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Practical equivalent continuum characterization of jointed rock masses

机译:节理岩体的实际等效连续体表征

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A simple practical method to characterize the strength and stiffness of jointed rock masses is presented in this paper. The empirical relations for the strength and stiffness of rock masses have been arrived based on the statistical analysis of a large amount of experimental data, which are used for representing the jointed rock mass as an equivalent continuum. The effect of joints in the rock mass is taken into account by a joint factor. These obtained relations are incorporated in a non-linear FEM code to represent the equivalent continuum analysis. The equivalent continuum model has been validated against experimental results for jointed rock masses with different joint fabric and joint orientation and also with the results from explicit modeling of joints using FEM. The developed model has also been applied to calculate the deformation around a large power station cavern in rhyolite rock at 200 m depth.
机译:本文提出了一种表征节理岩体强度和刚度的简单实用方法。基于大量实验数据的统计分析,得出了岩体强度和刚度的经验关系,这些数据用于将节理岩体表示为等效连续体。节理在岩体中的影响是由节理因素考虑的。将这些获得的关系合并到非线性FEM代码中,以表示等效的连续谱分析。已经针对具有不同节理结构和节理方位的节理岩体的实验结果验证了等效连续谱模型,并且还使用有限元方法对节理进行了显式建模。所开发的模型也已被用于计算200 m深度流纹岩中大型电站洞室周围的变形。

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