Description
The topic is an interpolation of the groundwater temperatures measured at the individual measuring points in September 20 131 m below the groundwater surface outside the quaternary Elbtal GWL. It is assumed that the temperature in the underground also balances itself independently of a concrete water flow in the rock body. Data base is a reference date measurement carried out in September 2013.
Resources
| Name | Format | Description | Link |
|---|---|---|---|
| view | Unknown | Open resource |