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NUMERICAL STUDY OF OSCILLATORY CONVECTION DURING MELTING OF ICE IN A RECTANGULAR ENCLOSURE
A numerical investigation concerning natural-convection-dominated melting process of ice inside a rectangular enclosure has been performed to assess the inception of temporally oscillatory convective flow and heat transfer at high Rayleigh numbers previously unexplored. Numerical simulations using a...
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Published in: | Numerical heat transfer. Part A, Applications Applications, 2001-10, Vol.40 (5), p.511-530 |
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container_title | Numerical heat transfer. Part A, Applications |
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creator | HO, C. J HO, M. J YEH, C. T |
description | A numerical investigation concerning natural-convection-dominated melting process of ice inside a rectangular enclosure has been performed to assess the inception of temporally oscillatory convective flow and heat transfer at high Rayleigh numbers previously unexplored. Numerical simulations using a finite-difference method on a fixed grid have been undertaken for the two-dimensional ice-melting process in the enclosure with an aspect ratio of 0.5 under the following ranges of the relevant physical parameters: Ra H = 10 6 ~ 7 2 10 7 , Ste = 0.101, and Sc = 0.1 and 0.5. Numerical results reveal that for Ste = 0.101 and Sc = 0.5 with Ra S 1.2 2 10 7 , temporally oscillatory convective flow and temperature fields arise in the water region during the melting process inside the enclosure. Supplemental to the numerical simulations, temperature visualization experiments by means of a thermochromic liquid crystal as tracer have been conducted in a test cell mimicking the physical configuration under consideration. |
doi_str_mv | 10.1080/10407780152619810 |
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J ; HO, M. J ; YEH, C. T</creator><creatorcontrib>HO, C. J ; HO, M. J ; YEH, C. T</creatorcontrib><description>A numerical investigation concerning natural-convection-dominated melting process of ice inside a rectangular enclosure has been performed to assess the inception of temporally oscillatory convective flow and heat transfer at high Rayleigh numbers previously unexplored. Numerical simulations using a finite-difference method on a fixed grid have been undertaken for the two-dimensional ice-melting process in the enclosure with an aspect ratio of 0.5 under the following ranges of the relevant physical parameters: Ra H = 10 6 ~ 7 2 10 7 , Ste = 0.101, and Sc = 0.1 and 0.5. Numerical results reveal that for Ste = 0.101 and Sc = 0.5 with Ra S 1.2 2 10 7 , temporally oscillatory convective flow and temperature fields arise in the water region during the melting process inside the enclosure. Supplemental to the numerical simulations, temperature visualization experiments by means of a thermochromic liquid crystal as tracer have been conducted in a test cell mimicking the physical configuration under consideration.</description><identifier>ISSN: 1040-7782</identifier><identifier>EISSN: 1521-0634</identifier><identifier>DOI: 10.1080/10407780152619810</identifier><identifier>CODEN: NHAAES</identifier><language>eng</language><publisher>London: Informa UK Ltd</publisher><subject>Buoyancy-driven instability ; Exact sciences and technology ; Fluid dynamics ; Fundamental areas of phenomenology (including applications) ; Heat flow in porous media ; Heat transfer ; Heat transfer in inhomogeneous media, in porous media, and through interfaces ; Hydrodynamic stability ; Physics</subject><ispartof>Numerical heat transfer. 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Supplemental to the numerical simulations, temperature visualization experiments by means of a thermochromic liquid crystal as tracer have been conducted in a test cell mimicking the physical configuration under consideration.</description><subject>Buoyancy-driven instability</subject><subject>Exact sciences and technology</subject><subject>Fluid dynamics</subject><subject>Fundamental areas of phenomenology (including applications)</subject><subject>Heat flow in porous media</subject><subject>Heat transfer</subject><subject>Heat transfer in inhomogeneous media, in porous media, and through interfaces</subject><subject>Hydrodynamic stability</subject><subject>Physics</subject><issn>1040-7782</issn><issn>1521-0634</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2001</creationdate><recordtype>article</recordtype><recordid>eNqNkF1LwzAUhosoOD9-gHe5EO-q5yRp14I3pauz0LXQtcK8KVnXwKRbZ9Kh_nszpngxRHNzXsjzvAnHsq4QbhE8uEPgMBx6gA510fcQjqyByWiDy_ixyebeNgA9tc60fgFzKPUH1nNaTqI8DoOETItyNCPZA8mmYZwkQZHlMxJm6VMUFnGWklGZx-mYTKKk2E0DxmFE4pQEJDdIkI7LJMhJlIZJNi3z6MI6kaLVzeXXPLfKh6gIH-0kG-8etGsHsLc5NDUIR3KPLWDugkd9yX0HkSFKIUyu6dyVQF029wTzFx40TDLfBSobyik7t272vRvVvW4b3Verpa6bthXrptvqirqewzgf_gfkiHTXiHuwVp3WqpHVRi1XQn1UCNVu3dXBuo1z_VUudC1aqcS6XuofERmj6BhsuMeWa9mplXjrVLuoevHRdurbOSiv-vfemPd_muz3_30CiVaahw</recordid><startdate>20011001</startdate><enddate>20011001</enddate><creator>HO, C. 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Numerical results reveal that for Ste = 0.101 and Sc = 0.5 with Ra S 1.2 2 10 7 , temporally oscillatory convective flow and temperature fields arise in the water region during the melting process inside the enclosure. Supplemental to the numerical simulations, temperature visualization experiments by means of a thermochromic liquid crystal as tracer have been conducted in a test cell mimicking the physical configuration under consideration.</abstract><cop>London</cop><pub>Informa UK Ltd</pub><doi>10.1080/10407780152619810</doi><tpages>20</tpages></addata></record> |
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source | Taylor and Francis Science and Technology Collection |
subjects | Buoyancy-driven instability Exact sciences and technology Fluid dynamics Fundamental areas of phenomenology (including applications) Heat flow in porous media Heat transfer Heat transfer in inhomogeneous media, in porous media, and through interfaces Hydrodynamic stability Physics |
title | NUMERICAL STUDY OF OSCILLATORY CONVECTION DURING MELTING OF ICE IN A RECTANGULAR ENCLOSURE |
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