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Koufoudi E., Cornou Cécile, Grange S., Dufour F., Imtiaz A. (2018). Quantification of the amplitude variability of the ground motion in Argostoli, Greece. Variability of linear and non-linear structural response of a single degree of freedom system. Bulletin of Earthquake Engineering, 16 (9), 3675-3685. ISSN 1570-761X

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Lien direct chez l'éditeur doi:10.1007/s10518-018-0313-0

Titre
Quantification of the amplitude variability of the ground motion in Argostoli, Greece. Variability of linear and non-linear structural response of a single degree of freedom system
Année de publication2018
Type de documentArticle référencé dans le Web of Science WOS:000439160200005
AuteursKoufoudi E., Cornou Cécile, Grange S., Dufour F., Imtiaz A.
SourceBulletin of Earthquake Engineering, 2018, 16 (9), p. 3675-3685. ISSN 1570-761X
RésuméThe term "spatial variability of seismic ground motions" denotes the differences in the amplitude and phase content of seismic motions. The effect of such spatial variability on the structural response is still an open issue. In-situ experiments may be helpful in order to answer the questions regarding both the quantification of the spatial variability of the ground motion within the dimensions of a structure as well as the effect on its dynamic response. The goal of the present study is to quantify the variability of the seismic ground motion accelerations in the shallow sedimentary basin of Argostoli, Greece, and thereafter to identify its effect on the linear and non-linear elasto-plastic response of a single degree of freedom system in terms of spectral displacements. Around 400 earthquakes are used, recorded by the 21-element very dense seismological array deployed in Argostoli with inter-station spacing ranging from 5 to 160 meters. The seismic motion variability, evaluated in terms of spectral accelerations, is found to be significant and to increase with inter-station distance and frequency. Thereafter, the amplitude variability in terms of spectral displacements, which is indeed the linear response of a single degree of freedom (SDOF) system with various fundamental periods, is compared with the amplitude variability of a SDOF with non-linear elasto-plastic response. The variability of the maximum top displacement of the linear single degree of freedom system is estimated to be on average 12% with larger variabilities to be observed within two narrow frequency ranges (between 1.5 and 1.7 Hz and between 3 and 4 Hz). Such high variabilities are caused by locally edge-generated diffracted surface waves. The non-linear perfectly elasto-platic structural response of the SDOF system shows that although the variability has the same trends as in the case of linear response, it is almost constantly increased by 5%.
Plan de classementGéophysique interne [066] ; Sciences fondamentales / Techniques d'analyse et de recherche [020]
Descr. géo.GRECE ; CEPHALONIE ; ARGOSTOLI
LocalisationFonds IRD [F B010073660]
Identifiant IRDfdi:010073660
Lien permanenthttp://www.documentation.ird.fr/hor/fdi:010073660

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