New ultrahigh pressure phases of H2O ice predicted using an adaptive genetic algorithm
Min Ji, Koichiro Umemoto, Cai-Zhuang Wang, Kai-Ming Ho, and Renata M., Wentzcovitch

TL;DR
This paper predicts three new ultrahigh pressure phases of H2O ice using an adaptive genetic algorithm, revealing complex phase transitions and structural changes up to 7 TPa.
Contribution
It introduces a novel computational approach to explore H2O ice phases, identifying new stable structures and transition sequences under extreme pressures.
Findings
Discovered three new high-pressure ice phases.
Identified a sequence of pressure-induced phase transitions.
All phases remain nonmetallic up to 7 TPa.
Abstract
We propose three new phases of H2O under ultrahigh pressure. Our structural search was performed using an adaptive genetic algorithm which allows an extensive exploration of crystal structure. The new sequence of pressure-induced transitions beyond ice X at 0 K should be ice X - Pbcm - Pbca - Pmc21 - P21 - P21/c phases. Across the Pmc21 - P21 transition, the coordination number of oxygen increases from 4 to 5 with a significant increase of density. All stable crystalline phases have nonmetallic band structures up to 7 TPa.
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Taxonomy
TopicsArctic and Antarctic ice dynamics · Methane Hydrates and Related Phenomena · Spacecraft and Cryogenic Technologies
