Effects of vertical throughflow and variable gravity field on double diffusive convection in a fluid layer

Diffusion (76R50) Nonlinear effects in hydrodynamic stability (76E30) Spectral methods applied to problems in fluid mechanics (76M22) Free convection (76R10) Convection in hydrodynamic stability (76E06) Diffusive and convective heat and mass transfer, heat flow (80A19)

Cites Work

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Heat and mass transfer by convection in multicomponent Navier-Stokes mixtures: absence of subcritical instabilities and global nonlinear stability via the Auxiliary System Method
Double-diffusive penetrative convection simulated via internal heating in an anisotropic porous layer with throughflow
Onset of convection in a porous medium with internal heat source and variable gravity
Penetrative convection in a fluid layer with throughflow
Thermal stability of a fluid layer under variable body forces
Convection in a variable gravity field
On the nonlinear stability of a fluid layer of a mixture heated and salted from below
The energy method, stability, and nonlinear convection.
Effects of throughflow and internal heat generation on the onset of convection in a fluid layer
The onset of convection in a magnetic nanofluid layer with variable gravity effects
Effects of spatially varying gravity, temperature and concentration fields on the stability of a chemically reacting fluid layer
Convective instability in a temperature and concentration field
Global stability of the conduction-diffusion solution
Convection in a porous medium with internal heat source and variable gravity effects
Steady subcritical thermohaline convection
Variable viscosity effects on convective instability in superposed fluid and porous layers
Global stability for penetrative convection with throughflow in a porous material
Nonlinear convection in a porous medium with inclined temperature gradient and variable gravity effects
Global nonlinear exponential stability of the conduction-diffusion solution for Schmidt numbers greater than Prandtl numbers
Slip boundary conditions and through flow effects on double-diffusive convection in internally heated heterogeneous Brinkman porous media

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