10.10. Porous Media Flow

The coupled pore-pressure thermal elements used in analyses involving porous media are listed in Coupled Pore-Pressure-Thermal Element Support.

The program models porous media containing fluid by treating the porous media as a multiphase material and applying an extended version of Biot's consolidation theory. The flow is considered to be a single-phase fluid. The porous media can be fully or partially saturated.[[426]][[432]] Optionally, heat transfer in the porous media can also be considered.

Following are the governing equations for Biot consolidation problems with heat transfer:

(10–113)

where:

σ=Total Cauchy stress

= = matrix differentiation operator (3D form shown)
=Bulk density of porous media
=Displacement
=Bulk specific weight of porous media
=Gravity load direction (not to be confused with gravity magnitude)
=Flow flux vector
= = Gradient operator (3D form shown)
=Biot coefficient

=Volumetric strain of the solid skeleton
=Pore pressure
=Compressibility parameter
=Degree of saturation of fluid
=Free strain
=Temperature
=Density-specific heat term
=Porosity
=Density of solid skeleton and fluid
=Specific heats of solid skeleton and fluid
=Thermal conductivity

The total stress relates to the effective stress and pore pressure by:

where:

= Second-order identity tensor

The relationship between the effective stress and the elastic strain of solid skeletons is given by:

where:

= Second-order elastic strain tensor
= Fourth-order elasticity tensor

The relationship between the fluid flow flux and the pore pressure is described by Darcy's Law:

where:

= second-order permeability tensor
= relative permeability
= specific weight of fluid

For displacement , pressure , and temperature as the unknown degrees of freedom, linearizing the governing equations gives:

(10–114)

The matrices are:

where:

= domain
= strain-displacement operator matrix
= displacement interpolation
= pressure interpolation
= temperature interpolation
= thermal load vector

The load force vector includes the body force and surface traction boundary conditions, the vector includes the flow source, and the vector includes the heat source. ([426])

Combining the linearized equations for porous media with the equation of motion gives the matrix equation:

(10–115)

where:

= structural damping matrix

The structural damping matrix can be input as Rayleigh damping (TB,SDAMP,,,,ALPD and/or TB,SDAMP,,,,BETD).

Additional Information

For related information, see the following documentation: