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首页> 外文期刊>Latin American Journal of Solids and Structures >Experimental study on granite and the determination of its true strain-rate effect
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Experimental study on granite and the determination of its true strain-rate effect

机译:花岗岩的实验研究及其真实应变率效应的确定

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摘要

To accurately determine the true strain-rate effect of granite in split Hopkinson pressure bar (SHPB) tests, systematic experimental studies from quasi-static to dynamic loading on the same batch of granite samples is required. Therefore, firstly, splitting, uniaxial and triaxial compression tests were used to study the mechanical response of granite under different static stress conditions with the MTS rock mechanics test system, and the impact compression tests were performed at different strain-rates by the split Hopkinson pressure bar (SHPB). The test results show that the compressive strength increases with the increase of confinement, but the increase rate decreases as the confinement gets larger. The axial failure strain also increases with the increase of confinement. Failure is related to the composition and structure of granite, as well as the stress state. With increasing confinement, the sample is more constrained, the elastic limit strain becomes smaller, and the elastic modulus becomes larger accordingly. In addition, shear slip failure takes place under triaxial compression. In the dynamic compression tests, the strain-rate affects not only the strength of granite, but also the degree of fragmentation and the breaking pattern. Also, it has been found that the dynamic compressive strength enhancement of rocks under impact loading is due to the combined effects of the material strain-rate, lateral inertia and end friction; however, in SHPB tests they are coupled together and could not be separated from each other. To determine the material strain-rate effect of rocks in the SHPB tests, the dynamic compressive strength enhancement caused by the lateral inertial effect and end friction effect needs to be removed. Assuming that the effect of the material strain-rate, lateral inertia and end friction is uncoupled, the numerical simulation method has been employed to simulate the SHPB tests on granite. The true strain-rate effect of granite in SHPB tests is thus determined.
机译:为了准确地确定霍普金森分压棒(SHPB)测试中花岗岩的真实应变率效应,需要对同一批花岗岩样品进行从准静态到动态载荷的系统实验研究。因此,首先,采用分体,单轴和三轴压缩试验,通过MTS岩石力学测试系统研究花岗岩在不同静应力条件下的力学响应,并通过霍普金森分压在不同应变率下进行冲击压缩试验。酒吧(SHPB)。试验结果表明,随着围限的增加,抗压强度增加,但随着围限的增大,抗压强度减小。轴向破坏应变也随着限制的增加而增加。破坏与花岗岩的组成和结构以及应力状态有关。随着限制的增加,样品受到更大的约束,弹性极限应变变小,并且弹性模量相应变大。另外,在三轴压缩下发生剪切滑移破坏。在动态压缩试验中,应变率不仅影响花岗岩的强度,而且还影响碎裂程度和断裂模式。同样,已经发现冲击载荷下岩石的动态抗压强度的提高是由于材料应变率,横向惯性和端部摩擦的综合作用所致。但是,在SHPB测试中,它们耦合在一起并且不能彼此分离。为了确定SHPB试验中岩石的材料应变率效应,需要消除由侧向惯性效应和端部摩擦效应引起的动态抗压强度增强。假设材料应变率,横向惯性和端部摩擦的影响是不相关的,则采用数值模拟方法来模拟花岗岩的SHPB试验。因此确定了SHPB测试中花岗岩的真实应变率效应。

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