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Prediction of soil effects on seismic motions: A comparative case study

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dc.contributor.author Bouckovalas, GD en
dc.date.accessioned 2014-03-01T01:13:16Z
dc.date.available 2014-03-01T01:13:16Z
dc.date.issued 1997 en
dc.identifier.issn 87552930 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/12404
dc.subject Case Study en
dc.subject.other Dynamic response en
dc.subject.other Soil mechanics en
dc.subject.other Soil structure interactions en
dc.subject.other Spectrum analysis en
dc.subject.other Average shear wave velocity en
dc.subject.other Earthquake resistance en
dc.title Prediction of soil effects on seismic motions: A comparative case study en
heal.type journalArticle en
heal.identifier.primary 10.1193/1.1585952 en
heal.identifier.secondary http://dx.doi.org/10.1193/1.1585952 en
heal.publicationDate 1997 en
heal.abstract Empirical predictions of soil effects on seismic ground shaking are related to 1-D seismic response analyses. The comparison focuses upon the peak ground acceleration (amax) and velocity (Vmax), the elastic acceleration response spectra (Sa) and the average horizontal Fourier amplitudes over a short and an intermediate period band (AHFA, AHFA*). Empirical predictions in terms of site geology are within the overall range of analytical predictions for amax and Vmax, but they do not depict the detailed effects of seismic motion and site characteristics. In addition, they agree to analytical predictions of Sa for relatively deep and flexible sites, but differ significantly for other sites. Empirical predictions in terms of the average shear wave velocity, agree well with analytical predictions for amax, Vmax, AHFA and AHFA* in the case of shallow and stiff sites subjected to weak seismic excitations, but they are relatively higher in the opposite case. Empirical predictions of Sa are generally within the range of analytical predictions, although empirically predicted peak amplification can not be related to resonance between the soil and the superstructure. en
heal.journalName Earthquake Spectra en
dc.identifier.doi 10.1193/1.1585952 en
dc.identifier.volume 13 en
dc.identifier.issue 3 en
dc.identifier.spage 333 en
dc.identifier.epage 361 en


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