Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations

Autores
Rubino, Jorge German; Monachesi, Leonardo Bruno; Müller, Tobias M.; Guarracino, Luis; Holliger, Klaus
Año de publicación
2013
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Oscillatory fluid movements in heterogeneous porous rocks induced by seismic waves cause dissipation of wave field energy. The resulting seismic signature depends not only on the rock compressibility distribution, but also on a statistically averaged permeability. This so-called equivalent seismic permeability does, however, not coincide with the respective equivalent flow permeability. While this issue has been analyzed for 1D media, the corresponding 2D and 3D cases remain unexplored. In this work, this topic is analyzed for 2D random medium realizations having strong permeability fluctuations. With this objective, oscillatory compressibility simulations based on the quasi-static poroelasticity equations are performed. Numerical analysis shows that strong permeability fluctuations diminish the magnitude of attenuation and velocity dispersion due to fluid flow, while the frequency range where these effects are significant gets broader. By comparing the acoustic responses obtained using different permeability averages, it is also shown that at very low frequencies the equivalent seismic permeability is similar to the equivalent flow permeability, while for very high frequencies this parameter approaches the arithmetic average of the permeability field. These seemingly generic findings have potentially important implications with regard to the estimation of equivalent flow permeability from seismic data.
Fil: Rubino, Jorge German. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universite de Lausanne; Suiza
Fil: Monachesi, Leonardo Bruno. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Müller, Tobias M.. Commonwealth Scientific and Industrial Research Organization; Australia
Fil: Guarracino, Luis. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Holliger, Klaus. Universite de Lausanne; Suiza
Materia
WAVE-INDUCED FLUID FLOW
SEISMIC PERMEABILITY
FLOW PERMEABILITY
SEISMIC WAVES
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/101635

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spelling Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuationsRubino, Jorge GermanMonachesi, Leonardo BrunoMüller, Tobias M.Guarracino, LuisHolliger, KlausWAVE-INDUCED FLUID FLOWSEISMIC PERMEABILITYFLOW PERMEABILITYSEISMIC WAVEShttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1https://purl.org/becyt/ford/2.7https://purl.org/becyt/ford/2Oscillatory fluid movements in heterogeneous porous rocks induced by seismic waves cause dissipation of wave field energy. The resulting seismic signature depends not only on the rock compressibility distribution, but also on a statistically averaged permeability. This so-called equivalent seismic permeability does, however, not coincide with the respective equivalent flow permeability. While this issue has been analyzed for 1D media, the corresponding 2D and 3D cases remain unexplored. In this work, this topic is analyzed for 2D random medium realizations having strong permeability fluctuations. With this objective, oscillatory compressibility simulations based on the quasi-static poroelasticity equations are performed. Numerical analysis shows that strong permeability fluctuations diminish the magnitude of attenuation and velocity dispersion due to fluid flow, while the frequency range where these effects are significant gets broader. By comparing the acoustic responses obtained using different permeability averages, it is also shown that at very low frequencies the equivalent seismic permeability is similar to the equivalent flow permeability, while for very high frequencies this parameter approaches the arithmetic average of the permeability field. These seemingly generic findings have potentially important implications with regard to the estimation of equivalent flow permeability from seismic data.Fil: Rubino, Jorge German. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universite de Lausanne; SuizaFil: Monachesi, Leonardo Bruno. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; ArgentinaFil: Müller, Tobias M.. Commonwealth Scientific and Industrial Research Organization; AustraliaFil: Guarracino, Luis. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; ArgentinaFil: Holliger, Klaus. Universite de Lausanne; SuizaAcoustical Society of America Institute of Physics2013-06info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/101635Rubino, Jorge German; Monachesi, Leonardo Bruno; Müller, Tobias M.; Guarracino, Luis; Holliger, Klaus; Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations; Acoustical Society of America Institute of Physics; Journal of the Acoustical Society of America; 134; 6; 6-2013; 4742-47510001-4966CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://scitation.aip.org/content/asa/journal/jasa/134/6/10.1121/1.4824967info:eu-repo/semantics/altIdentifier/doi/10.1121/1.4824967info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:09:18Zoai:ri.conicet.gov.ar:11336/101635instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 10:09:18.357CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations
title Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations
spellingShingle Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations
Rubino, Jorge German
WAVE-INDUCED FLUID FLOW
SEISMIC PERMEABILITY
FLOW PERMEABILITY
SEISMIC WAVES
title_short Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations
title_full Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations
title_fullStr Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations
title_full_unstemmed Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations
title_sort Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations
dc.creator.none.fl_str_mv Rubino, Jorge German
Monachesi, Leonardo Bruno
Müller, Tobias M.
