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<br />o <br />-..J <br />w <br />N <br /> <br />CHAPTER I <br /> <br />INTRODUCTION <br /> <br />The Colorado River basin is located in the arid southwest region <br /> <br />of the United States where irrigation is the primary source of water <br /> <br />for agriculture. Since the basin is projected to reach full development <br /> <br />in the pear future, the increasing demands on the water resources <br /> <br />require either improved efficiency in the management and use of the <br /> <br />available supply or importation of new water supplies. The most <br /> <br />severe factor limiting the full development and utilization of the river <br /> <br />system is the increasing mineral pollution, or salinity. The Colorado <br /> <br />River,has alwasy been one of the most saline rivers in the country, <br /> <br />but the increasing use has resulted in about 50% salinity increase in <br /> <br />the lower basin within historic times. (6)* <br /> <br />In recent years, both <br /> <br />transbasin transfers and reservoir losses have contributed to the <br /> <br />salinity problem by depleting water from the basin which would other- <br /> <br />wise dilute the streamflows. <br /> <br />Salinity has too often been thought of as a local problem to be <br /> <br />solved with little or no consideration of its effect on other users down- <br /> <br />stream. In an irrig'l-ted agricultural area it is important to establish <br /> <br />*Numbers in parenthesis indicate references. <br />