Page 214 - T. Anderson-Fracture Mechanics - Fundamentals and Applns.-CRC (2005)
P. 214

1656_C004.fm  Page 194  Thursday, April 21, 2005  5:38 PM





                       194                                   Fracture Mechanics: Fundamentals and Applications


                       growing crack remains small. At the other extreme, if the crack growth is sufficiently slow that the
                       creep zone spreads throughout the structure, C* is the appropriate characterizing parameter.
                          Riedel and Rice [50] analyzed the transition from short-time elastic behavior to long-time
                       viscous behavior. They assumed a simplified stress-strain rate law that neglects primary creep:

                                                             ˙ σ
                                                         ˙ ε =  +  A σ n                         (4.40)
                                                            E

                       for uniaxial tension. If a load is suddenly applied and then held constant, a creep zone gradually
                       develops in an elastic singularity zone, as discussed earlier. Riedel and Rice argued that the stresses
                       well within the creep zone can be described by

                                                               1
                                                              n  +1
                                                     σ     Ct()   σ =  ˜  n (, )               (4.41)
                                                                      θ
                                                      ij
                                                           AI r   ij
                                                            n 
                       where C(t) is a parameter that characterizes the amplitude of the local stress singularity in the creep
                       zone; C(t) varies with time and is equal to C* in the limit of long-time behavior. If the remote load
                       is fixed, the stresses in the creep zone relax with time, as creep strain accumulates in the crack-tip
                       region. For small-scale creep conditions, C(t) decays as 1/t according to the following relationship:
                                                             K ( −ν 2 )
                                                              2
                                                                1
                                                       Ct() =  I                                 (4.42)
                                                              n   E ( +1  t )
                       The approximate size of the creep zone is given by

                                                                         2
                                                                      n
                                                           2
                                                         I
                                            r  θ  t (, ) =  1   K     n  A ( +1  I  n E)  t    n  −1  r  θ  n ˜ (, )  (4.43)
                                                                ( π 
                                            c
                                                   2 π  E     21 − ν  2 )    c
                       At θ = 90°, ˜ r c  is a maximum and ranges from 0.2 to 0.5, depending on n. As r  increases in size,
                                                                                       c
                       C(t) approaches the steady-state value C*. Riedel and Rice defined a characteristic time for the
                       transition from short-time to long-time behavior:
                                                             2
                                                            K 1−(  ν 2 )
                                                        t =  I                                  (4.44a)
                                                         1  n     C +
                                                           (    E 1)  *
                       or

                                                               J
                                                         t =                                    (4.44b)
                                                         1   n  +
                                                            (    C 1) *
                       When significant crack growth occurs over time scales much less than t , the behavior can be
                                                                                   1
                       characterized by K , while C* is the appropriate parameter when significant crack growth requires
                                      I
                       times >> t . Based on a finite element analysis, Ehlers and Riedel [51] suggested the following
                               1
                       simple formula to interpolate between small-scale creep and extensive creep (short- and long-time
                       behavior, respectively):

                                                       Ct() ≈  C *  t  1  +  1                 (4.45)
                                                                t   
   209   210   211   212   213   214   215   216   217   218   219