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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/101635
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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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1842270075277541376 |
score |
13.13397 |