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Experimental Study on Dynamic Tensile Failure of Sandstone Specimens with Different Water Contents

机译:不同水分砂岩试样动态拉伸失效的实验研究

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Understanding the effect of water saturation on dynamic failure of rocks is of great importance to tunnel excavation at water-rich coal mines and prevention of rock bursts by water injection. Dynamic Brazilian disc tests are performed to study mechanical behaviour of sandstones in this paper. The results indicate that water saturation significantly weakens the dynamic tensile strength of sandstones and increases the specimen strain at which the specimen fails. The damage degree of sandstones reduces gradually with increasing water contents. Failure of the sandstone specimen includes the crack initiation at the center of the specimen, macroscopic crack propagation, and stretch of the macroscopic crack through the specimen. In addition, parallel macroscopic crack propagation is found in the specimen with a low water content. From the observation of fracture sections, microstructures are compact in the specimen with high water contents. This is due to the swell of the kaolinite in the specimen after water saturation. The failure mechanism of microstructures is typical brittle failure in the specimen with a high water content, whereas ductile fracture is found in the specimen with a low water content. Different failure processes of microstructures lead to the differences between mechanical properties and macroscopic failure characteristics of the specimens with various water contents.
机译:了解水饱和对岩石动态失效的影响非常重视富含水煤矿的隧道挖掘,并通过注水预防岩石爆发。进行动态巴西光盘测试,以研究本文的砂岩机械行为。结果表明,水饱和度显着削弱了砂岩的动态拉伸强度,并增加了样品失效的样品菌株。随着水含量的增加,砂岩的损伤程度逐渐减少。砂岩样品的失效包括在样本的中心,宏观裂纹传播和通过样本的宏观裂缝的裂缝引发。此外,在具有低含水量的试样中发现平行的宏观裂纹繁殖。从裂缝部分的观察开始,微结构在具有高水含量的试样中紧凑。这是由于在水饱和后标本中的高岭石膨胀。微观结构的失效机理是具有高含水量的样品中典型的脆性破坏,而延性裂缝在具有低含水量的试样中发现。微观结构的不同故障过程导致具有各种水含量的样本的机械性能和宏观故障特性之间的差异。

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