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Geothermal Energy

Science – Society – Technology

Fig. 2 | Geothermal Energy

Fig. 2

From: How temperatures derived from fluid flow and heat transport models impact predictions of deep geothermal potentials: the “heat in place” method applied to Hesse (Germany)

Fig. 2

Results show in columns from left to right thickness distribution and temperature derived with the Conductive Model at the middle reservoir depth [after Koltzer et al. (2019a)] and in the right column calculated HIP values for the three model units of Cenozoic (a–c), Buntsandstein (d–f) and Rotliegend (g–i) from top to bottom. In white regions the respective model unit is missing in the model region. Maps are shown in Gauß–Krüger DHDN Zone 3. Maps were created with ParaView (Squillacote et al. 2007) and the used graphics software was Adobe Illustrator (Adobe Inc. 2019)

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