Hydraulic Permeability
The hydraulic permeability of a membrane is the inverse of the fluid resistance normalized to the membrane area.
Experimentally it is found with
Where Q is the measured flow rate, is the pressure drop across the membrane and
is the membrane area.
It can be calculated from membrane properties with
Where is the fluid resistance of a pore (Hagen Pousille or Dagen),
is the area of a pore and
is the porosity.