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High-Pressure Shock Compression of Solids III pp 101–146Cite as

Effects of Shock Compression on Ceramic Materials

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Part of the book series: High-Pressure Shock Compression of Condensed Matter ((SHOCKWAVE))

Abstract

Shock wave propagation in a solid can generate conditions of ultra-high pressure (stress) sufficient to induce changes in the elastic rigidity and the crystal and electronic structures of the material. Hugoniot data are even now the most reliable (in situ and macroscopic) experimental information obtainable from shock compression research on solids. We can directly and precisely determine the pressure (stress)—density relation of condensed matter by measurement of Hugoniot parameters (shock velocity and particle velocity), because these parameters are comparable to ultrasonic data: derivative values of pressure with volume. From these data, the dynamic strength, phase transitions, equation of state (EOS), etc. can be studied. However, these experiments provide little information on microscopic effects because it is very difficult to perform in situ microscopic observations. This is due mainly to the very short duration of the shock process, during which the entropy increases and a hightemperature, compressed state that is heterogeneously deformed appears. However, shock compression research has long occupied an important position in the field of high-pressure science due to the aforementioned features, although its monopoly in generating pressures in the 100 GPa range has recently been lost due to development of diamond-anvil cells.

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  1. Tsutomu Mashimo
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    Lee Davison

  2. Department of Mechanical Engineering, University of New Mexico, Albuquerque, NM, 87131, USA

    Mohsen Shahinpoor

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Mashimo, T. (1998). Effects of Shock Compression on Ceramic Materials. In: Davison, L., Shahinpoor, M. (eds) High-Pressure Shock Compression of Solids III. High-Pressure Shock Compression of Condensed Matter. Springer, New York, NY. https://doi.org/10.1007/978-1-4612-2194-4_5

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