Critical Rayleigh number of natural convection in high porosity anisotropic horizontal porous layers

DOI10.1016/J.IJHEATMASSTRANSFER.2009.11.045zbMath1183.80059OpenAlexW2016937210MaRDI QIDQ2379504

Yasuaki Shiina, Makoto Hishida

Publication date: 19 March 2010

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

Full work available at URL: https://doi.org/10.1016/j.ijheatmasstransfer.2009.11.045

zbMATH Keywords

natural convectioncritical Rayleigh numberhorizontal fluid layerBénard convectioneffective thermal conductivityDarcy flowanisotropic porous layer

Mathematics Subject Classification ID

Navier-Stokes equations for incompressible viscous fluids (76D05) Flows in porous media; filtration; seepage (76S05) Free convection (76R10) Experimental work for problems pertaining to classical thermodynamics (80-05)

Related Items (5)

Boundary and inertia effects on the stability of natural convection in a vertical layer of an anisotropic Lapwood-Brinkman porous medium ⋮ Nonhomogeneous porosity and thermal diffusivity effects on a double-diffusive convection in anisotropic porous media ⋮ Cattaneo-LTNE effects on the stability of Brinkman convection in an anisotropic porous layer ⋮ Nonlinear stability in microfluidic porous convection problems ⋮ Nonlinear stability of convection in a porous layer with solid partitions

Cites Work

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• Study on the efficiency of effective thermal conductivities on melting characteristics of latent heat storage capsules
• Laminar viscous flow through regular arrays of parallel solid cylinders
• Thermoconvective instabilities in a horizontal porous layer
• Nonlinear thermal convection in anisotropic porous media
• Time-periodic convection in porous media: the evolution of Hopf bifurcations with aspect ratio
• Convection Currents in a Porous Medium

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