A phase field model for brine channels in sea ice

In this paper, we present a phenomenological mathematical model for describing the features of the brine channels in sea ice. The differential system is composed of the Ginzburg–Landau and Cahn–Hilliard equations, in addition to the heat equation, that controls the ice–liquid phase transition by the...

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Published in:Physica B: Condensed Matter
Main Authors: V. Berti, M. Fabrizio, GRANDI, Diego
Other Authors: V., Berti, M., Fabrizio, Grandi, Diego
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Online Access:http://hdl.handle.net/11392/2362491
https://doi.org/10.1016/j.physb.2013.05.023
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spelling ftunivferrarair:oai:sfera.unife.it:11392/2362491 2024-09-09T20:07:08+00:00 A phase field model for brine channels in sea ice V. Berti M. Fabrizio GRANDI, Diego V., Berti M., Fabrizio Grandi, Diego 2013 STAMPA http://hdl.handle.net/11392/2362491 https://doi.org/10.1016/j.physb.2013.05.023 eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000321697500018 volume:425 firstpage:100 lastpage:104 numberofpages:4 journal:PHYSICA. B, CONDENSED MATTER http://hdl.handle.net/11392/2362491 doi:10.1016/j.physb.2013.05.023 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-84886944069 Brine channel Phase field Cahn–Hilliard Solute separation info:eu-repo/semantics/article 2013 ftunivferrarair https://doi.org/10.1016/j.physb.2013.05.023 2024-06-19T13:38:16Z In this paper, we present a phenomenological mathematical model for describing the features of the brine channels in sea ice. The differential system is composed of the Ginzburg–Landau and Cahn–Hilliard equations, in addition to the heat equation, that controls the ice–liquid phase transition by the temperature and hence the establishment of brine channels. The compatibility of this system with the thermodynamic laws and a maximum theorem is proved Article in Journal/Newspaper Sea ice Università degli Studi di Ferrara: CINECA IRIS Physica B: Condensed Matter 425 100 104
institution Open Polar
collection Università degli Studi di Ferrara: CINECA IRIS
op_collection_id ftunivferrarair
language English
topic Brine channel
Phase field
Cahn–Hilliard
Solute separation
spellingShingle Brine channel
Phase field
Cahn–Hilliard
Solute separation
V. Berti
M. Fabrizio
GRANDI, Diego
A phase field model for brine channels in sea ice
topic_facet Brine channel
Phase field
Cahn–Hilliard
Solute separation
description In this paper, we present a phenomenological mathematical model for describing the features of the brine channels in sea ice. The differential system is composed of the Ginzburg–Landau and Cahn–Hilliard equations, in addition to the heat equation, that controls the ice–liquid phase transition by the temperature and hence the establishment of brine channels. The compatibility of this system with the thermodynamic laws and a maximum theorem is proved
author2 V., Berti
M., Fabrizio
Grandi, Diego
format Article in Journal/Newspaper
author V. Berti
M. Fabrizio
GRANDI, Diego
author_facet V. Berti
M. Fabrizio
GRANDI, Diego
author_sort V. Berti
title A phase field model for brine channels in sea ice
title_short A phase field model for brine channels in sea ice
title_full A phase field model for brine channels in sea ice
title_fullStr A phase field model for brine channels in sea ice
title_full_unstemmed A phase field model for brine channels in sea ice
title_sort phase field model for brine channels in sea ice
publishDate 2013
url http://hdl.handle.net/11392/2362491
https://doi.org/10.1016/j.physb.2013.05.023
genre Sea ice
genre_facet Sea ice
op_relation info:eu-repo/semantics/altIdentifier/wos/WOS:000321697500018
volume:425
firstpage:100
lastpage:104
numberofpages:4
journal:PHYSICA. B, CONDENSED MATTER
http://hdl.handle.net/11392/2362491
doi:10.1016/j.physb.2013.05.023
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-84886944069
op_doi https://doi.org/10.1016/j.physb.2013.05.023
container_title Physica B: Condensed Matter
container_volume 425
container_start_page 100
op_container_end_page 104
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