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dc.contributor.authorSrinivasacharya, D.-
dc.contributor.authorChamkha, A.J.-
dc.contributor.authorSurende, O.-
dc.contributor.authorRashad, A.M.-
dc.date.accessioned2025-01-27T11:22:17Z-
dc.date.available2025-01-27T11:22:17Z-
dc.date.issued2015-
dc.identifier.citation10.5098/hmt.6.19en_US
dc.identifier.urihttp://localhost:8080/xmlui/handle/123456789/2994-
dc.descriptionNITWen_US
dc.description.abstractThe aim of the present article is to analyze the influence of thermal and mass stratification on natural convection heat and mass transfer over a porous vertical plate with uniform and constant wall temperature and concentration in porous medium. The Brinkman-Forchheimer based model is employed to describe the flow in the porous medium. The nonlinear governing equations and their associated boundary conditions are initially cast into dimensionless forms by pseudo-similarity variables. The resulting system of nonlinear, coupled partial differential equations is then solved numerically. The influence of pertinent parameters on the dimensionless velocity, temperature, concentration, heat and mass transfer coefficients are presented graphically.en_US
dc.language.isoenen_US
dc.publisherFrontiers in Heat and Mass Transferen_US
dc.subjectThermal stratificationen_US
dc.subjectSolutal stratificationen_US
dc.titleNATURAL CONVECTION ON A POROUS VERTICAL PLATE IN A DOUBLY STRATIFIED NON-DARCY POROUS MEDIUMen_US
dc.typeArticleen_US
Appears in Collections:Mathematics

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