MR33C-2694
Is frictional healing slip-dependent?

Wednesday, 16 December 2015
Poster Hall (Moscone South)
Pathikrit Bhattacharya1, Allan M Rubin1, Kerry L Ryan2, Jacques Vincent Riviere3 and Chris Marone2, (1)Princeton University, Princeton, NJ, United States, (2)Pennsylvania State University Main Campus, University Park, PA, United States, (3)Los Alamos National Laboratory, Earth and Environmental Sciences, Los Alamos, NM, United States
Abstract:
Frictional re-strengthening of bare rock surfaces at very low stresses and near zero slip rate, as observed in the laboratory, is traditionally interpreted as showing support for purely time-dependent healing as embodied in the Aging law. However, while slide-hold-slide experiments on bare surfaces do show an apparent (purely) time-dependent increase in the static friction upon reslide, we show that the stress minima attained during the preceding holds show a strong slip-dependence which contradict the Aging law. A velocity strengthening Slip law explains such data much better. We also show that, large velocity step decreases, which drive the system far below steady state just like long holds, clearly support the slip-dependent response of the Slip law over the time-dependent healing contained in the Aging law.

But, while time-dependent healing has an intuitive physical picture in terms of growth of the 'real contact area' with time, it is more difficult to ascribe one to slip-dependent healing. Here, we explore the possibility that the slip-dependence arises out of an interplay between contact `quality' and `quantity' at the scale of the asperity contacts. First, to further study the slip-dependence of healing, we carry out large velocity step decreases and sequences of long slide-hold-slides on both bare rock and gouge. Secondly, to probe the micro-mechanical origins of healing, we complement our mechanical data with amplitudes and travel time data of ultrasonic P- and S- waves transmitted across the sliding interface. While ultrasonic P-wave transmissivity has been used as a proxy for 'real contact area' in friction experiments by Nagata et al. (2012, 2014) before, the simultaneous use of P- and S-phases in our experiments is designed specifically to probe contact rheology. Initial results show strong correlations between changes in friction, transmitted wave amplitudes and travel times in response to changes in slip rate. We also observe important differences between the friction and ultrasonic data which might illuminate the role of contact `quality' in determining frictional strength. Using the ultrasonic data along with numerical modeling and inversion of the friction data, we hope to probe the micro-mechanical origins of frictional healing and rate-and-state friction in general.