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PROJ00243
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Last modified
11/19/2009 11:43:13 AM
Creation date
10/5/2006 11:45:15 PM
Metadata
Fields
Template:
Loan Projects
Contract/PO #
C153680
Contractor Name
Santa Maria Reservoir Company
Water District
0
County
Hinsdale
Bill Number
SB 94-029
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 />Geotechnical Engineering Investigation <br /> <br /> <br /> <br />Case No. <br />1 <br /> <br />Factor of Safet <br />1. 929 <br /> <br />These factors of safety generally meet the nummum safety requirements of 1.5 for static <br />conditions and 1.2 for unusual or extreme conditions, as outlined in the Code of Colorado <br />Regulations, lICR9,9-88 and by the Bureau of Reclamation, Design Standards, Embankment <br />Dams, No 13, Chapter 4. <br /> <br />B. Seepage Evaluation <br /> <br />Method of Analyses <br /> <br />The seepage analysis was performed using the computer program ELF developed at <br />Harza. The program solves the hydraulic head distribution within a seepage domain and the <br />flow problem for the same conditions. ELF program is a modified version of FRESURF <br />written by Neuman and Witherspoon (1970). This program is a finite element procedure that <br />uses a two-step iterative cycle to determine the location of the free surface and adjusts the size <br />of the elements to the new location of the free surface at the end of each cycle. In the first <br />step, the head is equal to the elevation on the free surface and the seepage surface sections. In <br />the second step, the finite element equations are solved by imposing the rate of flow, dq = 0 <br />across the free surface sections and by setting the rate of flow across the seepage surfaces <br />equal to the amount calculated in the first step. At the conclusion of the first step, the location <br />of the free surface is adjusted to satisfy the zero pressure condition. Each step calculates the <br />head distribution within the seepage domain for a different free surface boundary condition. <br />This procedure was modified to take advantage of the fact that the head and the stream <br />function are solutions to similar differential equations by solving the flow problem in the first <br />step and the head problem in the second step of the iterative cycle. <br /> <br />Continental Dam <br /> <br />Page 14 <br />
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