Products: ABAQUS/Standard ABAQUS/CAE
Moisture swelling:
defines the saturation-driven volumetric swelling of the solid skeleton of a porous medium in partially saturated flow conditions;
can be used in the analysis of coupled wetting liquid flow and porous medium stress (see “Coupled pore fluid diffusion and stress analysis,” Section 6.7.1); and
can be either isotropic or anisotropic.
The moisture swelling model assumes that the volumetric swelling of the porous medium's solid skeleton is a function of the saturation of the wetting liquid in partially saturated flow conditions. The porous medium is partially saturated when the pore liquid pressure, 
, is negative (see “Effective stress principle for porous media,” Section 2.8.1 of the ABAQUS Theory Manual).
The swelling behavior is assumed to be reversible. The logarithmic measure of swelling strain is calculated with reference to the initial saturation so that
and 
are the volumetric swelling strains at the current and initial saturations. A typical curve is shown in Figure 20.7.6–1. The ratios 
, 
, and 
allow for anisotropic swelling as discussed below. Define the volumetric swelling strain, 
, as a tabular function of the wetting liquid saturation, s. The swelling strain must be defined for the range 
.
| Input File Usage: | *MOISTURE SWELLING |
| ABAQUS/CAE Usage: | Property module: material editor: Other |
You can define the initial saturation values as initial conditions. If no initial saturation values are given, the default is fully saturated conditions (saturation of 1.0). For partial saturation the initial saturation and pore fluid pressure must be consistent, in the sense that the pore fluid pressure must lie within the absorption and exsorption values for the initial saturation value (see “Permeability,” Section 20.7.2). If this is not the case, ABAQUS/Standard will adjust the saturation value as needed to satisfy this requirement.
| Input File Usage: | *INITIAL CONDITIONS, TYPE=SATURATION |
| ABAQUS/CAE Usage: | Initial saturation values are not supported in ABAQUS/CAE. |
Anisotropy can be included in moisture swelling behavior by defining the ratios , , and , such that two or more of the three ratios differ. If the ratios 
are not specified, ABAQUS/Standard assumes that the swelling is isotropic and that 
. The orientation of the moisture swelling strain directions depends on the user-specified local orientation (see “Orientations,” Section 2.2.5).
| Input File Usage: | Use both of the following options: |
*MOISTURE SWELLING *RATIOS The *RATIOS option should immediately follow the *MOISTURE SWELLING option. |
| ABAQUS/CAE Usage: | Property module: material editor: Other |
The moisture swelling model can be used only in elements that allow for pore pressure (see “Choosing the appropriate element for an analysis type,” Section 21.1.3).
