ForchheimerConstant
coupling parameter for porous media [kg/m^4]
While the constant defined in
DarcyConstant represents the classical Darcy relation for porous media of the form
\begin{align} -\nabla p = \tilde{\beta}_{D}{\vb u}\end{align}
one may further extend this by an inertial contribution of Forchheimer type by defining the constant \( \tilde{\beta}_{F}\) in
\begin{align} -\nabla p = \tilde{\beta}_{D}{\vb u} + \tilde{\beta}_{F} \|{\vb u}\|{\vb u}\end{align}
via
In case this constant is defined, \( \beta\) in
EquationsToSolve is given by \( \beta = \frac{1}{\rho}\left(\tilde{\beta}_{D} + \tilde{\beta}_{F}\|\mathbf{v} - \mathbf{v}_{\beta}\|\right)\).
Isotropic materials
If in the
RightHandSideExpression one argument is given, e.g.
then the porous material is assumed to be isotropic. Thus, \( \beta\) in
EquationsToSolve can be viewed as a scalar quantity.
Anisotropic materials
If DarcyConstant is specified for three perpendicular directions, three arguments can be supplied to
ForchheimerConstant, e.g.
Then, the constant &bx&, &by&, &bz& in
DarcyConstant are modified in the sense that \( &bx& = &bx& + &Fx&\|\mathbf{v} - \mathbf{v}_{\beta}\|\).
Notes