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Mixed Mode I,II and III analysis of multiple cracks in plane anisotropic solids by the BEM: a dislocation and point force approach
Affiliation:1. Lutsk National Technical University, Lvivska Str. 75, 43018 Lutsk, Ukraine;2. Bialystok University of Technology, Wiejska Str. 45C, 15-351 Bialystok, Poland;1. Welding and Joining Research Center, School of Industrial Engineering, Iran University of Science and Technology (IUST), Narmak 16846-13114, Tehran, Iran;2. School of Mechanical Engineering, Iran University of Science and Technology (IUST), Narmak 16846-13114, Tehran, Iran;3. Department of Mechanical and Mechatronics Engineering, University of Waterloo, 200 University Avenue West, Waterloo, ON N2L 3G1, Canada;4. Department of Mechanical Engineering, McGill University, Montreal, QC H3A 2K6, Canada;5. Department of Mechanics and Strength of Materials, Politehnica University of Timisoara, Blvd. M. Viteazu, No. 1, Timisoara 300222, Romania
Abstract:A direct boundary element method (BEM) for plane anisotropic elasticity is formulated for the generalized plane strain. It deals with the general case when the in-plane and out-of-plane deformations are coupled, including the special case when they are decoupled. The formulation is based on the distributions of point forces and dislocation dipoles following the physical interpretation of Somigliana's identity. We adopt Lekhnitskii-Eshelby-Stroh formalism for anisotropic elasticity and represent the point force and the dislocation, their dipoles, and continuous distributions systematically; the duality relations between the point force and the dislocation solutions are fully exploited. The analytical formulas for the displacement and the traction BEM are applied to the mixed mode crack analysis for multiply cracked anisotropic bodies. We extend the physical interpretation of Somigliana's identity to cracked bodies and represent the crack by the continuous distribution of dislocation dipoles. The mixed mode stress intensity factors (KI, KII and KIII) are determined accurately with the help of the conservation integrals of anisotropic elasticity.
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