日本地球惑星科学連合2016年大会

講演情報

インターナショナルセッション(ポスター発表)

セッション記号 S (固体地球科学) » S-IT 地球内部科学・地球惑星テクトニクス

[S-IT07] Structure and dynamics of Earth and Planetary deep interiors

2016年5月22日(日) 17:15 〜 18:30 ポスター会場 (国際展示場 6ホール)

コンビーナ:*芳野 極(岡山大学地球物質科学研究センター)、趙 大鵬(東北大学大学院理学研究科附属地震・噴火予知研究観測センター)、中川 貴司(海洋研究開発機構数理科学・先端技術研究分野)

17:15 〜 18:30

[SIT07-P05] Sound velocity and density of liquid iron sulfide up to 600 GPa by laser-shock compression

尾方 優士1、*境家 達弘1近藤 忠1寺崎 英紀1重森 啓介2弘中 陽一郎2 (1.大阪大学大学院理学研究科宇宙地球科学専攻、2.大阪大学レーザーエネルギー学研究センター)

キーワード:Sound velocity, Laser, Shock compression, Pyrrhotite, Earth's core

Sound velocity at Earth’s core conditions are one of the most important physical properties in Earth science because it can be directly compared with the seismological Earth model (PREM: Preliminary Reference Earth Model) [1]. The composition of solid inner core is estimated from the comparison of the model [1] and the extrapolation of sound velocities as a function of density of iron and iron alloys obtained by the static compression experiment [2, 3]. Birch’s law, a linear sound velocity−density relation [4], is used to extrapolate sound velocities to densities in the core condition. On the other hand, the composition of liquid outer core is estimated from the partitioning and solubility data in the inner core boundary condition for the composition of solid core. There has been some works for the sound velocity of iron and iron alloys on the Earth’s core condition by dynamic techniques using explosive [5], gas gun [5-9], and laser [10-12]. Huang et al. estimated that the outer core composition is Fe with 0.5 wt.% O and 9.5 wt.% S by the comparison of PREM and sound velocities of Fe-S-O system [9]. In this study, we measure the sound velocity and density of liquid iron sulfide by shock-compression method using high-power laser.
We conducted shock-compression experiments using a High Intensity Plasma Experimental Research (HIPER) system at the GEKKO-XII laser irradiation facility [10] at the Institute of Laser Engineering, Osaka University. The sample is pyrrhotite (Fe0.9S). The sound velocities and densities of shock-compressed pyrrhotite using the high-power laser were measured by x-ray radiography [10-12] at pressures up to 600 GPa.
Part of this work was performed under the joint research project of the Institute of Laser Engineering, Osaka University.

References
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