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PROJ00318
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Last modified
10/28/2011 3:02:57 PM
Creation date
10/5/2006 11:49:29 PM
Metadata
Fields
Template:
Loan Projects
Contract/PO #
C153618
Contractor Name
Greeley, City of
Contract Type
Loan
Water District
3
County
Larimer
Bill Number
SB 87-15
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 />at the crest as revealed by the boreholes. The embankment material In the old <br />dam was wet, gray, silty sand and gralle1, poorly compacted down to the contact <br />wi th sl i ght1y weathered foundati on bedrock. The wall s of the test pi t were <br />unstable because of the high phreatic surface within the embankment. Test pit <br />PP-13, along with the bore holes, indicate the 1972 crest and downstream slope <br />modifications were accomplished by excavating the entire dam crest down to the <br />service spillway conduit elevation and backfill ing the crest and downstream <br />slope wi th materi a1 s from the reservoi r area. It appears the vegetati on may <br />not have been removed prior to flattening the downstream slope. An <br />interpretive section through the dam is shown on Figure V.2. <br /> <br />Test pit PP-12 penetrated the upstream face of the dam, perpendicular to the <br />centerl ine, beginning from the berm at approximately elevation 9490: The <br />surface of the slope was covered with a single layer, up to four feet thick, <br />of hard angular riprap. The riprap is underlain by less than a foot of dark <br />gray to brown, clayey sand with ol'ganics, presumed to be the impervious <br />blanket placed during the 1972 repairs. Below the blanket layer, the pit <br />exposed a grayish-green sequence of alternating lenses of coarse to fine sand <br />with gravel, and sandy clay with organic material as was encountered in the <br />bore holes. The walls of the pit Were unstable due to the infiltration of <br />ground water through the pervious sand layers. A third test pit, PP-4, was <br />excavated through b1 ack organi c reservoi r sediments immedi ate1y upstream of <br />the out1 et works i n1 et to a depth of 8.0 feet, at whi ch ei ther bedrock or <br />large boulders were encountered. <br /> <br />2.1.3.2 Auxiliary Spillway <br /> <br />Three test pits, PP-7, PP-9, and PP-10, were excavated upstream of the <br />auxiliary spillway. All three pits revealed basically the same condition; <br />three to ni ne feet of sandy gravel 91 aci a1 till over1yi ng sl i ght1y weathered <br />bedrock. Test pit PP-B was excavated downstream of the auxiliary spillway <br />overflow section in the grassy area where seepage occurs when the reservoir is <br />filled. The test pit encountered sandy gravel to a depth of 15 feet at which <br />point bedrock was revealed. <br /> <br />'47- <br />
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