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A numerical study on the anisotropism behavior of infilled joint rockmass

机译:填充节理岩体各向异性行为的数值研究

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The anisotropy of rock mass was mainly due to the conditions of the joints.In order to study the anisotropism behavior of infilled joint rockmass a mathematical model of the filling material was implemented to the two-dimensional distinct element code-UDEC using FISH language.The numerical analysis on anisotropy of the rockmass having one set of infilled joints was conducted.The results showed that the value of the cohesion of the filling material had a large influence on the test results.And the compressive stress of the sample changed a lot when the joints were infilled compared to nonfilled joints rockmass.With the increasing of the dip angle the compressive stress increased first and then decreased, and increase again at a certain dip angle.
机译:岩体的各向异性主要取决于节理条件。为了研究填充节理岩体的各向异性行为,使用FISH语言对二维离散元代码UDEC进行了填充材料的数学模型。进行了一组填充节理的岩体各向异性的数值分析,结果表明,填充材料的内聚力值对试验结果影响很大。与非填充节理岩体相比,节理是充满的。随着倾角的增加,压应力先增大然后减小,并在一定的倾角下再次增大。

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