On the importance of normal vibrations in modeling of stick slip in rock sliding

被引:10
作者
Tworzydlo, WW
Hamzeh, ON
机构
关键词
D O I
10.1029/97JB01167
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
In this paper, numerical studies of friction-induced dynamic instabilities,in particular, stick-slip sliding of rocks, are presented. Of special interest is the importance of normal compliance of the interface and associated normal vibrations in the occurrence of dynamic instabilities. To clearly illustrate this importance, the interface is represented by the Oden-Martins constitutive model which does not exhibit explicit velocity or slip dependence of friction. This friction model is utilized in the context of a rather simple rigid body model to perform numerical studies representative of granite blocks in relative sliding at very slow overall velocities. The model represents a common experimental setting that has been used to study stick slip of sliding rock blocks. To capture the stick-slip phenomenon the detailed dynamic response of this system is modeled numerically. These studies indicate the importance of the normal compliance of the interface on the stability of sliding. In particular, dynamic coupling of the degrees of freedom contributes to dynamic instability of the system and can cause stick-slip motion. Both stable and unstable sliding are predicted and examined.
引用
收藏
页码:15091 / 15103
页数:13
相关论文
共 46 条
[1]   RUPTURE PROPAGATION WITH FINITE STRESS IN ANTIPLANE STRAIN [J].
ANDREWS, DJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1976, 81 (20) :3575-3582
[2]   RUPTURE VELOCITY OF PLANE STRAIN SHEAR CRACKS [J].
ANDREWS, DJ .
JOURNAL OF GEOPHYSICAL RESEARCH, 1976, 81 (32) :5679-5687
[3]  
ARONOV V, 1984, J TRIBOL-T ASME, V106, P54, DOI 10.1115/1.3260867
[4]   EXPERIMENTAL INVESTIGATION OF THE EFFECT OF SYSTEM RIGIDITY ON WEAR AND FRICTION-INDUCED VIBRATIONS [J].
ARONOV, V ;
DSOUZA, AF ;
KALPAKJIAN, S ;
SHAREEF, I .
JOURNAL OF LUBRICATION TECHNOLOGY-TRANSACTIONS OF THE ASME, 1983, 105 (02) :206-211
[5]   THE FRICTIONAL-PROPERTIES OF A SIMULATED GOUGE HAVING A FRACTAL PARTICLE DISTRIBUTION [J].
BIEGEL, RL ;
SAMMIS, CG ;
DIETERICH, JH .
JOURNAL OF STRUCTURAL GEOLOGY, 1989, 11 (07) :827-&
[6]   FAULT STABILITY INFERRED FROM GRANITE SLIDING EXPERIMENTS AT HYDROTHERMAL CONDITIONS [J].
BLANPIED, ML ;
LOCKNER, DA ;
BYERLEE, JD .
GEOPHYSICAL RESEARCH LETTERS, 1991, 18 (04) :609-612
[7]   RUPTURE MECHANISM AND INTERFACE SEPARATION IN FOAM RUBBER MODELS OF EARTHQUAKES - A POSSIBLE SOLUTION TO THE HEAT-FLOW PARADOX AND THE PARADOX OF LARGE OVERTHRUSTS [J].
BRUNE, JN ;
BROWN, S ;
JOHNSON, PA .
TECTONOPHYSICS, 1993, 218 (1-3) :59-67
[8]   FRICTIONAL CHARACTERISTICS OF GRANITE UNDER HIGH CONFINING PRESSURE [J].
BYERLEE, JD .
JOURNAL OF GEOPHYSICAL RESEARCH, 1967, 72 (14) :3639-&
[9]   STABLE SLIDING PRECEDING STICK-SLIP ON FAULT SURFACES IN GRANITE AT HIGH-PRESSURE [J].
BYERLEE, JD ;
SUMMERS, R .
PURE AND APPLIED GEOPHYSICS, 1975, 113 (1-2) :63-68
[10]   SEISMICITY SIMULATION WITH A RATE-DEPENDENT AND STATE-DEPENDENT FRICTION LAW [J].
CAO, TQ ;
AKI, K .
PURE AND APPLIED GEOPHYSICS, 1986, 124 (03) :487-513