JpGU-AGU Joint Meeting 2020

講演情報

[E] 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-IT31] 惑星中心核:構造,形成と進化

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)、Gerd Steinle-Neumann(Bayerisches Geoinstitut, Universitaet Bayreuth)、William F McDonough(Department of Earth Science and Research Center for Neutrino Science, Tohoku University, Sendai, Miyagi 980-8578, Japan)

[SIT31-P02] Mercury core size constrained from elastic properties of Fe-Ni-S-Si liquid

山田 伊織1、*寺崎 英紀1鶴岡 椋1神谷 朝香1近藤 忠1丹下 慶範2肥後 祐司2 (1.大阪大学大学院理学研究科、2.JASRI)

キーワード:Mercury、Sound velocity、iron-alloy、Core

Surface on Mercury is found to contain 1–4 wt% of sulfur from X-ray spectroscopy of the MESSENGER spacecraft (Nittler et al. 2011). The S content on the surface suggests that certain amounts of S and Si are likely to be contained in the Mercury core based on partitioning of S and Si between metal and silicate melts (Chabot et al. 2014).

In this study, we measured the VP of liquid Fe–Ni–S–Si up to 17 GPa and investigated the effect of pressure and alloying of S+Si on the VP to constrain the radius of Mercury core. High pressure experiments were performed using 1500 ton Kawai-type multianvil press at BL04B1 beamline, SPring-8 synchrotron facility. The P-wave velocity was measured using the pulse-echo overlap method.

The VP of Fe-Ni-S-Si liquids of this study locate in between reported VP of Fe-Ni-S and Fe-Ni-Si. Thus, there is an offset between S and Si effects on the VP. Based on the obtained elastic properties of liquid Fe-Ni-S-Si, we estimated the Mercury core radius which satisfies the observed total mass and moment of inertia of Mercury and discuss possible core composition.