2010
DOI: 10.1007/978-90-481-9544-2_5
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From Non-invasive Site Characterization to Site Amplification: Recent Advances in the Use of Ambient Vibration Measurements

Abstract: A series of investigations has been carried out over the last decade in Europe aimed at deriving quantitative information on site amplification from non-invasive techniques, based principally on surface wave interpretations of ambient noise measurements. The present paper focuses on their key outcomes regarding three main topics. First, methodological, hardware and software developments focusing on the acquisition and the processing of both single point and array microtremor measurements, led to an efficient t… Show more

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Cited by 42 publications
(32 citation statements)
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“…The Reader is referred to textbooks (e.g. Okada 2003;Foti et al 2014) and to the vast literature on the topic (for an overview, see Bard et al 2010;Socco et al 2010;Foti et al 2011;Schramm et al 2012;Yong et al 2013) for achieving the necessary knowledge on surface wave methods and for the theoretical details.…”
Section: Introductionmentioning
confidence: 99%
“…The Reader is referred to textbooks (e.g. Okada 2003;Foti et al 2014) and to the vast literature on the topic (for an overview, see Bard et al 2010;Socco et al 2010;Foti et al 2011;Schramm et al 2012;Yong et al 2013) for achieving the necessary knowledge on surface wave methods and for the theoretical details.…”
Section: Introductionmentioning
confidence: 99%
“…The simplicity and cost effectiveness come from the fact that each of the considered site parameters are easily available with non-invasive techniques: the shallow average velocities V SZ can be robustly estimated with active shallow seismic (MASW type: V S05 , V S10 , V S20 ), and passive array microtremor measurements (from V S05 to V S30 , see Renalier 2010 and Bard et al 2010), while the fundamental frequency is most generally provided by singlepoint microtremor measurements and H/V noise processing. Moreover the simplicity comes also from the fact that these functions keep a simple formulation with only two parameters (X ref1 and β gathered in the Appendix) for each frequency.…”
Section: Comparison With the Amplification Factors From Gmpesmentioning
confidence: 99%
“…Both fundamental and higher Rayleigh wave modes were used for the inversion. A further constraint for the inversion was introduced the right branch of the mean HVSR curve (Bard et al 2010) for the ellipticity function. The results of the joint inversion of dispersion curves (interpreted as fundamental and second higher mode of Rayleigh waves) and ellipticity curve are shown in Figs.…”
Section: Rietimentioning
confidence: 99%