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  5. Site effects study in the Serravalle village (NE Italy) by means of spectral ratios analyses relatively to multiple reference sites
 
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Site effects study in the Serravalle village (NE Italy) by means of spectral ratios analyses relatively to multiple reference sites

Author(s)
Restivo, A.  
OGS, Trieste  
Michelini, A.  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Barnaba, C.  
OGS, Trieste  
Language
English
Obiettivo Specifico
4.1. Metodologie sismologiche per l'ingegneria sismica
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Natural Hazards  
Issue/vol(year)
1/39 (2006)
Publisher
Springer
Pages (printed)
31-49
Date Issued
September 2006
DOI
10.1007/s11069-005-2960-0
URI
https://www.earth-prints.org/handle/2122/3163
Subjects
04. Solid Earth::04.06. Seismology::04.06.04. Ground motion  
Subjects

spectral ratios

reference sites

site effects

earthquake grounf mot...

Abstract
The area of Serravalle, sited in the northern part of the town of Vittorio Veneto (TV), NE Italy, has been the target of a seismic microzonation campaign. 10 seismic stations have been deployed for a 7 months period to record in continuous mode. Three stations were installed on bedrock outcrops and seven on sedimentary sites with variable cover thickness. Spectral analyses have been performed on the collected data-set using the Generalized Inversion Technique (GIT, e.g. Andrews, 1986). In particular, spectral ratios have been calculated for each station relatively to the average of the three reference, bedrock sites. The spectral ratios provide quantitative estimates of the seismic motion amplifications which occur in each of the monitored sites. Two sites show high values of amplification, 5 times larger than signal amplitude at the reference sites, in correspondence of well discernible peak frequencies of 5 Hz. Results for the other stations show smaller amounts of site amplification spreading over a broad range of frequencies. Sites where the highest amplifications were recorded all lie on the left bank of the Meschio River and in areas farther away from its outlet into the plain correlating with the presence of thick layers of Quaternary deposits.
Type
article
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Barnaba_etal2007.pdf

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Format

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Checksum (MD5)

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