A computer code for forward calculation and inversion of the H/V spectral ratio under the diffuse field assumption

被引:156
作者
Garcia-Jerez, Antonio [1 ,2 ]
Pina-Flores, Jose [3 ]
Sanchez-Sesma, Francisco J. [3 ]
Luzon, Francisco [1 ]
Perton, Mathieu [3 ]
机构
[1] Univ Almeria, Dept Quim & Fis, Almeria 04120, Spain
[2] Univ Granada, Inst Andaluz Geofis, C Prof Clavera 12, E-18071 Granada, Spain
[3] Univ Nacl Autonoma Mexico, CU, Inst Ingn, Coyoacan 04510, DF, Mexico
关键词
H/V computation; Diffuse wavefields; Full wavefield inversion; Elastodynamic Green's functions; SEISMIC NOISE; JOINT INVERSION; LAYERED EARTH; AMBIENT NOISE; HIGHER MODES; WAVE-FIELD; DISPERSION; OPTIMIZATION; ALGORITHM; SEARCH;
D O I
10.1016/j.cageo.2016.06.016
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
During a quarter of a century, the main characteristics of the horizontal-to-vertical spectral ratio of ambient noise HVSRN have been extensively used for site effect assessment. In spite of the uncertainties about the optimum theoretical model to describe these observations, over the last decade several schemes for inversion of the full HVSRN curve for near surface surveying have been developed. In this work, a computer code for forward calculation of H/V spectra based on the diffuse field assumption (DFA) is presented and tested. It takes advantage of the recently stated connection between the HVSRN and the elastodynamic Green's function which arises from the ambient noise interferometry theory. The algorithm allows for (1) a natural calculation of the Green's functions imaginary parts by using suitable contour integrals in the complex wavenumber plane, and (2) separate calculation of the contributions of Rayleigh, Love, P-SV and SH waves as well. The stability of the algorithm at high frequencies is preserved by means of an adaptation of the Wang's orthonormalization method to the calculation of dispersion curves, surface-waves medium responses and contributions of body waves. This code has been combined with a variety of inversion methods to make up a powerful tool for passive seismic surveying. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:67 / 78
页数:12
相关论文
共 54 条
[1]  
Aki K., 2002, QUANTITAVE SEISMOLOG, V2nd, P700
[2]  
Aki K., 1957, B EARTHQ RES I TOKYO, V35, P415
[3]   S-wave velocity profiling by joint inversion of microtremor dispersion curve and horizontal-to-vertical (H/V) spectrum [J].
Arai, H ;
Tokimatsu, K .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2005, 95 (05) :1766-1778
[4]   S-wave velocity profiling by inversion of microtremor H/V spectrum [J].
Arai, H ;
Tokimatsu, K .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2004, 94 (01) :53-63
[5]  
Ben-Menahem A., 2000, SEISMIC WAVES SOURCE, P1136
[6]   Free-mode surface-wave computations [J].
Buchen, PW ;
BenHador, R .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1996, 124 (03) :869-887
[7]   Solving the Surface-Wave Eigenproblem with Chebyshev Spectral Collocation [J].
Denolle, Marine A. ;
Dunham, Eric M. ;
Beroza, Gregory C. .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2012, 102 (03) :1214-1223
[8]  
Dunkin JW, 1965, Bull. Seismol. Soc. Am, V55, P335, DOI [10.1785/BSSA0550020335, DOI 10.1785/BSSA0550020335]
[9]   Inversion of local S-wave velocity structures from average H/V ratios, and their use for the estimation of site-effects [J].
Fäh, D ;
Kind, F ;
Giardini, D .
JOURNAL OF SEISMOLOGY, 2003, 7 (04) :449-467
[10]   Slowly-attenuating P-SV leaky waves in a layered elastic halfspace. Effects on the coherences of diffuse wavefields [J].
Garcia-Jerez, Antonio ;
Sanchez-Sesma, Francisco J. .
WAVE MOTION, 2015, 54 :43-57