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Dynamic response of fused quartz in the permanent densification region

机译:永久致密化区域中熔融石英的动态响应

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A shock wave investigation on fused quartz was performed in the permanent densification region, using a double stage light‐gas gun with dc x‐ray velocity meter and the electromagnetic particle velocity measurement technique. The elastic limit obtained in this work [(8.81±0.11) GPa] was somewhat lower than the published value. The compression curve obtained was quite different from the published curve and indicated that a rapid volume contraction occured just above the elastic limit. The tetrahedral coordinations seemed to remain at least up to 22 GPa, but above 16 GPa, they would be distorted or in some parts destroyed. The pressure of 16 GPa was considered as the limit of the permanent densification process, and the specific volume at atmospheric pressure interpolated along a hypothetical release adiabat was about 0.32 cm3/g.
机译:使用带有直流x射线速度计的双级轻气枪和电磁粒子速度测量技术,在永久致密化区域对熔融石英进行了冲击波研究。在这项工作中获得的弹性极限[(8.81±0.11)GPa]略低于公开值。获得的压缩曲线与公开的曲线完全不同,表明刚好在弹性极限以上发生了快速的体积收缩。四面体的配位似乎至少保持在22 GPa,但高于16 GPa时,它们会变形或部分破坏。 16 GPa的压力被认为是永久致密化过程的极限,沿着假想的释放绝热体插在大气压下的比容约为0.32 cm3 / g。

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    《Journal of Applied Physics》 |1981年第5期|P.3375-3382|共8页
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  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
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