Including poroelastic effects in the linear slip theory

Autores
Rubino, Jorge G.; Castromán, Gabriel A.; Müller, Tobias M.; Monachesi, Leonardo B.; Zyserman, Fabio I.; Holliger, Klaus
Año de publicación
2015
Idioma
español castellano
Tipo de recurso
artículo
Estado
versión aceptada
Descripción
Fil: Rubino, Jorge G. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.
Fil: Rubino, Jorge G. Universite de Lausanne; Suiza
Fil: Castromán, Gabriel A. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.
Fil: Castromán, Gabriel A. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Müller, Tobias M. Commonwealth Scientific and Industrial Research Organization; Australia
Fil: Monachesi, Leonardo B. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.
Fil: Monachesi, Leonardo B. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Zyserman, Fabio I. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.
Fil: Zyserman, Fabio I. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Holliger, Klaus. Universite de Lausanne; Suiza
Numerical simulations of seismic wave propagation in fractured media are often performed in the framework of the linear slip theory (LST). Therein, fractures are represented as interfaces and their mechanical properties are characterized through a compliance matrix. This theory has been extended to account for energy dissipation due to viscous friction within fluid-filled fractures by using complex-valued frequency-dependent compliances. This is, however, not fully adequate for fractured porous rocks in which wave-induced fluid flow (WIFF) between fractures and host rock constitutes a predominant seismic attenuation mechanism. In this letter, we develop an approach to incorporate WIFF effects directly into the LST for a 1D system via a complex-valued, frequency-dependent fracture compliance. The methodology is validated for a medium permeated by regularly distributed planar fractures, for which an analytical expression for the complex-valued normal compliance is determined in the framework of quasistatic poroelasticity. There is good agreement between synthetic seismograms generated using the proposed recipe and those obtained from comprehensive, but computationally demanding, poroelastic simulations.
Materia
Meteorología y Ciencias Atmosféricas
Fractures
Attenuation
Modeling
Seismic Attributes
Meteorología y Ciencias Atmosféricas
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/4.0/
Repositorio
RID-UNRN (UNRN)
Institución
Universidad Nacional de Río Negro
OAI Identificador
oai:rid.unrn.edu.ar:20.500.12049/2873
Acceder
id RIDUNRN_7673234b1d94b1583359c4af66c29106
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network_acronym_str RIDUNRN
repository_id_str 4369
network_name_str RID-UNRN (UNRN)
spelling Including poroelastic effects in the linear slip theoryRubino, Jorge G.Castromán, Gabriel A.Müller, Tobias M.Monachesi, Leonardo B.Zyserman, Fabio I.Holliger, KlausMeteorología y Ciencias AtmosféricasFracturesAttenuationModelingSeismic AttributesMeteorología y Ciencias AtmosféricasFil: Rubino, Jorge G. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.Fil: Rubino, Jorge G. Universite de Lausanne; SuizaFil: Castromán, Gabriel A. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.Fil: Castromán, Gabriel A. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; ArgentinaFil: Müller, Tobias M. Commonwealth Scientific and Industrial Research Organization; AustraliaFil: Monachesi, Leonardo B. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.Fil: Monachesi, Leonardo B. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; ArgentinaFil: Zyserman, Fabio I. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.Fil: Zyserman, Fabio I. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; ArgentinaFil: Holliger, Klaus. Universite de Lausanne; SuizaNumerical simulations of seismic wave propagation in fractured media are often performed in the framework of the linear slip theory (LST). Therein, fractures are represented as interfaces and their mechanical properties are characterized through a compliance matrix. This theory has been extended to account for energy dissipation due to viscous friction within fluid-filled fractures by using complex-valued frequency-dependent compliances. This is, however, not fully adequate for fractured porous rocks in which wave-induced fluid flow (WIFF) between fractures and host rock constitutes a predominant seismic attenuation mechanism. In this letter, we develop an approach to incorporate WIFF effects directly into the LST for a 1D system via a complex-valued, frequency-dependent fracture compliance. The methodology is validated for a medium permeated by regularly distributed planar fractures, for which an analytical expression for the complex-valued normal compliance is determined in the framework of quasistatic poroelasticity. There is good agreement between synthetic seismograms generated using the proposed recipe and those obtained from comprehensive, but computationally demanding, poroelastic simulations.2015-04info:eu-repo/semantics/articleinfo:eu-repo/semantics/acceptedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfRubino, Jorge G., Castromán, Gabriel A., Müller, Tobias M., Monachesi, Leonardo B., Zyserman, Fabio I. & et al. (2015). Including poroelastic effects in the linear slip theory. Society of Exploration Geophysicists; Geophysics; 80; 2; 51-560016-8033https://library.seg.org/doi/10.1190/geo2014-0409.1http://hdl.handle.net/11336/53573https://rid.unrn.edu.ar/jspui/handle/20.500.12049/2873https://dx.doi.org/10.1190/geo2014-0409.1spa80Geophysicsinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/4.0/reponame:RID-UNRN (UNRN)instname:Universidad Nacional de Río Negro2025-10-23T11:17:31Zoai:rid.unrn.edu.ar:20.500.12049/2873instacron:UNRNInstitucionalhttps://rid.unrn.edu.ar/jspui/Universidad públicaNo correspondehttps://rid.unrn.edu.ar/oai/snrdrid@unrn.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:43692025-10-23 11:17:31.374RID-UNRN (UNRN) - Universidad Nacional de Río Negrofalse
dc.title.none.fl_str_mv Including poroelastic effects in the linear slip theory
title Including poroelastic effects in the linear slip theory
spellingShingle Including poroelastic effects in the linear slip theory
Rubino, Jorge G.
