Formation of brine channels in sea ice

Liquid salty micro-channels (brine) between growing ice platelets in sea ice are an important habitat for CO2-binding microalgaea with great impact on polar ecosystems. The structure formation of ice platelets is microscopically described and a phase field model is developed. The pattern formation d...

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Published in:The European Physical Journal E
Main Authors: Morawetz, K., Thoms, S., Kutschan, B.
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Online Access:http://hdl.handle.net/21.11116/0000-0000-D4DF-6
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spelling ftpubman:oai:pure.mpg.de:item_2472379 2023-08-20T04:09:43+02:00 Formation of brine channels in sea ice Morawetz, K. Thoms, S. Kutschan, B. 2017-03-01 http://hdl.handle.net/21.11116/0000-0000-D4DF-6 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1140/epje/i2017-11512-x http://hdl.handle.net/21.11116/0000-0000-D4DF-6 European Physical Journal E Structure formation and active systems info:eu-repo/semantics/article 2017 ftpubman https://doi.org/10.1140/epje/i2017-11512-x 2023-08-01T23:29:11Z Liquid salty micro-channels (brine) between growing ice platelets in sea ice are an important habitat for CO2-binding microalgaea with great impact on polar ecosystems. The structure formation of ice platelets is microscopically described and a phase field model is developed. The pattern formation during solidification of the two-dimensional interstitial liquid is considered by two coupled order parameters, the tetrahedricity as structure of ice and the salinity. The coupling and time evolution of these order parameters are described by a consistent set of three model parameters. They determine the velocity of the freezing process and the structure formation, the phase diagram, the super-cooling and super-heating region, and the specific heat. The model is used to calculate the short-time frozen micro-structures. The obtained morphological structure is compared with the vertical brine pore space obtained from X-ray computed tomography. Article in Journal/Newspaper Sea ice Max Planck Society: MPG.PuRe The European Physical Journal E 40 3
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language English
topic Structure formation and active systems
spellingShingle Structure formation and active systems
Morawetz, K.
Thoms, S.
Kutschan, B.
Formation of brine channels in sea ice
topic_facet Structure formation and active systems
description Liquid salty micro-channels (brine) between growing ice platelets in sea ice are an important habitat for CO2-binding microalgaea with great impact on polar ecosystems. The structure formation of ice platelets is microscopically described and a phase field model is developed. The pattern formation during solidification of the two-dimensional interstitial liquid is considered by two coupled order parameters, the tetrahedricity as structure of ice and the salinity. The coupling and time evolution of these order parameters are described by a consistent set of three model parameters. They determine the velocity of the freezing process and the structure formation, the phase diagram, the super-cooling and super-heating region, and the specific heat. The model is used to calculate the short-time frozen micro-structures. The obtained morphological structure is compared with the vertical brine pore space obtained from X-ray computed tomography.
format Article in Journal/Newspaper
author Morawetz, K.
Thoms, S.
Kutschan, B.
author_facet Morawetz, K.
Thoms, S.
Kutschan, B.
author_sort Morawetz, K.
title Formation of brine channels in sea ice
title_short Formation of brine channels in sea ice
title_full Formation of brine channels in sea ice
title_fullStr Formation of brine channels in sea ice
title_full_unstemmed Formation of brine channels in sea ice
title_sort formation of brine channels in sea ice
publishDate 2017
url http://hdl.handle.net/21.11116/0000-0000-D4DF-6
genre Sea ice
genre_facet Sea ice
op_source European Physical Journal E
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1140/epje/i2017-11512-x
http://hdl.handle.net/21.11116/0000-0000-D4DF-6
op_doi https://doi.org/10.1140/epje/i2017-11512-x
container_title The European Physical Journal E
container_volume 40
container_issue 3
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