Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulations
- Autores
- Rubino, Jorge German; Velis, Danilo Ruben
- Año de publicación
- 2011
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- We studied the seismic attenuation and velocity dispersion effects produced by wave-induced fluid flow in weakly consolidated sandstones containing patchy carbon dioxide CO ð Þ2 -brine distributions. The analysis also focuses on the velocity pushdown because of the presence of this gas, as well as on the role of the wave-induced fluid flow (mesoscopic) effects on the amplitude variation with angle (AVA) seismic response of thin layers containing CO2, such as those found at the Utsira Sand, Sleipner field, offshore Norway. We found that this loss mechanism may play a key role on conventional surface seismic data, suggesting that further data analysis may provide useful information on the characteristics of the fluid distributions in these environments. Numerical experiments let us observe that although mesoscopic effects can be very significant in this kind of media, the seismic response of a given isolated thin layer computed considering such effects is very similar to that of a homogeneous elastic thin layer with a compressional velocity equal to that of the original porous rock averaged in the effective data bandwidth. This suggests that the thin-bed prestack spectral inversion method published by the authors could be used to estimate representative compressional velocities and layer thicknesses in these environments. In effect, results using realistic synthetic prestack seismic data show that isolated CO2- bearing thin beds can be characterized in terms of their thicknesses and representative compressional velocities. This information can be qualitatively related to CO2 saturations and volumes; thus, the prestack spectral inversion method could find application in the monitoring of the evolution of CO2 plumes at injection sites similar to that at the Sleipner field.
Fil: Rubino, Jorge German. 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; Argentina. Universite de Lausanne; Suiza
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; Argentina - Materia
-
Thin-bed
Patchy saturation
CO2 storage
Mesoscopic effects - 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:11336/198175
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Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulationsRubino, Jorge GermanVelis, Danilo RubenThin-bedPatchy saturationCO2 storageMesoscopic effectshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1We studied the seismic attenuation and velocity dispersion effects produced by wave-induced fluid flow in weakly consolidated sandstones containing patchy carbon dioxide CO ð Þ2 -brine distributions. The analysis also focuses on the velocity pushdown because of the presence of this gas, as well as on the role of the wave-induced fluid flow (mesoscopic) effects on the amplitude variation with angle (AVA) seismic response of thin layers containing CO2, such as those found at the Utsira Sand, Sleipner field, offshore Norway. We found that this loss mechanism may play a key role on conventional surface seismic data, suggesting that further data analysis may provide useful information on the characteristics of the fluid distributions in these environments. Numerical experiments let us observe that although mesoscopic effects can be very significant in this kind of media, the seismic response of a given isolated thin layer computed considering such effects is very similar to that of a homogeneous elastic thin layer with a compressional velocity equal to that of the original porous rock averaged in the effective data bandwidth. This suggests that the thin-bed prestack spectral inversion method published by the authors could be used to estimate representative compressional velocities and layer thicknesses in these environments. In effect, results using realistic synthetic prestack seismic data show that isolated CO2- bearing thin beds can be characterized in terms of their thicknesses and representative compressional velocities. This information can be qualitatively related to CO2 saturations and volumes; thus, the prestack spectral inversion method could find application in the monitoring of the evolution of CO2 plumes at injection sites similar to that at the Sleipner field.Fil: Rubino, Jorge German. 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; Argentina. Universite de Lausanne; SuizaFil: 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; ArgentinaSociety of Exploration Geophysicists2011-06info: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/11336/198175Rubino, Jorge German; Velis, Danilo Ruben; Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulations; Society of Exploration Geophysicists; Geophysics; 76; 3; 6-2011; 57-670016-80331942-2156CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://fcaglp.fcaglp.unlp.edu.ar/~velis/papers/CapaFinaCO2_Geop11.pdfinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:32:46Zoai:ri.conicet.gov.ar:11336/198175instacron: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 09:32:47.252CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulations |
title |
Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulations |
spellingShingle |
Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulations Rubino, Jorge German Thin-bed Patchy saturation CO2 storage Mesoscopic effects |
title_short |
Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulations |
