Page 465 - Biaxial Multiaxial Fatigue and Fracture
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Micmcmck Propagation  Under Non-Proportional Multiaxial Alternating Loading   449


           N,  is the number of cycles to failure, while C and z are material parameters. N,  is defined by
          the point of time when the crack has penetrated the wall. In our facility we are monitoring the
          gradient of the inner pressure and the outer pressure. If we have a wall penetrating cracking the
          gradient of the inner pressure various very quickly and the outer pressure increases. So we can
          determine the point of time of the wall-penetrating of the crack and out of this N,.
             it  can  be  seen  that  for different  phase  shifts  the  material  parameters  are  also  different.
          Furthermore, it can be observed that an increasing phase shift causes a higher life at the same
          equivalent  load.  This  indicates  that  the  failure  process  is  not  controlled  by  shear  stress
          exclusively.  Hydrostatic  stress  plays  an  important  role.  Similar  results  were  observed  by
          Mouguerou [6] and Ogata [7]. For a phase shift of 0 degree the hydrostatic stress reaches its
          maximum, while for a phase  shift of  180 degrees the hydrostatic stress is minimum.  If  the
           loading amplitudes, at a phase shift of  180 degrees have the same value, the hydrostatic stress
          even  vanishes.  It  may  therefore  be  supposed  that  a  higher  hydrostatic  stress  at  the  same
          equivalent stress reduces the lifetime.
             To obtain a correlation between the multiaxial experiments with different phase shifts on the
          one hand and the uniaxial reference experiments on the other hand, a multiaxiality factor  f,
          was introduced. Therewith, the Manson-Coffin relation was modified as follows:




           C'  and  z'  are  material  parameters  which  are  extracted  from  uniaxial  fatigue  experiments
          (C'  = 12.63,z' = -0.3395).fm is  a function of  the  multiaxial hydrostatic  stress  range  Aorltiaxia'
          referring  to  the  uniaxial  hydrostatic  stress  range  AoYa,  arising  for  the  same  equivalent
          plastic strain range A&;:





                           with  ~~~ltiaxial                                     (5)
                                      = 3[ max Trace(5) - min Trace(5)l






           From the uniaxial deformation data'determined, it results u = 425.7 and p = 0.2.
             The multiaxiality factors out of the different multiaxial experiments were investigated with
           Eq. (3). When plotting these multiaxiality factors over the ratio  AO~"~"~~' / bounimia' it can be
           seen that a linear function could describe this relation quite well:





           with  h=1.396  and  k=0.396. Thus it  results a  rather good  description  of  the lifetime by  the

           modified Manson-Coffin relation (Eq. 3). In Fig. 7 the ratio   is plotted over the number
           of cycles to failure on a double logarithmic scale. It can be seen that the results lie within an
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