Description
This group of topics includes annual data on the temperature distribution of groundwater in °C inside and outside the quaternary aquifer. The basis is the measurement of the groundwater temperature at a depth of 1 meter below the water level and 1 meter above the end of the groundwater measuring point.
Both the measuring points and the measured values are shown as well as an area-like interpolation.
For the area outside the contiguous Pleistocene aquifer, it is assumed that the temperature in the subsoil also compensates independently of a concrete water flow in the rock body.
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