Page 344 - Biaxial Multiaxial Fatigue and Fracture
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328                            S. POMMIER


              In  Fig. 6 are displayed iso-contours of the maximum principal strain component in copper
            for the same model, with the same set of orientations in uniaxial extension, shear and biaxial
            extension. As in Fig. 5, though the crystalline orientations of grains were defined to be random,
            the spatial distribution of strain in the model is not random. However, the patterns observed for
            the strain are different from those observed for the stress. There is roughly a rotation of 45"
           between the links of the maximum principal stress network and that of the maximum principal
            strain network. In uniaxial extension for example, the intensity of maximum principal strain is
            higher within links inclined of about 45" with the y axis, though the maximum principal strain
            direction is roughly  aligned with  the y  axis. This result is consistent with the experimental
            observations on TA6V (Fig. 2).

                         Aluminium              Irun
                                       -...
                                      I















                                                                  Zinc:


















            Fig.  7.  Intensity maps  of  the  maximum principal  stress component  (in  MPa)  in  uniaxial
            extension E~ = 0.1 %,  (a) aluminium, (b) iron, (c) copper, (d) zirconium, (e) titanium, (f) zinc.
              The  same  calculations  have  been  performed  for  aluminium,  iron,  copper,  zirconium,
            titanium and zinc. Similar results are obtained. If the same set of orientations is employed, the
            spatial distribution of the maximum principal stress in the three cubic crystals (aluminium, iron
            and copper) is very similar (Fig. 7. a,b,c).  The only difference is in the intensity of these links,
            which is higher  if the  elastic anisotropy of the crystal is increased. For  example, while the
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