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

The 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 P and SV in-plane wave assumptions, using two well known direct boundary-element-based numerical methods. After establishing the differen...

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Autores:
Gomez, Juan
Jaramillo, Juan Diego
Restrepo, Dorian
Valencia, Camilo
Tipo de recurso:
Fecha de publicación:
2013
Institución:
Universidad EAFIT
Repositorio:
Repositorio EAFIT
Idioma:
eng
OAI Identifier:
oai:repository.eafit.edu.co:10784/4219
Acceso en línea:
http://hdl.handle.net/10784/4219
Palabra clave:
Seismic site effects
Topographic effects
Elastic wave scattering
Diffraction of in-plane waves
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Author's post-print on any open access repository after 12 months after publication
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spelling 2014-09-23T14:56:23Z2013-102014-09-23T14:56:23ZJ. Gomez, Restrepo, D., Jaramillo, J., and Valencia, C., Analysis of the role of diffraction in topographic site effects using boundary element techniques, Earthq Sci, vol. 26, no. 5, pp. 341-350, 20141674-4519 (Print)1867-8777 (Online)http://hdl.handle.net/10784/421910.1007/s11589-013-0044-xThe 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 P and SV in-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.engSpringer. Seismological Society of ChinaUniversidad EAFIT. Departamento de Ingeniería MecánicaEarthquake Science. Volume 26, Issue 5 , pp 341-350http://dx.doi.org/10.1007/s11589-013-0044-xhttp://dx.doi.org/10.1007/s11589-013-0044-xAuthor's post-print on any open access repository after 12 months after publicationAcceso abiertohttp://purl.org/coar/access_right/c_abf2Analysis of the role of diffraction in topographic site effects using boundary element techniquesinfo:eu-repo/semantics/articlearticleinfo:eu-repo/semantics/publishedVersionpublishedVersionArtículohttp://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1Seismic site effectsTopographic effectsElastic wave scatteringDiffraction of in-plane wavesJuan Gomez (jgomezc1@eafit.edu.co)Gomez, JuanJaramillo, Juan DiegoRestrepo, DorianValencia, CamiloMecánica AplicadaEarthquake Science265341350ORIGINALart11589-013-0044-x.pdfart11589-013-0044-x.pdfVersion editor (closed)application/pdf2447736https://repository.eafit.edu.co/bitstreams/462b19ee-1ef9-4126-a023-484eb52f79c8/downloadf4fabf05b5f759b46e97141b232536adMD51LICENSElicense.txtlicense.txttext/plain; charset=utf-82556https://repository.eafit.edu.co/bitstreams/db156443-620e-47c9-8908-f990d6085fc4/download76025f86b095439b7ac65b367055d40cMD5210784/4219oai:repository.eafit.edu.co:10784/42192021-09-08 11:42:47.267restrictedhttps://repository.eafit.edu.coRepositorio Institucional Universidad EAFITrepositorio@eafit.edu.co
dc.title.eng.fl_str_mv Analysis of the role of diffraction in topographic site effects using boundary element techniques
title Analysis of the role of diffraction in topographic site effects using boundary element techniques
spellingShingle Analysis of the role of diffraction in topographic site effects using boundary element techniques
Seismic site effects
Topographic effects
Elastic wave scattering
Diffraction of in-plane waves
title_short Analysis of the role of diffraction in topographic site effects using boundary element techniques
title_full Analysis of the role of diffraction in topographic site effects using boundary element techniques
title_fullStr Analysis of the role of diffraction in topographic site effects using boundary element techniques
title_full_unstemmed Analysis of the role of diffraction in topographic site effects using boundary element techniques
title_sort Analysis of the role of diffraction in topographic site effects using boundary element techniques
dc.creator.fl_str_mv Gomez, Juan
Jaramillo, Juan Diego
Restrepo, Dorian
Valencia, Camilo
dc.contributor.eafitauthor.spa.fl_str_mv Juan Gomez (jgomezc1@eafit.edu.co)
dc.contributor.author.none.fl_str_mv Gomez, Juan
Jaramillo, Juan Diego
Restrepo, Dorian
Valencia, Camilo
dc.contributor.researchgroup.spa.fl_str_mv Mecánica Aplicada
dc.subject.keyword.eng.fl_str_mv Seismic site effects
Topographic effects
Elastic wave scattering
Diffraction of in-plane waves
topic Seismic site effects
Topographic effects
Elastic wave scattering
Diffraction of in-plane waves
description The 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 P and SV in-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.
publishDate 2013
dc.date.issued.none.fl_str_mv 2013-10
dc.date.available.none.fl_str_mv 2014-09-23T14:56:23Z
dc.date.accessioned.none.fl_str_mv 2014-09-23T14:56:23Z
dc.type.eng.fl_str_mv info:eu-repo/semantics/article
article
info:eu-repo/semantics/publishedVersion
publishedVersion
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http://purl.org/coar/resource_type/c_2df8fbb1
dc.type.local.spa.fl_str_mv Artículo
status_str publishedVersion
dc.identifier.citation.spa.fl_str_mv J. Gomez, Restrepo, D., Jaramillo, J., and Valencia, C., Analysis of the role of diffraction in topographic site effects using boundary element techniques, Earthq Sci, vol. 26, no. 5, pp. 341-350, 2014
dc.identifier.issn.none.fl_str_mv 1674-4519 (Print)
1867-8777 (Online)
dc.identifier.uri.none.fl_str_mv http://hdl.handle.net/10784/4219
dc.identifier.doi.none.fl_str_mv 10.1007/s11589-013-0044-x
identifier_str_mv J. Gomez, Restrepo, D., Jaramillo, J., and Valencia, C., Analysis of the role of diffraction in topographic site effects using boundary element techniques, Earthq Sci, vol. 26, no. 5, pp. 341-350, 2014
1674-4519 (Print)
1867-8777 (Online)
10.1007/s11589-013-0044-x
url http://hdl.handle.net/10784/4219
dc.language.iso.eng.fl_str_mv eng
language eng
dc.relation.ispartof.spa.fl_str_mv Earthquake Science. Volume 26, Issue 5 , pp 341-350
dc.relation.uri.none.fl_str_mv http://dx.doi.org/10.1007/s11589-013-0044-x
http://dx.doi.org/10.1007/s11589-013-0044-x
dc.rights.spa.fl_str_mv Author's post-print on any open access repository after 12 months after publication
dc.rights.coar.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.rights.local.spa.fl_str_mv Acceso abierto
rights_invalid_str_mv Author's post-print on any open access repository after 12 months after publication
Acceso abierto
http://purl.org/coar/access_right/c_abf2
dc.publisher.spa.fl_str_mv Springer. Seismological Society of China
dc.publisher.department.spa.fl_str_mv Universidad EAFIT. Departamento de Ingeniería Mecánica
institution Universidad EAFIT
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