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首页> 外文期刊>Journal Of The South African Institute Of Mining & Metallurgy >Effect of discontinuity roughness and orientation on the parameters of the rock failure criterion under triaxial compressive stress
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Effect of discontinuity roughness and orientation on the parameters of the rock failure criterion under triaxial compressive stress

机译:不连续性粗糙度和取向对三轴压缩应力下岩石破坏标准参数的影响

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Discontinuity roughness is one of the most important parameters for understanding the mechanical characteristics of jointed rock under triaxial compressive stress. Discontinuity roughness can vary in a wide range and can play an. important role in the failure mechanism of rock under triaxial stress, particularly with varying joint orientation angles and confining pressure. In this work; the effects of discontinuity roughness on rock strength under triaxial compressive stress were investigated. Different methods were applied to create cylindrical specimens with a wide range of discontinuity roughness and orientation angles. Fifteen groups of specimens with three different types of discontinuities roughness: tooth-shaped asperity (TSA), rough undulating (RU), and smooth and planar (SP) and five orientation angles (0,30,45 60, and 90 degrees) were tested, and in total 255 triaxial compression tests were carried out on jointed specimens. For specimens having different roughness and orientation angles of 45 and 60 degrees, failure took place in the direction of the discontinuity. Tooth-shaped asperities were interlocked and broken along the discontinuities, particularly under high confining pressures. For specimens having TSA discontinuity and an orientation angle of 60 degree, sliding occurred at one side of the teeth planes under uniaxial loading. Greater discontinuity interlocking and axial strength (σ1) were observed with increasing roughness and confining pressure. The results show that the roughness and orientation angle of discontinuities have a major effect on the parameters of jointed rock failure criteria. New relationships between the failure criteria parameters, roughness, orientation angle, and uniaxial compressive strength of jointed specimens have been derived.
机译:不连续性粗糙度是了解三轴压缩应力下关节岩石机械特性最重要的参数之一。不连续性粗糙度可以在宽范围内变化,并且可以发挥作用。三轴应力下岩石故障机理的重要作用,特别是具有不同的关节取向角度和限制压力。在这项工作中;研究了三轴压缩应力下不连续性粗糙度对岩石强度的影响。施加不同的方法以产生具有宽范围的不连续性粗糙度和取向角的圆柱形样本。十五组标本,具有三种不同类型的不连续性粗糙度:齿状粗糙(TSA),粗糙起伏(Ru),平滑和平面(SP)和五个取向角(0,30,450,60和90度)测试,并且在连接样品上进行了255个三轴压缩试验。对于具有不同粗糙度和45和60度的取向角的标本,在不连续的方向上发生故障。牙齿形粗糙沿着不连续互锁并破碎,特别是在高限制压力下。对于具有TSA不连续性的标本和60度的取向角,在单轴载荷下在牙齿平面的一侧发生滑动。观察到更大的不连续性互锁和轴向强度(σ1),随着粗糙度和限制压力而增加。结果表明,不连续性的粗糙度和取向角对关节岩石破坏标准的参数具有重大影响。衍生出关节标准的故障标准参数,粗糙度,取向角度和单轴抗压强度之间的新关系。

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