Analysis of the role of diffraction in topographic site effects using boundary element techniques

dc.citation.journalTitleEarthquake Science
dc.contributor.authorGomez, J.
dc.contributor.authorRestrepo, D.
dc.contributor.authorJaramillo, J.
dc.contributor.authorValencia, C.
dc.contributor.researchgroupMecánica Aplicadaspa
dc.date.accessioned2021-04-16T20:10:37Z
dc.date.available2021-04-16T20:10:37Z
dc.date.issued2013-01-01
dc.description.abstractThe role played by the diffraction field on the problem of seismic site effects is studied. For that purpose we solve and analyze simple scattering problems under PandSVin-plane wave assumptions, using two well known direct boundary-element-based numerical methods. After establishing the difference between scattered and diffracted motions, and introducing the concept of artificious and physically based incoming fields, we obtain the amplitude of the Fourier spectra for the diffracted part of the response: this is achieved after establishing the connection between the spatial distribution of the transfer function over the studied simple topographies and the diffracted field. From the numerical simulations it is observed that this diffracted part of the response is responsible for the amplification of the surface ground motions due to the geometric effect. Furthermore, it is also found that the diffraction field sets in a fingerprint of the topographic effect in the total ground motions. These conclusions are further supported by observations in the time-domain in terms of snapshots of the propagation patterns over the complete computational model. In this sense the geometric singularities are clearly identified as sources of diffraction and for the considered range of dimensionless frequencies it is evident that larger amplifications are obtained for the geometries containing a larger number of diffraction sources thus resulting in a stronger topographic effect. The need for closed-form solutions of canonical problems to construct a robust analysis method based on the diffraction field is identified. © The Seismological Society of China, Institute of Geophysics, China Earthquake Administration and Springer-Verlag Berlin Heidelberg 2013.eng
dc.identifierhttps://eafit.fundanetsuite.com/Publicaciones/ProdCientif/PublicacionFrw.aspx?id=1717
dc.identifier.doi10.1007/s11589-013-0044-x
dc.identifier.issn18678777
dc.identifier.issn127353spa
dc.identifier.otherSCOPUS;2-s2.0-84891795212
dc.identifier.urihttp://hdl.handle.net/10784/29172
dc.language.isoengeng
dc.publisherSeismological Society of China
dc.publisher.departmentUniversidad EAFIT. Departamento de Ingeniería Mecánicaspa
dc.relation.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-84891795212&doi=10.1007%2fs11589-013-0044-x&partnerID=40&md5=d6fe66048bfd07f99e3f3fd45beefed7
dc.rightshttps://v2.sherpa.ac.uk/id/publication/issn/1674-4519
dc.sourceEarthquake Science
dc.subject.keywordDiffraction of in-plane waveseng
dc.subject.keywordElastic wave scatteringeng
dc.subject.keywordSeismic site effectseng
dc.subject.keywordTopographic effectseng
dc.titleAnalysis of the role of diffraction in topographic site effects using boundary element techniqueseng
dc.typeinfo:eu-repo/semantics/articleeng
dc.typearticleeng
dc.typeinfo:eu-repo/semantics/publishedVersioneng
dc.typepublishedVersioneng
dc.type.localArtículospa

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