Frictional constitutive law at intermediate slip rates accounting for flash heating and thermally activated slip process

被引:38
作者
Noda, Hiroyuki [1 ,2 ]
机构
[1] Hiroshima Univ, Dept Earth & Planetary Syst Sci, Grad Sch Sci, Hiroshima 7398526, Japan
[2] Kyoto Univ, Div Earth & Planetary Sci, Grad Sch Sci, Kyoto, Japan
关键词
D O I
10.1029/2007JB005406
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A constitutive law in a rate- and state-dependent framework accounting for flash heating at microscopic contacts is proposed on the basis of a simple asperity model and a thermally activated slip process thought to cause logarithmic dependency of the friction coefficient on slip rate. This law is probably applicable in an intermediate slip rate regime (about 0.001-0.1 m/s), where contact time of asperities is shorter than a cutoff time for time-dependent healing, and a phase transformation such as melting does not take place at the microscopic contacts. The steady state friction coefficient, which is constructed numerically and derived analytically, depends on slip rate and background temperature, gives a good coverage of experimental data of gabbro friction at slip rate on the order of 0.1 m/s, and explains linear dependency of the friction coefficient of Al2O3 ceramics on temperature at around 0.1 m/s. Similar to the usual rate- and state-dependent friction law, the transition behavior on a sudden step in slip rate includes a positive direct effect and a following evolution effect, which are essential in considering the problems dealing with coupling of a frictional surface and surrounding elastic medium. This constitutive law illuminates the importance of the change in not only microscopic, but also macroscopic temperature; the latter, as well as the slip rate, probably changes dynamically during the nucleation of rupture and the coseismic phase.
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页数:12
相关论文
共 71 条
[1]   Influence of particle characteristics on granular friction [J].
Anthony, JL ;
Marone, C .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2005, 110 (B8) :1-14
[2]  
Archard JF., 1958, WEAR, V2, P438, DOI DOI 10.1016/0043-1648(59)90159-0
[3]   Contact dynamics and friction at a solid-solid interface: Material versus statistical aspects [J].
Baumberger, T .
SOLID STATE COMMUNICATIONS, 1997, 102 (2-3) :175-185
[4]   Constitutive relationships and physical basis of fault strength due to flash heating [J].
Beeler, N. M. ;
Tullis, T. E. ;
Goldsby, D. L. .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2008, 113 (B1)
[5]   Quantitative measure of the variation in fault rheology due to fluid-rock interactions [J].
Blanpied, ML ;
Marone, CJ ;
Lockner, DA ;
Byerlee, JD ;
King, DP .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1998, 103 (B5) :9691-9712
[6]   FRICTIONAL SLIP OF GRANITE AT HYDROTHERMAL CONDITIONS [J].
BLANPIED, ML ;
LOCKNER, DA ;
BYERLEE, JD .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1995, 100 (B7) :13045-13064
[7]   MICROMECHANICS OF ROCK FRICTION .2. QUANTITATIVE MODELING OF INITIAL FRICTION WITH CONTACT THEORY [J].
BOITNOTT, GN ;
BIEGEL, RL ;
SCHOLZ, CH ;
YOSHIOKA, N ;
WANG, W .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1992, 97 (B6) :8965-8978
[8]  
Bowden F. P., 1964, The friction and lubrication of Solids, Part II
[9]   THE SURFACE TEMPERATURE OF SLIDING SOLIDS [J].
BOWDEN, FP ;
THOMAS, PH .
PROCEEDINGS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL AND PHYSICAL SCIENCES, 1954, 223 (1152) :29-+
[10]  
BOWDEN FP, 1950, FRICTION LUBRICATI 1