Drinking water from dams
Layering of the dam
In lakes and reservoirs the water layers are arranged vertically. In summer and winter they are strictly separated due to the difference in temperature: the upper surface layer (epilimnion) is followed by the upper layer (metalimnion) and the deep layer (hypolimnion). In spring and autumn the water layers are completely circulated.
Stratification during summer stagnation
The raw water in the Steinbachtal dam is mainly taken from the lower part of the Hypolimnion due to the consistently good chemical / physical values. The upper withdrawal is only used in late autumn to bypass the thermocline.