J. Dunning et al., THE ROLE OF THE CHEMICAL ENVIRONMENT IN FRICTIONAL DEFORMATION - STRESS-CORROSION CRACKING AND COMMINUTION, Pure and Applied Geophysics, 143(1-3), 1994, pp. 151-178
The roles of chemically assisted crack and fracture propagation and ch
emically assisted comminution in frictional deformation are evaluated
in this study. Double cantilever beam (DCB) crack propagation data are
presented which show that the role of pH in chemically assisted fract
ure, and to a lesser extent the role of ionic concentration are import
ant in stress corrosion cracking. Data on very slow crack growth and t
he stress corrosion limit are also presented. These data suggest that
stress corrosion cracking may play an important role in compound earth
quakes and in asperity breakdown in faults. The comminution literature
is also reviewed in order to assess the role of chemically assisted c
omminution in frictional deformation. It appears that chemically assis
ted comminution may be important at low and high ionic strength becaus
e it may reduce the effective viscosity and the shear strength of faul
t gouge. At intermediate ionic concentration the role of pH, as an age
nt which enhances crack and fracture propagation, appears to be more i
mportant in reducing the coefficient of sliding friction.