Quartz structure transformation under a shock wave

被引：0
|
作者：
V. I. Vettegren’
V. S. Kuksenko
I. P. Shcherbakov
R. I. Mamalimov
机构：
[1] Russian Academy of Sciences,Ioffe Physical
来源：
Physics of the Solid State | 2015年 / 57卷
关键词：
Shock Wave; Reflectance Spectrum; Distorted Lattice; Fuse Quartz; Shock Wave Pressure;
D O I：
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中图分类号：
学科分类号：
摘要：
The structure of a fragment formed after quartz single-crystal fracture under a shock wave has been studied using the Fourier transform infrared spectroscopy (FTIR) method. The wave is initiated by electrical breakdown of air in a hole within the single crystal. It has been found that a layer ~0.15 μm thick consisting of “diaplectic glass,” i.e., quartz with a strongly distorted lattice, is formed on the fragment surface. A layer 2 μm thick with a compressed quartz lattice is located under it.
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页码：2458 / 2460
页数：2
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