Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures
- Autores
- Rubino, Jorge German; Quintal, Beatriz; Müller, Tobias M.; Guarracino, Luis; Jänicke, Ralf; Steeb, Holger; Holliger, Klaus
- Año de publicación
- 2015
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- An important characteristic of fractured rocks is their high seismic attenuation, which so far has been mainly attributed to wave-induced fluid flow (WIFF) between the fractures and the embedding matrix. The influence of fracture connectivity on seismic attenuation has, however, recently, only been investigated. Numerical compressibility and shear tests based on Biot’s quasi-static poro-elastic equations illustrate that an important manifestation of WIFF arises in the presence of fracture connectivity. The corresponding energy loss, which can be significant for both P- and S-waves, is mainly due to fluid flow within the connected fractures and is sensitive to the permeabilities as well as the lengths and intersection angles of the fractures. Correspondingly, this phenomenon contains valuable information on the governing hydraulic properties of fractured rocks and hence should be accounted for whenever realistic seismic models of such media are needed.
Fil: Rubino, Jorge German. Universite de Lausanne; Suiza. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Quintal, Beatriz. Universite de Lausanne; Suiza
Fil: Müller, Tobias M.. Commonwealth Scientific and Industrial Research Organization; Australia
Fil: Guarracino, Luis. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Jänicke, Ralf. Ruhr Universität Bochum; Alemania
Fil: Steeb, Holger. Ruhr Universität Bochum; Alemania
Fil: Holliger, Klaus. Universite de Lausanne; Suiza - Materia
-
Biot&Rsquo;S Theory
Embedding Matrix
Fracture Connectivity
Fractured Rocks
Seismic Attenuation
Wiff - 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:11336/53674
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Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fracturesRubino, Jorge GermanQuintal, BeatrizMüller, Tobias M.Guarracino, LuisJänicke, RalfSteeb, HolgerHolliger, KlausBiot&Rsquo;S TheoryEmbedding MatrixFracture ConnectivityFractured RocksSeismic AttenuationWiffhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1An important characteristic of fractured rocks is their high seismic attenuation, which so far has been mainly attributed to wave-induced fluid flow (WIFF) between the fractures and the embedding matrix. The influence of fracture connectivity on seismic attenuation has, however, recently, only been investigated. Numerical compressibility and shear tests based on Biot’s quasi-static poro-elastic equations illustrate that an important manifestation of WIFF arises in the presence of fracture connectivity. The corresponding energy loss, which can be significant for both P- and S-waves, is mainly due to fluid flow within the connected fractures and is sensitive to the permeabilities as well as the lengths and intersection angles of the fractures. Correspondingly, this phenomenon contains valuable information on the governing hydraulic properties of fractured rocks and hence should be accounted for whenever realistic seismic models of such media are needed.Fil: Rubino, Jorge German. Universite de Lausanne; Suiza. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Quintal, Beatriz. Universite de Lausanne; SuizaFil: Müller, Tobias M.. Commonwealth Scientific and Industrial Research Organization; AustraliaFil: Guarracino, Luis. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Jänicke, Ralf. Ruhr Universität Bochum; AlemaniaFil: Steeb, Holger. Ruhr Universität Bochum; AlemaniaFil: Holliger, Klaus. Universite de Lausanne; SuizaChina University of Geosciences2015-12info: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/11336/53674Rubino, Jorge German; Quintal, Beatriz; Müller, Tobias M.; Guarracino, Luis; Jänicke, Ralf; et al.; Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures; China University of Geosciences; Journal Of Earth Science; 26; 6; 12-2015; 785-7901674-487X1867-111XCONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1007/s12583-015-0613-0info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007%2Fs12583-015-0613-0info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:59:19Zoai:ri.conicet.gov.ar:11336/53674instacron: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 09:59:20.022CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures |
title |
Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures |
spellingShingle |
Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures Rubino, Jorge German Biot&Rsquo;S Theory Embedding Matrix Fracture Connectivity Fractured Rocks Seismic Attenuation Wiff |
title_short |
Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures |
