Articles | Volume 35, issue 1
https://doi.org/10.5194/sd-35-83-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/sd-35-83-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
An urban energy laboratory for monitoring and better understanding of subsurface processes related to low-enthalpy geothermal heat production – UrbEnLab
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
Fraunhofer Research Institution for Energy Infrastructures and Geotechnologies IEG, Cottbus, Germany
Hemmo A. Abels
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
Auke Barnhoorn
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
Claire Bossennec
Laboratoire d'Océanologie et de Géosciences, Université de Lille, ULCO, CNRS, IRD, Villeneuve-d'Ascq, France
Aoife K. Braiden
Research Management & Logistics Ltd, Dublin, Ireland
Maren Brehme
Department of Earth and Planetary Sciences, ETH Zürich, Zurich, Switzerland
Romain Chassagne
Bureau des Recherches Géologiques et Minières (BRGM), Orléans, France
Alexandros Daniilidis
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
Mathieu Darnet
Bureau des Recherches Géologiques et Minières (BRGM), Orléans, France
Guy Drijkoningen
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
Patrick Fulton
Cornell University, Ithaca, NY, USA
Virginie Harcouët-Menou
Flemish Institute for Technological Research (VITO), Mol, Belgium
Ernst Huenges
Klimainitiative Schwielowsee e.V., Schwielowsee, Germany
Stefan Jansen
Deltares, Unit Subsurface and Groundwater Systems, Utrecht, the Netherlands
Alexis Koulidis
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
Susanne Laumann
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
Haiyan Lei
Tianjin University, School of Mechanical Engineering, Tianjin, China
Joseph Moore
University of Utah, Energy and Geoscience Institute, Salt Lake City, Utah, USA
Paula Rulff
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
Thorben Schöfisch
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
Evert Slob
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
Philip J. Vardon
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
Liliana Vargas-Meleza
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
Department of Earth and Planetary Sciences, ETH Zürich, Zurich, Switzerland
Denis Voskov
Department of Geoscience and Engineering, Delft University of Technology, Delft, the Netherlands
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Jérémy Mayen, Pierre Polsenaere, Éric Lamaud, Marie Arnaud, Pierre Kostyrka, Jean-Marc Bonnefond, Philippe Geairon, Julien Gernigon, Romain Chassagne, Thomas Lacoue-Labarthe, Aurore Regaudie de Gioux, and Philippe Souchu
Biogeosciences, 21, 993–1016, https://doi.org/10.5194/bg-21-993-2024, https://doi.org/10.5194/bg-21-993-2024, 2024
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We deployed an atmospheric eddy covariance system to measure continuously the net ecosystem CO2 exchanges (NEE) over a salt marsh and determine the major biophysical drivers. Our results showed an annual carbon sink mainly due to photosynthesis of the marsh plants. Our study also provides relevant information on NEE fluxes during marsh immersion by decreasing daytime CO2 uptake and night-time CO2 emissions at the daily scale, whereas the immersion did not affect the annual marsh C balance.
Mohammadkarim Karimpour, Evert Slob, and Laura Valentina Socco
Solid Earth, 13, 1569–1583, https://doi.org/10.5194/se-13-1569-2022, https://doi.org/10.5194/se-13-1569-2022, 2022
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Near-surface characterisation is of great importance. Surface wave tomography (SWT) is a powerful tool to model the subsurface. In this work we compare straight-ray and curved-ray SWT at near-surface scale. We apply both approaches to four datasets and compare the results in terms of the quality of the final model and the computational cost. We show that in the case of high data coverage, straight-ray SWT can produce similar results to curved-ray SWT but with less computational cost.
Matthis Frey, Claire Bossennec, Lukas Seib, Kristian Bär, Eva Schill, and Ingo Sass
Solid Earth, 13, 935–955, https://doi.org/10.5194/se-13-935-2022, https://doi.org/10.5194/se-13-935-2022, 2022
Short summary
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The crystalline basement is considered a ubiquitous and almost inexhaustible source of geothermal energy in the Upper Rhine Graben. Interdisciplinary investigations of relevant reservoir properties were carried out on analogous rocks in the Odenwald. The highest hydraulic conductivities are expected near large-scale fault zones. In addition, the combination of structural geological and geophysical methods allows a refined mapping of potentially permeable zones.
Cited articles
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Voskov, D., Abels, H., Barnhoorn, A., Chen, Y., Daniilidis, A., Bruhn, D., Drijkoningen, G., Geiger, S. Laumann, S., Song, G., Vardon, P., Vargas Meleza, L., Verschuur, E., and Vondrak, A.: A research and production geothermal project on the TU Delft campus: initial modeling and establishment of a digital twin, 49th Stanford Workshop on Geothermal Reservoir Engineering, https://pangea.stanford.edu/ERE/db/GeoConf/papers/SGW/2024/Voskov.pdf (last access: 10 February 2026), 2024.
Short summary
A workshop on the the scientific value and use of a 4500 m deep borehole on the campus of TU Delft in the Netherlands was held in June 2024. The borehole will serve as an observation infrastructure for processes in the underground related to human activities, such as exploitation of energy resources like geothermal energy or storage of heat or gas. The location is of great interest for this purpose as there are already two deep geothermal wells and shallow wells for heat storage.
A workshop on the the scientific value and use of a 4500 m deep borehole on the campus of TU...

