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Numerical Heat Transfer, Part B: Fundamentals
An International Journal of Computation and Methodology
Volume 70, 2016 - Issue 5
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Original Articles

A new benchmark reference solution for double-diffusive convection in a heterogeneous porous medium

, , , &
Pages 373-392 | Received 22 Mar 2016, Accepted 23 Jun 2016, Published online: 26 Sep 2016
 

ABSTRACT

A new benchmark with a high accurate solution is proposed for the verification of numerical codes dealing with double-diffusive convection in a heterogeneous porous medium. The new benchmark is inspired by the popular problem of square porous cavity by assuming a stratified porous medium. A high accurate steady state solution is developed using the Fourier–Galerkin method. To this aim, the unknowns are expanded in double infinite Fourier series. The accuracy of the developed solution is assessed in terms of the truncation orders of the Fourier series. Comparison against finite element solutions highlights the worthiness of the proposed benchmark for numerical code validation.

Nomenclature

A=

stream function coefficient

B=

temperature coefficient

C=

dimensionless concentration

c=

specific heat at constant pressure [J kg−1 K−1]

=

concentration imposed at the left wall

=

concentration imposed at the right wall

D=

mass diffusivity [m2 s−1]

E=

concentration coefficient

g=

intensity of gravity [m s−2]

GrS=

solutal Grashof number based on H and the fluid properties

GrT=

thermal Grashof number based on H and the fluid properties

H=

size of the square enclosure [m]

K=

permeability of the porous medium [m2]

k=

thermal conductivity [W m−1 K−1]

K0=

permeability at the origin

=

average permeability

Le=

lewis number (= α/D)

N=

buoyancy ratio (=GrS/GrT)

Nc=

total number of Fourier coefficients

Nx=

truncation order in the x direction

Ny=

truncation order in the y direction

=

average Nusselt number

p=

dimensionless total pressure

Pr=

Prandtl number (= ν/α)

Rk=

ratio of thermal conductivity (=km/kf)

Ra=

local Rayleigh number

Ra0=

Rayleigh number at y = 0

=

average Rayleigh number

RF=

residual for the flow equation

RH=

residual for the heat transfer equation

RM=

residual for the mass transfer equation

=

average Sherwood number

T=

dimensionless temperature

t=

time [s]

=

temperature imposed at the left wall [K]

=

temperature imposed at the right wall [K]

u=

dimensionless horizontal velocity

umax=

maximum dimensionless horizontal velocity

v=

dimensionless vertical velocity

vmax=

maximum dimensionless vertical velocity

x=

dimensionless horizontal coordinate

y=

dimensionless vertical coordinate

α=

thermal diffusivity of the fluid [m2 s−1]

βC=

coefficient of expansion with mass

βT=

coefficient of expansion with temperature

ϵ=

porosity of the porous medium

δ=

Kronecher delta function

Γ=

matrix coefficient [Eq. (23)]

λ=

matrix coefficient [Eqs. (24) and (25)]

ν=

kinematic viscosity of the fluid [m2 s−1]

Ω=

matrix coefficient [Eq. (23)]

ω=

matrix coefficient [Eqs. (24) and (25)]

ϕ =

concentration change of variable

Π=

matrix coefficient [Eqs. (24) and (25)]

Ψ=

Galerkin trial function for flow equation

ψ=

dimensionless stream function

ρ=

density [kg m−3]

ρ0=

reference density of fluid [kg m−3]

σ=

ratio of specific heat (= (ρc)m/(ρc)f)

τ=

matrix coefficient [Eqs. (24) and (25)]

Θ=

Galerkin trial function for heat and mass equations

θ=

temperature change of variable

εd=

vector coefficient [Eqs. (24) and (25)]

φ=

matrix coefficient [Eqs. (24) and (25)]

ζ=

rate of change of the permeability in the y direction

Subscripts and Superscripts=
f=

fluid

m=

fluid-saturated porous medium

s=

solid matrix of the porous medium

*=

dimensionless parameter

Nomenclature

A=

stream function coefficient

B=

temperature coefficient

C=

dimensionless concentration

c=

specific heat at constant pressure [J kg−1 K−1]

=

concentration imposed at the left wall

=

concentration imposed at the right wall

D=

mass diffusivity [m2 s−1]

E=

concentration coefficient

g=

intensity of gravity [m s−2]

GrS=

solutal Grashof number based on H and the fluid properties

GrT=

thermal Grashof number based on H and the fluid properties

H=

size of the square enclosure [m]

K=

permeability of the porous medium [m2]

k=

thermal conductivity [W m−1 K−1]

K0=

permeability at the origin

=

average permeability

Le=

lewis number (= α/D)

N=

buoyancy ratio (=GrS/GrT)

Nc=

total number of Fourier coefficients

Nx=

truncation order in the x direction

Ny=

truncation order in the y direction

=

average Nusselt number

p=

dimensionless total pressure

Pr=

Prandtl number (= ν/α)

Rk=

ratio of thermal conductivity (=km/kf)

Ra=

local Rayleigh number

Ra0=

Rayleigh number at y = 0

=

average Rayleigh number

RF=

residual for the flow equation

RH=

residual for the heat transfer equation

RM=

residual for the mass transfer equation

=

average Sherwood number

T=

dimensionless temperature

t=

time [s]

=

temperature imposed at the left wall [K]

=

temperature imposed at the right wall [K]

u=

dimensionless horizontal velocity

umax=

maximum dimensionless horizontal velocity

v=

dimensionless vertical velocity

vmax=

maximum dimensionless vertical velocity

x=

dimensionless horizontal coordinate

y=

dimensionless vertical coordinate

α=

thermal diffusivity of the fluid [m2 s−1]

βC=

coefficient of expansion with mass

βT=

coefficient of expansion with temperature

ϵ=

porosity of the porous medium

δ=

Kronecher delta function

Γ=

matrix coefficient [Eq. (23)]

λ=

matrix coefficient [Eqs. (24) and (25)]

ν=

kinematic viscosity of the fluid [m2 s−1]

Ω=

matrix coefficient [Eq. (23)]

ω=

matrix coefficient [Eqs. (24) and (25)]

ϕ =

concentration change of variable

Π=

matrix coefficient [Eqs. (24) and (25)]

Ψ=

Galerkin trial function for flow equation

ψ=

dimensionless stream function

ρ=

density [kg m−3]

ρ0=

reference density of fluid [kg m−3]

σ=

ratio of specific heat (= (ρc)m/(ρc)f)

τ=

matrix coefficient [Eqs. (24) and (25)]

Θ=

Galerkin trial function for heat and mass equations

θ=

temperature change of variable

εd=

vector coefficient [Eqs. (24) and (25)]

φ=

matrix coefficient [Eqs. (24) and (25)]

ζ=

rate of change of the permeability in the y direction

Subscripts and Superscripts=
f=

fluid

m=

fluid-saturated porous medium

s=

solid matrix of the porous medium

*=

dimensionless parameter

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