Time-lapse critical reflection: does it really work in seismic monitoring of low porosity and high effective stress conditions?

Detalhes bibliográficos
Autor(a) principal: Artola,Fredy Alex Villaorduña
Data de Publicação: 2008
Outros Autores: Bastante,Vladimir Alvarado, Figueiró,Wilson Mouzer
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Revista Brasileira de Geofísica (Online)
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-261X2008000300006
Resumo: We present an evaluation of the time lapse critical reflection method from the point of view of sensitivity and uncertainty analysis. The purpose of this analysis is to establish the link between changes in the p-wave velocity in the reservoir, due to fluid substitution, and the critical distance (X C), a dynamic parameter. Two static parameters of the overburden are considered in the analysis: its thickness and its effective or equivalent P-wave velocity. Stochastic uncertainty analysis by means of Monte Carlo simulations was carried out to determine the sensitivity of X C to velocity contrast between that of the reservoir and the corresponding one to the overburden (incident medium). Results show that the effect of the velocity values in each medium, overburden and reservoir (reflecting medium), on estimates of X C depends on the velocity contrast between the two media. It turns out that the greater the velocity difference between the two media, the greater the effects associated with the reservoir P-wave velocity. On the other hand, the dependence of X C on overburden velocity (Vrms of the incident medium) is just the opposite. From the inversion viewpoint, predicting changes of the reservoir P-wave velocity from changes in critical distance is strongly dependent of the uncertainty in the initial estimate of the reservoir P-wave velocity, followed by degree of importance by the uncertainty in the overburden velocity. Other sources of uncertainty in this analysis turned out to be negligible. Geomechanical effects have not been accounted for in this analysis.
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spelling Time-lapse critical reflection: does it really work in seismic monitoring of low porosity and high effective stress conditions?critical reflectiontime-lapse seismicreservoir monitoringsensitivity analysisWe present an evaluation of the time lapse critical reflection method from the point of view of sensitivity and uncertainty analysis. The purpose of this analysis is to establish the link between changes in the p-wave velocity in the reservoir, due to fluid substitution, and the critical distance (X C), a dynamic parameter. Two static parameters of the overburden are considered in the analysis: its thickness and its effective or equivalent P-wave velocity. Stochastic uncertainty analysis by means of Monte Carlo simulations was carried out to determine the sensitivity of X C to velocity contrast between that of the reservoir and the corresponding one to the overburden (incident medium). Results show that the effect of the velocity values in each medium, overburden and reservoir (reflecting medium), on estimates of X C depends on the velocity contrast between the two media. It turns out that the greater the velocity difference between the two media, the greater the effects associated with the reservoir P-wave velocity. On the other hand, the dependence of X C on overburden velocity (Vrms of the incident medium) is just the opposite. From the inversion viewpoint, predicting changes of the reservoir P-wave velocity from changes in critical distance is strongly dependent of the uncertainty in the initial estimate of the reservoir P-wave velocity, followed by degree of importance by the uncertainty in the overburden velocity. Other sources of uncertainty in this analysis turned out to be negligible. Geomechanical effects have not been accounted for in this analysis.Sociedade Brasileira de Geofísica2008-09-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-261X2008000300006Revista Brasileira de Geofísica v.26 n.3 2008reponame:Revista Brasileira de Geofísica (Online)instname:Sociedade Brasileira de Geofísica (SBG)instacron:SBG10.1590/S0102-261X2008000300006info:eu-repo/semantics/openAccessArtola,Fredy Alex VillaorduñaBastante,Vladimir AlvaradoFigueiró,Wilson Mouzereng2008-12-12T00:00:00Zoai:scielo:S0102-261X2008000300006Revistahttp://www.scielo.br/rbgONGhttps://old.scielo.br/oai/scielo-oai.php||sbgf@sbgf.org.br1809-45110102-261Xopendoar:2008-12-12T00:00Revista Brasileira de Geofísica (Online) - Sociedade Brasileira de Geofísica (SBG)false
dc.title.none.fl_str_mv Time-lapse critical reflection: does it really work in seismic monitoring of low porosity and high effective stress conditions?
title Time-lapse critical reflection: does it really work in seismic monitoring of low porosity and high effective stress conditions?
spellingShingle Time-lapse critical reflection: does it really work in seismic monitoring of low porosity and high effective stress conditions?
