Use the Fluid and Matrix Properties node to define which domains contain porous material and to define the porous matrix properties, such as the porosity and permeability in these domains. The
Forchheimer Drag subnode is available from the context menu (right-click the parent node) or from the
Physics toolbar,
Attributes menu.
Choose domains from the Selection list, to solve for porous media flow governed by the Brinkman equations. In the domains not selected, the Free and Porous Media Flow interface solves for laminar flow governed by the Navier-Stokes (or Stokes) equations.
The default Porous material uses the
Domain material (the material defined for the domain) for the porous matrix. Select another material as needed.
The default Porosity εp (a dimensionless number between 0 and 1) uses values
From material as defined by the
Porous material selection. For
User defined enter another value or expression. The default is 0.
The default Permeability κbr (SI unit: m
2) uses values
From material as defined by the
Porous material selection. For
User defined select
Isotropic,
Diagonal,
Symmetric, or
Anisotropic from the list and then enter other values or expressions. The components of a permeability in the case that it is a tensor (
κxx,
κyy, and so on, representing an anisotropic permeability) are available as
fp.kappaxx,
fp.kappayy, and so on (using the default name
fp). The default is 0 m
2.
Enter a value or expression for an optional mass source (or sink) Source term Qbr (SI unit: kg/(m
3·s)). This term accounts for mass deposit and mass creation within domains. The physics interface assumes that the mass exchange occurs at zero velocity.
A correction factor (Bruggeman,
No Correction, or
User defined) to the mass transport parameters (defined in the
Transport Properties node)
can be applied for the porous domain. Species diffusivities and mobilities are automatically adjusted by the porous media corrections. For
User defined enter a value or expression for the
Conversion factor feff. The default is 1. Species diffusivities and mobilities are automatically adjusted by the porous media corrections.