Convection in a porous medium with horizontal and vertical temperature gradients

DOI10.1016/0017-9310(74)90085-4zbMath0325.76125OpenAlexW2023326190MaRDI QIDQ1225538

Jan Erik H. Weber

Publication date: 1974

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

Full work available at URL: http://urn.nb.no/URN:NBN:no-52921

Mathematics Subject Classification ID

Flows in porous media; filtration; seepage (76S05) Forced convection (76R05)

Related Items (9)

Absolute/convective instability dichotomy at the onset of convection in a porous layer with either horizontal or vertical solutal and inclined thermal gradients, and horizontal throughflow ⋮ Onset of electroconvective instability of Oldroydian viscoelastic liquid layer in Brinkman porous medium ⋮ Nonlinear thermal instability in a horizontal porous layer with an internal heat source and mass flow ⋮ Soret-driven thermosolutal convection induced by inclined thermal and solutal gradients in a shallow horizontal layer of a porous medium ⋮ Double-diffusive Hadley-Prats flow in a horizontal porous layer with a concentration based internal heat source ⋮ Unicellular natural circulation in a shallow horizontal porous layer heated from below by a constant flux ⋮ Three-dimensional absolute and convective instabilities at the onset of convection in a porous medium with inclined temperature gradient and vertical throughflow ⋮ Exact solutions for equations of flow and heat transfer in fluid saturated porous media ⋮ On Hadley flow in a porous layer with vertical heterogeneity

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