Miscible transfer of solute in different model fractures: From random to multiscale wall roughness

Autores
Auradou, Harold; Boschan, Alejandro; Chertcoff, Ricardo Héctor; D'angelo, María Verónica; Hulin, Jean-Pierre; Ippolito, Irene Paula
Año de publicación
2010
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Miscible tracer dispersion measurements in transparent model fractures with different types of wall roughness are reported. The nature (Fickian or not) of dispersion is determined by studying variations of the mixing front as a function of the distance travelled but also as a function of the lateral scale over which the tracer concentration is averaged. The dominant hydrodynamic dispersion mechanisms (velocity profile in the gap, velocity variations in the fracture plane) are established by comparing measurements using Newtonian and shear thinning fluids. For small monodisperse rugosities, front spreading is diffusive with a dominant geometrical dispersion (dispersion coefficient D ∝ Pe or constant dispersivity ld = D/U) at low Péclet numbers Pe; at higher Pe values, one has either ld ∝ Pe (i.e. Taylor dispersion) for obstacles of height smaller than the gap, or ld ∝ Pe0.35 for obstacles bridging the gap. For a self-affine multiscale roughness like in actual rocks and a relative shear displacement over(δ, →) of complementary walls, the aperture field is channelized in the direction perpendicular to over(δ, →). For a mean velocity over(U, →) parallel to the channels, the global front geometry reflects the velocity contrast between them and is predicted from the aperture field. For over(U, →) perpendicular to the channels, global front spreading is much reduced. Local spreading of the front thickness remains mostly controlled by Taylor dispersion except in the case of a very strong channelization parallel to over(U, →).
Fil: Auradou, Harold. Université Pierre et Marie Curie; Francia. Université Paris Sud; Francia
Fil: Boschan, Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Université Pierre et Marie Curie; Francia. Université Paris Sud; Francia. Universidad de Buenos Aires. Facultad de Ingeniería. Departamento de Física. Grupo de Medios Porosos; Argentina
Fil: Chertcoff, Ricardo Héctor. Universidad de Buenos Aires; Argentina
Fil: D'angelo, María Verónica. Université Pierre et Marie Curie; Francia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Université Paris Sud; Francia. Universidad de Buenos Aires. Facultad de Ingeniería. Departamento de Física. Grupo de Medios Porosos; Argentina
Fil: Hulin, Jean-Pierre. Université Pierre et Marie Curie; Francia. Université Paris Sud; Francia
Fil: Ippolito, Irene Paula. Universidad de Buenos Aires. Facultad de Ingeniería. Departamento de Física. Grupo de Medios Porosos; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Materia
DISPERSION
FRACTURES
MULTISCALE
ROUGHNESS
SELF-AFFINE
SHEAR-THINNING
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:11336/139157
Acceder
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oai_identifier_str oai:ri.conicet.gov.ar:11336/139157
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Miscible transfer of solute in different model fractures: From random to multiscale wall roughnessTransport miscible de solutés dans différentes fractures modèles : influence de la rugosité aléatoire ou multiéchellesAuradou, HaroldBoschan, AlejandroChertcoff, Ricardo HéctorD'angelo, María VerónicaHulin, Jean-PierreIppolito, Irene PaulaDISPERSIONFRACTURESMULTISCALEROUGHNESSSELF-AFFINESHEAR-THINNINGhttps://purl.org/becyt/ford/1.3https://purl.org/becyt/ford/1Miscible tracer dispersion measurements in transparent model fractures with different types of wall roughness are reported. The nature (Fickian or not) of dispersion is determined by studying variations of the mixing front as a function of the distance travelled but also as a function of the lateral scale over which the tracer concentration is averaged. The dominant hydrodynamic dispersion mechanisms (velocity profile in the gap, velocity variations in the fracture plane) are established by comparing measurements using Newtonian and shear thinning fluids. For small monodisperse rugosities, front spreading is diffusive with a dominant geometrical dispersion (dispersion coefficient D ∝ Pe or constant dispersivity ld = D/U) at low Péclet numbers Pe; at higher Pe values, one has either ld ∝ Pe (i.e. Taylor dispersion) for obstacles of height smaller than the gap, or ld ∝ Pe0.35 for obstacles bridging the gap. For a self-affine multiscale roughness like in actual rocks and a relative shear displacement over(δ, →) of complementary walls, the aperture field is channelized in the direction perpendicular to over(δ, →). For a mean velocity over(U, →) parallel to the channels, the global front geometry reflects the velocity contrast between them and is predicted from the aperture field. For over(U, →) perpendicular to the channels, global front spreading is much reduced. Local spreading of the front thickness remains mostly controlled by Taylor dispersion except in the case of a very strong channelization parallel to over(U, →).Fil: Auradou, Harold. Université