Decomposition and Terapascal Phases of Water Ice

Chris J. Pickard, Miguel Martinez-Canales, and Richard J. Needs
Phys. Rev. Lett. 110, 245701 – Published 11 June 2013
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Abstract

Computational searches for stable and metastable structures of water ice and other H:O compositions at TPa pressures have led us to predict that H2O decomposes into H2O2 and a hydrogen-rich phase at pressures of a little over 5 TPa. The hydrogen-rich phase is stable over a wide range of hydrogen contents, and it might play a role in the erosion of the icy component of the cores of gas giants as H2O comes into contact with hydrogen. Metallization of H2O is predicted at a higher pressure of just over 6 TPa, and therefore H2O does not have a thermodynamically stable low-temperature metallic form. We have also found a new and rich mineralogy of complicated water ice phases that are more stable in the pressure range 0.8–2 TPa than any predicted previously.

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  • Received 6 December 2012

DOI:https://doi.org/10.1103/PhysRevLett.110.245701

© 2013 American Physical Society

Authors & Affiliations

Chris J. Pickard* and Miguel Martinez-Canales

  • Department of Physics and Astronomy, University College London, Gower Street, London WC1E 6BT, United Kingdom

Richard J. Needs

  • Theory of Condensed Matter Group, Cavendish Laboratory, Cambridge CB3 0HE, United Kingdom

  • *c.pickard@ucl.ac.uk

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Issue

Vol. 110, Iss. 24 — 14 June 2013

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