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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 /> <br />'I <br /> <br />I <br />-I <br /> <br />I <br /> <br />,I' <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />0':'1778 <br /> <br />- 35 - <br /> <br />Detailed investigations, including further explorations with <br />a p01;er drill, will be made at all sites prior to final design and <br />construction. Laboratory tests will be made on samples of foundation <br />materials, as well as on any materials to be used in the embankment <br />of the dams. <br /> <br />3edimentation Investigations <br /> <br />Ho previous records of sediment production were available <br />for the area included in the Limon \'Iatershed. Sedimentation <br />rates at the proposed reservoir sites were based on a reconnaissance <br />of the watershed area above these sites, as well as on the results <br />of a reservoir sediment survey made in 1955 on the Ferguson Reservoir <br />in the Big :3andy Creek Vlatershed. <br /> <br />The Ferguson Reservoir is located on Willow Gulch about 12 <br />miles west of Limon. The drainage area above the reservoir is about <br />28 square miles and consists primarily of rangeland in comparable <br />condition to that in the Limon Hatershed. This reservoir had been <br />in operation for about 30 years at the time the emergency spillway <br />washed out in 1938. The rate of sediment cleposi tion in the reservoir <br />over this 30-year period was computed to be 0,12 acre-foot annually <br />per square mile of drainage area. <br /> <br />" <br /> <br />From a reconnaissance of the Limon \,atershed, it was concluded <br />that sediment production in the watershed is generally low. There <br />are no critical sediment source areas. Sheet erosion was estimated <br />to be the main source of sediment with minor mnounts being contributed <br />by gully and streambank erosion. Most of the area has a good grass <br />cover, and streambanks and beds generally are well protected by a <br />vegetative cover. There arealso several stock ponds on each of <br />the three mair. tributaries, These ponds tend to capture some of the <br />sediment "hich otherwise would be delivered to the f loodwater- <br />'. retarding reservoir sites. <br /> <br />In computing future rates of sedimentation at the proposed <br />reservoir sites, consideration was given to the a~mount of reduction <br />in secliment production that "ill result from proposed landrreatment <br />measures to be installed in the watershed, It is estimated that <br />these llleasures will reduce the capacity required for sediment <br />storage at the proposed reservoirs by about 5 percent. Consideration <br />was given to the fact that some land treatment measures in this <br />plall \iill become effective immediately after construction, '"hile <br />others will requiye several years from the start of the project to <br />becaee effective. <br />