Articles | Volume 12, issue 1
https://doi.org/10.5194/se-12-35-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/se-12-35-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
13 Jan 2021
Research article |
| 13 Jan 2021
| 13 Jan 2021
Characterization of discontinuities in potential reservoir rocks for geothermal applications in the Rhine-Ruhr metropolitan area (Germany)
Martin Balcewicz
CORRESPONDING AUTHOR
Department of Civil and Environmental Engineering, Bochum University of Applied Sciences, Am Hochschulcampus 1, 44801 Bochum, Germany
Institute of Geology, Mineralogy, and Geophysics, Ruhr University Bochum, Universitätsstraße 150, 44801 Bochum, Germany
Benedikt Ahrens
Fraunhofer IEG, Fraunhofer Research Institution for Energy Infrastructures and Geothermal Systems, Am Hochschulcampus 1, 44801 Bochum, Germany
Kevin Lippert
Fraunhofer IEG, Fraunhofer Research Institution for Energy Infrastructures and Geothermal Systems, Am Hochschulcampus 1, 44801 Bochum, Germany
Institute of Geology, Mineralogy, and Geophysics, Ruhr University Bochum, Universitätsstraße 150, 44801 Bochum, Germany
Erik H. Saenger
Department of Civil and Environmental Engineering, Bochum University of Applied Sciences, Am Hochschulcampus 1, 44801 Bochum, Germany
Fraunhofer IEG, Fraunhofer Research Institution for Energy Infrastructures and Geothermal Systems, Am Hochschulcampus 1, 44801 Bochum, Germany
Institute of Geology, Mineralogy, and Geophysics, Ruhr University Bochum, Universitätsstraße 150, 44801 Bochum, Germany
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Cited
17 citations as recorded by crossref.
- Neutron scattering: A subsurface application review M. Hosseini et al. 10.1016/j.earscirev.2021.103755
- Terpenoids in resinites from middle Cretaceous karst infillings in the Rhenish Massif (Rhineland, Germany): botanical source and preservation B. Simoneit et al. 10.1007/s00531-023-02351-0
- The resin sealed column (RESECO) setup for flow-through experiments on solid rocks under high temperature and high pore pressure conditions J. Grifka et al. 10.1007/s10040-022-02482-9
- Towards a better understanding of the geochemical proxy record of complex carbonate archives M. Mueller et al. 10.1016/j.gca.2024.04.029
- Geothermal reservoir characterisation of Devonian carbonates in North Rhine-Westphalia (W. Germany): Mineralogy- and depofacies-related extrapolation of petrophysical parameters K. Lippert et al. 10.1016/j.geothermics.2022.102549
- Spatial distribution of Mesozoic deposits and their temperature ranges within the Weser-Wiehengebirge Syncline of the inverted Lower Saxony Basin, Minden area, Germany A. Jüstel et al. 10.5194/adgeo-58-121-2023
- Geothermal Reservoir Characterisation of Devonian Carbonates in North Rhine-Westphalia (W. Germany) Mineralogy- and Depofacies-Related Extrapolation of Petrophysical Parameters K. Lippert et al. 10.2139/ssrn.4102877
- The risk of fluid-injection-induced fault reactivation in carbonate reservoirs: an investigation of a geothermal system in the Ruhr region (Germany) M. Kruszewski et al. 10.1007/s40948-023-00573-9
- Fines migration poses challenge for reservoir-wide chemical stimulation of geothermal carbonate reservoirs J. Grifka et al. 10.1016/j.renene.2023.119435
- Scaling in fractured geothermal carbonate reservoir rocks: An experimental approach O. Uwakwe et al. 10.1016/j.geothermics.2024.103199
- In situ stress database of the greater Ruhr region (Germany) derived from hydrofracturing tests and borehole logs M. Kruszewski et al. 10.5194/essd-14-5367-2022
- Structural controls on hydrothermal fluid flow in a carbonate geothermal reservoir: Insights from giant carbonate veins in western Germany L. Smeraglia et al. 10.1016/j.geothermics.2024.103149
- Pressure transient analysis to investigate a coupled fracture corridor and a fault damage zone causing an early thermal breakthrough in the North Alpine Foreland Basin M. Fadel et al. 10.1016/j.geoen.2023.212072
- Digital Rock Physics: A Geological Driven Workflow for the Segmentation of Anisotropic Ruhr Sandstone M. Balcewicz et al. 10.3389/feart.2021.673753
- In Situ Stress State of the Ruhr Region (Germany) and Its Implications for Permeability Anisotropy M. Kruszewski et al. 10.1007/s00603-021-02636-3
- 3D in situ stress state modelling and fault reactivation risk exemplified in the Ruhr region (Germany) M. Kruszewski et al. 10.1016/j.gete.2022.100386
- Porosity estimation of a geothermal carbonate reservoir in the German Molasse Basin based on seismic amplitude inversion S. Wadas & H. von Hartmann 10.1186/s40517-022-00223-5
17 citations as recorded by crossref.