title_full |
Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures |
title_fullStr |
Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures |
title_full_unstemmed |
Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures |
title_sort |
Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures |
dc.creator.none.fl_str_mv |
Rubino, Jorge German Quintal, Beatriz Müller, Tobias M. Guarracino, Luis Jänicke, Ralf Steeb, Holger Holliger, Klaus |
author |
Rubino, Jorge German |
author_facet |
Rubino, Jorge German Quintal, Beatriz Müller, Tobias M. Guarracino, Luis Jänicke, Ralf Steeb, Holger Holliger, Klaus |
author_role |
author |
author2 |
Quintal, Beatriz Müller, Tobias M. Guarracino, Luis Jänicke, Ralf Steeb, Holger Holliger, Klaus |
author2_role |
author author author author author author |
dc.subject.none.fl_str_mv |
Biot&Rsquo;S Theory Embedding Matrix Fracture Connectivity Fractured Rocks Seismic Attenuation Wiff |
topic |
Biot&Rsquo;S Theory Embedding Matrix Fracture Connectivity Fractured Rocks Seismic Attenuation Wiff |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
An important characteristic of fractured rocks is their high seismic attenuation, which so far has been mainly attributed to wave-induced fluid flow (WIFF) between the fractures and the embedding matrix. The influence of fracture connectivity on seismic attenuation has, however, recently, only been investigated. Numerical compressibility and shear tests based on Biot’s quasi-static poro-elastic equations illustrate that an important manifestation of WIFF arises in the presence of fracture connectivity. The corresponding energy loss, which can be significant for both P- and S-waves, is mainly due to fluid flow within the connected fractures and is sensitive to the permeabilities as well as the lengths and intersection angles of the fractures. Correspondingly, this phenomenon contains valuable information on the governing hydraulic properties of fractured rocks and hence should be accounted for whenever realistic seismic models of such media are needed. Fil: Rubino, Jorge German. Universite de Lausanne; Suiza. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Quintal, Beatriz. Universite de Lausanne; Suiza Fil: Müller, Tobias M.. Commonwealth Scientific and Industrial Research Organization; Australia Fil: Guarracino, Luis. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Jänicke, Ralf. Ruhr Universität Bochum; Alemania Fil: Steeb, Holger. Ruhr Universität Bochum; Alemania Fil: Holliger, Klaus. Universite de Lausanne; Suiza |
description |
An important characteristic of fractured rocks is their high seismic attenuation, which so far has been mainly attributed to wave-induced fluid flow (WIFF) between the fractures and the embedding matrix. The influence of fracture connectivity on seismic attenuation has, however, recently, only been investigated. Numerical compressibility and shear tests based on Biot’s quasi-static poro-elastic equations illustrate that an important manifestation of WIFF arises in the presence of fracture connectivity. The corresponding energy loss, which can be significant for both P- and S-waves, is mainly due to fluid flow within the connected fractures and is sensitive to the permeabilities as well as the lengths and intersection angles of the fractures. Correspondingly, this phenomenon contains valuable information on the governing hydraulic properties of fractured rocks and hence should be accounted for whenever realistic seismic models of such media are needed. |
publishDate |
2015 |
dc.date.none.fl_str_mv |
2015-12 |
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/11336/53674 Rubino, Jorge German; Quintal, Beatriz; Müller, Tobias M.; Guarracino, Luis; Jänicke, Ralf; et al.; Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures; China University of Geosciences; Journal Of Earth Science; 26; 6; 12-2015; 785-790 1674-487X 1867-111X CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/53674 |
identifier_str_mv |
Rubino, Jorge German; Quintal, Beatriz; Müller, Tobias M.; Guarracino, Luis; Jänicke, Ralf; et al.; Energy dissipation of P- and S-waves in fluid-saturated rocks: An overview focusing on hydraulically connected fractures; China University of Geosciences; Journal Of Earth Science; 26; 6; 12-2015; 785-790 1674-487X 1867-111X CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1007/s12583-015-0613-0 info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007%2Fs12583-015-0613-0 |
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 |
China University of Geosciences |
publisher.none.fl_str_mv |
China University of Geosciences |
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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1844613761006043136 |
score |
13.070432 |