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

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

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 Creators:
Giese, Rüdiger1, Author              
Bonnelye, A.1, Author              
Dick, P., Author
Boese, C. M.1, Author              
Lueth, S.2, Author              
Norden, Ben3, Author              
Plenkers, Katrin1, Author              
Esefelder, Roman2, Author              
Cunow, Christian3, Author              
Pei, Liang3, Author              
Fuchs, Sven3, Author              
Affiliations:
14.2 Geomechanics and Scientific Drilling, 4.0 Geosystems, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146035              
22.2 Geophysical Imaging of the Subsurface, 2.0 Geophysics, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_66027              
34.8 Geoenergy, 4.0 Geosystems, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146039              

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 Abstract: 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.

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 Dates: 20242024
 Publication Status: Finally published
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 Identifiers: DOI: 10.5194/egusphere-egu24-15607
GFZPOF: p4 T8 Georesources
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Title: EGU General Assembly 2024
Place of Event: Vienna, Austria and Online
Start-/End Date: 2024-04-14 - 2024-04-19

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Title: Abstracts
Source Genre: Proceedings
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