Chestermiller said:
in my judgment, there is asignificant advantage to formulating and solving the heat balance equation for the fluid using the so-called divergence representation of the equation (see below); this also provides the added advantage of automatically converting mass not only in the PDE form of the equation, but also when it is expressed in finite difference form.
Got it
Chestermiller said:
∂ρ∂t+∂ϕ∂x=0and∂(ρh)∂t+∂(ϕh)∂x=∂∂x(ϕl∂h∂x)+Uaϵ(TS−T)
To describe the above equations I would say the following, where every term is per unit volume:
1) The rate of increase of mass plus the rate at which mass leaves in the ##x## direction ##= 0##
2) The rate of increase of energy plus the rate at which energy leaves in the ##x## direction = the rate of axial dispersion in the x direction plus the heat transfer between the fluid and solid
(I notice we have arrived at the same equation I started the post with (!), just using enthalpy instead of temperature. Nice)
Chestermiller said:
In these equations, if we substitute ϕ=ρu for the axial mass flux, and express the thermal dispersion coefficient in the typical approximate form D = ul (where l is the characteristic thermal dispersion length parameter), these equations become
Understood
Chestermiller said:
In lieu of any definite information on the effects of fluid density on the dispersivity parameter l, it will probably be necessary to assume that l is a constant depending only on packing geometry and to treat it as an adjustable 'tuning" parameter.
Understood. I think I have seen some correlations for ##D## the axial dispersion coefficient but I guess this is of secondary importance for now.
The mass balance is straightforward, however I do have questions on the energy balance to clear up.
Points of confusion:
1) Are you using the term 'heat balance' and 'energy balance' interchangeably?
2) Is this an advection term: ##\frac{\partial (\phi h)}{\partial x}##? I'm not familiar with advection, other than its definition as the transfer of heat through fluid flow, so I guess this is it
3) So the axial dispersion coefficient is a 'catch all' term for a number of energy transport processes as far as I know (diffusion and conduction within the fluid, convection by the fluid in the axial direction, axial and transverse mixing of the fluid, etc, as far as I know). What terms are included in this term in our case?
4) The final term seems to be the convection between the fluid and the solid term. Why does this term not have a time or space derivative, because it will surely depend on space and time? Is it because 'time/space dependence' is built in, in the sense that ##T## and ##T_S## will change with time and space, meaning that the convection term will also change with time and space indirectly?
Chestermiller said:
In lieu of any definite information on the effects of fluid density on the dispersivity parameter l, it will probably be necessary to assume that l is a constant depending only on packing geometry and to treat it as an adjustable 'tuning" parameter.
Got it
So now instead of solving a fluid and solid energy balance, we will be solving the mass balance for the fluid, and the energy balance for the fluid/solid instead?