[S-IT31] 惑星中心核：構造，形成と進化

[SIT31-05] Sound velocity of B2-FeNiSi alloy at high pressure determined with inelastic X-ray scattering: Implications for the composition of the Earth's inner core

Serena Dominijanni¹、*大谷 栄治²、生田 大穣²、坂巻 竜也²、福井 宏之³、McCammon Catherine¹、Dubrovinsky Leonid¹、内山 裕士⁴、Baron Alfred⁵ (1.バイロイト大学バイエルン地球科学研究所、2.東北大学大学院理学研究科地学専攻、3.兵庫県立大学、4.高輝度光科学研究センター、5.理化学研究所)

キーワード：音速、内核、B2型FeNiSi合金、高圧、Ｘ線非弾性散乱

Geochemical and geophysical studies provide evidence that Earth’s core contains iron with 5-7 wt.% of nickel [1] and a small amount of light elements (such as silicon, sulfur, oxygen, hydrogen, and carbon) that can justify the observed density deficit with respect to pure iron [e.g., 2]. The cosmochemical abundance of Si and its involvement in chemical reactions at the core mantle boundary (CMB) indicate that it can be considered as one of the major alloying elements in the Earth’s core [1].

We measured the sound velocity of Fe₇₈Ni₇Si₁₅ alloy with a B2 structure at room temperature up to 90 GPa employing inelastic X-ray scattering to constrain the constitution of the inner core. The density of the alloy was also determined by X-ray diffraction under the same conditions. The relation of the P-wave velocity (vP) and density (ρ) of B2-Fe₇₈Ni₇Si₁₅ alloy follows Birch’s law. We discuss the possibility that the inner core is composed of the B2-Fe₇₈Ni₇Si₁₅ alloy or the mixture of hcp and B2 alloys based on Birch’s law determined here for B2-Fe₇₈Ni₇Si₁₅ alloy and that for hcp-Fe and FeSi alloys reported previously [3, 4]

References:
[1] McCDonough W.F. and Sun S., (1995), Chem. Geol. 120, 223-253;
[2] Dubrovinsky L., et al., (2000), Phy. Rev. Lett., 84, 1720-1723
[3] Sakamaki et al. (2016), Science Advances, 2, e1500802.
[4] Sakairi et al. (2018), Am Min., 102, 85-90.