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      Site occupancy of interstitial deuterium atoms in face-centred cubic iron

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          Abstract

          Hydrogen composition and occupation state provide basic information for understanding various properties of the metal–hydrogen system, ranging from microscopic properties such as hydrogen diffusion to macroscopic properties such as phase stability. Here the deuterization process of face-centred cubic Fe to form solid-solution face-centred cubic FeD x is investigated using in situ neutron diffraction at high temperature and pressure. In a completely deuterized specimen at 988 K and 6.3 GPa, deuterium atoms occupy octahedral and tetrahedral interstitial sites with an occupancy of 0.532(9) and 0.056(5), respectively, giving a deuterium composition x of 0.64(1). During deuterization, the metal lattice expands approximately linearly with deuterium composition at a rate of 2.21 Å 3 per deuterium atom. The minor occupation of the tetrahedral site is thermally driven by the intersite movement of deuterium atoms along the ‹111› direction in the face-centred cubic metal lattice.

          Abstract

          Knowledge of hydrogen content and coordination in deuterized metals is of importance. Here, the authors study the deuterization of face-centred cubic iron in-situ via neutron diffraction, observing the occupation by hydrogen of both octahedral and tetrahedral interstitial sites.

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          High-pressure chemistry of hydrogen in metals: in situ study of iron hydride.

          Optical observations and x-ray diffraction measurements of the reaction between iron and hydrogen at high pressure to form iron hydride are described. The reaction is associated with a sudden pressure-induced expansion at 3.5 gigapascals of iron samples immersed in fluid hydrogen. Synchrotron x-ray diffraction measurements carried out to 62 gigapascals demonstrate that iron hydride has a double hexagonal close-packed structure, a cell volume up to 17% larger than pure iron, and a stoichiometry close to FeH. These results greatly extend the pressure range over which the technologically important iron-hydrogen phase diagram has been characterized and have implications for problems ranging from hydrogen degradation and embrittlement of ferrous metals to the presence of hydrogen in Earth's metallic core.
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            Author and article information

            Journal
            Nat Commun
            Nat Commun
            Nature Communications
            Nature Pub. Group
            2041-1723
            26 September 2014
            : 5
            : 5063
            Affiliations
            [1 ]Quantum Beam Science Center, Japan Atomic Energy Agency , 1-1-1, Kouto, Sayo-cho, Sayo-gun, Hyogo 679-5148, Japan
            [2 ]Department of Physics, Chuo University , 21-13-27 Kasuga, Bunkyo-ku, Tokyo 112-8551, Japan
            [3 ]Quantum Beam Science Center, Japan Atomic Energy Agency , 2-4 Shirane Shirakata, Tokai-mura, Naka-gun, Ibaraki 319-1195, Japan
            [4 ]J-PARC Center, Japan Atomic Energy Agency , 2-4 Shirane Shirakata, Tokai-mura, Naka-gun, Ibaraki 319-1195, Japan
            [5 ]Geodynamics Research Center, Ehime University , 2-5 Bunkyo-cyo, Matsuyama, Ehime 790-8577, Japan
            [6 ]Institute for Materials Research, Tohoku University , 2-1-1 Katahira, Aoba-ku, Sendai 980-8577, Japan
            [7 ]WPI-Advanced Institute for Materials Research, Tohoku University , 2-1-1 Katahira, Aoba-ku, Sendai 980-8577, Japan
            Author notes
            Article
            ncomms6063
            10.1038/ncomms6063
            4200519
            25256789
            86432899-5eed-4c03-ace3-9b92174dffbb
            Copyright © 2014, Nature Publishing Group, a division of Macmillan Publishers Limited. All Rights Reserved.

            This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/4.0/

            History
            : 04 April 2014
            : 26 August 2014
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