首页> 外文期刊>Arabian Journal for Science and Engineering. Section A, Sciences >Numerical Simulation of the Failure Process and Mechanical Behavior of a Rock Material with Nonpersistent Cracks Under Compression
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Numerical Simulation of the Failure Process and Mechanical Behavior of a Rock Material with Nonpersistent Cracks Under Compression

机译:非持久性裂纹岩石材料受压破坏过程及力学行为的数值模拟

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The failure process and mechanical behavior of a rock material with nonpersistent cracks under compression are a hot and difficult issue in rock mechanics study. On the basis of the previous research, the initial constitutive models using the $$hbox {FLAC}^mathrm{3D}$$ FLAC 3 D code are adopted for determining the failure characteristic of the rock material with nonpersistent cracks under compression. The elastic–brittle and null models are used to simulate the mechanical behavior of the rock and the crack elements, respectively. Secondly, to simulate the crack propagation mode in the rock material, the superfine element division method is used to mesh the rock material model. As a result, the crack propagation path and the stress–strain curve of the rock material under compression are well simulated. In the adopted model, the effect of crack length, dip angle, interval, overlap distance, number and confining pressure on the crack propagation path and the rock material mechanical behavior under compression has all been taken into consideration. The calculations of the numerical model show that the uniaxial compressive strength decreases with increasing crack length, the occurrence position and the propagation path of wing. The secondary cracks vary greatly with different crack lengths and dip angles. With the increase in the crack interval and overlap distance, the interaction among the cracks decreases gradually with an increase in the compressive strength of the samples. The rock material compressive strength decreases with increasing crack number and increases with confining pressure. Finally, the validation of the simulation result is verified with the experimental model tests.
机译:在压缩作用下具有非持久性裂纹的岩石材料的破坏过程和力学行为是岩石力学研究中的热点和难点。在先前研究的基础上,采用使用$$ hbox {FLAC} ^ mathrm {3D} $$ FLAC 3 D代码的初始本构模型来确定具有非持久性裂纹的岩石材料在压缩下的破坏特性。弹性-脆性模型和零模型分别用于模拟岩石和裂缝单元的力学行为。其次,为了模拟岩石材料中的裂纹扩展模式,使用超细单元划分方法对岩石材料模型进行网格划分。结果,很好地模拟了岩石材料在压缩状态下的裂纹扩展路径和应力-应变曲线。在所采用的模型中,已经考虑了裂纹长度,倾角,间隔,重叠距离,数量和围压对裂纹扩展路径和受压岩石材料力学行为的影响。数值模型的计算表明,单轴抗压强度随着裂纹长度,机翼的出现位置和传播路径的增加而减小。次级裂纹随裂纹长度和倾角的不同而有很大差异。随着裂纹间距和重叠距离的增加,裂纹之间的相互作用随着样品抗压强度的增加而逐渐减小。岩石材料的抗压强度随裂纹数的增加而降低,随围压的增加而增加。最后,通过实验模型测试验证了仿真结果的有效性。

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