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38  Two-dimensional problems in elasticity

             so that





             and




             Also




             Substituting  as  before  in  Eq.  (1.21)  and  simplifying  by  use  of  the  equations  of
             equilibrium we have the compatibility equation for plane strain
                             (g+&)(n.x+oy)
                                                            ax
                                                            -+-  dY
                                                       1
                                                 =
                                                   --
                                                     I-u(ax      a,>
               The two equations of equilibrium together with the boundary conditions, from Eqs
             (1.7), and one of the compatibility equations (2.4) or (2.5) are generally sufficient for
             the determination of the stress distribution in a two-dimensional problem.





             The solution of problems in elasticity presents difficulties but the procedure may be
             simplified by the introduction of a stress function. For a particular  two-dimensional
             case the stresses are related  to a  single function  of x and y  such that substitution
             for  the stresses  in  terms  of  this  function  automatically  satisfies the  equations  of
             equilibrium no matter what form the function may take. However, a large proportion
             of the infinite number of functions which fulfil this condition are eliminated by  the
             requirement that the form of the stress function must also satisfy the two-dimensional
             equations of compatibility, (2.4) and (2.5), plus the appropriate boundary conditions.
               For simplicity let us consider the two-dimensional  case for which the body forces
             are  zero.  The problem  is  now  to  determine  a  stress-stress  function  relationship
             which satisfies the equilibrium conditions of








             and a  form  for  the  stress  function  giving stresses which  satisfy  the  compatibility
             equation
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