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 decomposes into 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 comes into contact with hydrogen. Metallization of is predicted at a higher pressure of just over 6 TPa, and therefore 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.
- Received 6 December 2012
DOI:https://doi.org/10.1103/PhysRevLett.110.245701
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