Shock compression response of diamond single crystals at multimegabar stresses
Abstract
Shock compressed diamond response at multi-megabar stresses – of fundamental interest to high pressure science and relevant for high energy density experiments related to inertial confinement fusion – is often assumed to be hydrodynamic. To explore this assumption, plate impact experiments were conducted to measure wave profiles in diamond single crystals shocked to ~900 GPa elastic impact stress (EIS). For the [110] and [111] orientations, two wave structures (elastic-inelastic response) were observed to ~900 GPa EIS; in contrast, single (overdriven) waves were observed at 480 GPa EIS and above for the [100] orientation. The elastic wave velocities for the [110] and [111] orientations were significantly larger than those for the [100] orientation. Strong orientation dependence was further observed for the elastic wave amplitudes; for [110] and [111] diamond, the amplitudes increased significantly with increasing elastic impact stress. The observed two-wave structures and the strong orientation dependence (elastic wave speeds and amplitudes) demonstrate unequivocally that the shock response of diamond single crystals is not hydrodynamic at stresses below the melt transition. As such, appropriate elastic-inelastic material descriptions are needed to accurately model the high stress response of diamond and other strong solids.
- Authors:
-
[1];
[2];
[1]
- Washington State Univ., Pullman, WA (United States). Inst. for Shock Physics and Dept. of Physics
- Washington State Univ., Pullman, WA (United States). Inst. for Shock Physics and Dept. of Physics; Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
- Publication Date:
- Research Org.:
- Washington State Univ., Pullman, WA (United States). Inst. for Shock Physics; Sandia National Lab. (SNL-NM), Albuquerque, NM (United States)
- Sponsoring Org.:
- USDOE National Nuclear Security Administration (NNSA)
- OSTI Identifier:
- 1632354
- Grant/Contract Number:
- NA0002007; NA0003525
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Physical Review B
- Additional Journal Information:
- Journal Volume: 101; Journal Issue: 18; Journal ID: ISSN 2469-9950
- Publisher:
- American Physical Society (APS)
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 36 MATERIALS SCIENCE; 75 CONDENSED MATTER PHYSICS, SUPERCONDUCTIVITY AND SUPERFLUIDITY
Citation Formats
Winey, J. M., Knudson, M. D., and Gupta, Y. M. Shock compression response of diamond single crystals at multimegabar stresses. United States: N. p., 2020.
Web. doi:10.1103/PhysRevB.101.184105.
Winey, J. M., Knudson, M. D., & Gupta, Y. M. Shock compression response of diamond single crystals at multimegabar stresses. United States. https://doi.org/10.1103/PhysRevB.101.184105
Winey, J. M., Knudson, M. D., and Gupta, Y. M. Fri .
"Shock compression response of diamond single crystals at multimegabar stresses". United States. https://doi.org/10.1103/PhysRevB.101.184105. https://www.osti.gov/servlets/purl/1632354.
@article{osti_1632354,
title = {Shock compression response of diamond single crystals at multimegabar stresses},
author = {Winey, J. M. and Knudson, M. D. and Gupta, Y. M.},
abstractNote = {Shock compressed diamond response at multi-megabar stresses – of fundamental interest to high pressure science and relevant for high energy density experiments related to inertial confinement fusion – is often assumed to be hydrodynamic. To explore this assumption, plate impact experiments were conducted to measure wave profiles in diamond single crystals shocked to ~900 GPa elastic impact stress (EIS). For the [110] and [111] orientations, two wave structures (elastic-inelastic response) were observed to ~900 GPa EIS; in contrast, single (overdriven) waves were observed at 480 GPa EIS and above for the [100] orientation. The elastic wave velocities for the [110] and [111] orientations were significantly larger than those for the [100] orientation. Strong orientation dependence was further observed for the elastic wave amplitudes; for [110] and [111] diamond, the amplitudes increased significantly with increasing elastic impact stress. The observed two-wave structures and the strong orientation dependence (elastic wave speeds and amplitudes) demonstrate unequivocally that the shock response of diamond single crystals is not hydrodynamic at stresses below the melt transition. As such, appropriate elastic-inelastic material descriptions are needed to accurately model the high stress response of diamond and other strong solids.},
doi = {10.1103/PhysRevB.101.184105},
journal = {Physical Review B},
number = 18,
volume = 101,
place = {United States},
year = {Fri May 08 00:00:00 EDT 2020},
month = {Fri May 08 00:00:00 EDT 2020}
}
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