Residual Entropy of Square Ice

Elliott Lieb

Research output: Contribution to journalArticle

474 Citations (Scopus)

Abstract

At low temperatures, ice has a residual entropy, presumably caused by an indeterminacy in the positions of the hydrogen atoms. While the oxygen atoms are in a regular lattice, each O-H-O bond permits two possible positions for the hydrogen atom, subject to certain constraints called the "ice condition." The statement of the problem in two dimensions is to find the number of ways of drawing arrows on the bonds of a square planar net so that precisely two arrows point into each vertex. If N is the number of molecules and (for large N) WN is the number of arrangements, then S=NklnW. Our exact result is W=(43)32.

Original languageEnglish (US)
Pages (from-to)162-172
Number of pages11
JournalPhysical Review
Volume162
Issue number1
DOIs
StatePublished - Dec 1 1967

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hydrogen atoms
ice
entropy
oxygen atoms
apexes
molecules

All Science Journal Classification (ASJC) codes

  • Physics and Astronomy(all)

Cite this

Lieb, Elliott. / Residual Entropy of Square Ice. In: Physical Review. 1967 ; Vol. 162, No. 1. pp. 162-172.
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Residual Entropy of Square Ice. / Lieb, Elliott.

In: Physical Review, Vol. 162, No. 1, 01.12.1967, p. 162-172.

Research output: Contribution to journalArticle

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