5.7 General Method of slices  

Fredlung and Krahn (1977) have shown that the equations of equilibrium can be formulated

quite generally. The formulation is the same for circular and non-circular slip surfaces (Figure 8).

Soil properties: c', ф',γ

Total normal stress:σ

Shear stress: τ

Pore water pressure: u

Failure criterion:  s=c'+(σ-u)tanф'

Mobilized shear strength: τ=s/FOS

P=σl; T=τl

T=(1/FOS)[c'l+(P-ul)tanф']

Figure 8: General method of slice

 

 

Resolving the forces vertically:

            Pcos

Rearranging ande substituting for T gives:

               P

Where

Resolving the forces horizontally:

             Tcos

Rearranging and substituting for T gives:

           

Overall moment of equilibrium about O yields:

           

Rearranging and substituting for T gives:

            FOS

For Circular slip surfaces f

           

            FOS

Overall force equilibrium:

           

           

                      

In order to solve for  and  P must be evaluated. To di this following assumptionms are made:

               Bishop (1955)

            (X/E) Constant   Spencer (1967)

            (X/E)   Morgenstern and Price (1965)

In general   and Bishop (1955) showed that  is much less sensitive to the assumption about interslice forces than