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 › peer-review

38 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 - 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, 2009.

Research output: Contribution to journal › Article › peer-review

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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title = "Shock hugoniot and temperature data for polystyrene obtained with quartz standard",

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.",

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

note = "Funding Information: This work was performed under the joint research project of the ILE, Osaka University. The authors gratefully acknowledge the valuable support for the experiments by ILE technical crews. The authors are also grateful to M. Koenig for the VISAR construction and D. Young for valuable discussions concerning the modified QEOS. This research was partially supported by grants for the Core-to-Core Program from the Japan Society for the Promotion of Science (JSPS) and for the Global COE Program, “Center for Electronic Devices Innovation,” from the Ministry of Education, Culture, Sports, Science and Technology of Japan. The contribution by F. H. Ree was performed under the auspices of the U.S. DOE by the Lawrence Livermore National Laboratory under Contract No. DE-AC52-07NA27344. ",

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T1 - Shock hugoniot and temperature data for polystyrene obtained with quartz standard

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.

N1 - Funding Information: This work was performed under the joint research project of the ILE, Osaka University. The authors gratefully acknowledge the valuable support for the experiments by ILE technical crews. The authors are also grateful to M. Koenig for the VISAR construction and D. Young for valuable discussions concerning the modified QEOS. This research was partially supported by grants for the Core-to-Core Program from the Japan Society for the Promotion of Science (JSPS) and for the Global COE Program, “Center for Electronic Devices Innovation,” from the Ministry of Education, Culture, Sports, Science and Technology of Japan. The contribution by F. H. Ree was performed under the auspices of the U.S. DOE by the Lawrence Livermore National Laboratory under Contract No. DE-AC52-07NA27344.

PY - 2009

Y1 - 2009

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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