Translations:Einzugsgebiet/45/en: Unterschied zwischen den Versionen
Ferrao (Diskussion | Beiträge) (Die Seite wurde neu angelegt: „with: {|style="margin-left: 40px;" |<math>d_i</math>: || proportional layer thickness of the respective original layer [mm] |- |<math>k_i</math>: || saturated…“) |
Ferrao (Diskussion | Beiträge) Keine Bearbeitungszusammenfassung |
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[[Datei:Schema_aktuelle_Verdunstung.png|thumb|Scheme of determination of the current evaporation]] | [[Datei:Schema_aktuelle_Verdunstung.png|thumb|Scheme of determination of the current evaporation]] | ||
The water balance equation for a soil layer is solved on the basis of the area-wise linear representation of the process functions infiltration, current evaporation (evaporation + transpiration), percolation, interflow and capillary rise, which influence soil moisture. The input variable for evaporation and transpiration is determined from the potential evaporation. | |||
The equation to be solved is: |
Version vom 13. Oktober 2020, 09:14 Uhr
with:
[math]\displaystyle{ d_i }[/math]: | proportional layer thickness of the respective original layer [mm] |
[math]\displaystyle{ k_i }[/math]: | saturated conductivity of the respective original layer [mm/h] |
[math]\displaystyle{ kf_V }[/math]: | saturated conductivity of the layer used within the program [mm/h] |
The water balance equation for a soil layer is solved on the basis of the area-wise linear representation of the process functions infiltration, current evaporation (evaporation + transpiration), percolation, interflow and capillary rise, which influence soil moisture. The input variable for evaporation and transpiration is determined from the potential evaporation. The equation to be solved is: