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Permeability model

The Permeability model tab describes how easily fluid moves through the soil. It appears for two- and three-phase materials; a single-phase material has no fluid to move.

The tab holds four sections. Which of them are shown depends on the number of phases.

Intrinsic permeability

The permeability of the soil skeleton itself, independent of the fluid in it.

Model Parameters Reference
Isotropic a single value, in length² Permeability
Kozeny-Carman c, de Permeability
User-defined

Dynamic viscosity

The viscosity of each fluid phase, in kPa·s. It is used together with the intrinsic permeability.

Row Shown at
μw (water) two or three phases
μa (air) three phases

Relative permeability-saturation relation

Shown for three-phase materials only. In unsaturated soil neither water nor air occupies the whole pore space, and this relation describes how the permeability of each falls away as the other takes over.

Model Parameters Reference
vanGenuchten kw,min, ka,min, n Van Genuchten
Brooks-Corey kw,min, ka,min, n Brooks & Corey
User-defined

Leaving the model unselected is allowed. Once one is chosen, its parameters must be filled.

Hydraulic conductivity scale

Intrinsic permeability is not the number most geotechnical engineers carry in their head — hydraulic conductivity is. The scale in the lower right does that conversion so the value being entered can be recognised:

\[ K = \frac{k \cdot \rho_w \cdot g}{\mu_w} \qquad \text{with } g = 10\ \mathrm{m/s^2} \]

The resulting K is marked on the Terzaghi soil-classification bands — clay, silt, fine and silty sand, sand, gravel — so an implausible permeability shows up at a glance. Entering a value that lands a sand in the clay band is a sign that k is wrong, or has been entered in the wrong units.

The scale is a readout, not an input. It cannot be typed into, and it updates live as the permeability, the water density or the water viscosity change. The water density comes from the Phase properties tab, so the marker moves when that is edited too.

Validation

For two- and three-phase materials an intrinsic permeability model must be chosen and its parameters filled. A relative permeability model is optional, but once selected its parameters are required as well.

Pressing Apply & Save with something missing shows a warning naming the problem, and the material stays open so it can be corrected.