Startseite Hydrogen occupation and hydrogen-induced volume expansion in Fe0.9Ni0.1Dx at high P-T conditions
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Hydrogen occupation and hydrogen-induced volume expansion in Fe0.9Ni0.1Dx at high P-T conditions

  • Chikara Shito , Hiroyuki Kagi ORCID logo EMAIL logo , Sho Kakizawa , Katsutoshi Aoki , Kazuki Komatsu , Riko Iizuka-Oku , Jun Abe , Hirioyuki Saitoh , Asami Sano-Furukawa ORCID logo und Takanori Hattori
Veröffentlicht/Copyright: 30. März 2023
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Abstract

The density of the Earth’s core is several percent lower than that of iron-nickel alloy under conditions of pressure and temperature equivalent to the Earth’s core. Hydrogen is one of the most promising constituents accounting for the density deficit, but hydrogen occupation sites and density decrease of iron-nickel alloy caused by hydrogenation have never been investigated. In this study, the phase relation and crystal structure of Fe0.9Ni0.1Hx(Dx) at high pressures and temperatures up to 12 GPa and 1000 K were clarified by in situ X-ray diffraction and neutron diffraction measurements. Under the P-T conditions of the present study, no deuterium atoms occupied tetragonal (T) sites of face-centered cubic (fcc) Fe0.9Ni0.1Dx, although the T-site occupation was previously reported for fcc FeHx(Dx). The deuterium-induced volume expansion per deuterium vD was determined to be 2.45(4) and 3.31(6) Å3 for fcc and hcp Fe0.9Ni0.1Dx, respectively. These vD values are significantly larger than the corresponding values for FeDx. The vD value for fcc Fe0.9Ni0.1Dx slightly increases with increasing temperature. This study suggests that only 10% of nickel in iron drastically changes the behaviors of hydrogen in metal. Assuming that vD is constant regardless of pressure, the maximum hydrogen content in the Earth’s inner core is estimated to be one to two times the amount of hydrogen in the oceans.


§ Special collection papers can be found online at http://www.minsocam.org/MSA/AmMin/special-collections.html.

‡ Present address: Research and Utilization Division, Japan Synchrotron Radiation Research Institute, 1-1-1 Kouto, Sayo-cho, Hyogo 679-5198, Japan


Acknowledgments and Funding

We are thankful to Hirotada Gotou for his technical support on X-ray and neutron diffraction experiments. We are grateful to the two anonymous reviewers whose comments greatly helped us to improve the manuscript. Neutron diffraction experiments were performed at the MLF of the J-PARC (Proposal Nos. 2020A0125 and 2020B0446). This study was supported by JSPS KAKENHI (Grant No. 18H05224).

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Received: 2021-10-13
Accepted: 2022-04-21
Published Online: 2023-03-30
Published in Print: 2023-04-25

© 2023 by Mineralogical Society of America

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