Shock hugoniot and temperature data for polystyrene obtained with quartz standard

N. Ozaki; T. Sano; M. Ikoma; K. Shigemori; T. Kimura; K. Miyanishi; T. Vinci; F. H. Ree; H. Azechi; T. Endo; Y. Hironaka; Y. Hori; A. Iwamoto; T. Kadono; H. Nagatomo; M. Nakai; T. Norimatsu; T. Okuchi; K. Otani; T. Sakaiya; K. Shimizu; A. Shiroshita; A. Sunahara; H. Takahashi; R. Kodama

doi:10.1063/1.3152287

Shock hugoniot and temperature data for polystyrene obtained with quartz standard

N. Ozaki, T. Sano, M. Ikoma, K. Shigemori, T. Kimura, K. Miyanishi, T. Vinci, F. H. Ree, H. Azechi, T. Endo, Y. Hironaka, Y. Hori, A. Iwamoto, T. Kadono, H. Nagatomo, M. Nakai, T. Norimatsu, T. Okuchi, K. Otani, T. SakaiyaK. Shimizu, A. Shiroshita, A. Sunahara, H. Takahashi, R. Kodama

Institute for Planetary Materials

Research output: Contribution to journal › Article

37 Citations (Scopus)

Abstract

Equation-of-state data, not only pressure and density but also temperature, for polystyrene (CH) are obtained up to 510 GPa. The region investigated in this work corresponds to an intermediate region, bridging a large gap between available gas-gun data below 60 GPa and laser shock data above 500 GPa. The Hugoniot parameters and shock temperature were simultaneously determined by using optical velocimeters and pyrometers as the diagnostic tools and the α -quartz as a new standard material. The CH Hugoniot obtained tends to become stiffer than a semiempirical chemical theoretical model predictions at ultrahigh pressures but is consistent with other models and available experimental data.

Original language	English
Article number	062702
Journal	Physics of Plasmas
Volume	16
Issue number	6
DOIs	https://doi.org/10.1063/1.3152287
Publication status	Published - Jul 20 2009

ASJC Scopus subject areas

Condensed Matter Physics

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Ozaki, N., Sano, T., Ikoma, M., Shigemori, K., Kimura, T., Miyanishi, K., Vinci, T., Ree, F. H., Azechi, H., Endo, T., Hironaka, Y., Hori, Y., Iwamoto, A., Kadono, T., Nagatomo, H., Nakai, M., Norimatsu, T., Okuchi, T., Otani, K., ... Kodama, R. (2009). Shock hugoniot and temperature data for polystyrene obtained with quartz standard. Physics of Plasmas, 16(6), [062702]. https://doi.org/10.1063/1.3152287

Shock hugoniot and temperature data for polystyrene obtained with quartz standard. / Ozaki, N.; Sano, T.; Ikoma, M.; Shigemori, K.; Kimura, T.; Miyanishi, K.; Vinci, T.; Ree, F. H.; Azechi, H.; Endo, T.; Hironaka, Y.; Hori, Y.; Iwamoto, A.; Kadono, T.; Nagatomo, H.; Nakai, M.; Norimatsu, T.; Okuchi, T.; Otani, K.; Sakaiya, T.; Shimizu, K.; Shiroshita, A.; Sunahara, A.; Takahashi, H.; Kodama, R.

In: Physics of Plasmas, Vol. 16, No. 6, 062702, 20.07.2009.

Research output: Contribution to journal › Article

Ozaki, N, Sano, T, Ikoma, M, Shigemori, K, Kimura, T, Miyanishi, K, Vinci, T, Ree, FH, Azechi, H, Endo, T, Hironaka, Y, Hori, Y, Iwamoto, A, Kadono, T, Nagatomo, H, Nakai, M, Norimatsu, T, Okuchi, T, Otani, K, Sakaiya, T, Shimizu, K, Shiroshita, A, Sunahara, A, Takahashi, H & Kodama, R 2009, 'Shock hugoniot and temperature data for polystyrene obtained with quartz standard', Physics of Plasmas, vol. 16, no. 6, 062702. https://doi.org/10.1063/1.3152287

Ozaki, N. ; Sano, T. ; Ikoma, M. ; Shigemori, K. ; Kimura, T. ; Miyanishi, K. ; Vinci, T. ; Ree, F. H. ; Azechi, H. ; Endo, T. ; Hironaka, Y. ; Hori, Y. ; Iwamoto, A. ; Kadono, T. ; Nagatomo, H. ; Nakai, M. ; Norimatsu, T. ; Okuchi, T. ; Otani, K. ; Sakaiya, T. ; Shimizu, K. ; Shiroshita, A. ; Sunahara, A. ; Takahashi, H. ; Kodama, R. / Shock hugoniot and temperature data for polystyrene obtained with quartz standard. In: Physics of Plasmas. 2009 ; Vol. 16, No. 6.

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abstract = "Equation-of-state data, not only pressure and density but also temperature, for polystyrene (CH) are obtained up to 510 GPa. The region investigated in this work corresponds to an intermediate region, bridging a large gap between available gas-gun data below 60 GPa and laser shock data above 500 GPa. The Hugoniot parameters and shock temperature were simultaneously determined by using optical velocimeters and pyrometers as the diagnostic tools and the α -quartz as a new standard material. The CH Hugoniot obtained tends to become stiffer than a semiempirical chemical theoretical model predictions at ultrahigh pressures but is consistent with other models and available experimental data.",

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AU - Ozaki, N.

AU - Sano, T.

AU - Ikoma, M.

AU - Shigemori, K.

AU - Kimura, T.

AU - Miyanishi, K.

AU - Vinci, T.

AU - Ree, F. H.

AU - Azechi, H.

AU - Endo, T.

AU - Hironaka, Y.

AU - Hori, Y.

AU - Iwamoto, A.

AU - Kadono, T.

AU - Nagatomo, H.

AU - Nakai, M.

AU - Norimatsu, T.

AU - Okuchi, T.

AU - Otani, K.

AU - Sakaiya, T.

AU - Shimizu, K.

AU - Shiroshita, A.

AU - Sunahara, A.

AU - Takahashi, H.

AU - Kodama, R.

PY - 2009/7/20

Y1 - 2009/7/20

N2 - Equation-of-state data, not only pressure and density but also temperature, for polystyrene (CH) are obtained up to 510 GPa. The region investigated in this work corresponds to an intermediate region, bridging a large gap between available gas-gun data below 60 GPa and laser shock data above 500 GPa. The Hugoniot parameters and shock temperature were simultaneously determined by using optical velocimeters and pyrometers as the diagnostic tools and the α -quartz as a new standard material. The CH Hugoniot obtained tends to become stiffer than a semiempirical chemical theoretical model predictions at ultrahigh pressures but is consistent with other models and available experimental data.

AB - Equation-of-state data, not only pressure and density but also temperature, for polystyrene (CH) are obtained up to 510 GPa. The region investigated in this work corresponds to an intermediate region, bridging a large gap between available gas-gun data below 60 GPa and laser shock data above 500 GPa. The Hugoniot parameters and shock temperature were simultaneously determined by using optical velocimeters and pyrometers as the diagnostic tools and the α -quartz as a new standard material. The CH Hugoniot obtained tends to become stiffer than a semiempirical chemical theoretical model predictions at ultrahigh pressures but is consistent with other models and available experimental data.

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