Effects of transverse magnetic field on mixed convection in wall plume of power-law fluids

DOI10.1016/0020-7225(93)90111-7zbMath0777.76099OpenAlexW1973565248MaRDI QIDQ1261680

Rama Subba Reddy Gorla, Shoichiro Nakamura, Jin Kook Lee, Ioan Pop

Publication date: 4 October 1993

Published in: International Journal of Engineering Science (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/0020-7225(93)90111-7

zbMATH Keywords

finite difference schemevertical adiabatic surfacenonsimilar boundary layer solutions

Mathematics Subject Classification ID

Non-Newtonian fluids (76A05) Magnetohydrodynamics and electrohydrodynamics (76W05) Free convection (76R10) Forced convection (76R05)

Related Items (8)

Effects of viscous dissipation and heat generation (absorption) in a thermal boundary layer of a non-Newtonian fluid over a continuously moving permeable flat plate ⋮ MHD flow of an Oldroyd-B fluid due to non-coaxial rotations of a porous disk and the fluid at infinity ⋮ Magnetohydrodynamic free convection boundary layer flow of a thermomicropolar fluid over a vertical plate ⋮ Influence of Hall current on the flows of a generalized Oldroyd-B fluid in a porous space ⋮ Nonsimilar solutions for free convection from a nonisothermal vertical plate in a micropolar fluid ⋮ Free convection in micropolar fluids over a uniformly heated vertical plate ⋮ Two-phase mixed convection nanofluid flow of a dusty tangent hyperbolic past a nonlinearly stretching sheet ⋮ Laminar boundary layer flow of power-law fluids over wavy surfaces

Cites Work

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• Mixed convection in wall plumes
• Mixed convection plume above a horizontal line source situated in a forced convection approach flow
• Mixed convection from a horizontal line source of heat
• Mixed convection in an axisymmetric buoyant plume
• Vertical mixed convection flow about a horizontal line source of heating or cooling
• A computer extended series examination of mixed convection in a buoyant plume
• MIXED CONVECTION IN AN AXISYMMETRIC BUOYANT PLUME
• Mixed convection in a two-dimensional buoyant plume
• The laminar plume above a line heat source in a transverse magnetic field

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