Translations:Einzugsgebiet/45/en

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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]
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:

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