Similarity between Shock-Induced Polymorphic Transitions in the Silica System

被引:0
|
作者
Kinelovskii, S. A. [1 ]
机构
[1] Russian Acad Sci, Siberian Branch, Lavrentyev Inst Hydrodynam, Novosibirsk, Russia
关键词
silica; quartz; coesite; stishovite; fused quartz; quartz ceramic; polymorphic transformation; similarity; Hugoniot; PHASE-TRANSITIONS; MODEL; TRANSFORMATION;
D O I
10.1134/S1063784223900103
中图分类号
O59 [应用物理学];
学科分类号
摘要
A set of experimental data on the thermodynamic parameters of polymorphic transitions in the silica system is considered. Analysis of these parameters in dimensionless form is performed. A fundamental result of the analysis is that the thermodynamic parameters of all silica polymorphs after transitions are described by a single universal Hugoniot of polymorphic transition. It is shown that the two-shock model of polymorphic transformations proposed earlier by the author describes all the results obtained in the analysis. A joint consideration of the experimental data and model calculations leads to the conclusion that during a polymorphic transformation, the density of the new phase is determined from the condition that the elastic pressure components after the first shock and after the polymorphic transition are equal.
引用
收藏
页码:S273 / S279
页数:7
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