Laboratory simulation of fault reactivation by fluid injection and implications for induced seismicity at the BedrettoLab, Swiss Alps

Fluid induced fault reactivation experiments will take place as part of the Fault Activation and Earthquake Rupture project (FEAR) at the BedrettoLab, an un-derground laboratory for geosciences and geo-energy excavated within the Rotondo massif (Swiss Alps). The aim of this publication is to characterize frictional properties and permeability of the main segment of the fault zone selected for limited fluid-induced fault reactivation experiments. Firstly, we characterized fault zone microstructures in the field and in thin sections. Secondly, we assessed fault gouge mineralogy by X-ray powder diffraction analysis, yielding a composition in agreement with similar fault gouges in the same area. Finally, we performed a detailed frictional and permeability characterization in laboratory, using BRAVA (Brittle Rock deformAtion Versatile Apparatus). We performed five frictional experiments, run at the actual in-situ conditions: four experiments for frictional properties characterization; and one further experiment where we stimulated the experimental fault by fluid pressurization applying a similar injection protocol designed for the in-situ hydraulic stimulation experiment. Additionally, we performed microstructural analysis on experimental samples to link frictional and permeability properties with fault fabric evolution. The integration of experimental results with field investigations suggests that the selected fault is potentially seismogenic and can be dynamically reactivated and controlled with hydraulic stimulation. This study highlights the importance of bridging the gap between laboratory and in-situ fault characterization, where experimental results become instrumental for the correct design of injection protocols such as those of FEAR project.

Automated summary

Fluid induced fault reactivation experiments were conducted at BedrettoLab to characterize frictional properties and permeability of a selected fault zone. Field investigation and X-ray powder diffraction analysis were used to characterize fault zone microstructures and fault gouge mineralogy. Frictional and permeability characterization were performed using BRAVA in the laboratory, and the experimental results were integrated with field investigations to identify the seismogenic potential and hydraulic stimulation feasibility of the selected fault.