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|Authors: ||Cultrera, G.*|
De Rubeis, V.*
|Title: ||Statistical investigation of site ef f ects with emphasis on sedimentary basins, using earthquake and ambient noise recordings|
|Issue Date: ||Sep-2010|
|Keywords: ||site effect|
|Abstract: ||During the last two decades, three empirical methods for assessing site effects have been
widely used: the Standard Spectral Ratio (SSR), the Horizontal-to-Vertical Spectral Ratio from earthquake recordings (HVSR) and the Horizontal-to-Vertical Spectral Ratio from ambient noise recordings (HVN). The SSR is considered the reference empirical method
to detect amplification as a function of frequency, while the HVSR and the HVN
realistically indicate fundamental frequency but, for the majority of the worldwide
examined sites, they cannot give reliable amplification curves as a function of
frequency. Given the fact that HVSR and especially HVN can be easily obtained, it is
challenging to search for any correlation with SSR amplification functions.
We used recordings from 168 sites worldwide, for which all three types of spectral ratios
were homogeneously processed (Haghsenas et al., Bull. Earthquake Eng. 2008). On this
data set we applied standard multivariate statistical analyses, namely, factor analysis and canonical correlation, to investigate and quantify -where it is possible- any correlation between spectral ratios for a certain number of the examined frequency bins. Results show that the correlation between HVN and HVSR is very good. Moreover, their correlation with broad band SSR can be statistically quantified and receive a satisfactory physical explanation.
In addition, we looked for the correlation of SSR, HVSR and HVN collected in sedimentary basins (a subset of the previous database) with geometrical and geophysical
parameters. T hese attempts were constrained by the limited amount of reliable in-situ
data. Among many, we select 5 parameters: Vs30, Hb, Vs_average/Hb, Hb/W_valley,
Hb/W_edge (where Hb is the bedrock’s depth below the station; Vs_average is the
average Vs from surface to bedrock; W_valley is 2D-width of the valley; W_edge is the
distance from the closest valley’s edge). T he analysis assesses that larger are the first 4 parameters, larger is the low-frequency amplification in HVSR and HVN, and lower the high-frequency contribution.
Although additional data would improve our statistical investigation and better establish quantitative correlation between spectral ratios and geophysical or/and geometrical characteristics of sedimentary basins, our results clearly show that statistical correlation between SSR and HVN-HVSR is present and modulated in specific frequency domains.
T his study has been performed in the framework of the T oK IT SAK-GR EC project
|Appears in Collections:||Conference materials|
04.06.04. Ground motion
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