Abstract
The effect of local thermal non-equilibrium on the onset of convection in a porous medium consisting of two horizontal layers is studied analytically. Linear stability theory is applied. Variations of permeability, fluid conductivity, solid conductivity, interphase heat transfer coefficient and porosity are considered. It is found that heterogeneity of permeability and fluid conductivity have a major effect, heterogeneity of interphase heat transfer coefficient and porosity have a lesser effect, while heterogeneity of solid conductivity is relatively unimportant.
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Abbreviations
- \(a\) :
-
Dimensionless horizontal wavenumber
- D :
-
d/dz
- \(h\) :
-
Interface heat transfer coefficient (incorporating the specific surface area) between the fluid and solid particles
- \(\hat{{h}}\) :
-
Parameter defined in Eq. (15)
- \(h_\mathrm{r}\) :
-
Interface heat transfer coefficient ratio, \(h_{2}/h_{1}\)
- \(g\) :
-
Gravitational acceleration
- g :
-
Gravitational acceleration vector
- \(H\) :
-
Dimensional layer depth
- \(k\) :
-
Thermal conductivity of the porous medium
- \(\hat{{k}}_{ f}\) :
-
Parameter defined in Eq. (15)
- \(k_{{ f}\mathrm{r}}\) :
-
Conductivity ratio, \(k_{f2}/k_{f1}\)
- \(\hat{{k}}_{ s}\) :
-
Parameter defined in Eq. (15)
- \(k_{{ s}\mathrm{r}}\) :
-
Conductivity ratio, \(k_{s2}/k_{s1}\)
- \(K\) :
-
Permeability of the porous medium
- \(K_\mathrm{r}\) :
-
Permeability ratio, \(K_{2}/K_{1}\)
- \(\hat{{K}}\) :
-
Parameter defined in Eq. (15)
- \(N\) :
-
Interface heat transfer parameter, \(\frac{h_1 H^{2}}{\phi _1 k_{f1}}\)
- \(P\) :
-
Dimensionless pressure, \(\frac{(\rho c)_{ f} K_1}{\mu k_{f1}}P^*\)
- \(P^{*}\) :
-
Pressure, excess over hydrostatic
- Ra :
-
Rayleigh number, \(\frac{\rho _0 g\beta K_1 H(T_\mathrm{h} -T_\mathrm{c} )}{\mu k_{f1} /(\rho c)_{ f}}\)
- \(t\) :
-
Dimensionless time, \(\frac{k_{f1}}{(\rho c)_{ f} H^{2}}t^{*}\)
- \(t^{*}\) :
-
Time
- \(T\) :
-
Dimensionless temperature, \(\frac{T^{*}-T_\mathrm{c}}{T_\mathrm{h} -T_\mathrm{c}}\)
- \(T^{*}\) :
-
Temperature
- \(T_\mathrm{c}\) :
-
Temperature at the upper boundary
- \(T_\mathrm{h}\) :
-
Temperature at the lower boundary
- \((u,v,w)\) :
-
Dimensionless velocity components, \(\frac{(\rho c)_{ f} H}{k_{f1}}(u^{*},v^*,w^*)\)
- \(\mathbf{u}^{*}\) :
-
Darcy velocity, (\(u^{*},v^{*},w^{*}\))
- \((x,y,z)\) :
-
Dimensionless Cartesian coordinates, \((x^{*},y^{*},z^{*})/H; \,\,z\) is the vertically-upward coordinate
- \((x^{*},y^{*},z^{*})\) :
-
Cartesian coordinates
- \(\alpha \) :
-
Modified thermal diffusivity ratio, \(\frac{(\rho c)_{s1}}{(\rho c)_{f1}}\frac{k_{f1}}{k_{s1}}\)
- \(\beta \) :
-
Volumetric expansion coefficient of the fluid
- \(\gamma \) :
-
Modified thermal conductivity ratio, \(\frac{\phi _1 k_{f1}}{(1-\phi _1 )k_{s1}}\)
- \(\delta \) :
-
Dimensionless layer depth ratio (interface position)
- \(\hat{{\delta }}\) :
-
Parameter defined in Eq. (15)
- \(\delta _\mathrm{r}\) :
-
Inverse solid fraction ratio, \(\frac{1-\phi _1}{1-\phi _2}\)
- \(\varepsilon \) :
-
Dimensionless small quantity
- \(\hat{{\varepsilon }}\) :
-
Parameter defined in Eq. (15)
- \(\varepsilon _\mathrm{r}\) :
-
Solid heat capacity ratio, \(\frac{(\rho c)_{s2}}{(\rho c)_{s1}}\)
- \(\mu \) :
-
Viscosity of the fluid
- \(\rho _{0}\) :
-
Fluid density at temperature \(T_\mathrm{c}\)
- \(\rho _{f}\) :
-
Fluid density
- \(\left( {\rho c} \right) _{ f}\) :
-
Heat capacity of the fluid
- \(\left( {\rho c} \right) _\mathrm{m}\) :
-
Effective heat capacity of the porous medium
- \((\rho c)_{ s}\) :
-
Heat capacity of the solid
- \(\phi \) :
-
Porosity
- \(\phi _\mathrm{r}\) :
-
Porosity ratio, \(\phi _{2}/\phi _{1}\)
- \(\mu \) :
-
Fluid viscosity
- B:
-
Basic state
- c:
-
Critical value
- f :
-
Fluid phase
- m:
-
Effective property for the porous medium
- r:
-
Relative quantity
- s :
-
Solid phase
- 1:
-
The region \(0\le z^{*}<\delta H\)
- 2:
-
The region \(\delta H\le z^{*}\le H\)
- \(^{\prime }\) :
-
Perturbation variable
- \(^{*}\) :
-
Dimensional variable
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Nield, D.A., Kuznetsov, A.V. Local Thermal Non-Equilibrium and Heterogeneity Effects on the Onset of Convection in a Layered Porous Medium. Transp Porous Med 102, 1–13 (2014). https://doi.org/10.1007/s11242-013-0224-0
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DOI: https://doi.org/10.1007/s11242-013-0224-0