Ground bottom flow formula (Water Overlay): Difference between revisions

From Tygron Preview Support Wiki
Jump to navigation Jump to search
No edit summary
Line 1: Line 1:
Underground seepage (from (or to) outside the project area) is calculated per cell.
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:
Line 7: Line 7:
: <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, calculate the actual amount of water seeping into (or out of) the ground from the bottom.
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>


Line 24: Line 24:
* <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