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Title: Extension of the Hugoniot and analytical release model of α-quartz to 0.2–3 TPa

In recent years, α-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 ~90–100 GPa along the principal Hugoniot α-quartz becomes reflective, and thus, shock velocities can be measured to high precision using velocity interferometry. The Hugoniot and release of α-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). Furthermore, we extend this analytical model to 200–3000 GPa (0.2–3 TPa) through additional α-quartz Hugoniot and release measurements, as well as first-principles molecular dynamics calculations.
Authors:
 [1] ;  [2] ;  [1]
  1. Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
  2. Sandia National Lab. (SNL-NM), Albuquerque, NM (United States); Washington State Univ., Pullman, WA (United States)
Publication Date:
Report Number(s):
SAND-2017-4961J
Journal ID: ISSN 0021-8979; 653198
Grant/Contract Number:
AC04-94AL85000; NA0003525
Type:
Accepted Manuscript
Journal Name:
Journal of Applied Physics
Additional Journal Information:
Journal Volume: 122; Journal Issue: 3; Journal ID: ISSN 0021-8979
Publisher:
American Institute of Physics (AIP)
Research Org:
Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
Sponsoring Org:
USDOE National Nuclear Security Administration (NNSA)
Country of Publication:
United States
Language:
English
Subject:
71 CLASSICAL AND QUANTUM MECHANICS, GENERAL PHYSICS
OSTI Identifier:
1372361
Alternate Identifier(s):
OSTI ID: 1372120

Desjarlais, M. P., Knudson, M. D., and Cochrane, K. R.. Extension of the Hugoniot and analytical release model of α-quartz to 0.2–3 TPa. United States: N. p., Web. doi:10.1063/1.4991814.
Desjarlais, M. P., Knudson, M. D., & Cochrane, K. R.. Extension of the Hugoniot and analytical release model of α-quartz to 0.2–3 TPa. United States. doi:10.1063/1.4991814.
Desjarlais, M. P., Knudson, M. D., and Cochrane, K. R.. 2017. "Extension of the Hugoniot and analytical release model of α-quartz to 0.2–3 TPa". United States. doi:10.1063/1.4991814. https://www.osti.gov/servlets/purl/1372361.
@article{osti_1372361,
title = {Extension of the Hugoniot and analytical release model of α-quartz to 0.2–3 TPa},
author = {Desjarlais, M. P. and Knudson, M. D. and Cochrane, K. R.},
abstractNote = {In recent years, α-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 ~90–100 GPa along the principal Hugoniot α-quartz becomes reflective, and thus, shock velocities can be measured to high precision using velocity interferometry. The Hugoniot and release of α-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). Furthermore, we extend this analytical model to 200–3000 GPa (0.2–3 TPa) through additional α-quartz Hugoniot and release measurements, as well as first-principles molecular dynamics calculations.},
doi = {10.1063/1.4991814},
journal = {Journal of Applied Physics},
number = 3,
volume = 122,
place = {United States},
year = {2017},
month = {7}
}

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