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Showing papers on "Boussinesq approximation (buoyancy) published in 2001"


Journal ArticleDOI
TL;DR: In this paper, the Navier-Stokes equations are simplified with the Boussinesq approximation and solved by a finite difference method, and the amplitude of fluctuations in spatially averaged kinetic energy density K tends to be large when fluid is stationary everywhere over some interval of time during each period, and has a peak when fluid begins to move continuously throughout one period.
Abstract: In this numerical study, we investigate natural convection in a two-dimensional square-section enclosure vibrating sinusoidally parallel to the applied temperature gradient in a zero-gravity field. The full Navier-Stokes equations are simplified with the Boussinesq approximation and solved by a finite difference method. Whereas the Prandtl number Pr is fixed to 7.1 (except for some test cases with Pr = 7.0, 6.8), the vibrational Rayleigh number Ra based on acceleration amplitude is varied from 1.0 x 10 4 to 1.0 x 10 5 , and dimensionless angular frequency ω is varied from 1.0 x 10° to 1.0 x 10 3 . In the tested range, time evolutions exhibit synchronous, 1/2-subharmonic and non-periodic responses, and flow patterns are characterized mainly by one- or two-cell structures. Flow-regime diagrams show considerable differences from results in a non-zero-mean-gravity field even at large acceleration amplitudes, and suggest that some parts of non-periodic-response regimes may be related to transitions between flow patterns. The amplitude of fluctuations in spatially averaged kinetic energy density K (equal to the difference between maximum and minimum kinetic energies over a cycle) tends to be large when fluid is stationary everywhere over some interval of time during each period, and has a peak when fluid begins to move continuously throughout one period. Such peaks are caused by impulsively started convection, and are not connected to resonant oscillations in a constant-gravity field.

47 citations


Journal ArticleDOI
L. Kalla1, Patrick Vasseur1, R. Benacer, H. Beji, R. Duval 
TL;DR: In this paper, a double-duffusive natural convection within a horizontal porous layer is studied both analytically and numerically, and the existence of multiple steady state solutions for a given set of the governing parameters is demonstrated.

32 citations


Journal ArticleDOI
TL;DR: In this paper, the Darcy model with the Boussinesq approximation is used to study double-diffusive natural convection in a shallow porous cavity, where the horizontal walls are subject to uniform fluxes of heat and mass, while the side vertical walls are exposed to a constant heat flux of intensity aq ′, where a is a real number.

23 citations


Journal ArticleDOI
TL;DR: In this paper, the physics of the Kelvin body force and the buoyancy it creates are explained using the Boussinesq approximation, and closed form and numerical similarity solutions for steady, laminar, two-dimensional plumes driven by the interaction of a line heat source and a non-uniform magnetic field are obtained and discussed.

11 citations