Page 270 - Intro to Tensor Calculus
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               Plane Strain

                   The plane strain assumption usually is applied in situations where there is a cylindrical shaped body
               whose axis is parallel to the z axis and loads are applied along the z−direction. In any x-y plane we assume
               that the surface tractions and body forces are independent of z. We set all strains with a subscript z equal
               to zero. Further, all solutions for the stresses, strains and displacements are assumed to be only functions
               of x and y and independent of z. Note that in plane strain the stress σ zz is different from zero.
                   In Cartesian coordinates the strain tensor is expressible in terms of its physical components which can
               be represented in the matrix form

                                                                           
                                              e 11  e 12  e 13   e xx  e xy  e xz
                                              e 21  e 22  e 23    =    e yx  e yy  e yz   .
                                              e 31  e 32  e 33   e zx  e zy  e zz

               If we assume that all strains which contain a subscript z are zero and the remaining strain components are
               functions of only x and y, we obtain a state of plane strain. For a state of plane strain, the stress components
               are obtained from the constitutive equations. The condition of plane strain reduces the constitutive equations
               to the form:
                                   1                                  E
                             e xx =  [σ xx − ν(σ yy + σ zz )]  σ xx =         [(1 − ν)e xx + νe yy ]
                                  E                             (1 + ν)(1 − 2ν)
                                   1
                             e yy =  [σ yy − ν(σ zz + σ xx )]         E
                                  E                        σ yy =  (1 + ν)(1 − 2ν)  [(1 − ν)e yy + νe xx ]
                                   1
                               0=   [σ zz − ν(σ xx + σ yy )]          E
                                  E                        σ zz =             [ν(e yy + e xx )]       (2.4.63)
                                  1+ ν                          (1 + ν)(1 − 2ν)
                       e xy = e yx =   σ xy
                                    E                     σ xy =  E
                                  1+ ν                          1+ ν  e xy
                       e zy = e yz =   σ yz =0
                                    E                      σ xz =0
                                  1+ ν
                       e zx = e xz =   σ xz =0             σ yz =0
                                    E
               where σ xx ,  σ yy ,  σ zz ,  σ xy ,  σ xz ,  σ yz are the physical components of the stress. The above constitutive
               equations imply that for a state of plane strain we will have

                                                σ zz = ν(σ xx + σ yy )
                                                      1+ ν
                                                e xx =     [(1 − ν)σ xx − νσ yy ]
                                                        E
                                                      1+ ν
                                                 e yy =    [(1 − ν)σ yy − νσ xx ]
                                                        E
                                                      1+ ν
                                                e xy =     σ xy .
                                                        E
               Also under these conditions the compatibility equations reduce to

                                                    2       2        2
                                                   ∂ e xx  ∂ e yy   ∂ e xy
                                                         +       =2      .
                                                    ∂y 2    ∂x 2    ∂x∂y
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