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1656_C02.fm  Page 100  Thursday, April 14, 2005  6:28 PM





                       100                                   Fracture Mechanics: Fundamentals and Applications


                       where  A is a real constant. Equation (A2.47) is equivalent to the Irwin modification of the
                       Westergaard approach if

                                                           z
                                                       2 ′() =φ  Z  − () z  A                   (A2.48)
                          Substituting Equation (A2.48) into Equation (A2.47) gives

                                                    σ xx  =  Z Re  y −  Z Im  A ′ − 2          (A2.49a)
                                                    σ yy  =  Z Re  y +  Z Im  ′                (A2.49b)
                                                    τ xy  y=− Re Z                             (A2.49c)

                       Comparing Equation (A2.49) with Equation (A2.31) and Equation (A2.46), it is obvious that the
                       Sih and Irwin modifications are equivalent, and 2A = σ .
                                                                    oxx
                          Sanford [41] showed that the Irwin-Sih approach is still too restrictive, and he proposed
                       replacing A with a complex function η(z):

                                                                     z
                                                          z
                                                      2 ′() =φ  Z  − () z  η  ()                (A2.50)
                       The modified stresses are given by
                                               σ  xx  =   y −  Z Im  y ′ + Im η  ′ − Re2  η Z Re  (A2.51a)

                                               σ  yy   Z Re  y +  Z Im  y ′ + Im η =  ′        (A2.51b)
                                               τ  xy     Z  y + Re η  ′ + Im η y=− Re          (A2.51c)


                       Equation (A2.51) represents the most general form of Westergaard-type stress functions. When
                       η(z) = a real constant for all z, Equation (A2.51) reduces to the Irwin-Sih approach, while Equation
                       (A2.51) reduces to the original Westergaard solution when η(z) = 0 for all z.
                          The function η can be represented as a polynomial of the form
                                                              M
                                                       η     ∑  α() z  m z =  m /2              (A2.52)
                                                             m=0
                       Combining Equation (A2.37), Equation (A2.50), and Equation (A2.52) and defining the origin at
                       the crack tip gives

                                                          K      M
                                                    2 ′ =  φ  I  −  ∑ α z  m/ 2                 (A2.53)
                                                           2πz      m
                                                                m = 0
                       which is consistent with the Williams [11, 38] asymptotic expansion.

                       A2.4  ELLIPTICAL INTEGRAL OF THE SECOND KIND

                       The solution of stresses in the vicinity of elliptical and semielliptical cracks in elastic solids [10, 44]
                       involves an elliptic integral of the second kind:
                                                        2 / π  c  2 − a  2
                                                                        d
                                                  Ψ=  ∫    1 −     sin φφ                       (A2.54)
                                                                      2
                                                       0       c 2
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