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Experimental investigation of mechanical behavior of bedded rock salt containing inclined interlayer

机译:含倾斜夹层层状岩盐力学行为的实验研究

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摘要

Uniaxial and triaxial compression tests have been carried out on specimens of rock salt, interlayers, and composite rock salt (containing inclined interlayers). In combination with failure mechanism analysis of the stratified rock structures, the variation and impact factors of bonding stresses between the layers have been investigated, and the fracture properties and failure mechanisms of inclined bedded rock salt have been revealed. The research demonstrated that the inclined interlayer influences the deformation and fracture properties of rock salt. Due to the composite mechanical characteristics, cracks primarily initiate near the interface region, and then propagate to the interlayer and the rock salt adjacent to it. The thickness of the interlayer affects the entire performance of the composite specimen and governs the development of the local fractures. Macro-cracks tend to form more easily in the test specimens that contain a medium-thick interlayer than in the ones containing only a thin interlayer. Increasing confining pressure gradually changes the overall mechanical behaviors from brittle to more ductile at higher confining pressure. The ductile behavior is characterized by differences of strain-hardening behaviors and also the geometry of cracks at different locations in the interlayer as compared to the results of uniaxial compression tests.
机译:已经对岩盐,夹层和复合岩盐(包含倾斜夹层)的样品进行了单轴和三轴压缩试验。结合层状岩石结构的破坏机理分析,研究了层间结合应力的变化及其影响因素,揭示了层状岩盐的断裂特性和破坏机理。研究表明,倾斜的夹层会影响盐岩的变形和断裂特性。由于复合机械特性,裂纹主要在界面区域附近引发,然后传播到中间层和与其相邻的岩盐。中间层的厚度影响复合材料试样的整体性能,并控制局部裂缝的发展。含有中等厚度夹层的试样比仅含有薄夹层的试样更容易形成宏观裂纹。在较高的围压下,围压的增加会逐渐使整体机械性能从脆性变为更具延性。与单轴压缩测试的结果相比,塑性行为的特征在于应变硬化行为的差异以及夹层中不同位置处的裂纹的几何形状。

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