Shock Compression of Coesite up to 950 GPa

Abstract Experimental investigations of silica under high pressure and temperature offer crucial insights into modeling of Earth and super‐Earths’ interiors. Despite extensive studies on Hugoniots of silica polymorphs like fused‐silica (2.20 g/cm 3 ), quartz (2.65 g/cm 3 ) and stishovite (4.29 g/cm 3 ) up to a terapascal, unexplored region of melting and liquid of silica at high pressures is leaved because of the Hugoniots dependence on ambient density. This emphasizes the urgence to supplement the phase diagram to constrain silica properties under extreme conditions. Here, the Hugoniot and shock temperature of coesite (2.92 g/cm 3 ) were studied by laser shock compression experiments up to 950 GPa. Our findings confirm shock‐induced superheating in coesite, revealing a higher Grüneisen parameter and lower electrical conductivity compared to those of fused‐silica and quartz along an isothermal line (<2 × 10 4 K). These results suggest unique properties of shocked coesite, which imply a warmer and longer‐lived silica magma ocean of earlier rocky‐planets.

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Publication Details

Journal
Geophysical Research Letters
Published
2024-12-19
DOI
https://doi.org/10.1029/2024gl109873
Citations
2
Primary Topic
High-pressure geophysics and materials
Type
article
Field-Weighted Citation Impact
1.07

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article

Shock Compression of Coesite up to 950 GPa

Pinwen Zhu, Xiaokang Feng, Liang Sun, Takayoshi Sano et al.
2 citations
Geophysical Research Letters
High-pressure geophysics and materials
1.07
article

Shock Compression of Coesite up to 950 GPa

Pinwen Zhu, Xiaokang Feng, Liang Sun, Takayoshi Sano, Jia Qu, Norimasa Ozaki, Keita Nonaka, Wenge Yang, Toshimori Sekine, Kento Katagiri
article en
2 citations

Abstract

Abstract Experimental investigations of silica under high pressure and temperature offer crucial insights into modeling of Earth and super‐Earths’ interiors. Despite extensive studies on Hugoniots of silica polymorphs like fused‐silica (2.20 g/cm 3 ), quartz (2.65 g/cm 3 ) and stishovite (4.29 g/cm 3 ) up to a terapascal, unexplored region of melting and liquid of silica at high pressures is leaved because of the Hugoniots dependence on ambient density. This emphasizes the urgence to supplement the phase diagram to constrain silica properties under extreme conditions. Here, the Hugoniot and shock temperature of coesite (2.92 g/cm 3 ) were studied by laser shock compression experiments up to 950 GPa. Our findings confirm shock‐induced superheating in coesite, revealing a higher Grüneisen parameter and lower electrical conductivity compared to those of fused‐silica and quartz along an isothermal line (<2 × 10 4 K). These results suggest unique properties of shocked coesite, which imply a warmer and longer‐lived silica magma ocean of earlier rocky‐planets.

Geophysical Research LettersVol. 51(24)
Jilin University (CN), Chinese Academy of Engineering (CN), Shanghai Advanced Research Institute (CN), Center for High Pressure Science and Technology Advanced Research (CN), State Key Laboratory of High Pressure and Superhard Materials (CN), The University of Osaka (JP)
Ministry of Education, Culture, Sports, Science and Technology, National Natural Science Foundation of China, Science and Technology Commission of Shanghai Municipality, Natural Science Foundation of Shandong Province, Japan Society for the Promotion of Science
Life below water
Openalex Percentile: Top 23%
High-pressure geophysics and materials
1.07
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