ProductsAbaqus/StandardAbaqus/Explicit The Mises stress potential is f(σ)=q, where q=√32S:S, in which S is the deviatoric stress: S=σ-13trace(σ)I=σ-13II:(σ). The potential is a circle in the plane normal to the hydrostatic axis in principal stress space. For this function, ∂f∂σ=1q32S, and ∂2f∂σ∂σ=1q(32ℑ-12II-∂f∂σ∂f∂σ) in which ℑ is the fourth-order unit tensor. Hill's stress function is a simple extension of the Mises function to allow anisotropic behavior. The function is f(σ)=√F(σy-σz)2+G(σz-σx)2+H(σx-σy)2+2Lτyz2+2Mτzx2+2Nτxy2, in terms of rectangular Cartesian stress components, where F,G,H,L,M,N are constants obtained by tests of the material in different orientations. They are defined as F=σ202(1ˉσ222+1ˉσ233-1ˉσ211), G=σ202(1ˉσ233+1ˉσ211-1ˉσ222), H=σ202(1ˉσ211+1ˉσ222-1ˉσ233), L=32(τ0ˉτ23)2, M=32(τ0ˉτ13)2, N=32(τ0ˉτ12)2, where σ0,ˉσ11,ˉσ22,ˉσ33,ˉτ12,ˉτ23,ˉτ13 are specified by the user and τ0=σ0/√3. ˉσ and ˉτ are the values of stress that make the potential equal to σ0 if only one stress component is nonzero. For this function ∂f∂σ=1fb, where b=[-G(σz-σx)+H(σx-σy)F(σy-σz)-H(σx-σy)-F(σy-σz)+G(σz-σx)2Nτxy2Mτzx2Lτyz]. In addition, ∂2f∂σ∂σ=1f(∂b∂σ-1f2bb), where ∂b∂σ=[G+H-H-G000-HF+H-F000-G-FF+G0000002N0000002M0000002L]. |