Ground bottom flow formula (Water Overlay): Difference between revisions
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Underground seepage | Underground seepage from outside the project area is calculated per grid cell. | ||
The water level change due to seepage is calculated using the following formula: | The water level change due to seepage is calculated using the following formula: | ||
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: <math>h_d(t) = h_{c_{x,y}} + h_{v,t}(t)</math> | : <math>h_d(t) = h_{c_{x,y}} + h_{v,t}(t)</math> | ||
Finally, | Finally, the actual amount of water seeping into the ground from the bottom is calculated as followed: | ||
: <math>\Delta w_{x,y} = {\Delta s_{x,y}}\cdot{ws}</math> | : <math>\Delta w_{x,y} = {\Delta s_{x,y}}\cdot{ws}</math> | ||
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* <math>h_{c_{x,y}}</math> and <math>c_{x,y}</math> can both be provided as spatially variable values. | * <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. | * <math>h_{d}(t)</math> can be provided as a set of values, variable over time. | ||
* A seepage head lower than the water level in the project is also allowed, resulting in water seeping out to a region outside the project area. | |||
==See also== | ==See also== |
Revision as of 09:03, 28 August 2020
Underground seepage from outside the project area is calculated per grid cell.
The water level change due to seepage is calculated using the following formula:
The external seepage head is variable over time by the introduction of hv,t
Finally, the actual amount of water seeping into the ground from the bottom is calculated as followed:
Where:
- = The water level change due to seepage, 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
- = seeped in water in m
Notes
- and can both be provided as spatially variable values.
- can be provided as a set of values, variable over time.
- A seepage head lower than the water level in the project is also allowed, resulting in water seeping out to a region outside the project area.
See also
- The formula is based on the formula of Pankow for estimating seepage
- Seepage result
- Seepage geotiffs
- Seepage fluctuation