Guarracino, Luis
Holliger, Klaus
author Rubino, Jorge German
author_facet Rubino, Jorge German
Monachesi, Leonardo Bruno
Müller, Tobias M.
Guarracino, Luis
Holliger, Klaus
author_role author
author2 Monachesi, Leonardo Bruno
Müller, Tobias M.
Guarracino, Luis
Holliger, Klaus
author2_role author
author
author
author
dc.subject.none.fl_str_mv WAVE-INDUCED FLUID FLOW
SEISMIC PERMEABILITY
FLOW PERMEABILITY
SEISMIC WAVES
topic WAVE-INDUCED FLUID FLOW
SEISMIC PERMEABILITY
FLOW PERMEABILITY
SEISMIC WAVES
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
https://purl.org/becyt/ford/2.7
https://purl.org/becyt/ford/2
dc.description.none.fl_txt_mv Oscillatory fluid movements in heterogeneous porous rocks induced by seismic waves cause dissipation of wave field energy. The resulting seismic signature depends not only on the rock compressibility distribution, but also on a statistically averaged permeability. This so-called equivalent seismic permeability does, however, not coincide with the respective equivalent flow permeability. While this issue has been analyzed for 1D media, the corresponding 2D and 3D cases remain unexplored. In this work, this topic is analyzed for 2D random medium realizations having strong permeability fluctuations. With this objective, oscillatory compressibility simulations based on the quasi-static poroelasticity equations are performed. Numerical analysis shows that strong permeability fluctuations diminish the magnitude of attenuation and velocity dispersion due to fluid flow, while the frequency range where these effects are significant gets broader. By comparing the acoustic responses obtained using different permeability averages, it is also shown that at very low frequencies the equivalent seismic permeability is similar to the equivalent flow permeability, while for very high frequencies this parameter approaches the arithmetic average of the permeability field. These seemingly generic findings have potentially important implications with regard to the estimation of equivalent flow permeability from seismic data.
Fil: Rubino, Jorge German. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universite de Lausanne; Suiza
Fil: Monachesi, Leonardo Bruno. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Müller, Tobias M.. Commonwealth Scientific and Industrial Research Organization; Australia
Fil: Guarracino, Luis. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Holliger, Klaus. Universite de Lausanne; Suiza
description Oscillatory fluid movements in heterogeneous porous rocks induced by seismic waves cause dissipation of wave field energy. The resulting seismic signature depends not only on the rock compressibility distribution, but also on a statistically averaged permeability. This so-called equivalent seismic permeability does, however, not coincide with the respective equivalent flow permeability. While this issue has been analyzed for 1D media, the corresponding 2D and 3D cases remain unexplored. In this work, this topic is analyzed for 2D random medium realizations having strong permeability fluctuations. With this objective, oscillatory compressibility simulations based on the quasi-static poroelasticity equations are performed. Numerical analysis shows that strong permeability fluctuations diminish the magnitude of attenuation and velocity dispersion due to fluid flow, while the frequency range where these effects are significant gets broader. By comparing the acoustic responses obtained using different permeability averages, it is also shown that at very low frequencies the equivalent seismic permeability is similar to the equivalent flow permeability, while for very high frequencies this parameter approaches the arithmetic average of the permeability field. These seemingly generic findings have potentially important implications with regard to the estimation of equivalent flow permeability from seismic data.
publishDate 2013
dc.date.none.fl_str_mv 2013-06
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/101635
Rubino, Jorge German; Monachesi, Leonardo Bruno; Müller, Tobias M.; Guarracino, Luis; Holliger, Klaus; Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations; Acoustical Society of America Institute of Physics; Journal of the Acoustical Society of America; 134; 6; 6-2013; 4742-4751
0001-4966
CONICET Digital
CONICET
url http://hdl.handle.net/11336/101635
identifier_str_mv Rubino, Jorge German; Monachesi, Leonardo Bruno; Müller, Tobias M.; Guarracino, Luis; Holliger, Klaus; Seismic wave attenuation and dispersion due to wave-induced fluid flow in rocks with strong permeability fluctuations; Acoustical Society of America Institute of Physics; Journal of the Acoustical Society of America; 134; 6; 6-2013; 4742-4751
0001-4966
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://scitation.aip.org/content/asa/journal/jasa/134/6/10.1121/1.4824967
info:eu-repo/semantics/altIdentifier/doi/10.1121/1.4824967
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Acoustical Society of America Institute of Physics
publisher.none.fl_str_mv Acoustical Society of America Institute of Physics
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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