Sea water freezing modes in a natural convection system

Sea ice is crucial in many natural processes and human activities. Understanding the dynamical couplings between the inception, growth and equilibrium of sea ice and the rich fluid mechanical processes occurring at its interface and interior is of relevance in many domains, ranging from geophysics t...

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Main Authors: Du, Yihong, Wang, Ziqi, Jiang, Linfeng, Calzavarini (admin), Enrico, Sun, Chao
Other Authors: Unité de Mécanique de Lille - ULR 7512 UML, Laboratoire de Mécanique de Lille - FRE 3723 LML, Tsinghua University Beijing THU
Format: Other/Unknown Material
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:https://hdl.handle.net/20.500.12210/93131
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spelling ftunivlilleoa:oai:lilloa.univ-lille.fr:20.500.12210/93131 2024-01-14T10:10:36+01:00 Sea water freezing modes in a natural convection system Du, Yihong Wang, Ziqi Jiang, Linfeng Calzavarini (admin), Enrico Sun, Chao Unité de Mécanique de Lille - ULR 7512 UML Laboratoire de Mécanique de Lille - FRE 3723 LML Tsinghua University Beijing THU 2023-04-10 application/octet-stream https://hdl.handle.net/20.500.12210/93131 Anglais eng Cambridge University Press (CUP) 10.1017/jfm.2023.215 Journal of Fluid Mechanics http://hdl.handle.net/20.500.12210/93131 info:eu-repo/semantics/openAccess Compte-rendu et recension critique d'ouvrage 2023 ftunivlilleoa https://doi.org/20.500.12210/93131 2023-12-20T17:11:47Z Sea ice is crucial in many natural processes and human activities. Understanding the dynamical couplings between the inception, growth and equilibrium of sea ice and the rich fluid mechanical processes occurring at its interface and interior is of relevance in many domains, ranging from geophysics to marine engineering. Here we investigate experimentally the complete freezing process of water with dissolved salt in a standard natural convection system, i.e. the prototypical Rayleigh–Bénard cell. Due to the presence of a mushy phase, the studied system is considerably more complex than the freezing of fresh water in the same conditions (Wang et al. , Proc. Natl Acad. Sci. USA , vol. 118, issue 10, 2021, e2012870118). We measure the ice thickness and porosity at the dynamical equilibrium state for different initial salinities of the solution and temperature gaps across the cell. These observables are non-trivially related to the controlling parameters of the system as they depend on the heat transport mode across the cell. We identify in the experiments five out of the six possible modes of heat transport. We highlight the occurrence of brine convection through the mushy ice and of penetrative convection in stably stratified liquid underlying the ice. A one-dimensional multi-layer heat flux model built on the known scaling relations of global heat transport in natural convection systems in liquids and porous media is proposed. Given the measured porosity of the ice, it allows us to predict the corresponding ice thickness, in a unified framework. 960 Other/Unknown Material Sea ice LillOA (Lille Open Archive - Université de Lille)
institution Open Polar
collection LillOA (Lille Open Archive - Université de Lille)
op_collection_id ftunivlilleoa
language English
description Sea ice is crucial in many natural processes and human activities. Understanding the dynamical couplings between the inception, growth and equilibrium of sea ice and the rich fluid mechanical processes occurring at its interface and interior is of relevance in many domains, ranging from geophysics to marine engineering. Here we investigate experimentally the complete freezing process of water with dissolved salt in a standard natural convection system, i.e. the prototypical Rayleigh–Bénard cell. Due to the presence of a mushy phase, the studied system is considerably more complex than the freezing of fresh water in the same conditions (Wang et al. , Proc. Natl Acad. Sci. USA , vol. 118, issue 10, 2021, e2012870118). We measure the ice thickness and porosity at the dynamical equilibrium state for different initial salinities of the solution and temperature gaps across the cell. These observables are non-trivially related to the controlling parameters of the system as they depend on the heat transport mode across the cell. We identify in the experiments five out of the six possible modes of heat transport. We highlight the occurrence of brine convection through the mushy ice and of penetrative convection in stably stratified liquid underlying the ice. A one-dimensional multi-layer heat flux model built on the known scaling relations of global heat transport in natural convection systems in liquids and porous media is proposed. Given the measured porosity of the ice, it allows us to predict the corresponding ice thickness, in a unified framework. 960
author2 Unité de Mécanique de Lille - ULR 7512 UML
Laboratoire de Mécanique de Lille - FRE 3723 LML
Tsinghua University Beijing THU
format Other/Unknown Material
author Du, Yihong
Wang, Ziqi
Jiang, Linfeng
Calzavarini (admin), Enrico
Sun, Chao
spellingShingle Du, Yihong
Wang, Ziqi
Jiang, Linfeng
Calzavarini (admin), Enrico
Sun, Chao
Sea water freezing modes in a natural convection system
author_facet Du, Yihong
Wang, Ziqi
Jiang, Linfeng
Calzavarini (admin), Enrico
Sun, Chao
author_sort Du, Yihong
title Sea water freezing modes in a natural convection system
title_short Sea water freezing modes in a natural convection system
title_full Sea water freezing modes in a natural convection system
title_fullStr Sea water freezing modes in a natural convection system
title_full_unstemmed Sea water freezing modes in a natural convection system
title_sort sea water freezing modes in a natural convection system
publisher Cambridge University Press (CUP)
publishDate 2023
url https://hdl.handle.net/20.500.12210/93131
genre Sea ice
genre_facet Sea ice
op_relation 10.1017/jfm.2023.215
Journal of Fluid Mechanics
http://hdl.handle.net/20.500.12210/93131
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/20.500.12210/93131
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