Assumed enhanced strain and the extended finite element methods: A unification of concepts

被引:84
作者
Borja, Ronaldo I. [1 ]
机构
[1] Stanford Univ, Dept Civil & Environm Engn, Stanford, CA 94305 USA
基金
美国国家科学基金会;
关键词
assumed enhanced strain; embedded strong discontinuity; extended finite element method; frictional crack;
D O I
10.1016/j.cma.2008.01.019
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
We present strong and weak forms of boundary-value problems for a solid with a cohesive-frictional crack. Two commonly used techniques for enhancing the finite element (FE) interpolation are considered: the assumed enhanced strain (AES) and the extended FE methods. We compare and contrast the FE approximations involved in these techniques. The AES method employs a piecewise constant interpolation of slip that is discontinuous across element boundaries. In contrast, the extended FE method interpolates slip continuously across element boundaries. Through numerical examples, we discuss the implications of these approximations to the calculated overall deformation field in the regime of infinitesimal deformation. With only a Heaviside enrichment, we find the AES method to predict larger slip (i.e., softer response) compared to the extended FE solution. We ascribe the discrepancy to the lack of higher-order crack tip enhancement in the extended FE solution. Finally, we compare the slip predicted by the above FE enhancement techniques to that calculated by classical nonlinear contact mechanics algorithm for the case where the crack traverses the element sides. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:2789 / 2803
页数:15
相关论文
共 76 条
[1]  
[Anonymous], 1998, NONLINEAR COMPUTATIO
[2]  
ARMERO F, 1995, P COMPUTATIONAL PLAS, V4, P547
[3]   Geological and mathematical framework for failure modes in granular rock [J].
Aydin, A ;
Borja, RI ;
Eichhubl, P .
JOURNAL OF STRUCTURAL GEOLOGY, 2006, 28 (01) :83-98
[4]  
Baant ZP., 1998, Fracture and size effect in concrete and other quasibrittle materials, V1st ed.
[5]  
Babuska I, 1997, INT J NUMER METH ENG, V40, P727, DOI 10.1002/(SICI)1097-0207(19970228)40:4<727::AID-NME86>3.0.CO
[6]  
2-N
[7]  
BAXEVANIS T, 2006, SECH, V1, P123
[8]  
Belytschko T, 1999, INT J NUMER METH ENG, V45, P601, DOI 10.1002/(SICI)1097-0207(19990620)45:5<601::AID-NME598>3.0.CO
[9]  
2-S
[10]   Compacting and dilating shear bands in porous rock:: Theoretical and experimental conditions [J].
Bésuelle, P .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2001, 106 (B7) :13435-13442