EGU24-15607, updated on 09 Mar 2024
https://doi.org/10.5194/egusphere-egu24-15607
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

CHENILLE: the fault-heating experiment in the URL Tournemire (France)

Rüdiger Giese1, Audrey Bonnelye2, Pierre Dick3, Carolin Boese1, Stefan Lueth1, Ben Norden1, Katrin Plenkers4, Roman Esefelder5, Christian Cunow1, Liang Pei1, and Sven Fuchs1
Rüdiger Giese et al.
  • 1Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Geomechanics and Scientific Drilling, Potsdam, Germany (rudi@gfz-potsdam.de)
  • 2Université de Lorraine, Georessources, Ecole des Mines de Nancy, France, (audrey.bonnelye@univ-lorraine.fr)
  • 3Institut de Radioprotection et de Sûreté Nucléaire (IRSN), Fontenay-aux-Roses, France, (pierre.dick@irsn.fr)
  • 4Gesellschaft für Material­prüfung und Geophysik (GmuG), Bad Nauheim, Germany (k.plenkers@gmug.eu)
  • 5Friedrich-Schiller-Universität, Institut für Geowissenschaften, Jena, Germany, (roman.esefelder@uni-jena.de)

The understanding of the coupled thermo-hydro-mechanical behavior of fault zones in naturally fractured rocks is essential both for fundamental and applied sciences and in particular for the safety assessment of radioactive waste disposal facilities. An international research program called CHENILLE was built to address key questions related to the impact of high temperatures (up to 120°C) on shear zones as well as fault reactivation processes in shale formations. Here, we report on an ongoing thermally controlled in-situ fluid injection experiment on a strike-slip fault zone outcropping at IRSN’s Tournemire Underground Research Laboratory (URL). This includes a series of laboratory experiments to understand the mechanical, hydraulic, structural and thermal evolution occurring within the fault zones during the thermal and hydraulic loading. Reported preliminary results comprise acoustic emission activity and active seismic monitoring results, the thermal diffusion and the temperature evolution measured in-situ with DTS in and around the fault and the corresponding numerical thermal simulation of the experimental setup.

How to cite: Giese, R., Bonnelye, A., Dick, P., Boese, C., Lueth, S., Norden, B., Plenkers, K., Esefelder, R., Cunow, C., Pei, L., and Fuchs, S.: CHENILLE: the fault-heating experiment in the URL Tournemire (France), EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-15607, https://doi.org/10.5194/egusphere-egu24-15607, 2024.