EGU2020-18041
https://doi.org/10.5194/egusphere-egu2020-18041
EGU General Assembly 2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Coupled processes in clay during tunnel excavation

Antonio Pio Rinaldi1,2, Yves Guglielmi2, Alba Zappone1, Florian Soom2, Michelle Robertson2, Paul Cook2, Maria Kakurina3, Quinn Wenning1, Dorothee Rebscher4, and Christophe Nussbaum5
Antonio Pio Rinaldi et al.
  • 1Swiss Seismological Service, ETH Zürich, Zürich, Switzerland (antoniopio.rinaldi@sed.ethz.ch)
  • 2Energy Geosciences Division, LBNL, Berkeley, CA, USA
  • 3Center for Hydrogeology and Geothermics, UNINE, Switzerland
  • 4Bundesanstalt für Geowissenschaften und Rohstoffe, BGR, Hannover, Deutschland
  • 5Federal Office of Topography, swisstopo, St-Ursanne, Switzerland

Tunnel excavations are known to perturb the hosting rock mass at long distances, with changes in the hydrogeological flow affecting, as well as deforming the rock mass, inducing subsidence in a zone above the tunnel. During the extension of the Mont Terri Underground Rock Laboratory, we had the unique opportunity to monitor the final part of the excavation of Gallery18 and the final breaktrough.

The joint effort of two experiments (CS-D lead by ETH Zurich and FS-B lead by LBNL) allowed for a detailed characterization of the poro-elastic response of the rock mass and the Mont Terri Main Fault Zone to the excavation. Geophysical, geomechanical, and hydrogeological monitoring include: (1) pressure monitoring in several borehole intervals; (2) deformation at a chain potentiometer and fiber optics grouted in boreholes (normal to bedding and parallel to fault zone), and platform-tilmeters installed at the tunnel floor, as well as detailed 3D displacement at the SIMFIP probe.

All monitoring systems detected major perturbations starting from 15 days before the breakthrough and continuing for several days after it. We summarize the observations and will combine numerical modelling and observed trend to conceptualized the pattern of poro-elastic deformation. The results of the analysis could help shedding light on the poro-elastic behaviour of clay, providing interesting hints for the modeling community and helping in planning of future nuclear waste repositories in such material.

How to cite: Rinaldi, A. P., Guglielmi, Y., Zappone, A., Soom, F., Robertson, M., Cook, P., Kakurina, M., Wenning, Q., Rebscher, D., and Nussbaum, C.: Coupled processes in clay during tunnel excavation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18041, https://doi.org/10.5194/egusphere-egu2020-18041, 2020

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