Neutron diffraction study of hydrogen site occupancy in Fe0.95Si0.05 at 14.7 GPa and 800 K-Reference-Cited by-同舟云学术

Neutron diffraction study of hydrogen site occupancy in Fe0.95Si0.05 at 14.7 GPa and 800 K

Published:2021 Issue:6 Volume:116 Page:309-313
ISSN:1345-6296
Container-title:Journal of Mineralogical and Petrological Sciences
language:en
Short-container-title:Journal of Mineralogical and Petrological Sciences

Author:

MORI Yuichiro¹,KAGI Hiroyuki¹,KAKIZAWA Sho²,KOMATSU Kazuki¹,SHITO Chikara¹,IIZUKA–OKU Riko¹,AOKI Katsutoshi¹,HATTORI Takanori³,SANO–FURUKAWA Asami³,FUNAKOSHI Ken–ichi⁴,SAITOH Hirouyki⁵

Affiliation:

1. Geochemical Research Center, Graduate School of Science, The University of Tokyo

2. Graduate School of Advanced Science and Engineering, Hiroshima University

3. J–PARC Center, Japan Atomic Energy Agency

4. CROSS Tokai Research Center for Neutron Science and Technology

5. Quantum Beam Science Research Directorate, National Institutes for Quantum and Radiological Science and Technology

Publisher

Japan Association of Mineralogical Sciences

Subject

Geology,Geophysics

Link

https://www.jstage.jst.go.jp/article/jmps/116/6/116_210825/_pdf

Reference27 articles.

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3. Dauphas, N., Poitrasson, F., Burkhardt, C., Kobayashi, H. and Kurosawa, K. (2015) Planetary and meteoritic Mg/Si and δ³⁰Si variations inherited from solar nebula chemistry. Earth and Planetary Science Letters, 427, 236–248.

4. Fukai, Y. (1984) The iron–water reaction and the evolution of the Earth. Nature, 308, 174–175.

5. Georg, R., Halliday, A., Schauble, E. and Reynolds, B.C. (2007) Silicon in the Earth’s core. Nature, 447, 1102–1106.

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