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Constitutive relation for 2D isotropic material

Short answer

For plane stress: {σ} = (E/(1-ν^2))[[1,ν,0],[ν,1,0],[0,0,(1-ν)/2]]{ε}. For plane strain: {σ} = (E/((1+ν)(1-2ν)))[[1-ν,ν,0],[ν,1-ν,0],[0,0,(1-2ν)/2]]{ε}. Both derived from 3D Hooke's law by setting σ_z=0 or ε_z=0.

Derive the constitutive relation for a two-dimensional problem of isotropic material.

For a two-dimensional problem the constitutive law depends on whether it is plane stress (thin body) or plane strain (long body). Start from the 3D Hooke's law of an isotropic material:

εx=1E[σx−ν(σy+σz)],εy=1E[σy−ν(σx+σz)],γxy=2(1+ν)Eτxy\varepsilon_x=\frac{1}{E}[\sigma_x-\nu(\sigma_y+\sigma_z)],\quad \varepsilon_y=\frac{1}{E}[\sigma_y-\nu(\sigma_x+\sigma_z)],\quad \gamma_{xy}=\frac{2(1+\nu)}{E}\tau_{xy}

Plane stress (σz=0\sigma_z=0)

For plane stress, put σz=0\sigma_z=0:

εx=σx−νσyE,εy=σy−νσxE,γxy=2(1+ν)Eτxy\varepsilon_x=\frac{\sigma_x-\nu\sigma_y}{E},\quad \varepsilon_y=\frac{\sigma_y-\nu\sigma_x}{E},\quad \gamma_{xy}=\frac{2(1+\nu)}{E}\tau_{xy}

and εz=−ν(σx+σy)/E\varepsilon_z=-\nu(\sigma_x+\sigma_y)/E. In matrix form {ε}=[C]{σ}\{\varepsilon\}=[C]\{\sigma\}:

{εxεyγxy}=1E[1−ν0−ν10002(1+ν)]{σxσyτxy}\begin{Bmatrix}\varepsilon_x\\\varepsilon_y\\\gamma_{xy}\end{Bmatrix}=\frac{1}{E}\begin{bmatrix}1&-\nu&0\\-\nu&1&0\\0&0&2(1+\nu)\end{bmatrix}\begin{Bmatrix}\sigma_x\\\sigma_y\\\tau_{xy}\end{Bmatrix}

Invert the first two equations: from Eεx=σx−νσyE\varepsilon_x=\sigma_x-\nu\sigma_y and Eεy=σy−νσxE\varepsilon_y=\sigma_y-\nu\sigma_x, we get σx=E1−ν2(εx+νεy)\sigma_x=\dfrac{E}{1-\nu^2}(\varepsilon_x+\nu\varepsilon_y) and σy=E1−ν2(εy+νεx)\sigma_y=\dfrac{E}{1-\nu^2}(\varepsilon_y+\nu\varepsilon_x). Also τxy=Gγxy=E2(1+ν)γxy\tau_{xy}=G\gamma_{xy}=\dfrac{E}{2(1+\nu)}\gamma_{xy}. Hence

{σxσyτxy}=E1−ν2[1ν0ν10001−ν2]{εxεyγxy}\begin{Bmatrix}\sigma_x\\\sigma_y\\\tau_{xy}\end{Bmatrix}=\frac{E}{1-\nu^2}\begin{bmatrix}1&\nu&0\\\nu&1&0\\0&0&\dfrac{1-\nu}{2}\end{bmatrix}\begin{Bmatrix}\varepsilon_x\\\varepsilon_y\\\gamma_{xy}\end{Bmatrix}

i.e. {σ}=[D]{ε}\{\sigma\}=[D]\{\varepsilon\} with the plane stress matrix [D][D] above.

Plane strain (εz=0\varepsilon_z=0)

From εz=1E[σz−ν(σx+σy)]=0\varepsilon_z=\frac{1}{E}[\sigma_z-\nu(\sigma_x+\sigma_y)]=0 we get σz=ν(σx+σy)\sigma_z=\nu(\sigma_x+\sigma_y). Substituting this into the first two equations,

εx=1+νE[(1−ν)σx−νσy],εy=1+νE[(1−ν)σy−νσx]\varepsilon_x=\frac{1+\nu}{E}[(1-\nu)\sigma_x-\nu\sigma_y],\qquad \varepsilon_y=\frac{1+\nu}{E}[(1-\nu)\sigma_y-\nu\sigma_x]

Solving these two equations for the stresses, and using τxy=Gγxy\tau_{xy}=G\gamma_{xy}, gives

{σxσyτxy}=E(1+ν)(1−2ν)[1−νν0ν1−ν0001−2ν2]{εxεyγxy}\begin{Bmatrix}\sigma_x\\\sigma_y\\\tau_{xy}\end{Bmatrix}=\frac{E}{(1+\nu)(1-2\nu)}\begin{bmatrix}1-\nu&\nu&0\\\nu&1-\nu&0\\0&0&\dfrac{1-2\nu}{2}\end{bmatrix}\begin{Bmatrix}\varepsilon_x\\\varepsilon_y\\\gamma_{xy}\end{Bmatrix}

The same relation follows from the plane stress one by replacing EE with E/(1−ν2)E/(1-\nu^2) and ν\nu with ν/(1−ν)\nu/(1-\nu).

✓ Answer checked by Claude Opus 5.5 (high effort)

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