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Deformability characteristics of a rock mass under true-triaxial stress compression

机译:真三轴应力压缩作用下岩体的变形特性

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In this paper an experimental study was planned on rock mass model with three joint sets under triaxial and true-triaxial stress states to assess the influence of joint geometry and stress ratios on deformational behaviour of rock mass. The physical models were composed of three continuous orthogonal joint sets in which joint set-I was inclined at angle theta = 0 deg, 20 deg, 40 deg, 60 deg, 80 deg and 90 deg with x-axis, joint set-II was produced at staggering s = 0.5 and joint set-III was kept always vertical. Thus, rock mass models with medium interlocked smooth joints (PHI_j = 36,8 deg) were simulated under true triaxial compression (sigma_1 > sigma_2 > sigma_3). Modulus of rock mass shows anisotropy with joint inclination 9 which diminishes with increase in sigma_2/sigma_3 ratio. The rock mass at 9 = 60 deg shows the highest modulus enhancement (599.9 percent) whereas it is minimum (32.3 percent) at theta = 90 deg, Further two empirical expressions for estimation of deformation modulus were suggested based on experimental results, which were developed by incorporating two basic concepts, e.g. Janbu's coefficients and joint factor, J_f.
机译:本文计划在三轴和真三轴应力状态下的三个节理的岩体模型上进行实验研究,以评估节理的几何形状和应力比对岩体变形行为的影响。物理模型由三个连续的正交关节组组成,其中关节组I与x轴的夹角为theta = 0度,20度,40度,60度,80度和90度,关节组II为在错开的s = 0.5时产生的结果,关节组III始终保持垂直。因此,在真正的三轴压缩(sigma_1> sigma_2> sigma_3)下,模拟了具有中等互锁的光滑节理(PHI_j = 36.8度)的岩体模型。岩体模量显示出各向异性,其中关节倾角9随着sigma_2 / sigma_3比的增加而减小。 9 = 60度时的岩体显示出最高的模量增强(599.9%),而在θ= 90度时则最小(32.3%),并根据实验结果提出了两个用于估算变形模量的经验表达式,通过合并两个基本概念,例如Janbu系数和联合因子J_f。

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