Fluxes through steady chimneys in a mushy layer during binary alloy solidification

Abstract Solute transport within solidifying binary alloys occurs predominantly by convection from narrow liquid chimneys within a porous mushy layer. We develop a simple model that elucidates the dominant structure and driving forces of the flow, which could be applied to modelling brine fluxes fro...

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Published in:Journal of Fluid Mechanics
Main Authors: Rees Jones, David W., Worster, M. Grae
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2013
Subjects:
Online Access:http://dx.doi.org/10.1017/jfm.2012.462
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022112012004624
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spelling crcambridgeupr:10.1017/jfm.2012.462 2024-03-03T08:48:45+00:00 Fluxes through steady chimneys in a mushy layer during binary alloy solidification Rees Jones, David W. Worster, M. Grae 2013 http://dx.doi.org/10.1017/jfm.2012.462 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022112012004624 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Journal of Fluid Mechanics volume 714, page 127-151 ISSN 0022-1120 1469-7645 Mechanical Engineering Mechanics of Materials Condensed Matter Physics journal-article 2013 crcambridgeupr https://doi.org/10.1017/jfm.2012.462 2024-02-08T08:27:06Z Abstract Solute transport within solidifying binary alloys occurs predominantly by convection from narrow liquid chimneys within a porous mushy layer. We develop a simple model that elucidates the dominant structure and driving forces of the flow, which could be applied to modelling brine fluxes from sea ice, where a cheaply implementable approach is essential. A horizontal density gradient within the mushy layer in the vicinity of the chimneys leads to baroclinic torque which sustains the convective flow. In the bulk of the mushy layer, the isotherms are essentially horizontal. In this region, we impose a vertically linear temperature field and immediately find that the flow field is a simple corner flow. We determine the strength of this flow by finding a similarity solution to the governing mushy-layer equations in an active region near the chimney. We also determine the corresponding shape of the chimney, the vertical structure of the solid fraction and the interstitial flow field. We apply this model first to a periodic, planar array of chimneys and show analytically that the solute flux through the chimneys is proportional to a mush Rayleigh number. Secondly we extend the model to three dimensions and find that an array of chimneys can be characterized by the average drainage area alone. Therefore we solve the model in an axisymmetric geometry and find new, sometimes nonlinear, relationships between the solute flux, the Rayleigh number and the other dimensionless parameters of the system. Article in Journal/Newspaper Sea ice Cambridge University Press The Chimney ENVELOPE(-55.748,-55.748,52.617,52.617) Journal of Fluid Mechanics 714 127 151
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Mechanical Engineering
Mechanics of Materials
Condensed Matter Physics
spellingShingle Mechanical Engineering
Mechanics of Materials
Condensed Matter Physics
Rees Jones, David W.
Worster, M. Grae
Fluxes through steady chimneys in a mushy layer during binary alloy solidification
topic_facet Mechanical Engineering
Mechanics of Materials
Condensed Matter Physics
description Abstract Solute transport within solidifying binary alloys occurs predominantly by convection from narrow liquid chimneys within a porous mushy layer. We develop a simple model that elucidates the dominant structure and driving forces of the flow, which could be applied to modelling brine fluxes from sea ice, where a cheaply implementable approach is essential. A horizontal density gradient within the mushy layer in the vicinity of the chimneys leads to baroclinic torque which sustains the convective flow. In the bulk of the mushy layer, the isotherms are essentially horizontal. In this region, we impose a vertically linear temperature field and immediately find that the flow field is a simple corner flow. We determine the strength of this flow by finding a similarity solution to the governing mushy-layer equations in an active region near the chimney. We also determine the corresponding shape of the chimney, the vertical structure of the solid fraction and the interstitial flow field. We apply this model first to a periodic, planar array of chimneys and show analytically that the solute flux through the chimneys is proportional to a mush Rayleigh number. Secondly we extend the model to three dimensions and find that an array of chimneys can be characterized by the average drainage area alone. Therefore we solve the model in an axisymmetric geometry and find new, sometimes nonlinear, relationships between the solute flux, the Rayleigh number and the other dimensionless parameters of the system.
format Article in Journal/Newspaper
author Rees Jones, David W.
Worster, M. Grae
author_facet Rees Jones, David W.
Worster, M. Grae
author_sort Rees Jones, David W.
title Fluxes through steady chimneys in a mushy layer during binary alloy solidification
title_short Fluxes through steady chimneys in a mushy layer during binary alloy solidification
title_full Fluxes through steady chimneys in a mushy layer during binary alloy solidification
title_fullStr Fluxes through steady chimneys in a mushy layer during binary alloy solidification
title_full_unstemmed Fluxes through steady chimneys in a mushy layer during binary alloy solidification
title_sort fluxes through steady chimneys in a mushy layer during binary alloy solidification
publisher Cambridge University Press (CUP)
publishDate 2013
url http://dx.doi.org/10.1017/jfm.2012.462
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022112012004624
long_lat ENVELOPE(-55.748,-55.748,52.617,52.617)
geographic The Chimney
geographic_facet The Chimney
genre Sea ice
genre_facet Sea ice
op_source Journal of Fluid Mechanics
volume 714, page 127-151
ISSN 0022-1120 1469-7645
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/jfm.2012.462
container_title Journal of Fluid Mechanics
container_volume 714
container_start_page 127
op_container_end_page 151
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