Publications des scientifiques de l'IRD

Bonnefoy Claudet S., Kohler A., Cornou Cécile, Wathelet M., Bard P. Y. (2008). Effects of Love waves on microtremor H/V ratio. Bulletin of the Seismological Society of America, 98 (1), p. 288-300. ISSN 0037-1106.

Titre du document
Effects of Love waves on microtremor H/V ratio
Année de publication
2008
Type de document
Article référencé dans le Web of Science WOS:000253494200019
Auteurs
Bonnefoy Claudet S., Kohler A., Cornou Cécile, Wathelet M., Bard P. Y.
Source
Bulletin of the Seismological Society of America, 2008, 98 (1), p. 288-300 ISSN 0037-1106
The horizontal-to-vertical (H/V) method has the potential to significantly contribute to site effects evaluation, in particular in urban areas. Within the European project, site effects assessment using ambient excitations (SESAME), we investigated the nature of ambient seismic noise in order to assess the reliability of this method. Through ID seismic noise modeling, we simulated ambient noise for a set of various horizontally stratified structures by computing efficiently the displacement and stress of dynamic Green's functions for a viscoelastic-layered half-space. We performed array analysis using the conventional semblance-based frequence-wavenumber method and the three-component modified spatial autocorrelation method on both vertical and horizontal components and estimated the contribution of different seismic waves (body/surface waves, Rayleigh/Love waves) at the H/V peak frequency. We show that the very common assumption that almost all the ambient noise energy would be carried by fundamental-mode Rayleigh waves is not justified. The relative proportion of different wave types depends on site conditions, and especially on the impedance contrast. For the ID horizontally layered structures presented here, the H/V peak frequency always provides a good estimate of the fundamental resonance frequency whatever the FIN peak origin (Rayleigh wave ellipticity, Airy phase of Love waves, S-wave resonance). We also infer that the relative proportion of Love waves in ambient noise controls the amplitude of the H/V peak.
Plan de classement
Géologie et formations superficielles [064]
Localisation
Fonds IRD [F B010083625]
Identifiant IRD
fdi:010083625
Contact
  • Coordonnées :
    Mission Science Ouverte (MSO)
    IRD - Délégation régionale Île-de-France & Ouest
    Campus Condorcet - Hôtel à projets
    8 cours des Humanités - 93322 Aubervilliers Cedex
    Horizon Pleins textes
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