Effects of flow inertia on vertical, natural convection in saturated, porous media

DOI10.1016/0017-9310(86)90126-2zbMath0594.76082OpenAlexW2000722647MaRDI QIDQ1077289

B. George

Publication date: 1986

Published in: International Journal of Heat and Mass Transfer (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/0017-9310(86)90126-2

zbMATH Keywords

porous mediaequationslayernon-similar solutionsplane plume flowsnon-similarboundary-layer approximationseffects of flow inertiamicrostructure of porous matrixnon-Darcy regimepure-Darcy flowsaturated,thermal boundaryuniform heat flux surfacevertical, natural convection

Mathematics Subject Classification ID

Flows in porous media; filtration; seepage (76S05) Free convection (76R10) Basic methods in fluid mechanics (76M99)

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Transient non-Darcy free convection with temperature dependent viscosity ⋮ Forced convective flow and heat transfer over a~porous plate in a Darcy-Forchheimer porous medium in presence of radiation ⋮ Non-Darcy regime mixed convection on vertical plates in saturated porous media with lateral mass flux ⋮ Analysis of heat transfer over a plate in a porous medium with a convective boundary condition ⋮ Computational study of MHD free convection flow of non-Newtonian tangent hyperbolic fluid from a vertical surface in porous media with Hall/ionslip currents and ohmic dissipation ⋮ Filling box flows in porous media ⋮ Impact of Transverse Magnetic Field Thermal Radiation on Non-darcy Forced Convection Flow

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