Frictional slip weakening and shear-enhanced crystallinity in simulated coal fault gouges at subseismic slip rates
Publisher: name: Utrecht University
Year: 2020
Subjects: subject: Natural Sciences - Earth and related environmental sciences (1.5)
subject: rate-dependent friction
subject: frictional healing
subject: slip-weakening
subject: coal maturity
subject: coal molecular structure
subject: Solid Earth &gt; Rocks / Minerals / Crystals &gt; Sedimentary Rocks &gt; Coal
subject: Spectroscopy &gt; Raman
subject: Scanning Electrone Microscope
subject: Optical Microscope
subject: X-Ray Diffractometer
subject: Triaxial
subject: coal
subject: Composition
subject: Friction
subject: Friction &gt; Imposed Slip &gt; Slide-Hold-Slide
subject: Friction &gt; Imposed Slip &gt; Rate-State
subject: Thermocouple
subject: EPOS
subject: multi-scale laboratories
subject: rock and melt physical properties

description: We report seven velocity stepping (VS) and one slide-hold-slide (SHS) friction experiments performed on simulated fault gouges prepared from bituminous coal, collected from the upper Silesian Basin of Poland. These experiments were performed at 25-45 MPa effective normal stress and 100 ℃, employing sliding velocities of 0.1-100 μm/s, using a conventional triaxial apparatus plus direct shear assembly. All samples showed marked slip weakening behaviour at shear displacements beyond ~1-2 mm, from a peak friction coefficient approaching ~0.5 to (near) steady state values of ~0.3, regardless of effective normal stress or whether vacuum dry flooded with distilled (DI) water at 15 MPa pore fluid pressure. Analysis of both unsheared and sheared samples by means of microstructural observation, micro-area X-ray diffraction (XRD) and Raman spectroscopy suggests that the marked slip weakening behaviour can be attributed to the development of R-, B- and Y- shear bands, with internal shear-enhanced coal crystallinity development. The SHS experiment performed showed a transient peak healing (restrengthening) effect that increased with the logarithm of hold time at a linearized rate of ~0.006. We also determined the rate-dependence of steady state friction for all VS samples using a full rate and state friction approach. This showed a transition from velocity strengthening to velocity weakening at slip velocities >1 μm/s in the coal sample under vacuum dry conditions, but at >10 μm/s in coal samples exposed to DI water at 15 MPa pore pressure. This may be controlled by competition between dilatant granular flow and compaction enhanced by presence of water. Together with our previous work on frictional properties of coal-shale mixtures, our results imply that the presence of a weak, coal-dominated patch on faults that cut or smear-out coal seams may promote unstable, seismogenic slip behaviour, though the importance of this in enhancing either induced or natural seismicity depends on local conditions. The data is provided in a folder with 10 subfolders for 10 experiments/samples, including friction, XRD and Raman data. Detailed information about the files in these subfolders as well as information on how the data is processed is given in the explanatory file Fan-et-al-2020-Data-Description.pdf. Contact person is Dr. Jinfeng Liu - Sun Yat-Sen University- liujinf5@mail.sysu.edu.cn