triwaco offers the possibility to simulate infiltration from lakes or hollows in the dunes and superficial discharge with the SF-module. In these cases the user defines de areas which are to be considered as (sub) surface water units. Such an area may be a catchment, slope or just a hollow in the landscape.
The surface water level is assumed to be the same over the entire area of a valley. The water level can change through time under influence of rainfall, evaporation, seepage and infiltration. Seepage occurring along a slope is discharged to an adjoining valley (surface run-off).
Surface water flow |