T-stress extraction

The T-stress represents a stress parallel to the crack faces at the crack tip. It is a useful quantity, not only in linear elastic crack analysis but also in elastic-plastic fracture studies.

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The asymptotic expansion of the stress field near a sharp crack in a linear elastic body with respect to r, the distance from the crack tip, is

σij=KI2πrfijI(θ)+KII2πrfijII(θ)+KIII2πrfijIII(θ)+Tδ1iδ1j+t1oδ1iδ2j+t2oδ2iδ2j+t3oδ2iδ3j++σ13oδ1iδ3j+(νT+Eε33)δ3iδ3j+O(r1/2)

(Williams, 1957), where r and θ are the in-plane polar coordinates centered at the crack tip. The local axes are defined so that the 1-axis lies in the plane of the crack at the point of interest on the crack front and is perpendicular to the crack front at this point; the 2-axis is normal to the plane of the crack (and thus is perpendicular to the crack front); and the 3-axis lies tangential to the crack front. to is the surface traction on the crack surfaces at the crack tip, and σ13o is a constant stress term for σ13. ε33 is the extensional strain along the crack front. In plane strain ε33=0; in plane stress the term (νT+Eε33)δ3iδ3j vanishes.

The T-stress usually arises in the discussions of crack stability and kinking for linear elastic materials. For small amounts of crack growth under Mode I loading, a straight crack path has been shown to be stable when T<0, whereas the path will be unstable and, therefore, will deviate from being straight when T>0 (Cotterell and Rice, 1980). A similar trend has been found in three-dimensional crack propagation studies by Xu, Bower, and Ortiz (1994). Hutchinson and Suo (1992) also showed how the advancing crack path is influenced by the T-stress once cracking initiates under mixed-mode loading. (The direction of crack initiation can be otherwise predicted using the criteria discussed in Prediction of the direction of crack propagation.)

The T-stress also plays an important role in elastic-plastic fracture analysis, even though the T-stress is calculated from the linear elastic material properties of the same solid containing the crack. The early study of Larsson and Carlsson (1973) demonstrated that the T-stress can have a significant effect on the plastic zone size and shape and that the small plastic zones in actual specimens can be predicted adequately by including the T-stress as a second crack-tip parameter. Some recent investigations (Bilby et al., 1986; Al-Ani and Hancock, 1991; Betegón and Hancock, 1991; Du and Hancock, 1991; Parks, 1992; and Wang, 1991) further indicate that the T-stress can correlate well with the tensile stress triaxiality of elastic-plastic crack-tip fields. The important feature observed in these works is that a negative T-stress can reduce the magnitude of the tensile stress triaxiality (also called the hydrostatic tensile stress) ahead of a crack tip; the more negative the T-stress becomes, the greater the reduction of tensile stress triaxiality. In contrast, a positive T-stress results only in modest elevation of the stress triaxiality. It was found that when the tensile stress triaxiality is high, which is indicated by a positive T-stress, the crack-tip field can be described adequately by the HRR solution (Hutchinson, 1968; Rice and Rosengren, 1968), scaled by a single parameter: the J-integral; that is, J-dominance will exist. When the tensile stress triaxiality is reduced (indicated by the T-stress becoming more negative), the crack-tip fields will quickly deviate from the HRR solution, and J-dominance will be lost (the asymptotic fields around the crack tip cannot be well characterized by the HRR fields). Thus, using the T-stress (calculated based on the load level and linear elastic material properties) to characterize the triaxiality of the crack-tip stress state and using the J-integral (calculated based on the actual elastic-plastic deformation field) to measure the scale of the crack-tip deformation provides a two-parameter fracture mechanics theory to describe the Mode I elastic-plastic crack-tip stresses and deformation in plane strain or three dimensions accurately over a wide range of crack configurations and loadings.

To extract the T-stress, we use an auxiliary solution of a line load, with magnitude f, applied in the plane of crack propagation and along the crack line:

σ11L=fπrcos3θ,        σ22L=fπrcosθsin2θ,        σ12L=fπrsinθcos2θ,
σ33L=fπrνcosθ,        σ13L=σ23L=0.

The term σ33L=0 for plane stress.

The interaction integral used is exactly the same as that for extracting the stress intensity factors:

Iint=limΓ0ΓnMqdΓ,

with M as

M=σ:εauxLI-σ(ux)auxL-σauxLux.

In the limit as r0, using the local asymptotic fields,

T=E¯[-Iint(s)f+νε33(s)-ξαΔΘ]+t2o,

where E¯=E and ξ=1 for plane stress; E¯=E/(1-ν2) and ξ=1+ν for plane strain, axisymmetry, and three dimensions; ε33 is zero for plane strain and plane stress; α is the thermal expansion coefficient; and ΔΘ is the temperature difference.

Iint(s) can be calculated by means of the same domain integral method used for J-integral calculation and the stress intensity factor extraction, which has been described in J-integral evaluation, and Stress intensity factor extraction. Iint(s) is doubled if only half the structure is modeled.