How fluid flow and heat transport models impact predictions of deep geothermal potentials: the "heat in place" method applied to Hesse (Germany)

Nora Koltzer; Judith Bott; Magdalena Scheck-Wenderoth; Kristian Bär

doi:https://doi.org/10.5194/egusphere-egu22-3378

[Back] [Session ERE2.4]

EGU22-3378

https://doi.org/10.5194/egusphere-egu22-3378

EGU General Assembly 2022

© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

How fluid flow and heat transport models impact predictions of deep geothermal potentials: the "heat in place" method applied to Hesse (Germany)

Nora Koltzer^1,2, Judith Bott¹, Magdalena Scheck-Wenderoth^1,2, and Kristian Bär³

Nora Koltzer et al.

¹Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, 4.5 Basin Modelling, Potsdam, Germany (nora.koltzer@gfz-potsdam.de)
²RWTH Aachen, Faculty of Georesources and Material Engineering, Aachen, Germany
³Technische Universität Darmstadt, Institute of Applied Geosciences, Department of Geothermal Science and Technology, Darmstadt, Germany

How to cite: Koltzer, N., Bott, J., Scheck-Wenderoth, M., and Bär, K.: How fluid flow and heat transport models impact predictions of deep geothermal potentials: the "heat in place" method applied to Hesse (Germany), EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-3378, https://doi.org/10.5194/egusphere-egu22-3378, 2022.

This abstract has been withdrawn on 22 Apr 2022.