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Geothermal Energy

Science – Society – Technology

Fig. 3 | Geothermal Energy

Fig. 3

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. 3

Difference maps of the HIP in the Cenozoic (a, b), Buntsandstein (c, d) and Rotliegend (e, f) model units from top to bottom. The HIP differences show the calculated HIP from the Conductive Model minus the Advective Model (a, c, e) and the calculated difference of the Conductive Model minus the Convective Model (b, d, f). With blue colours lower HIP is predicted with the Advective and Convective Models and with red colours, advection and convection lead to higher predicted HIP. 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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