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PROJ00235
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Last modified
2/1/2011 3:47:18 PM
Creation date
10/5/2006 11:44:57 PM
Metadata
Fields
Template:
Loan Projects
Contract/PO #
C153633
Contractor Name
Greeley, City of
Contract Type
Loan
Water District
3
County
Larimer
Bill Number
HB 91-1006
Loan Projects - Doc Type
Feasibility Study
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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 />I <br />I <br /> <br />were found, Grass cover on the dike portion of the embankment was somewhat sparse. <br />In the area which was covered with riprap, there were some small bushes and trees <br />beginning to grow. These were not significant at the time of our visit. There were no <br />evidences of significant erosion damage on the upstream slope. There were a few small <br />rodent holes along the upper portion of the slope which did not appear to affect the <br />integrity of the structure. <br /> <br />5,2.2,4 Downstream Face <br /> <br />Generally, the downstream face was sparsely covered with grasses, There were no <br />indications of cracks, settlements, depressions, or bulges on the downstream face, and <br />there were no indications of significant erosion, A ditch and berm have been <br />constructed on the road across the downstream face to direct water from the <br />downstream face. The discharge end of the ditch was beginning to erode back across <br />the downstream face of the dam. There were a number of small trees growing on the <br />downstream face, These were generally about 1 to 4 feet tall, except on the extreme <br />left end of the embankment, where there were a few aspen trees about 15 to 20 feet <br />tall. <br /> <br />5.2,2.5 Seepage <br /> <br />The seepage area between about Stations 114 + 00 and 117 + 00 was dry at the time of <br />our August 1990 visit This area was generally covered with vegetation and deadwood, <br />and did not show any evidences of erosion from flowing water. Several areas of <br />seepage were observed exiting into the right side of the discharge channel near the <br />energy dlssipator and extending about 60 feet downstream, These flows were clear and <br />no evidence of partlde migration was observed, The majority of the flow was confined <br />to an area about 10 feet by 10 feel, located about 60 feet downstream of the energy <br />dissipator. This area had been covered wtth gravel and stones, and the seepage was <br />collected and measured in a V-notch weir. It is estimated that 0,5 to 1 gallon per <br />minute of water was flowing through the V-notch weir at the time of our visit. <br /> <br />5-4 <br />
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