Translations:Einzugsgebiet/43/en
Version vom 25. November 2020, 14:42 Uhr von Froehlich (Diskussion | Beiträge)
The calculation of soil properties for the simulation layers is done by weighting them according to the given original thicknesses of the layers. In case of saturated conductivity the calculation is based on the principle of maintaining the continuity of the flow. For vertical flow, the velocity v at a given flow rate in one simulation layer should have the same value due to the continuity of the flow. Thus, the hydraulic gradient is no longer constant.