Soil water retention curve (Water Overlay): Difference between revisions
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This can be done via the Van Genuchten-Mualem formula: | This can be done via the Van Genuchten-Mualem formula: | ||
: <math>K(t) = Ks \cdot sqrt(Se) \cdot (1 - ( 1 - Se^n )^m )^2</math> | : <math>K(t) = Ks \cdot sqrt(Se) \cdot (1 - ( 1 - Se^n )^m )^2</math> | ||
Where: | |||
: <math>K(t)</math> = Is the calculated vertical hydraulic conductivity for the given saturation t (greek: θ) | |||
: <math>Se</math> = Is the effective saturation between 0-1 of the Unsaturated Zone. This is a fraction between Sr (assumed close to zero) and the [[Terrain_water_storage_percentage_(Water_Overlay)|Water storage percentage]]. | |||
: <math>n</math> = <math>n = 1 / m</math> | |||
: <math>m</math> = [[Terrain_van_genuchten_m_(Water_Overlay)|Van Genuchten Soil parameter]]. | |||
{{article end | {{article end | ||
Revision as of 15:41, 16 December 2025
| Icon | Attribute | Unit | Range | Description | Default value |
|---|---|---|---|---|---|
| SOIL_WATER_RETENTION_CURVE | m | Setting a Soil Water Retention Curve retains a fraction of the water in the Unsaturated Zone. | 0 |
This can be done via the Van Genuchten-Mualem formula:
Where:
- = Is the calculated vertical hydraulic conductivity for the given saturation t (greek: θ)
- = Is the effective saturation between 0-1 of the Unsaturated Zone. This is a fraction between Sr (assumed close to zero) and the Water storage percentage.
- =
- = Van Genuchten Soil parameter.
Notes
- This is still BETA functionality, disabled by default (value=0).
- For Van Genuchten-Mualem select 1.




