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Strength and deformability of small-scale rock mass models under large confinements

机译:大约束下小尺度岩体模型的强度和变形性

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摘要

Triaxial compression tests were performed to determine the strength and deformability of small-scale rock mass models with multiple joint sets and frequencies under confining stresses up to 12 MPa. The cubical sandstone specimens (80 x 80 x 80 mm(3)) with joint sets simulated by saw-cut surfaces were compressed to failure using a true triaxial load frame. The joint frequencies ranged from 26 to 76 joints per meter. The results indicate that the Hoek-Brown criterion with two material parameters (m and s) can describe rock mass strengths as well as the three parameter criteria of Sheorey, Yudhbir and Ramamurthy-Arora. The parameter s notably decreases with increasing joint frequency, while parameter m is less sensitive to joint frequency. The confining stresses tend to enhance the effects of joint frequencies on rock mass compressive strengths. The deformation moduli in the direction normal to the joints tend to be lower than those parallel to the joints. They decrease with increasing joint frequency. Goodman's equation was modified here to allow calculation of the deformation moduli of the rock mass along the three principal directions. The modified equation can sufficiently describe the deformation moduli normal and parallel to the joints for one-joint set and three-joint set specimens under all confining stresses.
机译:进行了三轴压缩测试,以确定在12 MPa以下的约束应力下具有多个节理和频率的小规模岩体模型的强度和可变形性。使用真正的三轴载荷框架将立方砂岩标本(80 x 80 x 80 mm(3))的接头组通过锯切表面模拟,将其压缩至破坏。关节频率范围为每米26至76个关节。结果表明,具有两个材料参数(m和s)的Hoek-Brown准则可以描述岩体强度以及Sheorey,Yudbbir和Ramamurthy-Arora的三个参数准则。参数s随关节频率的增加而显着降低,而参数m对关节频率的敏感性较小。围岩应力趋于增强节理频率对岩体抗压强度的影响。在垂直于关节的方向上的变形模量往往低于平行于关节的方向上的变形模量。它们随着关节频率的增加而减少。修改了古德曼方程,以便计算沿三个主要方向的岩体变形模量。修改后的方程可以充分地描述在所有约束应力下单接头和三接头试样的法向变形和平行于接头的变形模量。

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