Abstract
We investigate Rayleigh–Benard convection in a porous layer subjected to gravitational and Coriolis body forces, when the fluid and solid phases are not in local thermodynamic equilibrium. The Darcy model (extended to include Coriolis effects and anisotropic permeability) is used to describe the flow, whilst the two-equation model is used for the energy equation (for the solid and fluid phases separately). The linear stability theory is used to evaluate the critical Rayleigh number for the onset of convection and the effect of both thermal and mechanical anisotropy on the critical Rayleigh number is discussed.
Similar content being viewed by others
Abbreviations
- g * :
-
Acceleration due to gravity
- H * :
-
Height of the mushy layer
- ê z :
-
Unit vector in the z-direction
- k x ,k y ,k z :
-
Characteristic permeabilities in the x-, y- and z- directions
- L :
-
Length of the mushy layer
- p :
-
Reduced pressure
- Pr :
-
Prandtl number, ν*/κ *
- R :
-
Scaled Rayleigh number, Ra/π 2
- Ra :
-
Rayleigh number, \({\rho _{\ast 0} g_\ast \beta _\ast \Delta Tk_{\ast z} H_\ast \rho _{\ast f} c_{\ast f}}/({\kappa _{\ast fz} \mu _\ast})\)
- s x :
-
x-component of wavenumber
- s y :
-
y-component of wavenumber
- t :
-
Time
- T f :
-
Dimensionless temperature,(T f * −T C )(T H −T C )
- T s :
-
Dimensionless temperature,(T s * −T C)(T H −T C)
- u :
-
Horizontal x-component of the filtration velocity
- V :
-
Dimensionless filtration velocity vector, \(u\hat {e}_x +v\hat {e}_y +w\hat {e}_z\)
- v :
-
Horizontal y-component of filtration velocity
- w :
-
Vertical component of filtration velocity
- X :
-
Space vector, \(x\hat {e}_x +y\hat {e}_y +z\hat {e}_z\)
- x :
-
Horizontal length co-ordinate
- y :
-
Horizontal width co-ordinate
- z :
-
Vertical co-ordinate
- α :
-
Scaled wavenumber, s 2/π2
- β :
-
Thermal expansion coefficient
- η :
-
thermal conductivity ratio, \({\kappa _{\ast (.)x}}/{\kappa _{\ast (.)z}} {\kappa _{\ast (.)y}}/{\kappa _{\ast (.)z}}\)
- \(\phi\) :
-
Porosity
- κ :
-
Thermal conductivity
- λ :
-
Parameter akin to the Nield number
- μ :
-
Dynamic viscosity of the fluid
- ν :
-
Kinematic viscosity
- ρ :
-
Fluid density
- ω :
-
Angular velocity
- ξ :
-
Anisotropy ratio,\({k_{\ast x}}/{k_{\ast z}}{{k_{\ast y}} /{k_{\ast z}}}\)
- *:
-
Dimensional quantities
- o :
-
Rescaled parameters
- B :
-
Basic flow quantities
- cr:
-
Critical values
- f x , f y , f z :
-
Fluid conditions in the x-, y- and z- directions
- s x , s y , s z :
-
Solid conditions in the x-, y- and z- directions
References
Alex S.M., Patil P.R. (2000) Thermal instability in an anisotropic rotating porous medium. J. Fluid Mech. 252, 79–98
Banu N., Rees D.A.S. (2002) Onset of Darcy–Benard convection using a thermal non-equilibrium model. Int. J. Heat Mass Transfer. 45, 2221–2228
Bejan A. Convection Heat Transfer, 2nd edn. Wiley (1995)
Epherre J.F. (1975) Critère d’apparition de la convection naturelle dans une couche poreuse anisotrope. Rev. Gen. Therm. 168, 949–950
Govender, S.: On the effect of anisotropy on the stability of convection in rotating porous media, Trans Porous Media 64, 413–422 (2006a) (In Press)
Govender, S.: Coriolis effect on the stability of centrifugally driven convection in a rotating anisotropic porous layer subjected to gravity, Trans Porous Media (TiPM 264) (2006b) (In Press)
Kuznetsov, A.V.: Thermal nonequilibrium forced convection in porous media, Transport Phenomena in Porous Media, pp. 103–129. Pergamon (An imprint of Elsevier Science), Netherlands
Malashetty M.S., Shivakumara I.S., Kulkarni S. (2005) The onset of convection in an anisotropic porous layer using a thermal non-equilibrium model. Trans. Porous Media 60, 199–215
McKibbin R. (1986) Thermal convection in a porous layer: Effects of anisotropy and surface boundary conditions. Trans. in Porous Media 1, 271–292
Nield D.A., Bejan, A.: Convection in Porous Media. Springer (1992)
Storesletten L. (1993) Natural convection in a horizontal porous layer with anisotropic thermal diffusivity. Trans. Porous Media 12, 19–29
Vadasz P. (1992) Natural convection in porous media induced by the centrifugal body force: the solution for small aspect ratio. ASME J. Energy Res. Tech. 114, 250–254
Vadasz P. (1993a) Fluid flow through heterogenous porous media in a rotating square channel. Trans. Porous Media 12, 43–54
Vadasz P. (1993b) Three-dimensional free convection in a long rotating porous box: analytical solution. ASME J. Heat Transfer 115, 639–644
Vadasz P. (1994a) Stability of free convection in a narrow porous layer subject to rotation. Int. Comm. Heat Mass Transfer 21, 881–890
Vadasz P. (1994b) Centrifugally generated free convection in a rotating porous box. Int. J. Heat Mass Transfer. 37, 2399–2404
Vadasz P. (1995) Coriolis effect on free convection in a long rotating porous box subject to uniform heat generation. Int. J. Heat Mass Transfer 38, 2011–2018
Vadasz P. (1996a) Stability of free convection in a rotating porous layer distant from the axis of rotation. Trans. Porous Media 23, 153–173
Vadasz P. (1996b) Convection and stability in a rotating porous layer with alternating direction of the centrifugal body force. Int. J. Heat Mass Transfer 39, 1639–1647
Vadasz P. (1998) Coriolis effect on gravity driven convection in a rotating porous layer heated from below. J. Fluid. Mech. 376, 351–375
Vadasz P., Govender S. (1998) Two-dimensional convection induced by gravity and centrifugal forces in a rotating porous layer far away from the axis of rotation. Int. J. Rot. Mach. 4, 73–90
Vadasz P., Heerah A. (1998) Experimental confirmation and analytical results of centrifugally-driven free convection in a rotating porous media. J. Porous Media 1, 261–272
Vadasz P., Olek S. (1998) Transitions and chaos for free convection in a rotating porous layer. Int. J. Heat Mass Transfer 41, 1417–1435
Vadasz P. (2005) Explicit conditions for local thermal equilibrium in porous media heat conduction. Trans Porous Media 59(3): 341–355
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Govender, S., Vadasz, P. The effect of mechanical and thermal anisotropy on the stability of gravity driven convection in rotating porous media in the presence of thermal non-equilibrium. Transp Porous Med 69, 55–66 (2007). https://doi.org/10.1007/s11242-006-9063-6
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11242-006-9063-6