Application of extended finite element method to study crack propagation problems of orthotropic rock mass
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Application of extended finite element method to study crack propagation problems of orthotropic rock mass
Vol. 35, Issue 4, (2014)
作者机构:
1. 中国矿业大学 深部岩土力学与地下工程国家重点实验室,江苏,徐州,221116
2. 中国矿业大学 力学与建筑工程学院,江苏,徐州,221116
作者简介:
基金信息:
DOI:
CLC:O320
Online First:18 April 2014,
Published:2014
稿件说明:
移动端阅览
SHI Fang, GAO Feng, YANG Yu-gui. Application of extended finite element method to study crack propagation problems of orthotropic rock mass[J]. 2014, 35(4).
DOI:
SHI Fang, GAO Feng, YANG Yu-gui. Application of extended finite element method to study crack propagation problems of orthotropic rock mass[J]. 2014, 35(4).DOI:
Application of extended finite element method to study crack propagation problems of orthotropic rock mass
Sedimentary rocks such as shale and sandstone are very common in the fields of oil and unconventional gas drilling; and they are often characterized by orthotropy. The extended finite element method is used for crack propagation analysis of orthotropic rock mass and a Matlab program Betaxfem2D has been developed. Asymptotic crack tip displacement fields deduced by function of complex variable method are adopted as the crack tip displacement enrichment function; and mixed mode stress intensity factors are calculated by the interaction integral (M-integral) method. Besides
a modified maximum circumferential tensile stress criterion is adopted to determine crack propagation direction. Compared with conventional finite element method (FEM)
the results show that the extended finite element method needs less DOFs and less computer resources to achieve the same calculation accuracy. The extended finite element method program developed by this paper and the conventional FEM program are used to simulate the 4-point bending test of rock sample
and both of them show the same results. Numerical experiments show that crack propagation direction angle ? varies according to an approximate sine function with a period of π with the increase of α
i.e. the angle between the orthotropic material coordinate and the space coordinate. Besides
when shear modulus and Poisson ratio remain constant; the range of the sine function shrinks with the decrease of the ratio of the elasticity moduli E1 /E2
but the phase basically remains unchanged. So
the orthotropy of rock cannot be neglected when dealing with the fracture mechanics problems of sedimentary rock.
Determination of enrichment type of node in extended finite element method
Modeling initiation and propagation of main and secondary cracks of rock under combined compression and shear loading using extended finite element method
Analysis of multiple crack growth using extended finite element method
Experimental research on potential factors and abnormal phenomenon for measuring soil-water characteristic curve
Experimental study of rock salt dissolving characteristics under triaxial stress
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