The Bénard–Marangoni convection is studied in a three-dimensional container with thermally insulated lateral walls and prescribed heat flux at lower boundary. The upper surface of the incompressible, viscous fluid is assumed to be flat with temperature dependent surface tension. A Galerkin–Tau method with odd and even trial functions satisfying all the essential boundary conditions except the natural boundary conditions at the free surface has been used to solve the problem. The critical Marangoni and Rayleigh numbers are determined for the onset of steady convection as a function of aspect ratios x0 and y0 for the cases of Bénard–Marangoni, pure Marangoni and pure Bénard convections. It is observed that critical parameters are decreasing w...
Abstract: The three-dimensional instability of the thermocapillary convection in cylindrical undefor...
Thermal convection with shear flow has received widespread attention due to its importance in geophy...
The effects of a non-uniform temperature gradient and the Coriolis force on the onset of convection ...
In view of the interesting possibilities of controlling surface tension-driven convection, anticipat...
This manuscript addresses the linear stability analysis of a thermoconvective problem in an annular ...
he onset of Marangoni convection in a horizontal fluid layer with internal heat generation overlying...
12 pagesThe work described in this paper concerns the study of a Bénard–Marangoni convection problem...
Abstract: The onset of Marangoni convection in a horizontal fluid layer with a free surface overlyin...
In this paper, we study the onset of cellular convection in a horizontal fluid layer heated from bel...
The onset of cellular convection induced by surface tension gradients in a horizontal liquid layer h...
The onset of convection is studied in a rectangular channel filled with a fluid saturated porous med...
The effect of Brinkmann boundary layer on the onset of convection driven by surface tension gradient...
The onset of Marangoni convection in a horizontal fluid layer with internal heat generation overlyin...
Linear stability analysis is applied to investigate the effect of internal heat generation on Marang...
This research presents a new insight into Marangoni convection through investigating, both numerical...
Abstract: The three-dimensional instability of the thermocapillary convection in cylindrical undefor...
Thermal convection with shear flow has received widespread attention due to its importance in geophy...
The effects of a non-uniform temperature gradient and the Coriolis force on the onset of convection ...
In view of the interesting possibilities of controlling surface tension-driven convection, anticipat...
This manuscript addresses the linear stability analysis of a thermoconvective problem in an annular ...
he onset of Marangoni convection in a horizontal fluid layer with internal heat generation overlying...
12 pagesThe work described in this paper concerns the study of a Bénard–Marangoni convection problem...
Abstract: The onset of Marangoni convection in a horizontal fluid layer with a free surface overlyin...
In this paper, we study the onset of cellular convection in a horizontal fluid layer heated from bel...
The onset of cellular convection induced by surface tension gradients in a horizontal liquid layer h...
The onset of convection is studied in a rectangular channel filled with a fluid saturated porous med...
The effect of Brinkmann boundary layer on the onset of convection driven by surface tension gradient...
The onset of Marangoni convection in a horizontal fluid layer with internal heat generation overlyin...
Linear stability analysis is applied to investigate the effect of internal heat generation on Marang...
This research presents a new insight into Marangoni convection through investigating, both numerical...
Abstract: The three-dimensional instability of the thermocapillary convection in cylindrical undefor...
Thermal convection with shear flow has received widespread attention due to its importance in geophy...
The effects of a non-uniform temperature gradient and the Coriolis force on the onset of convection ...