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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 />Test resul ts of a potenti a1 impervi ous materi al source at the extreme south <br />end of the reservoir revealed a sandy silt (ML), inferior to soils from the <br />other borrow area as an impervi ous bl anket materi al. Further detai 1 s on <br />1 aboratory test resul ts for soil samp1 es from Peterson Dam and Reservoi r are <br />included in Appendix C. <br /> <br />2.3 Slope Stability of Existing Dam <br /> <br />2.3.1 Procedure <br /> <br />Static stabi 1i ty analyses of the exi sti ng embankment dam were performed usi ng <br />the Modi fi ed Bi shop 1 imi t equil ibri urn procedure. Two different embankment <br />loading conditions were analyzed. These loading conditions were: <br /> <br />A. Steady-State Seepage Conditions - The stability of the <br />downstream slope was analyzed wi th the reservoi r at <br />normal pool elevation 9510 (G.H. 32). This is the <br />reservoir level that will control the development of the <br />steady-state phreatic surface in the embankment. <br /> <br />B. Operational Conditions - The stability of the upstream <br />slope was analyzed for rapid reservoir drawdown <br />conditions from the normal pool elevation to the outlet <br />works inlet elevation. Rapid drawdown represents <br />emergency evacuation of the reservoir, or normal drainage <br />operation if the drawdown rate is on the order of 1 to 2 <br />feet per day. <br /> <br />2.3.2 Pore Pressures <br /> <br />Pore water pressures for steady-state seepage loading conditions can be <br />estimated as hydrostati c pressures below the steady-state phreati c surface. <br />The location of this phreatic surface can be estimated for homogeneous dams on <br />re1 ati ve1y impervi ous foundati ons by fol1 owi ng graphi ca1 procedures developed <br />by Casagrande ("Seepage Through Dams," Boston Society of Civil Engineers, <br /> <br />~50- <br />
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