Ground infiltration formula (Water Overlay): Difference between revisions

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Then calculate the distance of the unsaturated zone which can infiltrate.
Then calculate the distance of the unsaturated zone which can infiltrate.
: <math>d_{i} = min( d_{u} , \Delta t \cdot I_{u} )</math>
: <math>d_{i} = min( d_{u} , \Delta t \cdot I_{g} )</math>


Finally, calculate the actual amount of water infiltrating.
Finally, calculate the actual amount of water infiltrating.
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: <math>r</math> = Ratio of water to height in the unsaturated zone.
: <math>r</math> = Ratio of water to height in the unsaturated zone.
: <math>\Delta t</math> = Computational timestep.
: <math>\Delta t</math> = Computational timestep.
: <math>I_{u}</math> = The [[Terrain ground infiltration md (Water Overlay)|GROUND_INFILTRATION_MD]] of the underground terrain type.
: <math>I_{g}</math> = The [[Terrain ground infiltration md (Water Overlay)|GROUND_INFILTRATION_MD]] of the underground terrain type.
: <math>d_{i}</math> = The height distance in the unsaturated zone which can be subject to infiltration to the saturated zone.
: <math>d_{i}</math> = The height distance in the unsaturated zone which can be subject to infiltration to the saturated zone.
: <math>\Delta w_i</math> = The underground infiltration which takes place.
: <math>\Delta w_i</math> = The underground infiltration which takes place.

Revision as of 12:49, 25 January 2024

Underground infiltration (from the unsaturated zone to the saturated zone) is calculated per cell.

First the height of the unsaturated zone is calculated.

Then the ratio of water amount to unsaturated height is calculated.

Then calculate the distance of the unsaturated zone which can infiltrate.

Finally, calculate the actual amount of water infiltrating.

Where:

= The groundwater level, relative to datum.
= the datum height of the surface of cell c, set by the elevation or a Terrain elevation prequel.
= The height of the unsaturated zone.
= The amount of water in the unsaturated zone. The height of the water column if the equivalent amount of water was placed on the surface.
= Ratio of water to height in the unsaturated zone.
= Computational timestep.
= The GROUND_INFILTRATION_MD of the underground terrain type.
= The height distance in the unsaturated zone which can be subject to infiltration to the saturated zone.
= The underground infiltration which takes place.

Related

The following topics are related to this formula.

Formulas
Groundwater level formula
Surface infiltration formula
Underground seepage formula
Models
Underground model
Infiltration model
Tracer flow model