2008
DOI: 10.1016/j.ijsolstr.2007.07.020
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T-stress evaluation for slightly curved crack using perturbation method

Abstract: A general formulation for evaluating the T-stress at crack tips in a curved crack is introduced. In the formulation, a singular integral equation with the distribution of dislocation along the curve is suggested. For a slightly curved crack, a small parameter is generally assumed for the crack configuration. By using the assumption for the small parameter, the perturbation method is suggested and it reduces the singular integral equation into many successive singular integral equations. If the cracked plate ha… Show more

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Cited by 14 publications
(5 citation statements)
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“…7 , Fig. 8 ) and the relatively less penetrative field relationship, it can be implied that these structures are related to upper crust deformation process (s) which are related to secondary faults [ 30 ] and are developed by local stress perturbations [ [30] , [31] , [32] ] in the process of rifting caused by active/and far field stresses. Stress perturbations, and hence changes of positions of the principal stress axis σ 1 can occur as a result of pre- and post-seismic stress states differences [ [32] , [33] , [34] ] and pore pressure changes [ 35 ].…”
Section: Discussionmentioning
confidence: 99%
“…7 , Fig. 8 ) and the relatively less penetrative field relationship, it can be implied that these structures are related to upper crust deformation process (s) which are related to secondary faults [ 30 ] and are developed by local stress perturbations [ [30] , [31] , [32] ] in the process of rifting caused by active/and far field stresses. Stress perturbations, and hence changes of positions of the principal stress axis σ 1 can occur as a result of pre- and post-seismic stress states differences [ [32] , [33] , [34] ] and pore pressure changes [ 35 ].…”
Section: Discussionmentioning
confidence: 99%
“…Maerten et al, 2002) developed by local stress perturbations (e.g. Maerten et al, 2002;Chen et al, 2008;Feng et al, 2020) in the process of rifting caused by active / and far field stresses. Stress perturbations, and hence changes of positions of the principal stress axis σ 1 can occur as a result of pre-and post-seismic stress states differences (e.g.…”
Section: Table 1 -mentioning
confidence: 99%
“…The level set method of Osher et al [17] also provides an efficient way to carry out nodal enrichment, even in three -dimensional problems (as demonstrated by Moes et al [18], Gravouil et al [19] and Sukumar [20][21]). A couple of other researchers have employed analytical methods to propose a closed form solution for some particular shapes of cracks such as the arc crack and the cusp crack [22][23][24][25][26]. Budyn et al [27] also presented an XFEM formulation based on a triangular six-noded element to analyze cracked plane strain or plane stress problems.…”
Section: Introductionmentioning
confidence: 99%