Porous Medium
The Porous Medium node defines the properties of a porous medium filled with two phases in equilibrium: liquid water and moist air.
Isothermal drying of porous media is driven by the difference in relative humidity in the porous medium and its surroundings. This difference in relative humidity results in the evaporation of water and the release of moisture to the environment. There exist two drying mechanisms; evacuation of moisture by vapor molecular diffusion, and evaporation of the liquid water at the surface by capillary pressure gradients in the porous solid.
The Porous Medium node contains three default subnodes — the Liquid Water (Porous Medium) node, the Moist Air (Porous Medium) node, and the Porous Matrix (Porous Medium) node.
Coordinate System Selection
Select a coordinate system from the Coordinate system list for the interpretation of directions in anisotropic material properties. The default is the Global coordinate system, and the list contains any additional orthonormal coordinate system (except boundary coordinate systems) added under the Definitions node.
The subnodes inherit these coordinate system settings. In particular, the settings in the Permeability in the Porous Matrix (Porous Medium) subnode are set according to the coordinate system selected in this section.
Moisture Transport Properties
The Moisture function characterizes the relationship between the amount of accumulated water and the relative humidity in the porous material. The available options for the Moisture function are Moisture storage function or Capillary pressure. The selection determines how the liquid water saturation is computed.
When Moisture storage function is selected from the Moisture function list, the default Moisture storage function wcw) is taken From material. For User defined, enter another value or expression.
Select the Capillary model for the capillary flux:
When Capillary model is set to Kelvin’s law (default), a Darcy’s law based on the capillary pressure is used, and the capillary pressure itself is derived from the relative humidity by using Kelvin’s law, using the assumption that the liquid and gas phases are in equilibrium in the porous medium.
When Capillary model is set to Diffusion model, the capillary flux is derived from the gradient of the moisture content and the Moisture diffusivity Dw.
For User defined, set a value for the Capillary liquid flux density, Γc, to characterize the liquid transport as a function of the moisture content.
When or Capillary pressure is selected from the Moisture function list, select the Capillary pressure modelvan Genuchten or Brooks and Corey.
For van Genuchten, enter an Entry capillary pressure pec (SI unit: Pa), the Constitutive relations constant mvg, the Constitutive relations constant lvg (dimensionless), the Liquid water residual saturation srl, and the Moist air residual saturation srm.
For Brooks and Corey, enter an Entry capillary pressure pec (SI unit: Pa) and the Pore size distribution index λp, the Liquid water residual saturation srl, and the Moist air residual saturation srm.
See Porous Material in the COMSOL Multiphysics Reference Manual.
Location in user interface
Context Menus
Ribbon
Physics tab with Moisture Transport in Solids selected: