Wave attenuation in partially saturated porous rocks - New observations and interpretations across scales

Autores
Caspari, Eva; Qi, Qiaomu; Lopes, Sofia; Lebedev, Maxim; Gurevich, Boris; Rubino, Jorge German; Velis, Danilo Ruben; Clennell, Michael B.; Müller, Tobias M.
Año de publicación
2014
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Seismic waves propagating in porous rocks saturated with two immiscible fluids can be strongly attenuated. Predicting saturation effects on seismic responses requires a sound understanding of attenuation and velocity dependencies on the fluid distribution. Decoding these effects involves interpreting laboratory experiments, analyzing well-log data, and performing numerical simulations. Despite striking differences among scales, flow regimes, and frequency bands, some aspects of wave attenuation can be explained with a single
mechanism ? wave-induced pressure diffusion. Different facets of wave-induced pressure diffusion can be revealed across scales.
Fil: Caspari, Eva. Curtin University; Australia
Fil: Qi, Qiaomu. Curtin University; Australia
Fil: Lopes, Sofia. Curtin University; Australia
Fil: Lebedev, Maxim. Curtin University; Australia
Fil: Gurevich, Boris. Curtin University; Australia. Organización de Investigación Científica e Industrial del Commonwealth; Australia
Fil: Rubino, Jorge German. Universite de Lausanne; Suiza. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Velis, Danilo Ruben. 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. Departamento de Geofísica Aplicada; Argentina
Fil: Clennell, Michael B.. Organización de Investigación Científica e Industrial del Commonwealth; Australia
Fil: Müller, Tobias M.. Organización de Investigación Científica e Industrial del Commonwealth; Australia
Materia
Attenuation
Dispersion
porous rocks
fluid flow
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:11336/101679
Acceder
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repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Wave attenuation in partially saturated porous rocks - New observations and interpretations across scalesCaspari, EvaQi, QiaomuLopes, SofiaLebedev, MaximGurevich, BorisRubino, Jorge GermanVelis, Danilo RubenClennell, Michael B.Müller, Tobias M.AttenuationDispersionporous rocksfluid flowhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Seismic waves propagating in porous rocks saturated with two immiscible fluids can be strongly attenuated. Predicting saturation effects on seismic responses requires a sound understanding of attenuation and velocity dependencies on the fluid distribution. Decoding these effects involves interpreting laboratory experiments, analyzing well-log data, and performing numerical simulations. Despite striking differences among scales, flow regimes, and frequency bands, some aspects of wave attenuation can be explained with a single<br />mechanism ? wave-induced pressure diffusion. Different facets of wave-induced pressure diffusion can be revealed across scales.Fil: Caspari, Eva. Curtin University; AustraliaFil: Qi, Qiaomu. Curtin University; AustraliaFil: Lopes, Sofia. Curtin University; AustraliaFil: Lebedev, Maxim. Curtin University; AustraliaFil: Gurevich, Boris. Curtin University; Australia. Organización de Investigación Científica e Industrial del Commonwealth; AustraliaFil: Rubino, Jorge German. Universite de Lausanne; Suiza. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Velis, Danilo Ruben. 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. Departamento de Geofísica Aplicada; ArgentinaFil: Clennell, Michael B.. Organización de Investigación Científica e Industrial del Commonwealth; AustraliaFil: Müller, Tobias M.. Organización de Investigación Científica e Industrial del Commonwealth; AustraliaSociety of Exploration Geophysicists2014-06info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/101679Caspari, Eva; Qi, Qiaomu; Lopes, Sofia; Lebedev, Maxim; Gurevich, Boris; et al.; Wave attenuation in partially saturated porous rocks - New observations and interpretations across scales; Society of Exploration Geophysicists; The Leading Edge; 33; 6; 6-2014; 606-6141070-485XCONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1190/tle33060606.1info:eu-repo/semantics/altIdentifier/url/https://library.seg.org/doi/10.1190/tle33060606.1info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:38:55Zoai:ri.conicet.gov.ar:11336/101679instacron: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:34982025-09-29 10:38:55.691CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Wave attenuation in partially saturated porous rocks - New observations and interpretations across scales
title Wave attenuation in partially saturated porous rocks - New observations and interpretations across scales
spellingShingle Wave attenuation in partially saturated porous rocks - New observations and interpretations across scales
Caspari, Eva
Attenuation
Dispersion
porous rocks
fluid flow
title_short Wave attenuation in partially saturated porous rocks - New observations and interpretations across scales
title_full Wave attenuation in partially saturated porous rocks - New observations and interpretations across scales
title_fullStr Wave attenuation in partially saturated porous rocks - New observations and interpretations across scales
title_full_unstemmed Wave attenuation in partially saturated porous rocks - New observations and interpretations across scales
title_sort Wave attenuation in partially saturated porous rocks - New observations and interpretations across scales
dc.creator.none.fl_str_mv Caspari, Eva
Qi, Qiaomu
Lopes, Sofia
Lebedev, Maxim
Gurevich, Boris
Rubino, Jorge German
Velis, Danilo Ruben
Clennell, Michael B.
