Exact solutions for equations of flow and heat transfer in fluid saturated porous media

DOI10.1007/S13370-014-0258-7zbMath1325.76173OpenAlexW1995171944MaRDI QIDQ497028

E. T. Olodo, Villévo Adanhounme

Publication date: 23 September 2015

Published in: Afrika Matematika (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1007/s13370-014-0258-7

zbMATH Keywords

convectionboundary conditionspressure gradientporous matrix

Mathematics Subject Classification ID

PDEs in connection with fluid mechanics (35Q35) Flows in porous media; filtration; seepage (76S05) Solutions to PDEs in closed form (35C05)

Cites Work

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• Convection in a porous medium with inclined temperature gradient
• Convection in a porous medium with horizontal and vertical temperature gradients
• The Brinkman model for natural convection in a porous layer: Effects of nonuniform thermal gradient
• Influence of anisotropy on convection in porous media with nonuniform thermal gradient.
• Bounds on convection driven by internal heating

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