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202 Fracture Mechanics: Fundamentals and Applications
By inserting the above results into Equation (4.73), we see that J = C*. Thus C* is a special case
v
of J . The latter parameter is capable of taking account of a wide range of time-dependent material
v
behavior, and includes viscous creep as a special case.
Near the tip of the crack, the stresses and pseudo-strains are characterized by J through an
v
HRR-type relationship in the form of Equation (4.33). The viscoelastic J can also be determined
through a pseudo-energy release rate:
J =− 1 ∂ a ∂ ∫ ∆ e Pd∆ e (4.75)
v
B
0
∆ e
e
where ∆ is the pseudo-displacement in the loading direction, which is related to the actual
displacement by
∆ ∆ = {Dd e } (4.76)
Finally, for Mode I loading of a linear viscoelastic material in plane strain, J is related to the
v
stress-intensity factor as follows:
2
K 1( −ν 2 )
J = I E R (4.77)
v
The stress-intensity factor is related to specimen geometry, applied loads, and crack dimensions
through the standard equations outlined in Chapter 2.
4.3.2.4 Crack Initiation and Growth
When characterizing crack initiation and growth, it is useful to relate J to physical parameters
v
such as CTOD and fracture work, which can be used as local failure criteria. Schapery [59] derived
simplified relationships between these parameters by assuming a strip-yield-type failure zone ahead
of the crack tip, where a closure stress σ acts over ρ, as illustrated in Figure 4.20. While the
m
FIGURE 4.20 Failure zone at the crack tip in a viscoelastic material. This zone is modeled by surface tractions
within 0 < x < ρ.