Meteorología y Ciencias Atmosféricas
Fractures
Attenuation
Modeling
Seismic Attributes
Meteorología y Ciencias Atmosféricas
title_short Including poroelastic effects in the linear slip theory
title_full Including poroelastic effects in the linear slip theory
title_fullStr Including poroelastic effects in the linear slip theory
title_full_unstemmed Including poroelastic effects in the linear slip theory
title_sort Including poroelastic effects in the linear slip theory
dc.creator.none.fl_str_mv Rubino, Jorge G.
Castromán, Gabriel A.
Müller, Tobias M.
Monachesi, Leonardo B.
Zyserman, Fabio I.
Holliger, Klaus
author Rubino, Jorge G.
author_facet Rubino, Jorge G.
Castromán, Gabriel A.
Müller, Tobias M.
Monachesi, Leonardo B.
Zyserman, Fabio I.
Holliger, Klaus
author_role author
author2 Castromán, Gabriel A.
Müller, Tobias M.
Monachesi, Leonardo B.
Zyserman, Fabio I.
Holliger, Klaus
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv Meteorología y Ciencias Atmosféricas
Fractures
Attenuation
Modeling
Seismic Attributes
Meteorología y Ciencias Atmosféricas
topic Meteorología y Ciencias Atmosféricas
Fractures
Attenuation
Modeling
Seismic Attributes
Meteorología y Ciencias Atmosféricas
dc.description.none.fl_txt_mv Fil: Rubino, Jorge G. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.
Fil: Rubino, Jorge G. Universite de Lausanne; Suiza
Fil: Castromán, Gabriel A. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.
Fil: Castromán, Gabriel A. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Müller, Tobias M. Commonwealth Scientific and Industrial Research Organization; Australia
Fil: Monachesi, Leonardo B. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.
Fil: Monachesi, Leonardo B. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Zyserman, Fabio I. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.
Fil: Zyserman, Fabio I. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Holliger, Klaus. Universite de Lausanne; Suiza
Numerical simulations of seismic wave propagation in fractured media are often performed in the framework of the linear slip theory (LST). Therein, fractures are represented as interfaces and their mechanical properties are characterized through a compliance matrix. This theory has been extended to account for energy dissipation due to viscous friction within fluid-filled fractures by using complex-valued frequency-dependent compliances. This is, however, not fully adequate for fractured porous rocks in which wave-induced fluid flow (WIFF) between fractures and host rock constitutes a predominant seismic attenuation mechanism. In this letter, we develop an approach to incorporate WIFF effects directly into the LST for a 1D system via a complex-valued, frequency-dependent fracture compliance. The methodology is validated for a medium permeated by regularly distributed planar fractures, for which an analytical expression for the complex-valued normal compliance is determined in the framework of quasistatic poroelasticity. There is good agreement between synthetic seismograms generated using the proposed recipe and those obtained from comprehensive, but computationally demanding, poroelastic simulations.
description Fil: Rubino, Jorge G. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina.
publishDate 2015
dc.date.none.fl_str_mv 2015-04
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/acceptedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str acceptedVersion
dc.identifier.none.fl_str_mv Rubino, Jorge G., Castromán, Gabriel A., Müller, Tobias M., Monachesi, Leonardo B., Zyserman, Fabio I. & et al. (2015). Including poroelastic effects in the linear slip theory. Society of Exploration Geophysicists; Geophysics; 80; 2; 51-56
0016-8033
https://library.seg.org/doi/10.1190/geo2014-0409.1
http://hdl.handle.net/11336/53573
https://rid.unrn.edu.ar/jspui/handle/20.500.12049/2873
https://dx.doi.org/10.1190/geo2014-0409.1
identifier_str_mv Rubino, Jorge G., Castromán, Gabriel A., Müller, Tobias M., Monachesi, Leonardo B., Zyserman, Fabio I. & et al. (2015). Including poroelastic effects in the linear slip theory. Society of Exploration Geophysicists; Geophysics; 80; 2; 51-56
0016-8033
url https://library.seg.org/doi/10.1190/geo2014-0409.1
http://hdl.handle.net/11336/53573
https://rid.unrn.edu.ar/jspui/handle/20.500.12049/2873
https://dx.doi.org/10.1190/geo2014-0409.1
dc.language.none.fl_str_mv spa
language spa
dc.relation.none.fl_str_mv 80
Geophysics
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/4.0/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/4.0/
dc.format.none.fl_str_mv application/pdf
dc.source.none.fl_str_mv reponame:RID-UNRN (UNRN)
instname:Universidad Nacional de Río Negro
reponame_str RID-UNRN (UNRN)
collection RID-UNRN (UNRN)
instname_str Universidad Nacional de Río Negro
repository.name.fl_str_mv RID-UNRN (UNRN) - Universidad Nacional de Río Negro
repository.mail.fl_str_mv rid@unrn.edu.ar
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score 12.982451

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