Articles | Volume 13, issue 2
https://doi.org/10.5194/se-13-301-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-13-301-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
02 Feb 2022
Research article |
| 02 Feb 2022
| 02 Feb 2022
Multi-disciplinary characterizations of the BedrettoLab – a new underground geoscience research facility
Xiaodong Ma
CORRESPONDING AUTHOR
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Marian Hertrich
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Florian Amann
Engineering Geology and Hydrogeology, RWTH Aachen, 52062 Aachen,
Germany
Kai Bröker
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Nima Gholizadeh Doonechaly
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Valentin Gischig
CSD Ingenieure AG, 3097 Liebefeld, Switzerland
Rebecca Hochreutener
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Philipp Kästli
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Hannes Krietsch
Engineering Geology and Hydrogeology, RWTH Aachen, 52062 Aachen,
Germany
Michèle Marti
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Barbara Nägeli
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Morteza Nejati
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Anne Obermann
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Katrin Plenkers
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Antonio P. Rinaldi
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Alexis Shakas
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Linus Villiger
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Quinn Wenning
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Alba Zappone
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Falko Bethmann
Geo-Energie Suisse AG, 8004 Zürich, Switzerland
Raymi Castilla
Geo-Energie Suisse AG, 8004 Zürich, Switzerland
Francisco Seberto
Geo-Energie Suisse AG, 8004 Zürich, Switzerland
Peter Meier
Geo-Energie Suisse AG, 8004 Zürich, Switzerland
Thomas Driesner
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Simon Loew
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Hansruedi Maurer
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Martin O. Saar
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Stefan Wiemer
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
Domenico Giardini
Department of Earth Sciences, ETH Zürich, 8092 Zürich,
Switzerland
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Alba Zappone, Antonio Pio Rinaldi, Melchior Grab, Quinn C. Wenning, Clément Roques, Claudio Madonna, Anne C. Obermann, Stefano M. Bernasconi, Matthias S. Brennwald, Rolf Kipfer, Florian Soom, Paul Cook, Yves Guglielmi, Christophe Nussbaum, Domenico Giardini, Marco Mazzotti, and Stefan Wiemer
Solid Earth, 12, 319–343, https://doi.org/10.5194/se-12-319-2021, https://doi.org/10.5194/se-12-319-2021, 2021
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The success of the geological storage of carbon dioxide is linked to the availability at depth of a capable reservoir and an impermeable caprock. The sealing capacity of the caprock is a key parameter for long-term CO2 containment. Faults crosscutting the caprock might represent preferential pathways for CO2 to escape. A decameter-scale experiment on injection in a fault, monitored by an integrated network of multiparamerter sensors, sheds light on the mobility of fluids within the fault.
Larissa de Palézieux, Kerry Leith, and Simon Loew
Earth Surf. Dynam. Discuss., https://doi.org/10.5194/esurf-2020-85, https://doi.org/10.5194/esurf-2020-85, 2020
Revised manuscript not accepted
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Large creeping landslides are persistent features in mountainous landscapes. In order to quantify the long-term evolution of landslides and their interaction with river channels, we use a new metric for landslide-induced channel offset, which allows us to identify locations associated with increased landslide activity and estimate landslide displacement rates over a period of 1 Myr.
Camilla Rossi, Francesco Grigoli, Simone Cesca, Sebastian Heimann, Paolo Gasperini, Vala Hjörleifsdóttir, Torsten Dahm, Christopher J. Bean, Stefan Wiemer, Luca Scarabello, Nima Nooshiri, John F. Clinton, Anne Obermann, Kristján Ágústsson, and Thorbjörg Ágústsdóttir
Adv. Geosci., 54, 129–136, https://doi.org/10.5194/adgeo-54-129-2020, https://doi.org/10.5194/adgeo-54-129-2020, 2020
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We investigate the microseismicity occurred at Hengill area, a complex tectonic and geothermal site, where the origin of earthquakes may be either natural or anthropogenic. We use a very dense broadband seismic monitoring network and apply full-waveform based method for location. Our results and first characterization identified different types of microseismic clusters, which might be associated to either production/injection or the tectonic activity of the geothermal area.
Gregory Church, Melchior Grab, Cédric Schmelzbach, Andreas Bauder, and Hansruedi Maurer
The Cryosphere, 14, 3269–3286, https://doi.org/10.5194/tc-14-3269-2020, https://doi.org/10.5194/tc-14-3269-2020, 2020
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Short summary
In this field study, we repeated ground-penetrating radar measurements over an active englacial channel network that transports meltwater through the glacier. We successfully imaged the englacial meltwater pathway and were able to delimitate the channel's shape. Meltwater from the glacier can impact the glacier's dynamics if it reaches the ice–bed interface, and therefore monitoring these englacial drainage networks is important to understand how these networks behave throughout a season.
Hannes Krietsch, Valentin S. Gischig, Joseph Doetsch, Keith F. Evans, Linus Villiger, Mohammadreza Jalali, Benoît Valley, Simon Löw, and Florian Amann
Solid Earth, 11, 1699–1729, https://doi.org/10.5194/se-11-1699-2020, https://doi.org/10.5194/se-11-1699-2020, 2020
Sonja Martens, Maren Brehme, Viktor J. Bruckman, Christopher Juhlin, Johannes Miocic, Antonio P. Rinaldi, and Michael Kühn
Adv. Geosci., 54, 1–5, https://doi.org/10.5194/adgeo-54-1-2020, https://doi.org/10.5194/adgeo-54-1-2020, 2020
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Short summary
Questions on issues such as anthropogenic earthquakes and deep geothermal energy developments require a better understanding of the fractured rock. Experiments conducted at reduced scales but with higher-resolution observations can shed some light. To this end, the BedrettoLab was recently established in an existing tunnel in Ticino, Switzerland, with preliminary efforts to characterize realistic rock mass behavior at the hectometer scale.
Questions on issues such as anthropogenic earthquakes and deep geothermal energy developments...
