Using Rate and State Friction to Simulate Fluid Injection Laboratory Experiments
Fluid injection into the Earth’s crust for industrial applications, such as disposal of waste water from hydraulic fracturing, extraction of geothermal energy, and carbon sequestration, has caused seismic activity. The seismicity has raised concerns about safety and resulted in limiting or terminating the injection activities. A field experiment in the 1970s that demonstrated fluid injection could cause earthquakes helped to advanced our understanding of this basic mechanism. Nevertheless, there is still much that is not understood about the factors that give rise to induced seismicity. These include the amount and protocols of injection, and the hydrological and material behavior of the faults. Ultimately, field experiments are required in order to address these issues, but their interpretation is often complicated by uncertainties relating to hydraulic and mechanical structure, boundary conditions and stress state. Despite their limited size and time scales, laboratory experiments offer a more controlled environment to explore the interaction of material behavior and injection. This talk will present results for using rate and state friction to model three sets of laboratory experiments with fluid injection. This includes experiments in a double direct shear apparatus under creep conditions on simulated calcite fault gouge (Scuderi et al., EPSL, 2017), experiments on a shale (Scuderi and Collettini, JGR, 2018), and fluid pressure oscillations on granite in a triaxial apparatus (Noȅl et al., JGR, 2019). The comparison of the simulation results and the laboratory measurements shows that rate and friction does capture salient aspects of the experiment but there are clearly other factors that are not well understood. The simulations can explore a wider range of conditions, thereby revealing a richer behavior than is evident from the experiments.