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Introduction
Theoretical_Background
   Method of Slices
   Bishop
   Spencer
   Morgenstern & Price
Use of Limit Equilibrium
   Choice of Geometry
   Strengths & Pressures
   Long Term Problems
   Short Term Problems
   Summary
References
Input Instructions
   Geometry
   Boundary Forces
   Pore Pressures
   Strength Parameters
   Earthquake Loading
   Iteration Control
   M-P Method
   Convergence
Examples
   Example 1
   Example 2
   Example 3i
   Example 3ii
   Example 4
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Example 4
This example uses the same slope and slip surface geometry as example 3, and shows how TSLOPE can be used to carry out an effective stress analysis of rapid drawdown, or post-earthquake stability. Note that the post-earthquake analysis can be done in terms of total stress. In all cases the determination of the pre-earthquake or pre-rapid drawdown consolidation stresses is the same; the consolidation stresses used in this example are those calculated for example 3ii.
For the effective stress analysis we can show the excess pore pressures at large strains in terms of the effective normal stress at consolidation and the or Kc ratio, in the same way we showed the undrained shear strength in example 3ii. The curves below were reduced from the same set of data as were the undrained strengths shown in example 3ii, therefore the two sets of reduced data are consistent.

Pore pressure vs Normal stress

For the post-earthquake stability analysis the excess pore pressures are determined for each slice as a function of the normal stresses at consolidation. The excess pore pressures are added to static pore pressures giving the total pore pressure at the base of each slice as shown below.

Slip Surface

The CU triaxial test data used in this example, and in example 3 was obtained from static undrained tests which followed a prior undrained cyclic loading. Therefore the strength data may be more applicable to the post-earthquake analysis than to the rapid-drawdown analysis. For dilatant materials the excess pore pressures at large strains and the undrained strengths are generally independent of the initial pore pressures prior to the static undrained loading, therefore it is reasonable to use the same data for both examples.

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