10.9. 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 [[431]] [[437]]. Optionally, heat transfer in the porous media can also be considered.

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

(10–71)

where:

σ=Total Cauchy stress

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

=Volumetric strain of the solid skeleton
=Pore pressure
=Compressibility parameter
=Thermal expansion coefficient
=Temperature
=Flow source
=Specific heat capacity
=Thermal conductivity
=Heat source

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

where:

= degree of saturation of fluid
= 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:

(10–72)

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, and the vector includes the flow source, and the vector includes the heat source. ([431])

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

(10–73)

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:

Structural-Pore-Fluid-Diffusion-Thermal Analysis in the Mechanical APDL Coupled-Field Analysis Guide
Porous Media Material Properties in the Mechanical APDL Material Reference

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