Use este identificador para citar ou linkar para este item: http://repositorio.ufc.br/handle/riufc/61588
Tipo: Artigo de Periódico
Título: The influence of baffles on the natural convection in trapezoidal cavities
Autor(es): Fontana, Éliton
Silva, Adriano da
Mariani, Viviana Cocco
Marcondes, Francisco
Palavras-chave: Finite-volume methods
Data do documento: 2010
Instituição/Editor/Publicador: Taylor & Francis Group, LLC
Citação: FONTANA, Éliton; SILVA, Adriano da; MARIANI, Viviana Cocco; MARCONDES, Francisco. The influence of baffles on the natural convection in trapezoidal cavities. Numerical Heat Transfer, Part A: Applications An International Journal of Computation and Methodology, v. 58, p. 125–145, 2010.
Abstract: This article presents an investigation into natural convection in trapezoidal cavities. It examines a cavity whose floor and upper inclined walls are both adiabatic, while the vertical walls are isothermal. For these isothermal walls, we consider two thermal boundary conditions. Under the first condition, the short wall on the left side is heated as the tall one on the right side is cooled. The second condition is the reverse of the first—the short wall is cooled as the tall one is heated. Considering laminar conditions and a two-dimensional system, steady-state computations are carried out to assess the effects of one and two baffles, the baffle's height (H b ), Rayleigh number, 103 ≤ Ra ≤ 106, and three Prandtl number values. To demonstrate the various effects, the results from several designed case studies are shown in terms of isotherms, streamlines, and local and average Nusselt numbers in order. Predictions reveal that the second baffle decreases the cavity's fluid flow and heat transfer. As the height of the baffle rises, the heat transfer drops drastically. Also, two baffles produce more pronounced thermal stratification than only one.
URI: http://www.repositorio.ufc.br/handle/riufc/61588
ISSN: 1040-7782 print
1521-0634 online
Aparece nas coleções:DEMM - Artigos publicados em revista científica

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