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If the runoff generation is calculated with the soil moisture simulation, the elementary surface concept is applied at the same time. A catchment area element is thereby divided into any number of hydrologically homogeneous areas, i.e. areas of the same soil type and the same land use. For each elementary area there is exactly one assignment of land use and soil type. The amount of water resulting from an elementary surface is set at the element exit, i.e. all elementary surfaces release water with the same time delay, independent of their location in the catchment area.