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<br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />O~1774 <br /> <br />- 31 - <br /> <br />INVESTIGATIONS AND ANALYSES <br /> <br />The investigations and analyses made in formulating and <br />evaluating this project follow the established Soil Conservation <br />Service Technical Standards and requirements and conform to Federal <br />and State laws and regulations. <br /> <br />The follo",ing investigations and ol:udies are also in accord <br />l;ith agreements reached with sponsors and planning groups as <br />discussed in "Basis for Project Formulation." <br /> <br />Hydrology and Hydraulics <br /> <br />The Limon Watershed lies in the central plains of eastern <br />Colorado where the principal source of moisture for flood-producing <br />summer thunderstorms in the region is tropical maritime air from the <br />Gulf of Hexico, Unstable maritime tropical air is transported <br />into the region under the influence of a low pressure area to the <br />south of Colorado, Severe chunderstorms are initiated, either by <br />the local instability of the air mass, or along a squall line <br />preceding a cold front for~med by the ntrusion of cold Pacific air <br />from the north, <br /> <br />These convective type storms are usually of short duration <br />and high intensity and normally are liwi ted to a ten to hlenty- <br />square mile area for the intense portion of the stonn. The maximtun <br />recorded twenty-four hour precipitation amount at Limon is 3,87 inches <br />in April 25, 1935, <br /> <br />Hydrologic investigations were related to the probability of <br />various flood magnitudes and to the location and area of resulting <br />damage. This relationship supported the economic justification of <br />the reco~"ended plan. Approved standard criteria and methods were <br />used in hydrologlc development. <br /> <br />\Jatershed soil and cover conditions were evaluated from <br />detailed surveys made by the soil scientist and range conservationist. <br />The two surveys were correlated with the state soil scientist and <br />the state conservation engineer. A soil-cover complex number of 79 <br />was determined for present condition and a soil-cover complex number <br />of 77 was determined for future conditions with land treatment <br />applied, The composite soil-cover complex nurr~er of 77 ,las used <br />for determining runoff for evaluations, <br />