The effects of a nonuniform temp. gradient and magnetic field on the onset of convection driven by surface tension in a horizontal layer of Boussinesq fluid with suspended particles confined between an upper free/adiabatic boundary and a lower rigid/isothermal boundary are considered. A linear stability anal. is performed. The microrotation is assumed to vanish at the boundaries. The Galerkin technique is used to obtain the eigenvalues. The effect of various parameters on the onset of convection was analyzed. Six different nonuniform temp. profiles are considered and their comparative effect on onset is discussed. It is obsd. that the elec. conducting fluid layer with suspended particles heated from below is more stable compared to ...
This paper studied the problem of Bénard-Marangoni convection in a horizontal fluid layer heated fro...
Microgravity conditions pose unique challenges for fluid handling and heat transfer applications. By...
The onset of Marangoni convection driven by surface tension gradients in a thin horizontal fluid lay...
77-83The effects of a non-uniform temperature gradient and magnetic field on the onset of convectio...
The effects of a non-uniform temperature gradient and magnetic field on the onset of convection driv...
The effect of a non-uniform basic temperature gradient on the onset of convection driven by surface ...
The effects of magnetic field and non-uniform basic temperature gradient on the onset of Rayleigh-B...
Effect of a non-uniform basic temperature gradient and magnetic field on the onset of Marangoni conv...
The effects of a non-uniform temperature gradient and the Coriolis force on the onset of convection ...
The effect of non-uniform temperature gradient and a uniform magnetic field on the onset of magneto-...
The effect of non-uniform temperature gradient on the onset of Rayleigh-Bénard-Marangoni- Magneto-co...
Microgravity conditions pose unique challenges for fluid handling and heat transfer applications. By...
The combined effects of a uniform vertical magnetic field and a nonuniform basic temperature profile...
The problem of thermal convection in a fluid layer driven by either buoyancy (Bénard) or thermocapi...
With the presence of a uniform vertical magnetic field and suspended particles, thermocapillary inst...
This paper studied the problem of Bénard-Marangoni convection in a horizontal fluid layer heated fro...
Microgravity conditions pose unique challenges for fluid handling and heat transfer applications. By...
The onset of Marangoni convection driven by surface tension gradients in a thin horizontal fluid lay...
77-83The effects of a non-uniform temperature gradient and magnetic field on the onset of convectio...
The effects of a non-uniform temperature gradient and magnetic field on the onset of convection driv...
The effect of a non-uniform basic temperature gradient on the onset of convection driven by surface ...
The effects of magnetic field and non-uniform basic temperature gradient on the onset of Rayleigh-B...
Effect of a non-uniform basic temperature gradient and magnetic field on the onset of Marangoni conv...
The effects of a non-uniform temperature gradient and the Coriolis force on the onset of convection ...
The effect of non-uniform temperature gradient and a uniform magnetic field on the onset of magneto-...
The effect of non-uniform temperature gradient on the onset of Rayleigh-Bénard-Marangoni- Magneto-co...
Microgravity conditions pose unique challenges for fluid handling and heat transfer applications. By...
The combined effects of a uniform vertical magnetic field and a nonuniform basic temperature profile...
The problem of thermal convection in a fluid layer driven by either buoyancy (Bénard) or thermocapi...
With the presence of a uniform vertical magnetic field and suspended particles, thermocapillary inst...
This paper studied the problem of Bénard-Marangoni convection in a horizontal fluid layer heated fro...
Microgravity conditions pose unique challenges for fluid handling and heat transfer applications. By...
The onset of Marangoni convection driven by surface tension gradients in a thin horizontal fluid lay...