Symmetry and the critical slip distance in rate and state friction laws

Andrew P. Rathbun, Chris Marone

Research output: Contribution to journalArticle

12 Citations (Scopus)

Abstract

We performed laboratory experiments to investigate the processes responsible for rate and state friction (RSF) behavior in fault rocks. We focused on the symmetry of the frictional constitutive response to velocity changes and the mechanics of the critical friction slip distance Dc. Experiments were conducted in double direct shear at 1 and 25 MPa normal stress, at room temperature, and for shearing velocity from 1 to 300 μm/s. We studied three granular materials and bare surfaces of Westerly granite. Ruina's law, which predicts frictional symmetry between velocity increases and decreases, better matches our data than Dieterich's law, which predicts that velocity decreases should evolve to steady state at a smaller displacement. However, for granular shear, in some cases Dc is smaller for velocity increases than for velocity decreases, contrary to expectations from either law. On bare granite surfaces, the frictional response is symmetric for velocity increases/decreases. Two distinct length scales for Dc and two-state variables are required for granular shear in some cases. We hypothesize that asymmetry and two-state behavior are caused by shear localization and changes in shear fabric in fault gouge. Our measurements show that during steady state frictional shear, dilation after a velocity increase is smaller than compaction after a decrease. Normal stress oscillations cause a marked decrease in D c. Reduction of Dc reduces frictional stability, enhancing the possibility of seismic slip. Our experiments show that shear localization and fabric within the fault gouge can influence the RSF parameters that dictate earthquake nucleation and dynamic rupture. Key Points Ruina law best fits lab data Localization changes the frictional response Localization enhances the possibility of seismic slip

Original languageEnglish (US)
Pages (from-to)3728-3741
Number of pages14
JournalJournal of Geophysical Research: Solid Earth
Volume118
Issue number7
DOIs
StatePublished - Jul 1 2013

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symmetry
slip
friction
Friction
shear
fault gouge
granite
rate
Granular materials
Experiments
granular materials
dilation
shearing
Shearing
westerly
nucleation
mechanics
rupture
compaction
asymmetry

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Cite this

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abstract = "We performed laboratory experiments to investigate the processes responsible for rate and state friction (RSF) behavior in fault rocks. We focused on the symmetry of the frictional constitutive response to velocity changes and the mechanics of the critical friction slip distance Dc. Experiments were conducted in double direct shear at 1 and 25 MPa normal stress, at room temperature, and for shearing velocity from 1 to 300 μm/s. We studied three granular materials and bare surfaces of Westerly granite. Ruina's law, which predicts frictional symmetry between velocity increases and decreases, better matches our data than Dieterich's law, which predicts that velocity decreases should evolve to steady state at a smaller displacement. However, for granular shear, in some cases Dc is smaller for velocity increases than for velocity decreases, contrary to expectations from either law. On bare granite surfaces, the frictional response is symmetric for velocity increases/decreases. Two distinct length scales for Dc and two-state variables are required for granular shear in some cases. We hypothesize that asymmetry and two-state behavior are caused by shear localization and changes in shear fabric in fault gouge. Our measurements show that during steady state frictional shear, dilation after a velocity increase is smaller than compaction after a decrease. Normal stress oscillations cause a marked decrease in D c. Reduction of Dc reduces frictional stability, enhancing the possibility of seismic slip. Our experiments show that shear localization and fabric within the fault gouge can influence the RSF parameters that dictate earthquake nucleation and dynamic rupture. Key Points Ruina law best fits lab data Localization changes the frictional response Localization enhances the possibility of seismic slip",
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Symmetry and the critical slip distance in rate and state friction laws. / Rathbun, Andrew P.; Marone, Chris.

In: Journal of Geophysical Research: Solid Earth, Vol. 118, No. 7, 01.07.2013, p. 3728-3741.

Research output: Contribution to journalArticle

TY - JOUR

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