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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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Bishop's Simplified Method

In Bishop's Simplified Method the effect of the inter-slice force is eliminated by assuming that the vertical component of the inter-slice forces is zero. The forces on a typical slice are shown in Figure 3 and consist of:

  1. the slice weight, W
  2. the pseudo-static seismic force, kW, in which k is the seismic coefficient
  3. the pore pressure force, U ( = u . l )
  4. the effective normal force on base, P'
  5. the mobilized shear force, Shear force equation
  6. the resultant of boundary forces perpendicular and parallel to the top of the slice, N and M
  7. the horizontal slide forces, En and En+1

Figure 3
Figure 3 Force polygon for Bishop's Simplified Method.

Solving force equilibrium in the vertical direction, thereby eliminating the side forces, yields;

Equation 4 (4)

or rearranging and solving for P':

Equation 5 (5)

Once the normal force at the base of each slice is found, overall moment equilibrium yields and implicit expression for the factor of safety:

Equation 6 (6)

where yk, aN and aM are appropriate moment arms and is given by

Equation 7 (7)

Whitman and Bailey (1967) point out a rare numerical difficulty with this method. When is negative the possibility exists that the denominator in Equation 5 could be negative, or worse, zero. When this occurs, a warning is printed and the resisting moment is set to zero.

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