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Investigation on Properties of Rock Joint in Compression Dynamic Test

机译:岩石动态压缩试验中节理特性的研究

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This paper is devoted to investigate rock joint interaction with stress waves by split Hopkinson pressure bar (SHPB) during wave propagation on dynamic loading. Taking two different specimens from the intact specimen (Series N) and the joint specimen (Series J), this study focused on three aspects: the influence of joint specimens on waveform propagation, inversion analysis of rock joint parameters using the waveform transmission coefficient, and the influence of the joint on rock specimens. With an increase in impact air pressure, compared with the intact sample, the transmittance and reflectance of joint specimens showed the opposite change rule; the closure rate change process of rock joint was converted from an exponential function to a linear function; the peak strength of the intact specimens was higher than the joint specimens at the same impact pressure above 19.58%, 21.21%, 21.56%, and 22.68% (mean values), respectively; and the strain rates (mean value) of the intact specimens were respectively 1.61, 1.31, 1.20, and 1.09 times that of the joint specimens.
机译:本文致力于研究动荷载作用下波浪传播过程中裂口霍普金森压力棒(SHPB)对岩石节理与应力波的相互作用。从完整样本(N系列)和节理样本(J系列)中选取两个不同的样本,本研究集中在三个方面:节理样本对波形传播的影响,使用波形传输系数对岩石节理参数进行反演分析和节理对岩石标本的影响。随着冲击空气压力的增加,与完整样品相比,接头样品的透射率和反射率显示出相反的变化规律。岩石节理的闭合率变化过程由指数函数转换为线性函数。在相同的冲击压力下(均值)分别高于19.58%,21.21%,21.56%和22.68%时,完整样品的峰值强度高于联合样品。完整样品的应变率(平均值)分别是关节样品的1.61、1.31、1.20和1.09倍。

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