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Free energy landscapes for homogeneous nucleation of ice for a monatomic water model.

Abstract:
We simulate the homogeneous nucleation of ice from supercooled liquid water at 220 K in the isobaric-isothermal ensemble using the MW monatomic water potential. Monte Carlo simulations using umbrella sampling are performed in order to determine the nucleation free energy barrier. We find the Gibbs energy profile to be relatively consistent with that predicted by classical nucleation theory; the free energy barrier to nucleation was determined to be ~18 k(B)T and the critical nucleus comprised ~85 ice particles. Growth from the supercooled liquid gives clusters that are predominantly cubic, whilst starting with a pre-formed subcritical nucleus of cubic or hexagonal ice results in the growth of predominantly that phase of ice only.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1063/1.3677192

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Institution:
University of Oxford
Role:
Author
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Institution:
University of Oxford
Division:
MPLS
Department:
Chemistry
Sub department:
Physical & Theoretical Chem
Role:
Author


Publisher:
American Institute of Physics
Journal:
Journal of chemical physics More from this journal
Volume:
136
Issue:
5
Pages:
054501
Publication date:
2012-02-01
DOI:
EISSN:
1089-7690
ISSN:
0021-9606


Language:
English
Keywords:
Pubs id:
pubs:186286
UUID:
uuid:6584d94b-7868-4e5b-ab0e-c84e587e7bdc
Local pid:
pubs:186286
Source identifiers:
186286
Deposit date:
2013-03-20

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