Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Effects of temperature on friction: Constitutive equations and experiments with quartz gouge

Journal Article · · Journal of Geophysical Research
DOI:https://doi.org/10.1029/93JB03110· OSTI ID:57408
 [1]
  1. Saint Louis Univ., St. Louis, MO (United States)

A state-variable constitutive relation that can describe the dependence of friction on temperature at or near steady state conditions is presented. The relation is derived from existing state-variable relations used to describe velocity dependence and the assumption that the micro-mechanisms of friction are thermally activated and follow an Arrhenius relationship. The relation adequately describes the transient and steady friction behavior displayed in sliding experiments on 1.5-mm-thick layers of fine-grained (less than 100 micron diameter) quartz gouge. Gouge layers were sheared up to 10 mm between rough steel surfaces at a constant effective confining pressure of 20 MPa and under room-dry or water-saturated conditions in a servo-controlled triaxial apparatus. In each experiment, velocity was stepped between 4, 0.4, and 0.04 microns/s at constant temperature, and temperature was stepped between 24, 57, and 82 C at a constant velocity of 0.04 microns/s. Coefficient of friction was calculated from measurements of sample strength using corrections for all apparatus effects including the temperature and velocity dependent strength of the metal sleeves used to isolate the sample and of the graphite-lubricated interface that allowed lateral slip of the sample halves. Experiments indicate that (1) an abrupt increase in temperature induces a transient friction response similar to that induced by a step decrease in velocity, (2) the transient friction response is relatively symmetric for steps up and steps down in temperature, and (3) the characteristic slip distance for friction to evolve to steady state after step changes in temperature is the same as after step changes in velocity. The apparent activation energy determined for wet quartz gouge at the test conditions is 89 +/- 23 kJ/mol. (Abstract Truncated)

OSTI ID:
57408
Journal Information:
Journal of Geophysical Research, Journal Name: Journal of Geophysical Research Journal Issue: B4 Vol. 99; ISSN JGREA2; ISSN 0148-0227
Country of Publication:
United States
Language:
English

Similar Records

Stabilizing Effect of High Pore Fluid Pressure on Slip Behaviors of Gouge-bearing Faults
Journal Article · Thu Aug 29 00:00:00 EDT 2019 · Journal of Geophysical Research. Solid Earth · OSTI ID:1609825

A new apparatus for the concurrent measurement of friction and permeability evolution in fault gouge
Journal Article · Tue Jul 02 00:00:00 EDT 2019 · International Journal of Rock Mechanics and Mining Sciences · OSTI ID:1614204

Ensemble Shear Strength, Stability, and Permeability of Mixed Mineralogy Fault Gouge Recovered From 3D Granular Models
Journal Article · Thu Jan 24 23:00:00 EST 2019 · Journal of Geophysical Research. Solid Earth · OSTI ID:1614206