Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic Study

Autores
Monachesi, Leonardo Bruno; Wollner, Uri; Dvorkin, Jack
Año de publicación
2020
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
A patchy saturated two-layered porous rock, with each layer filled with a different fluid, is examined. We assume that this system is probed by an elastic wave having a wavelength much larger than the layers' thicknesses. We also assume that the diffusion length is smaller than the thickness of an individual layer, which implies hydraulic disconnection between layers. In the context of Gassmann's fluid substitution theory, we analytically derived an exact expression for the effective fluid bulk modulus assuming that both layers have the same porosity, dry frame, and mineral matrix properties. In addition we derived an approximate solution that works well at relatively high porosities. Both solutions are expressed as a weighted average of the arithmetic and harmonic averages of individual bulk moduli of the pore fluid. These weights are explicitly given as functions of the porosity, the fractional thicknesses of both layers, and the elastic moduli of the constituents. For the approximate solution, one does not require explicit knowledge of the shear modulus of the rock. The comparison with laboratory data showed that, in the case where a porous, isotropic rock is filled with water and gas, the approximate solution can be used to model the measured data for high values of water saturation.
Fil: Monachesi, Leonardo Bruno. Universidad Nacional de Río Negro; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina
Fil: Wollner, Uri. University of Stanford; Estados Unidos
Fil: Dvorkin, Jack. King Fahd University Of Petroleum And Minerals; Arabia Saudita
Materia
Patchy
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:11336/183839

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spelling Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic StudyMonachesi, Leonardo BrunoWollner, UriDvorkin, JackPatchyhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1A patchy saturated two-layered porous rock, with each layer filled with a different fluid, is examined. We assume that this system is probed by an elastic wave having a wavelength much larger than the layers' thicknesses. We also assume that the diffusion length is smaller than the thickness of an individual layer, which implies hydraulic disconnection between layers. In the context of Gassmann's fluid substitution theory, we analytically derived an exact expression for the effective fluid bulk modulus assuming that both layers have the same porosity, dry frame, and mineral matrix properties. In addition we derived an approximate solution that works well at relatively high porosities. Both solutions are expressed as a weighted average of the arithmetic and harmonic averages of individual bulk moduli of the pore fluid. These weights are explicitly given as functions of the porosity, the fractional thicknesses of both layers, and the elastic moduli of the constituents. For the approximate solution, one does not require explicit knowledge of the shear modulus of the rock. The comparison with laboratory data showed that, in the case where a porous, isotropic rock is filled with water and gas, the approximate solution can be used to model the measured data for high values of water saturation.Fil: Monachesi, Leonardo Bruno. Universidad Nacional de Río Negro; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; ArgentinaFil: Wollner, Uri. University of Stanford; Estados UnidosFil: Dvorkin, Jack. King Fahd University Of Petroleum And Minerals; Arabia SauditaBlackwell Publishing2020-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/183839Monachesi, Leonardo Bruno; Wollner, Uri; Dvorkin, Jack; Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic Study; Blackwell Publishing; Journal of Geophysical Research: Solid Earth; 125; 1; 1-2020; 1-122169-93132169-9356CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1029/2019JB018267info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-10T13:15:44Zoai:ri.conicet.gov.ar:11336/183839instacron: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:34982025-09-10 13:15:44.284CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic Study
title Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic Study
spellingShingle Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic Study
Monachesi, Leonardo Bruno
Patchy
title_short Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic Study
title_full Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic Study
title_fullStr Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic Study
title_full_unstemmed Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic Study
title_sort Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic Study
dc.creator.none.fl_str_mv Monachesi, Leonardo Bruno
Wollner, Uri
Dvorkin, Jack
author Monachesi, Leonardo Bruno
author_facet Monachesi, Leonardo Bruno
Wollner, Uri
Dvorkin, Jack
author_role author
author2 Wollner, Uri
Dvorkin, Jack
author2_role author
author
dc.subject.none.fl_str_mv Patchy
topic Patchy
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv A patchy saturated two-layered porous rock, with each layer filled with a different fluid, is examined. We assume that this system is probed by an elastic wave having a wavelength much larger than the layers' thicknesses. We also assume that the diffusion length is smaller than the thickness of an individual layer, which implies hydraulic disconnection between layers. In the context of Gassmann's fluid substitution theory, we analytically derived an exact expression for the effective fluid bulk modulus assuming that both layers have the same porosity, dry frame, and mineral matrix properties. In addition we derived an approximate solution that works well at relatively high porosities. Both solutions are expressed as a weighted average of the arithmetic and harmonic averages of individual bulk moduli of the pore fluid. These weights are explicitly given as functions of the porosity, the fractional thicknesses of both layers, and the elastic moduli of the constituents. For the approximate solution, one does not require explicit knowledge of the shear modulus of the rock. The comparison with laboratory data showed that, in the case where a porous, isotropic rock is filled with water and gas, the approximate solution can be used to model the measured data for high values of water saturation.
Fil: Monachesi, Leonardo Bruno. Universidad Nacional de Río Negro; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Patagonia Norte. Instituto de Investigación en Paleobiología y Geología; Argentina
Fil: Wollner, Uri. University of Stanford; Estados Unidos
Fil: Dvorkin, Jack. King Fahd University Of Petroleum And Minerals; Arabia Saudita
description A patchy saturated two-layered porous rock, with each layer filled with a different fluid, is examined. We assume that this system is probed by an elastic wave having a wavelength much larger than the layers' thicknesses. We also assume that the diffusion length is smaller than the thickness of an individual layer, which implies hydraulic disconnection between layers. In the context of Gassmann's fluid substitution theory, we analytically derived an exact expression for the effective fluid bulk modulus assuming that both layers have the same porosity, dry frame, and mineral matrix properties. In addition we derived an approximate solution that works well at relatively high porosities. Both solutions are expressed as a weighted average of the arithmetic and harmonic averages of individual bulk moduli of the pore fluid. These weights are explicitly given as functions of the porosity, the fractional thicknesses of both layers, and the elastic moduli of the constituents. For the approximate solution, one does not require explicit knowledge of the shear modulus of the rock. The comparison with laboratory data showed that, in the case where a porous, isotropic rock is filled with water and gas, the approximate solution can be used to model the measured data for high values of water saturation.
publishDate 2020
dc.date.none.fl_str_mv 2020-01
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/11336/183839
Monachesi, Leonardo Bruno; Wollner, Uri; Dvorkin, Jack; Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic Study; Blackwell Publishing; Journal of Geophysical Research: Solid Earth; 125; 1; 1-2020; 1-12
2169-9313
2169-9356
CONICET Digital
CONICET
url http://hdl.handle.net/11336/183839
identifier_str_mv Monachesi, Leonardo Bruno; Wollner, Uri; Dvorkin, Jack; Effective Pore Fluid Bulk Modulus at Patchy Saturation: An Analytic Study; Blackwell Publishing; Journal of Geophysical Research: Solid Earth; 125; 1; 1-2020; 1-12
2169-9313
2169-9356
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1029/2019JB018267
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
dc.publisher.none.fl_str_mv Blackwell Publishing
publisher.none.fl_str_mv Blackwell Publishing
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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