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<br />" <br /> <br />~' <br /> <br />I <br />,. <br /> <br />. <br /> <br />G) Ict<g7 <br /> <br />WELLTON-!10HAWK ONFA.Rl1 IRRIGATION IMPROVE~.ENT PROGRAH <br /> <br />HISTQRc' <br /> <br />The Well ton-Mohawk Irrigation and Drainage District is located <br />i~ Yuma County in southwestern Arizona. The west e~d of the OlS- <br />trict lies about 7 miles east of the confluence of the Gila an2 <br />Colorado Rivers. The district is bordered on the west by the Gila <br />Mountains and extends east 40 miles to the Moha~k Mountains. <br /> <br />Irrigation began in the area before the turn of the centu~y <br />with water diverted from the Gila River. As upstream development <br />along the Gila River occurred, flows in the river gradually dimin- <br />ised. In 1915, the farmers started using water from pumped ~ells. <br />The ground water gradually became saline and lands went out Qf <br />production. <br /> <br />Facilities for <br />water were included <br />was to serve 75,000 <br /> <br />transport and distribution of Colorado <br />in the 1947 Gila Reauthorization Act. <br />acres of land in the district. <br /> <br />River <br />The watel:' <br /> <br />Colorado River water was first delivered to the district in <br />1952. As a result of the irrigation project, the water table rose <br />rapidly. Drainage problems developed and drainage wells were in- <br />stalled in 1957. This drainage water was pumped into the Gila River <br />channel. The drainage water was initially quite saline, averaging <br />about 6,000 parts per million (ppm) of total dissolved solids. The <br />concrete-lined Wellton-Mohawk majn conveyance channel was constructed <br />in the early 196005 to carry the ,pumped drainage water to the Colorado <br />River. These flows were d~livered to Mexico at the International <br />Boundary in accordance with the 1944 water treaty. <br /> <br />The average annual salinity of the water delivered to Mexico <br />increased from about 800 ppm of total dissolved solids in 1961 to <br />nearly 1,500 ppm in 1962. This increase was due partly to the dis- <br />charge from the We11ton-t1oha'Nk District. In addition, there '....as a <br />marked decrease in other Coloradc Rive~ flows reaching Mexico. <br /> <br />Minutes No. 218 and 241 of the Internatior.al Boundary and Water <br />Commission were int€rim solutions that resulted in a reduction of <br />average annu21 salini~y of the Colo~~dG River at Imge~ial D2m to <br />l~:':C; .-::~;:-[ L""! ~~i7~, Cn ';12q:...:::::;: 30: 1372, th~ PresioEnt of the iJ,~it'2d <br /> <br />---, <br />.. - - <br />-,. - -.. - ~- <br /> <br />" . - <br />-. - . -' -,~ - -- <br /> <br />-.-'.-"--".""'- <br />-,- --. - . --- <br /> <br />. . ~ - <br />.- -- <br /> <br />_,:.. 2~: ':;;:::'=:-. <br /> <br />:::!:-':i:..3.;:;- <br /> <br />llshed ~ "p~rrn2n~n~ an~ deiini~ive solution to ~he internatlonal problem <br /> <br />.:- ~ ~ ~ ~ " ..... , <br />... --.. - - <br /> <br />'::.~-,:::; ::-:"::'~-:C:lr:.8." <br /> <br />-2- <br />