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                       142                                 Fracture Mechanics: Fundamentals and Applications





































                       FIGURE 3.36 Evolution of the Q parameter with deformation in two geometries. Taken from O’Dowd, N.P.
                       and Shih, C.F., ‘‘Family of Crack-Tip Fields Characterized by a Triaxiality Parameter–I. Structure of Fields.’’
                       Journal of the Mechanics and Physics of Solids,  Vol. 39, 1991, pp. 898–1015.

                       3.6.2.1 The J-Q Toughness Locus
                       Classical single-parameter fracture mechanics assumes that fracture toughness is a material con-
                       stant. With the J-Q theory, however, an additional degree of freedom has been introduced, which
                       implies that the critical J value for a given material depends on Q:
                                                                Q
                                                          J  c  J =  c  ()                       (3.71)
                       Thus fracture toughness is no longer viewed as a single value; rather, it is a curve that defines a
                       critical locus of J and Q values.
                          Figure 3.37 is a plot of critical J values (for cleavage fracture) as a function of Q [29]. Although
                       there is some scatter, the trend in Figure 3.37 is clear. The critical J increases as Q becomes more
                       negative.  This trend is consistent with Figures 3.27–3.31.  That is, fracture toughness tends to
                       increase as the constraint decreases. The Q parameter is a direct measure of the relative stress
                       triaxiality (constraint) at the crack tip.
                          Since the T stress is also an indication of the level of crack-tip constraint, a J-T failure locus
                       can be constructed [27, 28]. Such plots have similar trends to J-Q plots, but the ordering of data
                       points sometimes differs. That is, the relative ranking of geometries can be influenced by whether
                       the constraint is quantified by T or Q. Under well-contained yielding, T and Q are uniquely related
                       (Figure 3.35), but the T stress loses its meaning for large-scale yielding. Thus, a J-T toughness
                       locus is unreliable when significant yielding precedes fracture.
                          The single-parameter fracture mechanics theory assumes that toughness values obtained from
                       laboratory specimens can be transferred to structural applications. Two-parameter approaches such
                       as the J-Q theory imply that the laboratory specimen must match the constraint of the structure,
                       i.e., the two geometries must have the same Q at failure in order for the respective J  values to be
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