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<br />o <br />, ..... <br />o <br />~ <br />::".1 <br />(=.) <br /> <br />Introduction <br /> <br />Salinity has long been a major problem in the agricultural use of land in <br />the West and is considered the most significant water qual ity problem in <br />the Colorado River Basin. Salt problems are not new as ancient civiliza- <br />tions flourished with irrigation of fertile valley lands but dwind,ed as <br />silt and s~lt accumulations forced much of the land out of production. <br />About 3.4 million acres of land are irrigated in the Co"lorado River Basin <br />and nearly an irrigation farmers have to be concerned I"tith sal inity prob- <br />lems. Either they are concerned with maintaining a salt balance in the <br />root zone suitable to the crops grown or they should be concerned with the <br />quality of the return flows to the streams. In basins I"lhere mineral qual- <br />. ity of water is a problem, the users of land either affect or are affected <br />by the salt problem. But, like sediment salinity in water is a result of <br />the i nte racti on of water with soi 1 and other geo I og1 c fo rmati ons and as <br />such can be influenced by man's actions only to a degree. Maintaining high <br />standards in the use and manaqement of land and water resources is the basic <br />and long-range solution to the problem of increasing salt loading of stream- <br />flow. <br /> <br />The occurrence of salinity of the water of the Colorado River is wel, docu- <br />mented in the 1971 Environmental Protection Agency report, "The Mineral <br />Quality Problem in the Colorado River Basin" and in U. S. Department of the <br />Interior progress reports on "Quality of 14atet', Colorado River Basin." The <br />---Grand Valley is seen as one of the principal irrigated areas contributing <br />salt to the Colorado. This paper results from an examination of existing <br />information on sal inity in this area and further analysis of the role of <br />deep percolation and surface runoff from farm irrigation systems on salt <br />pick up. Because ~djacent upland drainage areas also contribute salts to <br />the Colorado River, this aspect is examined also. More reliable data and <br />analysis of many aspects of salt loading from irrigated areas and diffused <br />land sources are needed before impacts of alternative control programs can <br />be adequately determined. <br /> <br />i <br />