宇宙惑星科学(P) | |||
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セッション小記号 | 宇宙惑星科学複合領域・一般(CG) | ||
セッションID | P-CG22 | ||
タイトル | 和文 | Shock responses of planetary materials elucidated from meteorites and dynamic compression experiments | |
英文 | Shock responses of planetary materials elucidated from meteorites and dynamic compression experiments | ||
タイトル短縮名 | 和文 | Shock responses of planetary materials elucidated from meteorites and dynamic compression experiments | |
英文 | Shock responses of planetary materials | ||
代表コンビーナ | 氏名 | 和文 | 関根 利守 |
英文 | Toshimori Sekine | ||
所属 | 和文 | 大阪大学大学院工学研究科 | |
英文 | Graduate School of Engineering, Osaka University | ||
共同コンビーナ 1 | 氏名 | 和文 | 奥地 拓生 |
英文 | Takuo Okuchi | ||
所属 | 和文 | 岡山大学惑星物質研究所 | |
英文 | Institute for Planetary Materials, Okayama University | ||
発表言語 | E | ||
スコープ | 和文 | Impact phenomena had played essential roles in the process of planetary evolution. Recent analytical and experimental developments reveal a new prospective on the effects of shock-compression process for planetary materials. For deeper understanding of such shock effects, it is necessary to evaluate the detailed shock conditions from the observations of naturally-shocked planetary materials, and to compare them with the results on the planetary materials experienced a wide range of known shock conditions. Several metastable phases, that have not been known before, have recently been identified in shocked meteorites. They suggest that the shock state is often not in equilibrium and that it is more complicated process than ever thought. Experimental techniques including laser-driven shock compression and x-ray free electron laser diagnostics have been progressed to successfully simulate a wide range of shock conditions. The recent results indicate that shocked grains are fractured and rotated at relatively low pressures, and that they are subsequently transformed into denser phases or melts, or their mixtures at pressures of a few 100s GPa. Understanding of such shock dynamics requires another prospect, which is qualitatively different from the static high pressure and high temperature consensus. Therefore, it is timely to have an international symposium on dynamics of planetary materials. | |
英文 | Impact phenomena had played essential roles in the process of planetary evolution. Recent analytical and experimental developments reveal a new prospective on the effects of shock-compression process for planetary materials. For deeper understanding of such shock effects, it is necessary to evaluate the detailed shock conditions from the observations of naturally-shocked planetary materials, and to compare them with the results on the planetary materials experienced a wide range of known shock conditions. Several metastable phases, that have not been known before, have recently been identified in shocked meteorites. They suggest that the shock state is often not in equilibrium and that it is more complicated process than ever thought. Experimental techniques including laser-driven shock compression and x-ray free electron laser diagnostics have been progressed to successfully simulate a wide range of shock conditions. The recent results indicate that shocked grains are fractured and rotated at relatively low pressures, and that they are subsequently transformed into denser phases or melts, or their mixtures at pressures of a few 100s GPa. Understanding of such shock dynamics requires another prospect, which is qualitatively different from the static high pressure and high temperature consensus. Therefore, it is timely to have an international symposium on dynamics of planetary materials. | ||
発表方法 | 口頭および(または)ポスターセッション | ||
招待講演 | Yongjae Lee (Yonsei University) Hao Liu (Laser fusion research center) Ai-Cheng Zhang (School of Earth Sciences and Engineering, Nanjing University, China) 富岡 尚敬 (海洋研究開発機構高知コア研究所) 尾崎 典雅 (大阪大学) 鹿山 雅裕 (東北大学大学院理学研究科地学専攻) |
時間 | 講演番号 | タイトル | 発表者 | 予稿原稿 |
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口頭発表 5月28日 PM1 | ||||
13:45 - 14:00 | PCG22-01 | Shock-induced phase transformation in howardite-eucrite-diogenite meteorites | Ai-Cheng Zhang | 予稿 |
14:00 - 14:15 | PCG22-02 | 隕石における結晶格子剪断誘起のケイ酸塩高圧相の準安定的形成 | 富岡 尚敬 | 予稿 |
14:15 - 14:30 | PCG22-03 | Can high-pressure polymorphs clarify an ordinary chondrite parent-body breakup? | 宮原 正明 | 予稿 |
14:30 - 14:45 | PCG22-04 | Linking occurrence and texture of dense silicate minerals in shocked meteorites with laser-shock experimental results of Mg2SiO4 analyzed by XFEL probe | 奥地 拓生 | 予稿 |
14:45 - 15:00 | PCG22-05 | Laser-shock evolution of organic molecules in carbonaceous meteorite | 薮田 ひかる | 予稿 |
15:00 - 15:15 | PCG22-06 | Shock barometer using cathodoluminescence and synchrotron angle-dispersive x-ray diffraction analyses of minerals | 鹿山 雅裕 | 予稿 |
口頭発表 5月28日 PM2 | ||||
15:30 - 15:45 | PCG22-07 | Dynamic Compression at Pohang X-ray Free Electron Laser Facility (PAL-XFEL) | Yongjae Lee | 予稿 |
15:45 - 16:00 | PCG22-08 | Exploration of extreme melt states of silicate usign high-power laser and XFEL | 尾崎 典雅 | 予稿 |
16:00 - 16:15 | PCG22-09 | Hugoniot measurements for silicate: Understanding silicate magma under the planetary impacts | 梅田 悠平 | 予稿 |
16:15 - 16:30 | PCG22-10 | An experimental design to determine iron melting at the Earth’s core conditions via in-situ X-ray diffraction technique at high power laser facility | Hao Liu | 予稿 |
16:30 - 16:45 | PCG22-11 | Study on transport properties of liquid iron and iron alloy under high temperature and high pressure using the laser shock technique | 宮西 宏併 | 予稿 |
16:45 - 17:00 | PCG22-12 | Laser shock compression in LFRC | Liang Sun | 予稿 |
講演番号 | タイトル | 発表者 | 予稿原稿 |
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ポスター発表 5月28日 AM2 | |||
PCG22-P01 | 議論 | 奥地 拓生 | 予稿 |
PCG22-P02 | Shock-compressed behavior of quartz by XFEL | 佐藤 友子 | 予稿 |
PCG22-P04 | Laser-shock experiments of dense polymorphs of Mg2SiO4: technical developments using synthetic single crystals | Narangoo Purevjav | 予稿 |
PCG22-P05 | Richtmyer-Meshkov instability in inhomogeneous density materials and its application to planetary science | 佐野 孝好 | 予稿 |
PCG22-P06 | Impact-induced dehydration reactions of Fe- and Al-hydrates as potential storage, carrier and source of water | 鳥羽瀬 翼 | 予稿 |
PCG22-P07 | Crystallization of amorphous MgSiO3 by shock compression | 荒砂 茜 | 予稿 |
PCG22-P08 | First-principle study of the structural and electronic properties of N-doped MgAl2O4 spinel | Chi Pui Tang | 予稿 |
PCG22-P09 | Transparency of shock-compressed single crystal diamond | 片桐 健登 | 予稿 |
PCG22-P10 | Pb-Pb dating of the NWA 7203 angrite and relationship to its shock metamorphism | 林 秀幸 | 予稿 |
PCG22-P11 | 高強度レーザーを用いた衝撃試SiO2の高圧相回収 | 近藤 忠 | 予稿 |
PCG22-P12 | Hugoniot measurement of calcite under meteorite collision condition | 福井 敬也 | 予稿 |
PCG22-P13 | Direct observation of the transformation toughening of tetragonal stabilized zirconia under shock deformation condition by ns time-resolved XRD. | 高木 壮大 | 予稿 |