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20  Basic elasticity

              In a similar manner
                                          2
                                         d r,,  - d2E,   a2E-
                                              -
                                         -- +L                                   (1.22)
                                         ayaz   az2   ay2
                                                                                 (1.23)

                If we now differentiate rx, with respect to x and z and add the result to T:.,,   differ-
              entiated with respect toy and x, we obtain




              or





              Substituting from Eqs (1.18) and (1.21) and rearranging
                                                                                 (1.24)


              Similarly

                                                                                 (1.25)

              and

                                                                                 (1.26)

                Equations (I .21)-( 1.26) are the six equations of strain compatibility which must be
              satisfied in the solution of three-dimensional  problems in elasticity.





              Although we have derived the compatibility equations and the expressions for strain
              for the general three-dimensional state of  strain we  shall be mainly concerned with
              the two-dimensional case described in Section 1.4. The corresponding state of strain,
              in  which it  is assumed that  particles of  the body  suffer displacements in  one  plane
              only, is known as plane strain. We shall suppose that this plane is, as for plane stress,
              the xy plane. Then E_, "/.uz and -yr_ become zero and Eqs (I. 18) and (1.20) reduce to
                                              dU        dV
                                         E,  = -,   E!  = -                      (1.27)
                                              dX        aY
              and
                                                 dv   du
                                           T.yy  = - + -                         ( 1.28)
                                                 ax  ay
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