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于丙子, 陈连礼, 叶伟泉. 三维空间的节理单元[J]. 岩土工程学报, 1983, 5(3): 1-11.
引用本文: 于丙子, 陈连礼, 叶伟泉. 三维空间的节理单元[J]. 岩土工程学报, 1983, 5(3): 1-11.
Yu Bingzi, Chen Lianli, Ye Weiquan. A Three Dimensional Joint Element[J]. Chinese Journal of Geotechnical Engineering, 1983, 5(3): 1-11.
Citation: Yu Bingzi, Chen Lianli, Ye Weiquan. A Three Dimensional Joint Element[J]. Chinese Journal of Geotechnical Engineering, 1983, 5(3): 1-11.

三维空间的节理单元

A Three Dimensional Joint Element

  • 摘要: 岩体是一种被不连续结构面切割的不连续介质。为了对不连续结构面进行三维有限元分析,本文从变分原理和等参单元的概念入手推导了无厚度节理元和变厚度节理元的刚度,以供三维有限元分析之用,并用算例比较了这两种单元的精度。

     

    Abstract: Rock mass is a discontinuum separated by structural surfaces. In order to study the structural surfaces with the three dimensional finite element method, in this paper the characters of joints without thickness and joints with variant thickness are given based on the variatibnal principle and the idea of isoparametric elements.Besides, the precision of these two kinds of element is compared with calculated examples.

     

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