Atomic distribution and local structure in ice VII from in situ neutron diffraction

Author:

Yamashita Keishiro1ORCID,Komatsu Kazuki1ORCID,Klotz Stefan2ORCID,Fabelo Oscar3ORCID,Fernández-Díaz Maria T.3,Abe Jun4ORCID,Machida Shinichi4,Hattori Takanori5,Irifune Tetsuo6,Shinmei Toru6ORCID,Sugiyama Kazumasa7,Kawamata Toru7,Kagi Hiroyuki1ORCID

Affiliation:

1. Geochemical Research Center, Graduate School of Science, The University of Tokyo, Bunkyo-ku 113-0033, Japan

2. Institut de Minéralogie, de Physique des Matériaux et de Cosmochimie, CNRS UMR 7590, Sorbonne Université, Muséum National d’Histoire Naturelle, F-75252 Paris, France

3. Institut Laue-Langevin, F-38042 Grenoble Cedex 9, France

4. Neutron Science and Technology Center, Comprehensive Research Organization for Science and Society, Tokai, Naka 319-1106, Japan

5. J-PARC Center, Japan Atomic Energy Agency, Tokai-mura 319-1195, Japan

6. Geodynamics Research Center, Ehime University, Matsuyama 790-8577, Japan

7. Institute for Materials Research, Tohoku University, Aoba-ku 980-8577, Japan

Abstract

Ice polymorphs show extraordinary structural diversity depending on pressure and temperature. The behavior of hydrogen-bond disorder not only is a key ingredient for their structural diversity but also controls their physical properties. However, it has been a challenge to determine the details of the disordered structure in ice polymorphs under pressure, because of the limited observable reciprocal space and inaccuracies related to high-pressure techniques. Here, we present an elucidation of the disordered structure of ice VII, the dominant high-pressure form of water, at 2.2 GPa and 298 K, from both single-crystal and powder neutron-diffraction techniques. We reveal the three-dimensional atomic distributions from the maximum entropy method and unexpectedly find a ring-like distribution of hydrogen in contrast to the commonly accepted discrete sites. In addition, total scattering analysis at 274 K clarified the difference in the intermolecular structure from ice VIII, the ordered counterpart of ice VII, despite an identical molecular geometry. Our complementary structure analyses robustly demonstrate the unique disordered structure of ice VII. Furthermore, these findings are related to proton dynamics, which drastically vary with pressure, and will contribute to an understanding of the structural origin of anomalous physical properties of ice VII under pressures.

Funder

MEXT | Japan Society for the Promotion of Science

Publisher

Proceedings of the National Academy of Sciences

Subject

Multidisciplinary

Cited by 4 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

1. Hydrogen bond symmetrisation in D2O ice observed by neutron diffraction;Nature Communications;2024-06-27

2. Disordered Structure in Ice VII Observed by Neutron Technique;The Review of High Pressure Science and Technology;2023-12-01

3. The hydrogen-bond network in sodium chloride tridecahydrate: analogy with ice VI;Acta Crystallographica Section B Structural Science, Crystal Engineering and Materials;2023-09-13

4. Advancing neutron diffraction for accurate structural measurement of light elements at megabar pressures;Scientific Reports;2023-03-23

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