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Experimental and Numerical Studies on Crack Initiation and Coalescence in Sandy Mudstone with Prefabricated Cross-Flaws Under Uniaxial Compression

机译:单轴压缩下具有预制跨缺陷的砂质泥岩中裂纹启动和聚结的实验性和数值研究

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The purpose of this paper is to study the crack initiation, propagation, and coalescence of the sandy mudstone sample with two sets of prefabricated cross-flaws under uniaxial compression. This study is different from previous studies on single or multiple parallel prefabricated flaws. The prefabricated cross-flaws are characterized by the dip of the rock bridge with the direction of the main flaw ( ) and the angle between the direction of main and minor flaws ( ). The effects of these two parameters on crack initiation, propagation, coalescence, crack initiation stress, and coalescence stress are analyzed. Moreover, numerical simulation of the uniaxial compression experiments is performed using PFC2D with a flat-joint model, and the simulation results are in good agreement with those from the experiments. The results demonstrate that the dip angle of the rock bridge with the direction of the main flaw ( ) has strong effects on the crack initiation and coalescence stresses. The larger the angle between the direction of main and minor flaws , the greater the crack initiation and coalescence stresses. The crack initiation stress is reduced for the case with cross-flaws compared with that with non-cross-flaws. Meanwhile, the connection type of main flaws and the width of the crack coalescence zone are difficult to observe through the experiments and are discovered from the numerical simulation.
机译:本文的目的是研究裂纹萌生,增殖和沙质泥岩样品的聚结具有两组单轴压缩下预制横缺陷。这项研究是从单个或多个并行预制缺陷以往的研究不同。预制横缺陷由岩桥与()中的主缺陷的方向和)主要和次要缺陷的方向之间的角度(倾角表征。上裂纹萌生,扩展,聚结,裂纹萌生的应力,和聚结应力这两个参数的影响进行了分析。而且,使用颗粒流具有平坦关节模型进行单轴压缩试验的数值模拟,仿真结果与那些从实验吻合良好。该结果表明,岩桥与主缺陷()的方向的倾角对裂纹的萌生和聚结的应力强烈影响。主要和次要缺陷的方向之间的角度越大,裂纹的萌生和聚结的应力越大。裂纹萌生的应力减小为与,与非交叉的缺陷相比,交叉的缺陷的情况。同时,主缺陷的连接类型和裂纹聚结区的宽度是难以通过实验来观察并从数值模拟被发现。

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