首页 | 本学科首页   官方微博 | 高级检索  
     

模拟三维裂纹问题的多尺度扩展有限元法
引用本文:王 振,余天堂. 模拟三维裂纹问题的多尺度扩展有限元法[J]. 岩土力学, 2014, 35(9): 2702-2708
作者姓名:王 振  余天堂
作者单位:河海大学 力学与材料学院,南京 210098
基金项目:国家自然科学基金项目(No. 51179063)
摘    要:
扩展有限元法模拟裂纹时独立于网格,因此该方法是目前求解裂纹问题最有效的数值方法。为了在计算代价不大的情况,实现大型结构分析中考虑小裂纹或提高裂纹附近精度,在裂纹附近一般采用小尺度单元,其他区域采用大尺度单元。提出了分析三维裂纹问题的多尺度扩展有限元法,在需要的地方采用小尺度单元。基于点插值构造了六面体任意节点单元。所有尺度单元都采用8节点六面体单元,这样六面体任意节点单元可方便有效地连接不同尺度单元。采用互作用积分法计算三维应力强度因子。边裂纹和中心圆裂纹算例分析结果表明,该方法是正确和有效的。

关 键 词:扩展有限元法  三维裂纹  六面体任意节点单元  多尺度  互作用积分法  应力强度因子  
收稿时间:2014-01-27

A multiscale extended finite element method for modeling three-dimensional crack problems
WANG Zhen,YU Tian-tang. A multiscale extended finite element method for modeling three-dimensional crack problems[J]. Rock and Soil Mechanics, 2014, 35(9): 2702-2708
Authors:WANG Zhen  YU Tian-tang
Affiliation:College of Mechanics and Materials, Hohai University, Nanjing 210098, China
Abstract:
Owing to the mesh-independent crack modeling, the extended finite element method (XFEM) is up to now most effective approach for modeling crack problem. In order to consider small cracks in the analysis of large structure or improve the accuracy around the cracks at a low cost, the fine-scale mesh is generally required around the cracks, whereas the coarse-scale mesh is used outside the cracks. A multiscale XFEM for three-dimensional crack modeling is proposed, which enables one to use a refined mesh only where it is required. The arbitrary-node hexahedron element is developed based on the point interpolation method. The eight-node hexahedron element is used for any scale element; thus the arbitrary-node hexahedron element can conveniently and effectively connect elements with different scales. The three-dimensional stress intensity factors are evaluated with the interaction integral method. Examples including an edge-crack problem and a central circle crack problem are given to illustrate the correctness and efficiency of the proposed method.
Keywords:extended finite element method(XFEM)  three-dimensional cracks  arbitrary-node hexahedron element  multiscale  interaction integral method  stress intensity factors
点击此处可从《岩土力学》浏览原始摘要信息
点击此处可从《岩土力学》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号