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Onset of Convection in Two-Dimensional Porous Cavities with Open and Conducting Boundaries

TLDR
In this article, the onset of thermal convection in two-dimensional porous cavities heated from below is studied theoretically, and the critical Rayleigh number is calculated as a function of geometric parameters, including the tilt angle of the rectangle and ellipse.
Abstract
The onset of thermal convection in two-dimensional porous cavities heated from below is studied theoretically. An open (constant-pressure) boundary is assumed, with zero perturbation temperature (thermally conducting). The resulting eigenvalue problem is a full fourth-order problem without degeneracies. Numerical results are presented for rectangular and elliptical cavities, with the circle as a special case. The analytical solution for an upright rectangle confirms the numerical results. Streamlines penetrating the open cavities are plotted, together with the isotherms for the associated closed thermal cells. Isobars forming pressure cells are depicted for the perturbation pressure. The critical Rayleigh number is calculated as a function of geometric parameters, including the tilt angle of the rectangle and ellipse. An improved physical scaling of the Darcy–Benard problem is suggested. Its significance is indicated by the ratio of maximal vertical velocity to maximal temperature perturbation.

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Journal ArticleDOI

Two-dimensional Darcy-Bénard Convection evolving in Fourier Space

TL;DR: In this article , a nonlinear transient convection in a porous rectangle heated from below is studied by an analytically based method, where Fourier series for the temperature and stream function are applied, where each Fourier coefficient evolves in time according to a coupled set of ordinary differential equations.
References
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Book

Convection in Porous Media

TL;DR: In this paper, an introduction to convection in porous media assumes the reader is familiar with basic fluid mechanics and heat transfer, going on to cover insulation of buildings, energy storage and recovery, geothermal reservoirs, nuclear waste disposal, chemical reactor engineering and the storage of heat-generating materials like grain and coal.
Journal ArticleDOI

Convection of a fluid in a porous medium

E. R. Lapwood
TL;DR: In this article, it was shown that under certain conditions convective flow may occur in fluid which permeates a porous stratum and is subject to a vertical temperature gradient, on the assumption that the flow obeys Darcy's law.
Journal ArticleDOI

Convection Currents in a Porous Medium

TL;DR: In this paper, it was shown that the minimum temperature gradient for which convection can occur is approximately 4π2h2μ/kgρ0α D2, where h2 is the thermal diffusivity, g is the acceleration of gravity, μ is the viscosity, k is the permeability, α is the coefficient of cubical expansion, ρ 0 is the density at zero temperature, and D is the thickness of the layer; this exceeds the limiting gradient found by Rayleigh for a simple fluid by a factor of 16D2/27π2
Journal ArticleDOI

Onset of Thermohaline Convection in a Porous Medium

TL;DR: In this article, the problem of the onset of convection, induced by buoyancy effects resulting from vertical thermal and solute concentration gradients, in a horizontal layer of a saturated porous medium, is treated by linear perturbation analysis.
Journal ArticleDOI

The stability of a viscous liquid in a vertical tube containing porous material

TL;DR: In this paper, it was shown that the ratio κ / Dϵ = 0·633, where D is the molecular diffusivity of the solute when the porous medium is absent, is a property of the porous material alone and can be determined directly by diffusion measurements.
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