title_full |
Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulations |
title_fullStr |
Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulations |
title_full_unstemmed |
Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulations |
title_sort |
Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulations |
dc.creator.none.fl_str_mv |
Rubino, Jorge German Velis, Danilo Ruben |
author |
Rubino, Jorge German |
author_facet |
Rubino, Jorge German Velis, Danilo Ruben |
author_role |
author |
author2 |
Velis, Danilo Ruben |
author2_role |
author |
dc.subject.none.fl_str_mv |
Thin-bed Patchy saturation CO2 storage Mesoscopic effects |
topic |
Thin-bed Patchy saturation CO2 storage Mesoscopic effects |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
We studied the seismic attenuation and velocity dispersion effects produced by wave-induced fluid flow in weakly consolidated sandstones containing patchy carbon dioxide CO ð Þ2 -brine distributions. The analysis also focuses on the velocity pushdown because of the presence of this gas, as well as on the role of the wave-induced fluid flow (mesoscopic) effects on the amplitude variation with angle (AVA) seismic response of thin layers containing CO2, such as those found at the Utsira Sand, Sleipner field, offshore Norway. We found that this loss mechanism may play a key role on conventional surface seismic data, suggesting that further data analysis may provide useful information on the characteristics of the fluid distributions in these environments. Numerical experiments let us observe that although mesoscopic effects can be very significant in this kind of media, the seismic response of a given isolated thin layer computed considering such effects is very similar to that of a homogeneous elastic thin layer with a compressional velocity equal to that of the original porous rock averaged in the effective data bandwidth. This suggests that the thin-bed prestack spectral inversion method published by the authors could be used to estimate representative compressional velocities and layer thicknesses in these environments. In effect, results using realistic synthetic prestack seismic data show that isolated CO2- bearing thin beds can be characterized in terms of their thicknesses and representative compressional velocities. This information can be qualitatively related to CO2 saturations and volumes; thus, the prestack spectral inversion method could find application in the monitoring of the evolution of CO2 plumes at injection sites similar to that at the Sleipner field. Fil: Rubino, Jorge German. 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; Argentina. Universite de Lausanne; Suiza 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; Argentina |
description |
We studied the seismic attenuation and velocity dispersion effects produced by wave-induced fluid flow in weakly consolidated sandstones containing patchy carbon dioxide CO ð Þ2 -brine distributions. The analysis also focuses on the velocity pushdown because of the presence of this gas, as well as on the role of the wave-induced fluid flow (mesoscopic) effects on the amplitude variation with angle (AVA) seismic response of thin layers containing CO2, such as those found at the Utsira Sand, Sleipner field, offshore Norway. We found that this loss mechanism may play a key role on conventional surface seismic data, suggesting that further data analysis may provide useful information on the characteristics of the fluid distributions in these environments. Numerical experiments let us observe that although mesoscopic effects can be very significant in this kind of media, the seismic response of a given isolated thin layer computed considering such effects is very similar to that of a homogeneous elastic thin layer with a compressional velocity equal to that of the original porous rock averaged in the effective data bandwidth. This suggests that the thin-bed prestack spectral inversion method published by the authors could be used to estimate representative compressional velocities and layer thicknesses in these environments. In effect, results using realistic synthetic prestack seismic data show that isolated CO2- bearing thin beds can be characterized in terms of their thicknesses and representative compressional velocities. This information can be qualitatively related to CO2 saturations and volumes; thus, the prestack spectral inversion method could find application in the monitoring of the evolution of CO2 plumes at injection sites similar to that at the Sleipner field. |
publishDate |
2011 |
dc.date.none.fl_str_mv |
2011-06 |
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/11336/198175 Rubino, Jorge German; Velis, Danilo Ruben; Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulations; Society of Exploration Geophysicists; Geophysics; 76; 3; 6-2011; 57-67 0016-8033 1942-2156 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/198175 |
identifier_str_mv |
Rubino, Jorge German; Velis, Danilo Ruben; Seismic characterization of thin beds containing patchy carbon dioxide-brine distributions: A study based on numerical simulations; Society of Exploration Geophysicists; Geophysics; 76; 3; 6-2011; 57-67 0016-8033 1942-2156 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/http://fcaglp.fcaglp.unlp.edu.ar/~velis/papers/CapaFinaCO2_Geop11.pdf |
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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1844613002047782912 |
score |
13.070432 |