The Local Thermal Non-Equilibrium Interface implements heat transfer in porous media for which the temperatures into the porous matrix and the fluid are not in equilibrium.
The fluid velocity is often deduced from a porous velocity up, coming for example from Darcy’s law or Brinkman equations, according to:
The Local Thermal Non-Equilibrium multiphysics coupling adds the exchanged opposite heat sources
qsf(Tf − Ts) and
qsf(Ts − Tf) that one phase receives from or releases to the other when respective temperatures differ. The porous temperature,
T, has the following definition (
Ref. 32):
The Local Thermal Non-Equilibrium multiphysics feature provides a built-in correlation for
qsf in the spherical pellet bed configuration (2.14, 2.15, and 2.16 in
Ref. 13):
The specific surface area, asf (SI unit: 1/m), for a bed packed with spherical particles of radius
rp is:
The interstitial heat transfer coefficient, hsf (SI unit: W/(m
2·K)), satisfies the relation:
where β = 10 for spherical particles, and
Nu is the fluid-to-solid Nusselt number derived from following correlation (
Ref. 14):
The Prandtl number, Pr, and particle Reynolds number,
Rep, are defined by:
Because the Local Thermal Non-Equilibrium multiphysics coupling multiplies each energy equation by its volume fraction, θp and
(1 − θp) for solid and fluid phases respectively, a heat source or heat flux defined in a couple heat transfer interface is also accounted with that ratio. As shown in
Equation 4-25 and
Equation 4-26, the volumetric heat sources
θpQs and
(1 − θp)Qf are applied to the energy equations while the
Heat Source features of each physics interface specify
Qs and
Qf.