Numerical Simulation of Ground Rotations along 2D Topographical Profiles under the Incidence of Elastic Plane Waves

被引:37
作者
Godinho, L. [1 ]
Mendes, P. Amado [1 ]
Tadeu, A. [1 ]
Cadena-Isaza, A. [2 ]
Smerzini, C. [3 ]
Sanchez-Sesma, F. J. [2 ]
Madec, R. [4 ,5 ]
Komatitsch, D. [4 ,5 ]
机构
[1] Univ Coimbra, Dept Civil Engn, Ctr Invest Ciencias Construcao, P-3030788 Coimbra, Portugal
[2] Univ Nacl Autonoma Mexico, Inst Ingn, Mexico City 04510, DF, Mexico
[3] EUCENTRE, ROSE Sch, I-27100 Pavia, Italy
[4] Univ Pau & Pays Adour, CNRS, UMR 5212, Lab Modelisat & Imagerie Geosci Pau, F-64013 Pau, France
[5] INRIA MAGIQUE 3D, F-64013 Pau, France
关键词
3-DIMENSIONAL SCATTERING; MOTION; COMPONENTS; EARTHQUAKE; TILT; CALIFORNIA; VALLEY; SH; SV;
D O I
10.1785/0120080096
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
The surface displacement field along a topographical profile of an elastic half-space subjected to the incidence of elastic waves can be computed using different numerical methods. The method of fundamental solutions (MFS) is one of such techniques in which the diffracted field is constructed by means of a representation in terms of the Green's functions for discrete forces located outside the domain of interest. From the enforcement of boundary conditions, such forces can be computed; thus, the ground motion can be calculated. One important advantage of MFS over boundary integral techniques is that singularities are avoided. The computation of ground-motion rotations implies the application of the rotational operator to the displacement field. This can be done using either numerical derivatives or analytical expressions to compute the rotational Green's tensor. We validate the method using exact analytical solutions in terms of both displacement and rotation, which are known for simple geometries. To demonstrate the accuracy for generic geometries, we compare results against those obtained using the spectral-element method. We compute surface rotations for incoming plane waves (P, SV, and Rayleigh) near a topographical profile. We point out the effects of topography on rotational ground motion in both frequency and time domains.
引用
收藏
页码:1147 / 1161
页数:15
相关论文
共 45 条
[1]  
Aki K., 2002, Quantitative Seismology
[2]  
[Anonymous], 2013, SPECTRAL ELEMENT MET, DOI [DOI 10.1029/157GM13, 10.1029/157GM13]
[3]  
Atluri S.N., 2004, The Meshless Method (MLPG) for Domain and BIE Discretization
[4]   ON THE EFFECTIVE SEISMIC INPUT FOR NON-LINEAR SOIL STRUCTURE INTERACTION SYSTEMS [J].
BIELAK, J ;
CHRISTIANO, P .
EARTHQUAKE ENGINEERING & STRUCTURAL DYNAMICS, 1984, 12 (01) :107-119
[5]  
BOUCHON M, 1982, B SEISMOL SOC AM, V72, P1717
[6]   ROTATIONAL COMPONENTS OF THE SURFACE GROUND MOTION DURING AN EARTHQUAKE [J].
CASTELLANI, A ;
BOFFI, G .
EARTHQUAKE ENGINEERING & STRUCTURAL DYNAMICS, 1986, 14 (05) :751-767
[7]  
Cochard A., 2006, Earthquake Source Asymmetry, Structural Media and Rotation Effects
[8]   The method of fundamental solutions for elliptic boundary value problems [J].
Fairweather, G ;
Karageorghis, A .
ADVANCES IN COMPUTATIONAL MATHEMATICS, 1998, 9 (1-2) :69-95
[9]   On the characteristics of ground motion rotational components using Chiba dense array data [J].
Ghayamghamian, M. R. ;
Nouri, G. R. .
EARTHQUAKE ENGINEERING & STRUCTURAL DYNAMICS, 2007, 36 (10) :1407-1429
[10]  
Godinho L, 2007, CMC-COMPUT MATER CON, V5, P117