Exciting news! We're transitioning to the Statewide California Earthquake Center. Our new website is under construction, but we'll continue using this website for SCEC business in the meantime. We're also archiving the Southern Center site to preserve its rich history. A new and improved platform is coming soon!

Investigation of transient and hysteretic flash-weakening behavior observed in high-speed friction experiments

Monica R. Barbery, Frederick M. Chester, & Judith S. Chester

Published August 15, 2020, SCEC Contribution #10726, 2020 SCEC Annual Meeting Poster #145

Friction, µ, during seismic slip reflects deformation over a range of length-scales, but fundamentally arises from physical and chemical processes operating at µm-scale contact junctions. In past SCEC research we documented inhomogeneous flash-temperatures, T, at the mm-scale with thermal imaging during high-speed, rock-on-rock friction experiments. By machining groove patterns in sliding surfaces to control mm-scale contact life-time, LT, and rest time, RT, we found that µ-weakening at constant sliding-velocity, V, is consistent with the steady-state model for flash weakening, where µ depends on V at µm-scale contact junctions and on the local mm-scale surface-T distribution. Through thermal modeling we determined the spatial variation of local normal stress and of local µ on the sliding surfaces. Given the different time-frame for heating and cooling of µm- and mm-scale contacts during sliding, we hypothesize that observations of transient µ in the lab, particularly during decelerating phases of slip, reflect the local surface-T dependence on the slip- and thermal-history of contacts at mm and larger length scales. More recently, we conducted a series of high-speed experiments on grooved surfaces in a double-direct shear configuration that achieves ~30 mm of high-speed slip at a macroscopic normal stress of 9 MPa. IR thermographs of the sliding surfaces at 300 Hz record the evolution of surface-T distribution during and after sliding. This series of experiments employed two different contact LT/RT histories, steps to three different velocities between 900 and 300 mm/s, and several different V history scenarios of a constant V followed by a final stage of sliding at decreasing V to arrest over slip distances of 1 to 30 mm. The experiments document an increase in macroscopic frictional weakening from an increase in average T and peak surface-T associated with an increase in V, or with a decrease in contact RT. During the decreasing V stages, µ increases as V decreases displaying hysteretic behavior and occurrence of stick-slip events in which the stress drop decreases with decreasing V. The data display a variety of friction behaviors and surface-T distributions that we will analyze through thermo-mechanical modeling to test the hypothesis above, as well as to determine if the conventional flash-weakening model can reproduce all observed behaviors using a single set of material-property and µm-scale contact values (e.g., contact dimension and strength).

Key Words
rock friction, flash weakening, temperature weakening

Citation
Barbery, M. R., Chester, F. M., & Chester, J. S. (2020, 08). Investigation of transient and hysteretic flash-weakening behavior observed in high-speed friction experiments. Poster Presentation at 2020 SCEC Annual Meeting.


Related Projects & Working Groups
Fault and Rupture Mechanics (FARM)