Laserfiche WebLink
<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 />I <br />I <br /> <br />25 feet and an 18-foot crest width. A cutoff trench will be constructed beneath <br />the dam to reduce seepage along the foundation. A toe drain and a blanket drain <br />will be constructed on the downstream side of the dam. Because the dam is <br />being constructed in a natural depression, the drain outfall pipe will have to <br />extend approximately 4000 feet toward Barnesville Reservoir in order to allow <br />gravity flow out of the drains. The reservoir will be designed to store up to 1600 <br />ac-ft of water. Typical details for Cornish Plains Reservoir are shown in Figure 5. <br /> <br />Barnesville Equalizer <br /> <br />Barnesville Equalizer would be located in a natural depression on the south side <br />of the North Side Extension that will be filled by gravity flow of water diverted <br />from the ditch. Barnesville Equalizer will require a dam along the south side and <br />a dam along the west side. The total length of the dams will be approximately <br />1230 feet and the maximum embankment height will be approximately 5 feet. An <br />18-foot crest width will be used to allow vehicles to travel easily along the top of <br />the dam. The reservoir will be designed to store up to 300 ac-ft of water. Inlet <br />flow to Barnesville Equalizer will be from a ditch diversion structure constructed <br />in the North Side Extension. The concrete diversion structure will be comprised <br />of a silt trap, two Obermeyer Gates, and an overflow spillway. The Obermeyer <br />Gates will be used to check flow in the ditch and to control flow into Barnesville <br />Equalizer. Both gates will have automatic controls for regulating flow in the ditch <br />and into the reservoir. The overflow spillway will serve to catch and control <br />surges in the ditch caused by localized storms. Typical details for the Barnesville <br />Equalizer are shown in Figure 6. The proposed ditch diversion structure is <br />shown in Figure 7. <br /> <br />Geotechnical Evaluation <br /> <br />Reservoir Sites <br /> <br />The soils on the site consist of fine sand overburden underlain by a layer of well- <br />graded sand and gravel. Bedrock at the Barnesville Equalizer site consists of <br />shale. At the Drury and Cornish Plains sites, the bedrock consists of sandstone. <br /> <br />The soil survey of Weld County by the Soil Conservation Service indicates that <br />the reservoir basins are dominated by Heldt Clay Loam. Renohill Clay Loam <br />appears on the north and south abutments with Longmont Clay also in the south <br />abutment area. Kim Loam emerges on the western edge of the basin. <br /> <br />The soils encountered on the site are predominantly fine sand and sand with <br />gravel. BH-2/PZ at the Drury Reservoir site showed clay from the surface to <br />approximately seven feet below grade where the material transitioned to sand <br />with gravel. In all of the other borings on the proposed sites, overburden sand <br />and sand with gravel were encountered from the surface to depths ranging from <br />approximately twenty to thirty-two feet. At the Barnesville Equalizer site, shale <br /> <br />New Cache Feasibility Study <br /> <br />10 <br />