Artola,Fredy Alex Villaorduña
critical reflection
time-lapse seismic
reservoir monitoring
sensitivity analysis
title_short Time-lapse critical reflection: does it really work in seismic monitoring of low porosity and high effective stress conditions?
title_full Time-lapse critical reflection: does it really work in seismic monitoring of low porosity and high effective stress conditions?
title_fullStr Time-lapse critical reflection: does it really work in seismic monitoring of low porosity and high effective stress conditions?
title_full_unstemmed Time-lapse critical reflection: does it really work in seismic monitoring of low porosity and high effective stress conditions?
title_sort Time-lapse critical reflection: does it really work in seismic monitoring of low porosity and high effective stress conditions?
author Artola,Fredy Alex Villaorduña
author_facet Artola,Fredy Alex Villaorduña
Bastante,Vladimir Alvarado
Figueiró,Wilson Mouzer
author_role author
author2 Bastante,Vladimir Alvarado
Figueiró,Wilson Mouzer
author2_role author
author
dc.contributor.author.fl_str_mv Artola,Fredy Alex Villaorduña
Bastante,Vladimir Alvarado
Figueiró,Wilson Mouzer
dc.subject.por.fl_str_mv critical reflection
time-lapse seismic
reservoir monitoring
sensitivity analysis
topic critical reflection
time-lapse seismic
reservoir monitoring
sensitivity analysis
description We present an evaluation of the time lapse critical reflection method from the point of view of sensitivity and uncertainty analysis. The purpose of this analysis is to establish the link between changes in the p-wave velocity in the reservoir, due to fluid substitution, and the critical distance (X C), a dynamic parameter. Two static parameters of the overburden are considered in the analysis: its thickness and its effective or equivalent P-wave velocity. Stochastic uncertainty analysis by means of Monte Carlo simulations was carried out to determine the sensitivity of X C to velocity contrast between that of the reservoir and the corresponding one to the overburden (incident medium). Results show that the effect of the velocity values in each medium, overburden and reservoir (reflecting medium), on estimates of X C depends on the velocity contrast between the two media. It turns out that the greater the velocity difference between the two media, the greater the effects associated with the reservoir P-wave velocity. On the other hand, the dependence of X C on overburden velocity (Vrms of the incident medium) is just the opposite. From the inversion viewpoint, predicting changes of the reservoir P-wave velocity from changes in critical distance is strongly dependent of the uncertainty in the initial estimate of the reservoir P-wave velocity, followed by degree of importance by the uncertainty in the overburden velocity. Other sources of uncertainty in this analysis turned out to be negligible. Geomechanical effects have not been accounted for in this analysis.
publishDate 2008
dc.date.none.fl_str_mv 2008-09-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-261X2008000300006
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-261X2008000300006
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/S0102-261X2008000300006
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv text/html
dc.publisher.none.fl_str_mv Sociedade Brasileira de Geofísica
publisher.none.fl_str_mv Sociedade Brasileira de Geofísica
dc.source.none.fl_str_mv Revista Brasileira de Geofísica v.26 n.3 2008
reponame:Revista Brasileira de Geofísica (Online)
instname:Sociedade Brasileira de Geofísica (SBG)
instacron:SBG
instname_str Sociedade Brasileira de Geofísica (SBG)
instacron_str SBG
institution SBG
reponame_str Revista Brasileira de Geofísica (Online)
collection Revista Brasileira de Geofísica (Online)
repository.name.fl_str_mv Revista Brasileira de Geofísica (Online) - Sociedade Brasileira de Geofísica (SBG)
repository.mail.fl_str_mv ||sbgf@sbgf.org.br
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