Müller, Tobias M.
author Caspari, Eva
author_facet Caspari, Eva
Qi, Qiaomu
Lopes, Sofia
Lebedev, Maxim
Gurevich, Boris
Rubino, Jorge German
Velis, Danilo Ruben
Clennell, Michael B.
Müller, Tobias M.
author_role author
author2 Qi, Qiaomu
Lopes, Sofia
Lebedev, Maxim
Gurevich, Boris
Rubino, Jorge German
Velis, Danilo Ruben
Clennell, Michael B.
Müller, Tobias M.
author2_role author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Attenuation
Dispersion
porous rocks
fluid flow
topic Attenuation
Dispersion
porous rocks
fluid flow
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Seismic waves propagating in porous rocks saturated with two immiscible fluids can be strongly attenuated. Predicting saturation effects on seismic responses requires a sound understanding of attenuation and velocity dependencies on the fluid distribution. Decoding these effects involves interpreting laboratory experiments, analyzing well-log data, and performing numerical simulations. Despite striking differences among scales, flow regimes, and frequency bands, some aspects of wave attenuation can be explained with a single<br />mechanism ? wave-induced pressure diffusion. Different facets of wave-induced pressure diffusion can be revealed across scales.
Fil: Caspari, Eva. Curtin University; Australia
Fil: Qi, Qiaomu. Curtin University; Australia
Fil: Lopes, Sofia. Curtin University; Australia
Fil: Lebedev, Maxim. Curtin University; Australia
Fil: Gurevich, Boris. Curtin University; Australia. Organización de Investigación Científica e Industrial del Commonwealth; Australia
Fil: Rubino, Jorge German. Universite de Lausanne; Suiza. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Velis, Danilo Ruben. 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. Departamento de Geofísica Aplicada; Argentina
Fil: Clennell, Michael B.. Organización de Investigación Científica e Industrial del Commonwealth; Australia
Fil: Müller, Tobias M.. Organización de Investigación Científica e Industrial del Commonwealth; Australia
description Seismic waves propagating in porous rocks saturated with two immiscible fluids can be strongly attenuated. Predicting saturation effects on seismic responses requires a sound understanding of attenuation and velocity dependencies on the fluid distribution. Decoding these effects involves interpreting laboratory experiments, analyzing well-log data, and performing numerical simulations. Despite striking differences among scales, flow regimes, and frequency bands, some aspects of wave attenuation can be explained with a single<br />mechanism ? wave-induced pressure diffusion. Different facets of wave-induced pressure diffusion can be revealed across scales.
publishDate 2014
dc.date.none.fl_str_mv 2014-06
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/11336/101679
Caspari, Eva; Qi, Qiaomu; Lopes, Sofia; Lebedev, Maxim; Gurevich, Boris; et al.; Wave attenuation in partially saturated porous rocks - New observations and interpretations across scales; Society of Exploration Geophysicists; The Leading Edge; 33; 6; 6-2014; 606-614
1070-485X
CONICET Digital
CONICET
url http://hdl.handle.net/11336/101679
identifier_str_mv Caspari, Eva; Qi, Qiaomu; Lopes, Sofia; Lebedev, Maxim; Gurevich, Boris; et al.; Wave attenuation in partially saturated porous rocks - New observations and interpretations across scales; Society of Exploration Geophysicists; The Leading Edge; 33; 6; 6-2014; 606-614
1070-485X
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1190/tle33060606.1
info:eu-repo/semantics/altIdentifier/url/https://library.seg.org/doi/10.1190/tle33060606.1
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
dc.publisher.none.fl_str_mv Society of Exploration Geophysicists
publisher.none.fl_str_mv Society of Exploration Geophysicists
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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score 13.070432

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