Stress intensity factors of square crack inclined to interface of transversely isotropic bi-material

DOI10.1016/J.ENGANABOUND.2006.07.006zbMath1195.74056OpenAlexW2055011205MaRDI QIDQ1958269

Yanyan Li

Publication date: 28 September 2010

Published in: Engineering Analysis with Boundary Elements (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/j.enganabound.2006.07.006

zbMATH Keywords

fundamental solutionsfracture mechanicsstress intensity factortransverse isotropydual boundary element methodbi-material

Mathematics Subject Classification ID

Brittle fracture (74R10) Boundary element methods applied to problems in solid mechanics (74S15) Stress concentrations, singularities in solid mechanics (74G70)

Related Items (8)

Gurtin and Murdoch's surface effect on the elastic behavior of an elastic half space subjected to body forces ⋮ Edge singularities in 3D elastic anisotropic and multi-material domains ⋮ Dual boundary element method for analyzing three-dimensional cracks in layered and graded halfspaces ⋮ Analysis of cracked transversely isotropic and inhomogeneous solids by a special BIE formulation ⋮ Three-dimensional stress intensity factors of a central square crack in a transversely isotropic cuboid with arbitrary material orientations ⋮ DDFS\(^{\text{3D}}\): a set of open-source codes leveraging hybrid 3D displacement discontinuity method and fictitious stress method to simulate fractures ⋮ Stress intensity factors of square cracks in one-layered transversely isotropic halfspaces subject to internal expansion or tensile traction ⋮ Boundary element analysis of mixed‐mode stress intensity factors in an anisotropic cuboid with an inclined surface crack

Uses Software

• BEMECH

Cites Work

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• Three-dimensional analysis of cracks in layered transversely isotropic media
• The dual boundary element method: Effective implementation for crack problems
• Effective numerical treatment of boundary integral equations: A formulation for three‐dimensional elastostatics
• Point Force Solution for an Infinite Transversely Isotropic Solid

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