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The ArtemIS project: Assessment for medium-depth geothermal energy utilization in Germany

Authors

Weydt,  Leandra M.
External Organizations;

Agemar,  Thorsten
External Organizations;

Erb,  Michael
External Organizations;

Mantei,  Niklas
External Organizations;

Dobrzinski,  Nicole
External Organizations;

Weber,  Josef
External Organizations;

Sperlich,  Sebastian
External Organizations;

van der Vaart,  Jeroen
External Organizations;

Bär,  Kristian
External Organizations;

Moeck,  Inga
External Organizations;

/persons/resource/sass

Sass,  Ingo
4.3 Geoenergy, 4.0 Geosystems, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

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Fulltext (public)

5035279.pdf
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Citation

Weydt, L. M., Agemar, T., Erb, M., Mantei, N., Dobrzinski, N., Weber, J., Sperlich, S., van der Vaart, J., Bär, K., Moeck, I., Sass, I. (2025): The ArtemIS project: Assessment for medium-depth geothermal energy utilization in Germany. - Advances in Geosciences, 65, 199-210.
https://doi.org/10.5194/adgeo-65-199-2025


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5035279
Abstract
To date, most geothermal projects in Germany have focused on deep geothermal systems, while resources at intermediate depths have only been explored to a small extend. However, medium-depth geothermal systems have a high potential for heat generation, even in areas previously considered less favorable for deep geothermal energy, and could make a significant contribution to Germany's heat supply. To accelerate the heat transition and to become independent of fossil fuels, the ArtemIS project aims to assess the medium-depth geothermal systems in Germany, covering all types of geological plays and providing regional information for different geothermal applications. Interactive heat transition profiles are being developed containing all relevant subsurface information required for preliminary geothermal assessment, such as geological descriptions of potential geothermal reservoirs, reservoir thickness, hydraulic and thermal rock properties, and fluid chemistry. In addition, static 3D geological models are being created as the basis for 3D numerical reservoir models using COMSOL Multiphysics to simulate the regional heat potential and different geothermal scenarios, including the performance of hydrothermal doublets. The investigation of well logs and core sample data of the Upper Maastrichtian Calcarenites in the North German Basin indicates a good geothermal potential, but notable lateral and vertical heterogeneities regarding reservoir thickness, grain size or glauconite content throughout the study area need to be considered during exploration. The first COMSOL simulation results highlight the impact of inter-well distance and reservoir thickness on operational parameters such as the occurrence time of thermal breakthrough and cooling rate in a multi-well array. Likewise, a 3D structural model of the Upper Rhine Graben was created and used to assess the regional heat supply, indicating a high potential for heat production in the sedimentary units at intermediate depths. The results of the ArtemIS project will be integrated into the publicly available web platform “Geothermal Information System – GeotIS”, which will provide general information, data, and modelling results in a user-friendly way for non-professionals such as local communities and municipal energy suppliers.