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:
(10–112)  | 
where:
| σ | = | Total Cauchy stress | 
| 
                             
                                  | = | 
                             | 
| 
                             | = | 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 | 
| 
                             | = | 
                             | 
| 
                             | = | 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:
| 
                     | 
The relationship between the effective stress and the elastic strain of solid skeletons is given by:
where:
| 
                     | 
| 
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The relationship between the fluid flow flux and the pore pressure is described by Darcy's Law:
where:
| 
                     | 
| 
                     | 
| 
                     | 
For displacement , pressure 
, and temperature 
 as the unknown degrees of freedom, linearizing the governing equations
            gives:
(10–113)  | 
The matrices are:
| 
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| 
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| 
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| 
                     | 
| 
                     | 
| 
                     | 
| 
                     | 
| 
                     | 
| 
                     | 
| 
                     | 
| 
                     | 
| 
                     | 
where:
| 
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| 
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| 
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| 
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| 
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| 
                     | 
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:
(10–114)  | 
where:
| 
                     | 
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: