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Extended Finite Element Method for the Analysis of Discontinuities in Rock Masses

机译:岩体间断面分析的扩展有限元方法

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摘要

The strength and deformability of rock mass primarily depend on the condition of joints and their spacing and partially on the engineering properties of rock matrix. Till today, numerical analysis of discontinuities e.g. joint, fault, shear plane and others is conducted placing an interface element in between two adjacent rock matrix elements. However, the applicability of interface elements is limited in rock mechanics problems having multiple discontinuities due to its inherent numerical difficulties often leading to non-convergent solution. Recent developments in extended finite element method (XFEM) having strong discontinuity imbedded within a regular element provide an opportunity to analyze discrete discontinuities in rock masses without any numerical difficulties. This concept is based on partition of unity principle and can be used for cohesive rock joints. This paper summarizes the mathematical frameworks for the implementation of strong discontinuities in 3 and 6 nodded triangular elements and also provides numerical examples of the application of XFEM in one and two dimensional problems with single and multiple discontinuities.
机译:岩体的强度和可变形性主要取决于节理的条件及其间距,部分取决于岩体的工程特性。直到今天,不连续性的数值分析,例如进行节理,断层,剪切平面和其他方法,将界面元素放置在两个相邻的岩石矩阵元素之间。然而,由于其固有的数值困难常常导致非收敛解,因此界面元件的适用性在具有多个不连续性的岩石力学问题中受到限制。具有强不连续性的扩展有限元方法(XFEM)的最新发展嵌入到常规元素中,为分析岩体中的离散不连续性提供了机会,而没有任何数值上的困难。该概念基于统一原则的划分,可用于粘性岩石节理。本文总结了在3个和6个点状三角形单元中实现强不连续性的数学框架,并提供了XFEM在具有一维和多个不连续性的一维和二维问题中应用的数值示例。

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