also states that "the <br />provisions which are dependent for their implementation on the Con- <br />struction of works or on other measures which require expenditure <br />of funds by the United States shall become effective upon notifica- <br />tion by the United States to Mexico of the authorization by the <br />United States Congress of said funds, which will be sought promptly." <br /> <br />After January I, 1974, or the authorization by the Congress, which- <br />ever comes later, and until the necessary measures under the <br />permanent solution are completed, the United States will have to <br />bypass all of the Well ton-Mohawk drainage (estimated at between <br />175,000 and 220,000 acre-feet/year) and replace it with water of <br />Imperial Dam quality to maintain the differential specified in <br />Minute No. 24.2. <br /> <br />The Well ton-Mohawk Irrigation and Drainage District extends from <br />about 8 miles east of the confluence of the Colorado and Gila Rivers <br />eas,terly along the Gila River Valley and on bordering mesas for <br />approximately 45 miles. <br /> <br />The Well ton-Mohawk Division of the Gila Project was authorized for <br />irrigation of 75,000 acres. In 1972, about 62,000 acres were being <br />irrigated. The troubles with the Well ton-Mohawk drainages date <br />back to the early 1900's when irrigation commenced using waters <br />diverted from the Gila River. After upstream developments, Gila <br />River flows diminished and ground water was used. An underground <br />basaltic rock barrier at the Dome Narrows near the west end of the <br />project area effectively prevents underground flow from the area. <br />As irrigation from wells continued, the constant cycling of the water <br />from the ground water reservoir to irrigation and then deep percolation <br />back to the ground water reservoir caused the water to become highly <br />saline. The first project water from the Colorado River was delivered <br />in 1952. The imported water which was not used in evapotranspiration <br />percolated underground and joined the ground water body, resulting <br />in a rising water table. This in turn dictated the construction of <br />a 'pumped drainage system from wells conveyed originally in a concrete' <br />lined channel to the Gila River about 8 miles above its confluence <br />with the Colorado River. Because of the many years of recycling <br />ground water, the drainage was pretty saline, about 6,000 ppm. This <br />has been declining as the aquifer is being refreshened with Colorado <br />River water. <br /> <br />In 1962, the Main Outlet Drain was completed, conveying the drainage <br />to the Colorado River. By 1963, the Main Outlet Drain Extension was <br />completed, permitting delivery of water above or below Morelos Dam. <br /> <br />11 <br /> <br />