Pierre et Marie Curie; Francia. Université Paris Sud; FranciaFil: Boschan, Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Université Pierre et Marie Curie; Francia. Université Paris Sud; Francia. Universidad de Buenos Aires. Facultad de Ingeniería. Departamento de Física. Grupo de Medios Porosos; ArgentinaFil: Chertcoff, Ricardo Héctor. Universidad de Buenos Aires; ArgentinaFil: D'angelo, María Verónica. Université Pierre et Marie Curie; Francia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Université Paris Sud; Francia. Universidad de Buenos Aires. Facultad de Ingeniería. Departamento de Física. Grupo de Medios Porosos; ArgentinaFil: Hulin, Jean-Pierre. Université Pierre et Marie Curie; Francia. Université Paris Sud; FranciaFil: Ippolito, Irene Paula. Universidad de Buenos Aires. Facultad de Ingeniería. Departamento de Física. Grupo de Medios Porosos; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaElsevier France-Editions Scientifiques Medicales Elsevier2010-07info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/139157Auradou, Harold; Boschan, Alejandro; Chertcoff, Ricardo Héctor; D'angelo, María Verónica; Hulin, Jean-Pierre; et al.; Miscible transfer of solute in different model fractures: From random to multiscale wall roughness; Elsevier France-Editions Scientifiques Medicales Elsevier; Comptes Rendus Geoscience; 342; 7-8; 7-2010; 644-6521631-0713CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1631071309000601info:eu-repo/semantics/altIdentifier/doi/10.1016/j.crte.2009.03.003info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:33:56Zoai:ri.conicet.gov.ar:11336/139157instacron: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 09:33:56.936CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Miscible transfer of solute in different model fractures: From random to multiscale wall roughness
Transport miscible de solutés dans différentes fractures modèles : influence de la rugosité aléatoire ou multiéchelles
title Miscible transfer of solute in different model fractures: From random to multiscale wall roughness
spellingShingle Miscible transfer of solute in different model fractures: From random to multiscale wall roughness
Auradou, Harold
DISPERSION
FRACTURES
MULTISCALE
ROUGHNESS
SELF-AFFINE
SHEAR-THINNING
title_short Miscible transfer of solute in different model fractures: From random to multiscale wall roughness
title_full Miscible transfer of solute in different model fractures: From random to multiscale wall roughness
title_fullStr Miscible transfer of solute in different model fractures: From random to multiscale wall roughness
title_full_unstemmed Miscible transfer of solute in different model fractures: From random to multiscale wall roughness
title_sort Miscible transfer of solute in different model fractures: From random to multiscale wall roughness
dc.creator.none.fl_str_mv Auradou, Harold
Boschan, Alejandro
Chertcoff, Ricardo Héctor
D'angelo, María Verónica
Hulin, Jean-Pierre
Ippolito, Irene Paula
author Auradou, Harold
author_facet Auradou, Harold
Boschan, Alejandro
Chertcoff, Ricardo Héctor
D'angelo, María Verónica
Hulin, Jean-Pierre
Ippolito, Irene Paula
author_role author
author2 Boschan, Alejandro
Chertcoff, Ricardo Héctor
D'angelo, María Verónica
Hulin, Jean-Pierre
Ippolito, Irene Paula
author2_role author
author
author
author
author
dc.subject.none.fl_str_mv DISPERSION
FRACTURES
MULTISCALE
ROUGHNESS
SELF-AFFINE
SHEAR-THINNING
topic DISPERSION
FRACTURES
MULTISCALE
ROUGHNESS
SELF-AFFINE
SHEAR-THINNING
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.3
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Miscible tracer dispersion measurements in transparent model fractures with different types of wall roughness are reported. The nature (Fickian or not) of dispersion is determined by studying variations of the mixing front as a function of the distance travelled but also as a function of the lateral scale over which the tracer concentration is averaged. The dominant hydrodynamic dispersion mechanisms (velocity profile in the gap, velocity variations in the fracture plane) are established by comparing measurements using Newtonian and shear thinning fluids. For small monodisperse rugosities, front spreading is diffusive with a dominant geometrical dispersion (dispersion coefficient D ∝ Pe or constant dispersivity ld = D/U) at low Péclet numbers Pe; at higher Pe values, one has either ld ∝ Pe (i.e. Taylor dispersion) for obstacles of height smaller than the gap, or ld ∝ Pe0.35 for obstacles bridging the gap. For a self-affine multiscale roughness like in actual rocks and a relative shear displacement over(δ, →) of complementary walls, the aperture field is channelized in the direction perpendicular to over(δ, →). For a mean velocity over(U, →) parallel to the channels, the global front geometry reflects the velocity contrast between them and is predicted from the aperture field. For over(U, →) perpendicular to the channels, global front spreading is much reduced. Local spreading of the front thickness remains mostly controlled by Taylor dispersion except in the case of a very strong channelization parallel to over(U, →).
