Strain rate decomposition
An additive strain rate decomposition is assumed:
where dε is the total strain rate, dεel is the elastic strain rate, and dεpl is the inelastic (plastic) strain rate.
ProductsAbaqus/StandardAbaqus/Explicit The Mohr-Coulomb failure or strength criterion has been widely used for geotechnical applications. Indeed, a large number of the routine design calculations in the geotechnical area are still performed using the Mohr-Coulomb criterion. The Mohr-Coulomb criterion assumes that failure is controlled by the maximum shear stress and that this failure shear stress depends on the normal stress. This can be represented by plotting Mohr's circle for states of stress at failure in terms of the maximum and minimum principal stresses. The Mohr-Coulomb failure line is the best straight line that touch es these Mohr's circles (Figure 1). Thus, the Mohr-Coulomb criterion can be written as τ=c-σtanϕ,
where τ is the shear stress, σ is the normal stress (negative in compression), c is the cohesion of the material, and ϕ is the material angle of friction. ![]() From Mohr's circle, τ=scosϕ,σ=σm+ssinϕ.
Substituting for τ and σ, the Mohr-Coulomb criterion can be rewritten as s+σmsinϕ-ccosϕ=0,
where s=12(σ1-σ3)
is half of the difference between the maximum and minimum principal stresses (and is, therefore, the maximum shear stress) and σm=12(σ1+σ3)
is the average of the maximum and minimum principal stresses (the normal stress). Thus, unlike the Drucker-Prager criterion, the Mohr-Coulomb criterion assumes that failure is independent of the value of the intermediate principal stress. The failure of typical geotechnical materials generally includes some small dependence on the intermediate principal stress, but the Mohr-Coulomb model is generally considered to be sufficiently accurate for most applications. This failure model has vertices in the deviatoric stress plane (see Figure 2). ![]() |