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.
ForchheimerConstant($Material$) = ( 1.0 ) # scalar Forchheimer constant of 1.0 [kg/m^4]
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.
ForchheimerConstant($Material$) = ( &Fx&, &Fy&, &Fz& )
Then, the constant &bx&, &by&, &bz& in DarcyConstant are modified in the sense that \( &bx& = &bx& + &Fx&\|\mathbf{v} - \mathbf{v}_{\beta}\|\).

Notes