日本地球惑星科学連合2021年大会

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[E] 口頭発表

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-IT18] 惑星中心核:内部構造・形成・進化

2021年6月3日(木) 10:45 〜 12:15 Ch.24 (Zoom会場24)

コンビーナ:寺崎 英紀(岡山大学理学部)、大谷 栄治(東北大学大学院理学研究科地学専攻)、F William McDonough(Department of Earth Science and Research Center for Neutrino Science, Tohoku University, Sendai, Miyagi 980-8578, Japan)、Attilio Rivoldini(Royal Observatory of Belgium)、座長:William F McDonough(University of Maryland College Park)、大谷 栄治(東北大学大学院理学研究科地学専攻)

10:50 〜 11:05

[SIT18-09] Effect of the core structure on the nutation of Mars

*Attilio Rivoldini1、Guillaume Morard2、Daniele Antonangeli3、Tim Van Hoolst1、Sébastien Le Maistre1、Véronique Dehant1 (1.Royal Observatory of Belgium、2.Université Grenoble Alpes、3.Sorbonne Université)

キーワード:Mars, core, InSight

Nutations are periodic changes in the orientation of the planet mainly due to the gravitational interaction with the Sun. The amplitude of the nutations dependents on a well known forcing and on the interior structure of Mars and in particular on the liquid core. One of the prime objectives of the RISE experiment on the ongoing InSight mission is to measure precisely the nutations of Mars and from the data infer the radius of its core and constrain its chemical composition.

Sulfur is commonly considered to be the main light element in the core of Mars, but the amount required to match the core density inferred from geodesy data is in excess of 25wt%. This is significantly larger than what is expected from geochemical modeling. Another candidate light element that can dissolve appreciably in liquid iron-sulfur at Mars core conditions is oxygen.

In this study, we build a new thermodynamic model of liquid iron-oxygen-sulfur to describe the thermoelastic properties of the core and investigate how the thermal structure of the core and its thermoelastic properties affect nutations.