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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Format: | Journal article |
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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. |
first_indexed | 2024-03-07T02:02:17Z |
format | Journal article |
id | oxford-uuid:9dc43388-c585-46aa-8de3-2ec830be5eab |
institution | University of Oxford |
last_indexed | 2024-03-07T02:02:17Z |
publishDate | 2010 |
record_format | dspace |
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 |