Slowly-attenuating P-SV leaky waves in a layered elastic halfspace. Effects on the coherences of diffuse wavefields

被引:10
作者
Garcia-Jerez, Antonio [1 ,2 ]
Sanchez-Sesma, Francisco J. [3 ]
机构
[1] Univ Granada, Inst Andaluz Geofis, E-18071 Granada, Spain
[2] Univ Granada, Dept Fis Teor & Cosmos, E-18071 Granada, Spain
[3] Univ Nacl Autonoma Mexico, Inst Ingn, CU, Coyoacan 04510, DF, Mexico
关键词
Rayleigh waves; Leaky modes; Green's functions; Diffuse wavefields; SPECTRAL RATIO; H/V RATIO; AMBIENT NOISE; MICROTREMOR; MODES; INVERSION; SEISMOGRAMS; ARRAYS; EARTH; TOOL;
D O I
10.1016/j.wavemoti.2014.11.010
中图分类号
O42 [声学];
学科分类号
070206 ; 082403 ;
摘要
In the context of the classical real-frequency and complex-wavenumber (k) integral representation of elastodynamic Green's function for a plane layered elastic medium, leaky modes are defined as those waves associated with complex-k poles in the P-SV integrands representing continuations of the higher Rayleigh modes below their cutoff frequencies. Nevertheless, for some types of models, the path of the leaky-mode poles through the complex plane (for varying frequency) can intercept the real k axis at particular frequencies, canceling the complex character which was conferring to these wave the exponential decay as the horizontal distance increases. Starting from the Haskell-Harkrider formulation, the characteristics of these slowly-attenuating leaky waves and their excitation by surface forces are investigated. The conditions for existence and their frequency are evaluated for the particular case of an elastic layer over a halfspace. Some numerical simulations point to the detectability of these waves around the fundamental resonance of vertical S waves f(S0) in standard frequency-domain observables defined for random elastic wavefields. These results provide new insights into the behavior of coherences of ambient seismic vibrations when a high velocity contrast exists. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:43 / 57
页数:15
相关论文
共 40 条
[1]  
Aki K., 1957, B EARTHQ RES I TOKYO, V35, P415
[2]   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
[3]  
Asten M.W., 2006, P 3 INT S EFF SURF G
[4]  
Ben-Menahem A., 2000, Seismic Waves And Sources, V2nd edn
[5]   Effects of Love waves on microtremor H/V ratio [J].
Bonnefoy-Claudet, Sylvette ;
Koehler, Andreas ;
Cornou, Cecile ;
Wathelet, Marc ;
Bard, Pierre-Yves .
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, 2008, 98 (01) :288-300
[6]   H/V ratio:: a tool for site effects evaluation.: Results from 1-D noise simulations [J].
Bonnefoy-Claudet, Sylvette ;
Cornou, Cecile ;
Bard, Pierre-Yves ;
Cotton, Fabrice ;
Moczo, Peter ;
Kristek, Jozef ;
Fah, Donat .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2006, 167 (02) :827-837
[7]  
BOUCHON M, 1977, B SEISMOL SOC AM, V67, P259
[8]   Subsoil structure and site effects: A comparison between results from SPAC and HVSR in sites of complex geology [J].
Chavez-Garcia, Francisco J. ;
Manakou, Maria V. ;
Raptakis, Dimitris G. .
SOIL DYNAMICS AND EARTHQUAKE ENGINEERING, 2014, 57 :133-142
[9]   Love wave contribution to the ambient vibration H/V amplitude peak observed with array measurements [J].
Endrun, Brigitte .
JOURNAL OF SEISMOLOGY, 2011, 15 (03) :443-472
[10]  
Ewing W.M., 1957, ELASTIC WAVES LAYERE