Double-layer ice from first principles

被引:29
作者
Chen, Ji [1 ]
Schusteritsch, Georg [2 ]
Pickard, Chris J. [2 ,3 ]
Salzmann, Christoph G. [4 ]
Michaelides, Angelos [1 ]
机构
[1] UCL, Thomas Young Ctr, London Ctr Nanotechnol, Dept Phys & Astron, Gower St, London WC1E 6BT, England
[2] Univ Cambridge, Dept Mat Sci & Met, 27 Charles Babbage Rd, Cambridge CB3 0FS, England
[3] Tohoku Univ, Adv Inst Mat Res, Aoba Ku, 2-1-1 Katahira, Sendai, Miyagi 9808577, Japan
[4] UCL, Dept Chem, 20 Gordon St, London WC1H 0AJ, England
基金
英国工程与自然科学研究理事会; 欧洲研究理事会;
关键词
CONFINED WATER; SQUARE ICE; MONOLAYER ICE; BILAYER ICE; TEMPERATURE; LIQUID; POLYMORPHISM; HYDROGEN; PHASES;
D O I
10.1103/PhysRevB.95.094121
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
The formation of monolayer and multilayer ice with a square lattice structure has recently been reported on the basis of transmission electron microscopy experiments, renewing interest in confined two-dimensional ice. Here we report a systematic density functional theory study of double-layer ice in nanoconfinement. A phase diagram as a function of confinement width and lateral pressure is presented. Included in the phase diagram are honeycomb hexagonal, square-tube, hexagonal-close-packed, and buckled-rhombic structures. However, contrary to experimental observations, square structures do not feature: our most stable double-layer square structure is predicted to be metastable. This study provides general insight into the phase transitions of double-layer confined ice and a fresh theoretical perspective on the stability of square ice in graphene nanocapillary experiments.
引用
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页数:8
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