Abstract
We consider the effect of local thermal nonequilibrium on the stability properties of convection in a vertical porous channel heated and cooled from the sides. On using an energy stability analysis of the linearised stability equations, we show that the system remains unconditionally stable to small-amplitude disturbances.
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Abbreviations
- c :
-
Specific heat
- g :
-
Gravity
- h :
-
Interfacial heat transfer coefficient
- H :
-
Nondimensional form of h
- k :
-
Disturbance wavenumber
- L :
-
Width of the layer
- K :
-
Permeability
- p :
-
Pressure
- Ra :
-
Darcy–Rayleigh number
- t :
-
Time
- u :
-
Horizontal velocity
- v :
-
Vertical velocity
- x :
-
Horizontal coordinate
- y :
-
Vertical coordinate
- α :
-
Diffusivity ratio
- β :
-
Thermal expansion coefficient
- γ :
-
Scaled conductivity ratio
- θ :
-
Fluid temperature
- Θ:
-
Disturbance fluid temperature
- \({\overline{\Theta}}\) :
-
Complex conjugate of Θ
- λ:
-
Exponential growth rate
- μ :
-
Dynamic viscosity
- ρ :
-
Density
- \({\phi}\) :
-
Solid temperature
- Φ:
-
Disturbance solid temperature
- \({\overline{\Phi}}\) :
-
Complex conjugate of Φ
- ψ :
-
Stream function
- Ψ:
-
Disturbance stream function
- c:
-
Cold surface
- f:
-
Fluid phase
- h:
-
Hot surface
- s:
-
Solid phase
- ref:
-
Reference value
- ′:
-
Derivative with respect to x
- \({\hat{}}\) :
-
Dimensional
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Rees, D.A.S. The Effect of Local Thermal Nonequilibrium on the Stability of Convection in a Vertical Porous Channel. Transp Porous Med 87, 459–464 (2011). https://doi.org/10.1007/s11242-010-9694-5
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DOI: https://doi.org/10.1007/s11242-010-9694-5