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

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 e...

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Главные авторы: Reinhardt, A, Doye, J
Формат: Journal article
Язык:English
Опубликовано: American Institute of Physics 2012
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author Reinhardt, A
Doye, J
author_facet Reinhardt, A
Doye, J
author_sort Reinhardt, A
collection OXFORD
description 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.
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spelling oxford-uuid:6584d94b-7868-4e5b-ab0e-c84e587e7bdc2022-03-26T18:26:00ZFree energy landscapes for homogeneous nucleation of ice for a monatomic water model.Journal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:6584d94b-7868-4e5b-ab0e-c84e587e7bdcEnglishSymplectic Elements at OxfordAmerican Institute of Physics2012Reinhardt, ADoye, JWe 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.
spellingShingle Reinhardt, A
Doye, J
Free energy landscapes for homogeneous nucleation of ice for a monatomic water model.
title Free energy landscapes for homogeneous nucleation of ice for a monatomic water model.
title_full Free energy landscapes for homogeneous nucleation of ice for a monatomic water model.
title_fullStr Free energy landscapes for homogeneous nucleation of ice for a monatomic water model.
title_full_unstemmed Free energy landscapes for homogeneous nucleation of ice for a monatomic water model.
title_short Free energy landscapes for homogeneous nucleation of ice for a monatomic water model.
title_sort free energy landscapes for homogeneous nucleation of ice for a monatomic water model
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AT doyej freeenergylandscapesforhomogeneousnucleationoficeforamonatomicwatermodel