Japan Geoscience Union Meeting 2021

Presentation information

[E] Oral

S (Solid Earth Sciences ) » S-IT Science of the Earth's Interior & Techtonophysics

[S-IT18] Planetary cores: Structure, formation, and evolution

Thu. Jun 3, 2021 10:45 AM - 12:15 PM Ch.24 (Zoom Room 24)

convener:Hidenori Terasaki(Faculty of Science, Okayama University), Eiji Ohtani(Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University), 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), Chairperson:William F McDonough(University of Maryland College Park), Eiji Ohtani(Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University)

10:50 AM - 11:05 AM

[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)

Keywords: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.