Slip-stick and the evolution of frictional strength

被引:230
作者
Ben-David, Oded [1 ]
Rubinstein, Shmuel M. [1 ]
Fineberg, Jay [1 ]
机构
[1] Hebrew Univ Jerusalem, Racah Inst Phys, IL-91904 Jerusalem, Israel
基金
以色列科学基金会;
关键词
RATE-DEPENDENT FRICTION; PHYSICAL ANALYSIS; DYNAMIC FRICTION; STATIC FRICTION; FAULTS; EARTHQUAKES; NUCLEATION; TRANSITION; RUPTURE; LAWS;
D O I
10.1038/nature08676
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The evolution of frictional strength has great fundamental and practical importance. Applications range from earthquake dynamics(1-4) to hard-drive read/write cycles(5). Frictional strength is governed by the resistance to shear of the large ensemble of discrete contacts that forms the interface that separates two sliding bodies. An interface's overall strength is determined by both the real contact area and the contacts' shear strength(6,7). Whereas the average motion of large, slowly sliding bodies is well-described by empirical friction laws(3,8-10), interface strength is a dynamic entity that is inherently related to both fast processes such as detachment/re-attachment(11-14) and the slow process of contact area rejuvenation(6,7,13,15,16). Here we show how frictional strength evolves from extremely short to long timescales, by continuous measurements of the concurrent local evolution of the real contact area and the corresponding interface motion (slip) from the first microseconds when contact detachment occurs to large (100-second) timescales. We identify four distinct and inter-related phases of evolution. First, all of the local contact area reduction occurs within a few microseconds, on the passage of a crack-like front. This is followed by the onset of rapid slip over a characteristic time, the value of which suggests a fracture-induced reduction of contact strength before any slip occurs. This rapid slip phase culminates with a sharp transition to slip at velocities an order of magnitude slower. At slip arrest, 'ageing' immediately commences as contact area increases on a characteristic timescale determined by the system's local memory of its effective contact time before slip arrest. We show how the singular logarithmic behaviour generally associated with ageing is cut off at short times(16). These results provide a comprehensive picture of how frictional strength evolves from the short times and rapid slip velocities at the onset of motion to ageing at the long times following slip arrest.
引用
收藏
页码:76 / 79
页数:4
相关论文
共 27 条
[1]   Physical analysis of the state- and rate-dependent friction law. II. Dynamic friction [J].
Baumberger, T ;
Berthoud, P ;
Caroli, C .
PHYSICAL REVIEW B, 1999, 60 (06) :3928-3939
[2]   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)
[3]   Dynamic ruptures in recent models of earthquake faults [J].
Ben-Zion, Y .
JOURNAL OF THE MECHANICS AND PHYSICS OF SOLIDS, 2001, 49 (09) :2209-2244
[4]   COLLECTIVE BEHAVIOR OF EARTHQUAKES AND FAULTS: CONTINUUM-DISCRETE TRANSITIONS, PROGRESSIVE EVOLUTIONARY CHANGES, AND DIFFERENT DYNAMIC REGIMES [J].
Ben-Zion, Yehuda .
REVIEWS OF GEOPHYSICS, 2008, 46 (04)
[5]   Physical analysis of the state- and rate-dependent friction law: Static friction [J].
Berthoud, P ;
Baumberger, T ;
G'Sell, C ;
Hiver, JM .
PHYSICAL REVIEW B, 1999, 59 (22) :14313-14327
[6]  
Bowden F., 2001, FRICTION LUBRICATION
[7]   MODELING OF ROCK FRICTION .1. EXPERIMENTAL RESULTS AND CONSTITUTIVE EQUATIONS [J].
DIETERICH, JH .
JOURNAL OF GEOPHYSICAL RESEARCH, 1979, 84 (NB5) :2161-2168
[8]   EARTHQUAKE NUCLEATION ON FAULTS WITH RATE-DEPENDENT AND STATE-DEPENDENT STRENGTH [J].
DIETERICH, JH .
TECTONOPHYSICS, 1992, 211 (1-4) :115-134
[9]   DIRECT OBSERVATION OF FRICTIONAL CONTACTS - NEW INSIGHTS FOR STATE-DEPENDENT PROPERTIES [J].
DIETERICH, JH ;
KILGORE, BD .
PURE AND APPLIED GEOPHYSICS, 1994, 143 (1-3) :283-302
[10]   TIME-DEPENDENT FRICTION IN ROCKS [J].
DIETERICH, JH .
JOURNAL OF GEOPHYSICAL RESEARCH, 1972, 77 (20) :3690-+