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)

Geothermal Energy

Research

Judith Bott¹  Magdalena Scheck-Wenderoth²  Nora Koltzer³  Kristian Bär⁴ 

[1]Basin Modelling, Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany

[2]Basin Modelling, Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany

[3]Faculty of Georesources and Material Engineering, RWTH Aachen, Aachen, Germany

[4]Basin Modelling, Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany

[5]Faculty of Georesources and Material Engineering, RWTH Aachen, Aachen, Germany

[6]Fraunhofer Research Institution for Energy Infrastructures and Geothermal Systems IEG, Bochum, Germany

[7]GeoThermal Engineering GmbH, Karlsruhe, Germany

关键词: Upper Rhine Graben;    Hessen;    Heat in place;    3D Hydrothermal Model;    Geothermal energy;    Geothermal potential;    Heat transport;   

DOI  :  10.1186/s40517-023-00245-7

 received in 2022-03-02, accepted in 2022-12-31,  发布年份 2022

来源: Springer

【 授权许可】

CC BY   
© The Author(s) 2023

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