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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 discrete 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和模型试验分析三裂纹岩石的峰值强度、应力-应变曲线及裂纹扩展特性,并验证了离散元数值模拟方法的可行性。为此,依次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强度影响较大,中间竖向裂纹对裂纹岩石的峰值强度影响较小。加载过程中裂纹尖端最先出现应力集中现象,最后形成两条呈约70°的主裂纹贯通三条预制裂纹。随着围压的增大,三裂纹岩石的单轴抗压强度先增大后减小。随着裂纹长度的增加,三裂纹岩石的单轴抗压强度不断减小。

     

    Abstract: In order to study the static damage characteristics of the tri-cracked rock, the discrete element numerical simulation software PFC2D and model tests were used to analyse the peak strength, stress-strain curve and crack propagation characteristics of the tri-cracked rock, and to verify the feasibility of the discrete element numerical simulation method. To this end, the mechanical response mechanism of the three-cracked rock under uniaxial compressive loading was analysed by sequentially varying the horizontal envelope pressure and crack length of the rock. The results of this study show that:(1) The intermediate transverse crack has a greater effect on the peak strength of the cracked rock, and the intermediate vertical crack has a smaller effect on the peak strength of the cracked rock. (2) The stress concentration at the crack tip was the first to appear during the loading process, and finally two main cracks at about 70° were formed through the three precast cracks. (3) The uniaxial compressive strength of the tri-cracked rock first increases and then decreases as the surrounding pressure increases. (4) As the crack length increases, the uniaxial compressive strength of the tri-cracked rock decreases.

     

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