Abstract
Commensurate adsorbed surface phases, particularly p×1 rectangular and 3×3 hexagonal phases, exhibit two (or more) classes of domain wall, reflecting a lower than ideal symmetry; these compete statistically and undergo wetting transitions. Scaling arguments and model calculations indicate that new types of continuous melting transitions, possibly already seen in Kr on graphite, can thereby arise.
Original language | English (US) |
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Pages (from-to) | 793-796 |
Number of pages | 4 |
Journal | Physical review letters |
Volume | 49 |
Issue number | 11 |
DOIs | |
State | Published - 1982 |
Externally published | Yes |
All Science Journal Classification (ASJC) codes
- General Physics and Astronomy