Fil: Auradou, Harold. Université Pierre et Marie Curie; Francia. Université Paris Sud; Francia
Fil: Boschan, Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Université Pierre et Marie Curie; Francia. Université Paris Sud; Francia. Universidad de Buenos Aires. Facultad de Ingeniería. Departamento de Física. Grupo de Medios Porosos; Argentina
Fil: Chertcoff, Ricardo Héctor. Universidad de Buenos Aires; Argentina
Fil: D'angelo, María Verónica. Université Pierre et Marie Curie; Francia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Université Paris Sud; Francia. Universidad de Buenos Aires. Facultad de Ingeniería. Departamento de Física. Grupo de Medios Porosos; Argentina
Fil: Hulin, Jean-Pierre. Université Pierre et Marie Curie; Francia. Université Paris Sud; Francia
Fil: Ippolito, Irene Paula. Universidad de Buenos Aires. Facultad de Ingeniería. Departamento de Física. Grupo de Medios Porosos; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
description Miscible tracer dispersion measurements in transparent model fractures with different types of wall roughness are reported. The nature (Fickian or not) of dispersion is determined by studying variations of the mixing front as a function of the distance travelled but also as a function of the lateral scale over which the tracer concentration is averaged. The dominant hydrodynamic dispersion mechanisms (velocity profile in the gap, velocity variations in the fracture plane) are established by comparing measurements using Newtonian and shear thinning fluids. For small monodisperse rugosities, front spreading is diffusive with a dominant geometrical dispersion (dispersion coefficient D ∝ Pe or constant dispersivity ld = D/U) at low Péclet numbers Pe; at higher Pe values, one has either ld ∝ Pe (i.e. Taylor dispersion) for obstacles of height smaller than the gap, or ld ∝ Pe0.35 for obstacles bridging the gap. For a self-affine multiscale roughness like in actual rocks and a relative shear displacement over(δ, →) of complementary walls, the aperture field is channelized in the direction perpendicular to over(δ, →). For a mean velocity over(U, →) parallel to the channels, the global front geometry reflects the velocity contrast between them and is predicted from the aperture field. For over(U, →) perpendicular to the channels, global front spreading is much reduced. Local spreading of the front thickness remains mostly controlled by Taylor dispersion except in the case of a very strong channelization parallel to over(U, →).
publishDate 2010
dc.date.none.fl_str_mv 2010-07
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/11336/139157
Auradou, Harold; Boschan, Alejandro; Chertcoff, Ricardo Héctor; D'angelo, María Verónica; Hulin, Jean-Pierre; et al.; Miscible transfer of solute in different model fractures: From random to multiscale wall roughness; Elsevier France-Editions Scientifiques Medicales Elsevier; Comptes Rendus Geoscience; 342; 7-8; 7-2010; 644-652
1631-0713
CONICET Digital
CONICET
url http://hdl.handle.net/11336/139157
identifier_str_mv Auradou, Harold; Boschan, Alejandro; Chertcoff, Ricardo Héctor; D'angelo, María Verónica; Hulin, Jean-Pierre; et al.; Miscible transfer of solute in different model fractures: From random to multiscale wall roughness; Elsevier France-Editions Scientifiques Medicales Elsevier; Comptes Rendus Geoscience; 342; 7-8; 7-2010; 644-652
1631-0713
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1631071309000601
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.crte.2009.03.003
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
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Elsevier France-Editions Scientifiques Medicales Elsevier
publisher.none.fl_str_mv Elsevier France-Editions Scientifiques Medicales Elsevier
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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