Γ-convergence for a fault model with slip-weakening friction and periodic barriers

被引:12
作者
Ionescu, IR [1 ]
Onofrei, D
Vernescu, B
机构
[1] Univ Savoie, Math Lab, F-73376 Le Bourget Du Lac, France
[2] Worcester Polytech Inst, Dept Math Sci, Worcester, MA 01609 USA
关键词
Gamma-convergence; slip-weakening friction; Steklov problem;
D O I
10.1090/S0033-569X-05-00981-7
中图分类号
O29 [应用数学];
学科分类号
070104 ;
摘要
We consider a three-dimensional elastic body with a plane fault under a slip-weakening friction. The fault has epsilon-periodically distributed holes, called (small-scale) barriers. This problem arises in the modeling of the earthquake nucleation on a large-scale fault. In each epsilon-square of the epsilon-lattice on the fault plane, the friction contact is considered outside an open set T-epsilon (small-scale barrier) of size r(epsilon) < epsilon, compactly inclosed in the epsilon-square. The solution of each epsilon-problem is found as local minima for an energy with both bulk and surface terms. The first eigenvalue of a symmetric and compact operator K-epsilon provides information about the stability of the solution. Using Gamma-convergence techniques, we study the asymptotic behavior as E tends to 0 for the friction contact problem. Depending on the values of c =: lim(epsilon -> 0) r(epsilon) /epsilon(2) we obtain different limit problems. The asymptotic analysis for the associated spectral problem is performed using G-convergence for the sequence of operators K-epsilon. The limits of the eigenvalue sequences and the associated eigenvectors are eigenvalues and respectively eigenvectors of a limit operator. From the physical point of view our result can be interpreted as follows: i) if the barriers are too large (i.e. c = infinity), then the fault is locked (no slip), ii) if c > 0, then the fault behaves as a fault under a slip-dependent friction. The slip weakening rate of the equivalent fault is smaller than the undisturbed fault. Since the limit slip-weakening rate may be negative, a slip-hardening effect can also be expected. iii) if the barriers are too small (i.e. c = 0), then the presence of the barriers does not affect the friction law on the limit fault.
引用
收藏
页码:747 / 778
页数:32
相关论文
共 35 条
[1]   Nucleation of rupture under slip dependent friction law:: Simple models of fault zone -: art. no. 2324 [J].
Ampuero, JP ;
Vilotte, JP ;
Sánchez-Sesma, FJ .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2002, 107 (B12)
[2]  
Ansini N, 2004, ASYMPTOTIC ANAL, V39, P113
[3]   Asymptotic analysis of periodically-perforated nonlinear media [J].
Ansini, N ;
Braides, A .
JOURNAL DE MATHEMATIQUES PURES ET APPLIQUEES, 2002, 81 (05) :439-451
[4]  
AOCHI H, 2001, J GEOPHYS RES, V107, DOI DOI 10.1028/2000JB000032
[5]  
Attouch H., 1984, Applicable Mathematics Series
[6]  
Braides A., 1996, ARCH RATION MECH AN, V135, P297
[7]   HOMOGENIZATION OF BOUNDARIES BY EPICONVERGENCE IN LINEAR ELASTICITY [J].
BRILLARD, A ;
LOBO, M ;
PEREZ, E .
ESAIM-MATHEMATICAL MODELLING AND NUMERICAL ANALYSIS-MODELISATION MATHEMATIQUE ET ANALYSE NUMERIQUE, 1990, 24 (01) :5-26
[8]   Initiation of antiplane shear instability under slip dependent friction [J].
Campillo, M ;
Ionescu, IR .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1997, 102 (B9) :20363-20371
[9]   Instability of a periodic system of faults [J].
Campillo, M ;
Dascalu, C ;
Ionescu, IR .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2004, 159 (01) :212-222
[10]   On the effective friction law of a heterogeneous fault [J].
Campillo, M ;
Favreau, P ;
Ionescu, IR ;
Voisin, C .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2001, 106 (B8) :16307-16322