Shock wave reflection from a layer of a finely dispersed medium with low concentrations

K. Bashirova, C. Mikhaylenko
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Abstract

The paper investigates the propagation of a shock wave when interacting with a loosely packed granular medium. The continuous two-phase mathematical model presented in this work allows one to numerically describe the propagation of a shock wave in the channel of a shock tube, the achievement of a layer of granular filling by the shock wave, and the reflection of the wave. It was shown that the granular medium partially transmits the shock wave, but mostly corresponds to it. This reflection differs from the reflection of a shock wave from a solid wall. The nature of the reflection of the shock wave depends on the density of the granules. In particular, it has been shown that a granular medium of lower density, due to the increased mobility of individual particles, leads to some amplification of the reflected wave. It is also shown that the reflected wave in this case forms two pronounced peaks. It should be noted that the pressure passed in the layer of the granular medium, on the contrary, turns out to be the greater, the heavier the particles of the granular medium.
从低浓度的细分散介质层反射的冲击波
本文研究了激波与松散颗粒介质相互作用时的传播。本文提出的连续两相数学模型可以用数值方法描述激波在激波管通道中的传播、激波对颗粒层的填充以及激波的反射。结果表明,颗粒介质部分传递激波,但大部分与激波相对应。这种反射不同于从固体壁上反射的冲击波。冲击波反射的性质取决于颗粒的密度。特别是,已经表明,由于单个粒子的迁移率增加,密度较低的颗粒介质会导致反射波的某些放大。在这种情况下,反射波形成两个明显的波峰。需要注意的是,颗粒介质层内传递的压力,相反,颗粒介质的颗粒越重,传递的压力越大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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