- Neutron scattering: A subsurface application review M. Hosseini et al. 10.1016/j.earscirev.2021.103755
- Terpenoids in resinites from middle Cretaceous karst infillings in the Rhenish Massif (Rhineland, Germany): botanical source and preservation B. Simoneit et al. 10.1007/s00531-023-02351-0
- The resin sealed column (RESECO) setup for flow-through experiments on solid rocks under high temperature and high pore pressure conditions J. Grifka et al. 10.1007/s10040-022-02482-9
- Towards a better understanding of the geochemical proxy record of complex carbonate archives M. Mueller et al. 10.1016/j.gca.2024.04.029
- Geothermal reservoir characterisation of Devonian carbonates in North Rhine-Westphalia (W. Germany): Mineralogy- and depofacies-related extrapolation of petrophysical parameters K. Lippert et al. 10.1016/j.geothermics.2022.102549
- Spatial distribution of Mesozoic deposits and their temperature ranges within the Weser-Wiehengebirge Syncline of the inverted Lower Saxony Basin, Minden area, Germany A. Jüstel et al. 10.5194/adgeo-58-121-2023
- Geothermal Reservoir Characterisation of Devonian Carbonates in North Rhine-Westphalia (W. Germany) Mineralogy- and Depofacies-Related Extrapolation of Petrophysical Parameters K. Lippert et al. 10.2139/ssrn.4102877
- The risk of fluid-injection-induced fault reactivation in carbonate reservoirs: an investigation of a geothermal system in the Ruhr region (Germany) M. Kruszewski et al. 10.1007/s40948-023-00573-9
- Fines migration poses challenge for reservoir-wide chemical stimulation of geothermal carbonate reservoirs J. Grifka et al. 10.1016/j.renene.2023.119435
- Scaling in fractured geothermal carbonate reservoir rocks: An experimental approach O. Uwakwe et al. 10.1016/j.geothermics.2024.103199
- In situ stress database of the greater Ruhr region (Germany) derived from hydrofracturing tests and borehole logs M. Kruszewski et al. 10.5194/essd-14-5367-2022
- Structural controls on hydrothermal fluid flow in a carbonate geothermal reservoir: Insights from giant carbonate veins in western Germany L. Smeraglia et al. 10.1016/j.geothermics.2024.103149
- Pressure transient analysis to investigate a coupled fracture corridor and a fault damage zone causing an early thermal breakthrough in the North Alpine Foreland Basin M. Fadel et al. 10.1016/j.geoen.2023.212072
- Digital Rock Physics: A Geological Driven Workflow for the Segmentation of Anisotropic Ruhr Sandstone M. Balcewicz et al. 10.3389/feart.2021.673753
- In Situ Stress State of the Ruhr Region (Germany) and Its Implications for Permeability Anisotropy M. Kruszewski et al. 10.1007/s00603-021-02636-3
- 3D in situ stress state modelling and fault reactivation risk exemplified in the Ruhr region (Germany) M. Kruszewski et al. 10.1016/j.gete.2022.100386
- Porosity estimation of a geothermal carbonate reservoir in the German Molasse Basin based on seismic amplitude inversion S. Wadas & H. von Hartmann 10.1186/s40517-022-00223-5
Latest update: 13 Dec 2024
Short summary
The geothermal potential of a carbonate reservoir in the Rhine-Ruhr area, Germany, was investigated by field and laboratory investigations. The carbonate layer of interest is approx. 150 m thick; located at 4 to 6 km depth; and might extend below Essen, Bochum, and Dortmund. We proposed focusing on discontinuities striking NNW–SSE for geothermal applications, as these are the most common, strike in the direction of the main horizontal stress, and dominate reservoir fluid flow.
The geothermal potential of a carbonate reservoir in the Rhine-Ruhr area, Germany, was...
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