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HYDRO28780
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Last modified
8/24/2016 8:47:54 PM
Creation date
11/20/2007 9:50:36 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1979195
IBM Index Class Name
Hydrology
Doc Date
2/24/2004
Doc Name
Design Technical Memorandum
From
GEI Consultants, Inc.
To
Denver Water
Media Type
D
Archive
No
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Hazeltine/Road Runners Rest IllBrinkmann-Woodward Gravel Pits Lining Project -Design Technical Memorandum <br />Denver W ater <br />August 2003 <br />Section 3 -Slope Stability Analyses <br />3.1 General <br />GEI performed two-dimensional static slope stability analyses to estimate the location of the <br />failure surface for the selected factor of safety (FOS) for the interior (reservoir side) and <br />exterior (Bull Seep and South Platte River sides) slopes along the alignment of the cutoff wall. <br />The purpose of this analysis was to identify the zone where the cutoff wall should be located to <br />provide an acceptable FOS against damage associated with slope movement as shown on <br />Figure 3.1. We used the computer program STABLSM (Purdue, 1998) to perform the iterative <br />task of identifying a potential failure surface. We used the modified Bishop method to perform <br />these limit equilibrium calculations. <br />3.2 General Assumptions and Slope Stability Design Criteria <br />Reclamation and permanent design of side slopes of the reservoir is not part of the scope of this <br />phase of the project, and analysis of permanent slopes will be conducted by Denver Water <br />during subsequent phases of the project. GEI conducted the slope stability analyses to select <br />the horizontal alignment of the soil-bentonite wall and identify areas where earthwork will be <br />required to support the soil-bentonite cutoff wall until permanent reclamation can be <br />completed. <br />The stability of a slope in engineering practice is typically indexed to a FOS against failure <br />determined using limit equilibrium concepts and the method of slices. In the limit equilibrium <br />analysis, the FOS is the relationship between the resisting forces (shear strength of the soil <br />and/or bedrock) and the driving forces (weight of soil and other loads) satisfying either <br />moment or force equilibrium, or both. A FOS of less than 1.0 indicates instability. <br />The design of the reservoir side slopes should include a FOS larger than 1.0 to account for: 1) <br />variations in subsurface conditions, 2) uncertainties associated with interpreting limited data <br />(i.e., estimating subsurface stratigraphy between widely spaced borings and material properties <br />from limited laboratory tests), and 3) the economic cost and operational impact of slope failure. <br />Our stability analyses were based on the following general assumptions and design criteria: <br />The gravel pits would be mined to the top of bedrock and the bottom of the reservoir <br />will be at the top of bedrock. Top of bedrock is generally around El. 5000, except for <br />the eastern part of the reservoir where the top of bedrock is at about El. 4968. <br />GEI Consultants, Inc. 8 o?osoo?-ov-=i in-uvdn~ro~z~y~r>, <br />
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