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...
Published in: | Physica B: Condensed Matter |
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Online Access: | http://hdl.handle.net/11392/2362491 https://doi.org/10.1016/j.physb.2013.05.023 |
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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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1809939814815891456 |