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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />,I <br />I <br />fI <br />~ <br /> <br />\. <br /> <br />1404 <br /> <br />SAMPLING AREA DESCRIPTION AND CHARACTERISTICS <br /> <br />SAMPLING AREA LClCATION AND DESCRIPTION <br /> <br />The sampling area includes the Arkansas River valley from just east of Pueblo, Colorado <br />to the Colorado - Kansas border in Prowers County, The area is approximately 150 miles in <br />length and occupies about 400 square miles, <br /> <br />AGRICULTURAL HISTORY AND WATER USE IN THE AREA <br /> <br />The agricultural economy of the Arkansas river basin is based on irrigated and dry land <br />farming, and livestock production. The principal irrigated crops are alfalfa, corn, sorghum, winter <br />wheat, melons, onions, and dry beans, Small grains, chiefly wheat, are the principal dry land fann <br />crops. The livestock consists mostly of beef and dairy cattle although some hogs and sheep are <br />raised, <br /> <br />Several large canals for diverting water for irrigation were constructed in the late 1800's. <br />Water for irrigation is also diverted from several reservoirs. Because shortages of surface water <br />occur during years of low runoff and the timing of runoff does not coincide with irrigation <br />requirements, irrigation wells have been drilled in the valley to supplement the surface-water <br />supply, In some areas groundwater pumped from wells is the sole supply for irrigation, <br /> <br />Many of the towns and some industries in the area also obtain water from wells. Although <br />nearly all the large-capacity wells are in the valleys, small-capacity domestic and stock wells have <br />been constructed both in the valleys and on the uplands since early settlement of the region. The <br />upland areas that are without adequate surface or groundwater supplies for irrigation total about <br />250,000 acres and are used largely for dry land farming and for grazing, <br /> <br />The principal industries in the area are related to the processing of agricultural products; <br />they include vegetable processing plants, alfalfa mills, vegetable warehouses, and confined animal <br />feeding, Deposits of sand and gravel are exploited for the fabrication of concrete products and <br />building roads, <br /> <br />GEClWGY <br /> <br />The rocks that crop out in the lower Arkansas River Valley are sedimentary and range in <br />age from Early Cretaceous to Recent. The oldest rocks, which are of Early Cretaceous age, are <br />the Dakota sandstone, the Carlile shale, and the Niobrara formation, Most of the major valleys <br />contain Quaternary deposits of alluvium, terrace deposits, and dune sand, <br /> <br />The alluvium in the Arkansas River valley was deposited in a channel eroded into the <br />underlying bedrock and consists mainly of heterogeneous mixtures of clay, sand, and gravel, or <br />lenses of these materials, Pebbles, cobbles, and boulders occur as erratics, The particles generally <br />are well rounded to subrounded and range from well sorted to poorly sorted, Extensive lenses of <br />clay are present within the alluvium, These clay lenses are most prevalent in the tributary valleys <br />