Weak Velocity Weakening of Augite with Concomitant Intergranular
Pressure Solution under Hydrothermal Conditions
Abstract
To fully understand the constitutive parameters and the associated
mechanism in the velocity-weakening behavior of pyroxene observed in a
previous study (He et al., 2013), we employed pure augite
(clinopyroxene) as simulated gouge sample to run velocity stepping
sliding tests under hydrothermal conditions with temperatures of 101-607
°C, effective normal stress of 200 MPa with 30 MPa pore pressure and
axial loading rates of 0.1-1.0 μm/s. From our experiments, we found
that: (1) Velocity-strengthening behavior was observed at temperatures
of 101-203 °C, the steady-state velocity dependence transitioned to
velocity weakening at ~215 °C, and the velocity
weakening persisted up to 607 °C, the highest temperature in our
experiments. The absolute (b-a) values were revealed to range from
0.0009 to 0.0014, and the inferred average b/a values ranged from
1.15-1.18, both indicating quite weak velocity weakening at temperatures
of 303-607 °C. (2) Inferred constitutive parameters through numerical
fitting to rate and state friction laws show that the healing effect of
friction (b value) has an increasing trend with temperature increase up
to 403 °C, indicating an Arrhenius-type thermally-activated creep
mechanism behind the healing effect. (3) In addition to microstructural
observation of deformed samples that shows remarkable size reduction
(crushed grains reduced to scales typically below 1-2 μm) in both
intensely sheared regions and moderately sheared regions, ubiquitous
precipitated particles (50-100 nm) with platy morphologies were observed
to attach to the surfaces of crushed grains, which are typical
signatures of intergranular pressure solution process, suggesting that
pressure solution was commonly activated at intergranular contacts. (4)
No recognizable crystalline plasticity was observed. Our microstructural
observation together with the comparison of experimental data with
model’s prediction, implies that intergranular pressure solution process
at the frictional contacts may be the most likely mechanism operating at
the frictional contacts and governing the healing effect for augite.