Page 223 - T. Anderson-Fracture Mechanics - Fundamentals and Applns.-CRC (2005)
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1656_C004.fm  Page 203  Thursday, April 21, 2005  5:38 PM





                       Dynamic and Time-Dependent Fracture                                         203


                       material in the failure zone may be severely damaged and contain voids and other discontinuities,
                       it is assumed that the surrounding material can be treated as a continuum. If σ  does not vary with
                                                                                     m
                       x, applying Equation (3.44) gives
                                                          J = σδ  e                              (4.78)
                                                               m
                                                           v
                             e
                       where δ  is the pseudo-crack-tip-opening displacement, which is related to the actual CTOD through
                       a hereditary integral of the form of Equation (4.77). Thus the CTOD is given by


                                                               J
                                                        δ     ( / σ = {Dd  m  )}                 (4.79)
                                                                v
                       Although σ  was assumed to be independent of x at time t, Equation (4.79) permits σ  to vary
                                                                                              m
                                m
                       with time. The CTOD can be utilized as a local failure criterion: If crack initiation occurs at δ , i
                       the J  at initiation can be inferred from Equation (4.79). If δ  is assumed to be constant, the critical
                                                                       i
                          v
                       J  would, in general, depend on the strain rate. A more general version of Equation (4.79) can be
                       v
                       derived by allowing σ  to vary with x.
                                         m
                          An alternative local failure criterion is the fracture work w . Equating the work input to the
                                                                           f
                       crack tip to the energy required to advance the crack tip by da results in the following energy
                       balance at initiation:
                                                        ∫ 0 δ i σ  m  δ d  w = 2  f              (4.80)

                       assuming unit thickness and Mode I loading. This energy balance can also be written in terms of
                       a time integral:


                                                       ∫ 0 τ ι σ m  δ ∂ t ∂  dt = 2 w f          (4.81)



                       Inserting Equation (4.79) into Equation (4.81) gives

                                                  ∫ 0 τ ι σ m  ∂{ Dd J t ∂  v  σ /  m  )} dt = 2 w f  (4.82)
                                                            (



                       If σ  is independent of time, it cancels out of Equation (4.82), which then simplifies to
                          m
                                                                 J ∂
                                                  E  R  ∫ 0 τ ι D  t  i  t ( − τ  i  ∂τ v  d , )  τ  w = 2  f  (4.83)


                                               −1
                       For an elastic material, D = E  and J  = 2w . If the failure zone is viscoelastic and the surrounding
                                                     v
                                                          f
                                              R
                       continuum is elastic, J  may vary with time. If the surrounding continuum is viscous,  D  t =  − (  t )/(  v  E τ  R  , )
                                       v
                       where t  is a constant with units of time. Inserting this latter result into Equation (4.83) and integrating
                            v
                       by parts gives
                                                        t v  −1 ∫  t i  J dt = 2 w f             (4.84)
                                                             v
                                                           0
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