一种分析二维任意分布多裂纹的求解方法  被引量:3

A Numerical Algorithm for Solving Two-dimensional Arbitrary Distribution of Multiple Cracks

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作  者:许强[1] 杨冬升[1] 

机构地区:[1]同济大学建筑工程系,上海200092

出  处:《同济大学学报(自然科学版)》2013年第3期374-380,共7页Journal of Tongji University:Natural Science

摘  要:基于虚边界元最小二乘法求解多域组合问题的基本思想,将每一裂纹视为一对子域;并且借鉴了边界型无网格法中紧支径向基函数插值的基本思想,在每一子域的虚边界上近似构造虚拟源函数.建立了用于分析二维多裂纹问题的一种虚边界无网格最小二乘的计算格式.依据子域定义,在计算过程中无需像边界元直接法中"常规子域法"那样在裂纹面的延伸边界上额外增添附加子域,从而减少了计算量,尤其避免了由附加子域所引起的因划分单元数或配点数不足或不当而带来的计算误差.为数值论证该方法的可行性和计算精度,以及讨论任意分布多裂纹间的相互影响,分别给出了单向受拉无限大板的中心裂纹、三等长共线且相邻间距不同的裂纹算例;由数值比较可知该方法具有较高的计算精度.The sudy is based on the basic idea to solve multi- domain combinations with virtual boundary element least square method, namely, each crack can be treated as a pair of sub-domains,and the basic idea to resort to the interpolation of the compactly supported radial basis function commonly used in boundary-type meshless methods. This virtual source function is constructed approximately on the virtual boundary corresponding to each sub-domain. The computational scheme with the virtual boundary meshless least squares to analyze two-dimensional multi-crack problems is established. According to the definition about sub-domain in this paper, the added extra sub-domains on the boundary extended along the crack surface as "conventional sub-domain method" in the direct boundary element method can be neglected, thereby reducing the amount of computation. Especially, the calculation error due to inadequate number of elements or the lack of collocation points configured on the boundary of the additional sub-domains and the improper configuration is avoided. Finally, some examples, such as a single center crack, third-adjacent spacing of different length collinear cracks, are given to verify the feasibility and accuracy of the proposed numerical algorithm and the interaction between multiple cracks with arbitrary distribution is revealed. The results prove the method to be superior to other methods in terms of its accuracy.

关 键 词:虚边界 无网格 径向基函数 应力强度因子 多裂纹 

分 类 号:O346.1[理学—固体力学]

 

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