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Extension of the Hugoniot and analytical release model of α-quartz to 0.2-3 TPa
被引:46
作者:
Desjarlais, M. P.
[1
]
Knudson, M. D.
[1
,2
]
Cochrane, K. R.
[1
]
机构:
[1] Sandia Natl Labs, Albuquerque, NM 87123 USA
[2] Washington State Univ, Inst Shock Phys, Pullman, WA 99164 USA
关键词:
AUGMENTED-WAVE METHOD;
REFRACTIVE-INDEX;
AEROGEL;
D O I:
10.1063/1.4991814
中图分类号:
O59 [应用物理学];
学科分类号:
摘要:
In recent years, alpha-quartz has been used prolifically as an impedance matching standard in shock wave experiments in the multi-Mbar regime (1 Mbar = 100 GPa = 0.1 TPa). This is due to the fact that above similar to 90-100 GPa along the principal Hugoniot alpha-quartz becomes reflective, and thus, shock velocities can be measured to high precision using velocity interferometry. The Hugoniot and release of alpha-quartz have been studied extensively, enabling the development of an analytical release model for use in impedance matching. However, this analytical release model has only been validated over a range of 300-1200 GPa (0.3-1.2 TPa). Here, we extend this analytical model to 200-3000 GPa (0.2-3 TPa) through additional alpha-quartz Hugoniot and release measurements, as well as first-principles molecular dynamics calculations. Published by AIP Publishing.
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