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Analysis of Phase Transformations in Shock-Compressed Potassium Chloride and α-Quartz in Terms of X-ray Crystallography

机译:X射线晶体学分析冲击压缩氯化钾和α-石英的相变

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摘要

X-ray diffraction patterns of shock-compressed samples of potassium chloride and α-quartz were analyzed in order to estimate the physical state of the substance in the phase coexistence region and the effect of the relaxation process on the location of experimental Hugoniot points in this region. The experimental results are consistent with the interpretation that the state of a substance on the transition curve connecting the Hugoniots of the initial phase and the high-pressure phase can be represented as a state of the substance with an incomplete relaxation process. The degree of incompleteness is determined by the ratio of the residence time of the substance at the shock front to the full time of the relaxation process.
机译:分析了氯化钾和α-石英的冲击压缩样品的X射线衍射图谱,以估计该物质在相存区域内的物理状态以及弛豫过程对实验Hugoniot点位置的影响。地区。实验结果与以下解释一致:将初始相和高压相的Hugoniots连接起来的过渡曲线上的物质状态可以表示为松弛过程不完全的物质状态。不完全程度取决于物质在冲击波前沿的停留时间与松弛过程的整个时间之比。

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