Ground bottom flow formula (Water Overlay): Difference between revisions
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* <math>\Delta t</math> = Computational timestep in seconds. | * <math>\Delta t</math> = Computational timestep in seconds. | ||
* <math>h_{x,y}</math> = Ground water head in the grid cell. | * <math>h_{x,y}</math> = Ground water head in the grid cell. | ||
* <math>h_{d,t}</math> = ground water level (or head) of the external zone causing the seepage at time t, in meters | * <math>h_{d,t}</math> = additional ground water level (or head) of the external zone causing the seepage at time t, in meters | ||
* <math>h_{ | * <math>h_{c_{x,y}}</math> = constant ground water level (or head) of the external zone causing the seepage, in meters | ||
* <math>h_{v,t}</math> = additional variation of seepage head over time | * <math>h_{v,t}</math> = additional variation of seepage head over time | ||
* <math>c</math> = resistance of the separating layer in days | * <math>c</math> = resistance of the separating layer in days | ||
* <math>ws</math> = water storage fraction of the soil | * <math>ws</math> = water storage fraction of the soil | ||
==Notes== | |||
* <math>h_{c_{x,y}}</math> and <math>c_{x,y}</math> can both be provided as spatially variable values. | |||
* <math>h_{d,t}</math> can be provided as a set of values, variable over time. | |||
==See also== | ==See also== |
Revision as of 09:38, 14 August 2020
Underground seepage (from (or to) outside the project area) is calculated per cell.
The seepage is calculated using the following formula:
The external seepage head is variable over time by the introduction of hv,t
Finally, calculate the actual amount of water seeping into (or out of) the ground from the bottom.
Where:
- = The underground seepage which takes place, in meters.
- = Computational timestep in seconds.
- = Ground water head in the grid cell.
- = additional ground water level (or head) of the external zone causing the seepage at time t, in meters
- = constant ground water level (or head) of the external zone causing the seepage, in meters
- = additional variation of seepage head over time
- = resistance of the separating layer in days
- = water storage fraction of the soil
Notes
- and can both be provided as spatially variable values.
- can be provided as a set of values, variable over time.
See also
- The formula is based on the formula of Pankow for estimating seepage
- Seepage result
- Seepage geotiffs
- Seepage fluctuation