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Simulation Study for Interface Crack Propagation in Layered Salt Rock Subjected to Compress and Shear Load

机译:分层盐岩界面裂纹传播仿真研究,进行压缩和剪切载荷

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In order to study the effects of interlayer strength, interface strength and interface dip angle on the propagation of interface crack in layered salt rock subjected to compress and shear load, traction-separation cohesive behavior is introduced within the framework of extended finite element method (XFEM) to simulate the crack propagation. The Abaqus software is used to simulate the process of crack propagation in layered salt rock with tilted interface and under uniaxial compression. The stimulation results indicate that new cracks which deviate from original crack will appear under compress and shear load. The influences of interlayer type and interface strength on interface crack are mainly in terms of crack length. Meanwhile, the length and initiation angle of crack are both influenced by interface dip angle. The crack length in layered salt rock containing weak interlayer is larger than that of salt rock containing hard interlayer. The increase of interface strength will lead to the increased crack length, while the increased inclination of interface will shorten the length and crack initiation angle.
机译:为了研究层间强度,界面强度和接口倾角对界面盐岩中的界面裂纹传播进行压缩和剪切载荷的影响,在延长有限元方法框架内引入了牵引分离的粘性行为(XFEM )模拟裂缝传播。 ABAQUS软件用于模拟层状盐岩中的裂纹传播过程,具有倾斜界面和单轴压缩。刺激结果表明,偏离原始裂缝的新裂缝将出现压缩和剪切载荷。层间类型和界面强度对界面裂缝的影响主要是裂缝长度。同时,裂缝的长度和发起角度都受接口倾角的影响。含有弱层间层状盐岩中的裂缝长度大于含有硬层间的盐岩。界面强度的增加将导致裂缝长度的增加,而界面的倾斜度增加将缩短长度和裂纹启动角度。

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