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基于离散元法三裂纹岩石裂纹扩展特征的试验与数值研究

Experimental and numerical study of crack propagation characteristics of tri-cracked rocks based on distinct element method

  • 摘要: 为研究三裂纹岩石的静力学破坏特征,采用离散元数值模拟软件PFC2D和模型试验方法,分析三裂纹岩石的峰值应力、应力—应变曲线及裂纹扩展特性,验证离散元数值模拟方法的可行性。通过改变岩石的水平围压和裂纹长度,分析单轴压缩载荷作用下三裂纹岩石的力学响应机制。研究结果表明:中间横向裂纹对裂纹岩石的峰值应力影响较大,中间竖向裂纹对裂纹岩石的峰值应力影响较小;加载过程中裂纹尖端最先出现应力集中现象,最后形成2条约70°的主裂纹贯通3条预制裂纹;随着围压的增大,三裂纹岩石的峰值应力先增大后减小;随着裂纹长度的增加,三裂纹岩石的峰值应力不断减小。

     

    Abstract: In order to study the static damage characteristics of the tri-cracked rock, the distinct element numerical simulation software PFC2D and model tests were used to analyze the peak strength, stress-strain curve and crack propagation characteristics of the tri-cracked rock, and to verify the feasibility of the distinct element numerical simulation method. By varying the horizontal confining pressure and crack length of rock, the mechanical response mechanism of the tri-cracked rock under uniaxial compressive loading was analyzed. The results show that the intermediate transverse crack has a greater effect on the peak stress of the cracked rock, and the intermediate vertical crack has a less effect on the peak stress of the cracked rock. During the loading process, stress concentration occurs at the crack tip primarily and ultimately two main cracks of about 70° are formed through three prefabricated cracks. With the increase of confining pressure, the peak stress of the tri-cracked rock increases first and then decreases.

     

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