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320                               Chapter 7  Yielding and Fracture under Combined Stresses

                                     σ
                      (a) ductile     3            yield




                                                            σ
                                                             2

                                                fracture
                                               σ
                                                1
                                                                σ
                                                                 3      yield



                                    (b) brittle
                                                                                    σ
                                                                                     2


                                                                        σ
                                                                         1
                                                        fracture

            Figure 7.24 Relationships of the limiting surfaces for yielding and fracture for materials that
            usually behave in a ductile manner, and also for materials that usually behave in a brittle
            manner.


            yielding (at least for metals) is taken to be a cylinder or other prismatic shape that is symmetrical
            about the line σ 1 = σ 2 = σ 3 , such as the surfaces of Figs. 7.6 and 7.9. Limiting surfaces for fracture
            are, in general, similar to those for the modified Mohr theory (as discussed previously and illustrated
            in Fig. 7.21), although the boundaries may actually be smooth curves.
               The situation is illustrated in Fig. 7.24. For certain states of stress, the yield surface is encoun-
            tered first, whereas for others the fracture surface is encountered first. The relative dimensions of
            the two surfaces change for different materials. For normally ductile materials, fracture prior to
            yielding is not expected, except for stress states involving a large hydrostatic tension. The stress
            may be increased by varying amounts beyond yielding before fracture occurs, depending on the
            amount of hydrostatic compression. However, for normally brittle materials, there is a contrasting
            behavior, as fracture occurs prior to yielding, except for stress states involving a large hydrostatic
            compression. Thus, if a wide range of stress states are of interest for any material, it is important to
            consider the possibility that either yielding or fracture may occur first.

            7.9.2 Time-Dependent Effects of Cracks
            As already noted, normally brittle materials usually contain, or easily develop, small flaws or other
            geometric features that are equivalent to small cracks. Brittle failure generally occurs as a result
            of such cracks growing and joining. This process is often time dependent, principally because it
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