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首页> 外文期刊>The Journal of Strain Analysis for Engineering Design >Experimental and numerical study on crack propagation and coalescence in rock-like materials under compression
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Experimental and numerical study on crack propagation and coalescence in rock-like materials under compression

机译:压缩下岩石状材料裂纹繁殖与聚结的实验性和数值研究

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摘要

The discontinuous crack surface in a rock affects the stability of the whole rock system. The experiments in this paper were carried out by prefabricating rock-like specimens with different types of flaws, then the specimens were tested under uniaxial compression. Moreover, based on the theory of particle flow, PFC~(2D)software was used for numerical simulation, and the comparative analysis of the experimental and simulative results was carried out to obtain the crack initiation sequence, propagation phenomenon, and failure mode of rock specimens with different flaw types. The results indicated that the wing crack started at the tip of flaw and the form of crack assumed split failure, followed by shear failure caused by the secondary crack. The tensile failure degree decreases and the influence of shear failure increases with the increase of flaw angle. The wing crack and secondary initiation stress value is 35%–55% and 85%–95% of the peak stress value. Crack coalescence appeared in adjacent flaws of rock-like specimens with multiple parallel single flaws, single-cross flaws and double-cross flaws, and the coalescence phenomenon always occurs when the stress peak value is reached. With the number of flaws increasing, the splitting failure of rock-like specimens became more and more serious, the splitting failure of double cross-flaw specimen is the most serious. As for the specimen with single-cross flaw, the wing crack would be produced at the tip of the flaw with larger obliquity. The results of this paper may offer certain reference value for the study on the mechanism of rock crack.
机译:岩石中的不连续裂缝表面会影响整个岩石系统的稳定性。本文的实验是通过预制用不同类型的瑕疵预制岩样标本进行的进行,然后在单轴压缩下进行试样。此外,基于颗粒流理论,PFC〜(2D)软件用于数值模拟,进行实验性和模拟结果的比较分析,以获得岩石的裂纹启动序列,传播现象和失效模式具有不同缺陷类型的标本。结果表明,翼裂在漏洞尖端开始,裂缝的形式假设发生故障,其次是由二次裂纹引起的剪切失效。拉伸失效度降低,随着缺陷角的增加,剪切失效的影响增加。翼裂和二次起始应力值为峰值应力值的35%-55%和85%-95%。裂缝结合出现在具有多个平行单缺陷,单十字缺陷和双交叉缺陷的岩样标本的相邻漏洞中,并且在达到应力峰值时总是发生聚结现象。随着缺陷的数量增加,岩石状标本的分裂失败变得越来越严重,双交叉缺陷样本的分裂失败是最严重的。对于具有单十字缺陷的标本,翼裂将在缺陷的尖端处产生较大的倾斜。本文的结果可以为岩石裂纹机制的研究提供一定的参考价值。

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