Convection and heat transfer in layered sloping warm-water aquifers

What convective flow is induced if a geologically-tratified groundwater aquifer is subject to a vertical temperature gradient? How strong is the flow? What is the nett heat transfer? Is the flow stable? How does the convection affect the subsequent species distribution if a pollutant finds its way i...

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Main Authors: McKibbin, R, Hale, N, Style, R, Walters, N
Format: Journal article
Published: 2010
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author McKibbin, R
Hale, N
Style, R
Walters, N
author_facet McKibbin, R
Hale, N
Style, R
Walters, N
author_sort McKibbin, R
collection OXFORD
description What convective flow is induced if a geologically-tratified groundwater aquifer is subject to a vertical temperature gradient? How strong is the flow? What is the nett heat transfer? Is the flow stable? How does the convection affect the subsequent species distribution if a pollutant finds its way into the aquifer? This paper begins to address such questions. Quantitative models for buoyancy-driven fluid flow in long, sloping warm-water aquifers with both smoothly- and discretely-layered structures are formulated. The steady-state profiles are calculated for the temperature and for the fluid specific volume flux (Darcy velocity) parallel to the boundaries in a sloping system subjected to a perpendicular temperature gradient, at low Rayleigh numbers. The conducted and advected heat fluxes are compared and it is shown that the system acts somewhat like a heat pipe. The maximum possible ratio of naturally advected-to-conducted heat transfer is determined, together with the corresponding permeability and thermal conductivity profiles.
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spelling oxford-uuid:9dc43388-c585-46aa-8de3-2ec830be5eab2022-03-27T00:45:27ZConvection and heat transfer in layered sloping warm-water aquifersJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:9dc43388-c585-46aa-8de3-2ec830be5eabMathematical Institute - ePrints2010McKibbin, RHale, NStyle, RWalters, NWhat convective flow is induced if a geologically-tratified groundwater aquifer is subject to a vertical temperature gradient? How strong is the flow? What is the nett heat transfer? Is the flow stable? How does the convection affect the subsequent species distribution if a pollutant finds its way into the aquifer? This paper begins to address such questions. Quantitative models for buoyancy-driven fluid flow in long, sloping warm-water aquifers with both smoothly- and discretely-layered structures are formulated. The steady-state profiles are calculated for the temperature and for the fluid specific volume flux (Darcy velocity) parallel to the boundaries in a sloping system subjected to a perpendicular temperature gradient, at low Rayleigh numbers. The conducted and advected heat fluxes are compared and it is shown that the system acts somewhat like a heat pipe. The maximum possible ratio of naturally advected-to-conducted heat transfer is determined, together with the corresponding permeability and thermal conductivity profiles.
spellingShingle McKibbin, R
Hale, N
Style, R
Walters, N
Convection and heat transfer in layered sloping warm-water aquifers
title Convection and heat transfer in layered sloping warm-water aquifers
title_full Convection and heat transfer in layered sloping warm-water aquifers
title_fullStr Convection and heat transfer in layered sloping warm-water aquifers
title_full_unstemmed Convection and heat transfer in layered sloping warm-water aquifers
title_short Convection and heat transfer in layered sloping warm-water aquifers
title_sort convection and heat transfer in layered sloping warm water aquifers
work_keys_str_mv AT mckibbinr convectionandheattransferinlayeredslopingwarmwateraquifers
AT halen convectionandheattransferinlayeredslopingwarmwateraquifers
AT styler convectionandheattransferinlayeredslopingwarmwateraquifers
AT waltersn convectionandheattransferinlayeredslopingwarmwateraquifers