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D4.2 – Analysis of temperature ranges and fluid flow rates in a 3D subsurface model

Deliverable D4.2 covers the progress of work done in Task 4.1 of workpackage 4. This task aims at generating a detailed 3D geological model of the subsurface of the city of Geilenkirchen. Geologically speaking, this area belongs to the lower Rhine Embayment and comprises tertiary sediments unconformably overlying carboniferous sediments. Neu-Teveren, a settlement adjacent to the NATO-Airbase of Teveren, is planned to be fully restructured within the next years. In the course of reconstruction, space heating and cooling by geothermal direct heat supply is one option, which will be presented to potential stakeholders.