A variational formulation to image inclusions in 2D travel time cross hole tomography
Autor(a) principal: | |
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Data de Publicação: | 2003 |
Outros Autores: | |
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=S0102-261X2003000300006 |
Resumo: | It was developed a simple and high speed method with the purpose to model inclusions of irregular forms (simply connected and convex domain) in the context of cross hole travel time 2D tomography. The extension to 3D can be easily implemented and is not covered in this paper. The following assumptions were made: a) Homogeneus host medium (therefore straight ray propagation assumed) b) Homogeneus inclusion. c) Not very high velocity contrast between host medium (V1) and the inclusion (V2). The algorithm calculate the host velocity V1 considering the (straight) ray between source 1 and receiver 1, and considering that this ray not intersect the anomaly. Then the velocity V2 of the inclusion is estimated upon determining the difference deltat among measured times source i - receiver j and corresponding calculated times. If the global difference is negative signifies that V2 will be greater than V1 and viceversa. The small values of deltat are treated as outliers and therefore eliminated. The last initial parameters needed by the algorithm are the coordinates of the center of the inclusion, which are estimated by a graphical procedure. Afterwards the program approximates the contour of the inclusion using the Nelder-Mead 'simplex' algorithm. At last the perfomance of the algorithm was applied with real data. |
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A variational formulation to image inclusions in 2D travel time cross hole tomographyTomographyCross HoleSimplex DownhillVariationalNelder MeadIt was developed a simple and high speed method with the purpose to model inclusions of irregular forms (simply connected and convex domain) in the context of cross hole travel time 2D tomography. The extension to 3D can be easily implemented and is not covered in this paper. The following assumptions were made: a) Homogeneus host medium (therefore straight ray propagation assumed) b) Homogeneus inclusion. c) Not very high velocity contrast between host medium (V1) and the inclusion (V2). The algorithm calculate the host velocity V1 considering the (straight) ray between source 1 and receiver 1, and considering that this ray not intersect the anomaly. Then the velocity V2 of the inclusion is estimated upon determining the difference deltat among measured times source i - receiver j and corresponding calculated times. If the global difference is negative signifies that V2 will be greater than V1 and viceversa. The small values of deltat are treated as outliers and therefore eliminated. The last initial parameters needed by the algorithm are the coordinates of the center of the inclusion, which are estimated by a graphical procedure. Afterwards the program approximates the contour of the inclusion using the Nelder-Mead 'simplex' algorithm. At last the perfomance of the algorithm was applied with real data.Sociedade Brasileira de Geofísica2003-12-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-261X2003000300006Revista Brasileira de Geofísica v.21 n.3 2003reponame:Revista Brasileira de Geofísica (Online)instname:Sociedade Brasileira de Geofísica (SBG)instacron:SBG10.1590/S0102-261X2003000300006info:eu-repo/semantics/openAccessImhof,Armando LuisCalvo,Carlos Adolfoeng2007-01-24T00:00:00Zoai:scielo:S0102-261X2003000300006Revistahttp://www.scielo.br/rbgONGhttps://old.scielo.br/oai/scielo-oai.php||sbgf@sbgf.org.br1809-45110102-261Xopendoar:2007-01-24T00:00Revista Brasileira de Geofísica (Online) - Sociedade Brasileira de Geofísica (SBG)false |
dc.title.none.fl_str_mv |
A variational formulation to image inclusions in 2D travel time cross hole tomography |
title |
A variational formulation to image inclusions in 2D travel time cross hole tomography |
spellingShingle |
A variational formulation to image inclusions in 2D travel time cross hole tomography Imhof,Armando Luis Tomography Cross Hole Simplex Downhill Variational Nelder Mead |
title_short |
A variational formulation to image inclusions in 2D travel time cross hole tomography |
title_full |
A variational formulation to image inclusions in 2D travel time cross hole tomography |
title_fullStr |
A variational formulation to image inclusions in 2D travel time cross hole tomography |
title_full_unstemmed |
A variational formulation to image inclusions in 2D travel time cross hole tomography |
title_sort |
A variational formulation to image inclusions in 2D travel time cross hole tomography |
author |
Imhof,Armando Luis |
author_facet |
Imhof,Armando Luis Calvo,Carlos Adolfo |
author_role |
author |
author2 |
Calvo,Carlos Adolfo |
author2_role |
author |
dc.contributor.author.fl_str_mv |
Imhof,Armando Luis Calvo,Carlos Adolfo |
dc.subject.por.fl_str_mv |
Tomography Cross Hole Simplex Downhill Variational Nelder Mead |
topic |
Tomography Cross Hole Simplex Downhill Variational Nelder Mead |
description |
It was developed a simple and high speed method with the purpose to model inclusions of irregular forms (simply connected and convex domain) in the context of cross hole travel time 2D tomography. The extension to 3D can be easily implemented and is not covered in this paper. The following assumptions were made: a) Homogeneus host medium (therefore straight ray propagation assumed) b) Homogeneus inclusion. c) Not very high velocity contrast between host medium (V1) and the inclusion (V2). The algorithm calculate the host velocity V1 considering the (straight) ray between source 1 and receiver 1, and considering that this ray not intersect the anomaly. Then the velocity V2 of the inclusion is estimated upon determining the difference deltat among measured times source i - receiver j and corresponding calculated times. If the global difference is negative signifies that V2 will be greater than V1 and viceversa. The small values of deltat are treated as outliers and therefore eliminated. The last initial parameters needed by the algorithm are the coordinates of the center of the inclusion, which are estimated by a graphical procedure. Afterwards the program approximates the contour of the inclusion using the Nelder-Mead 'simplex' algorithm. At last the perfomance of the algorithm was applied with real data. |
publishDate |
2003 |
dc.date.none.fl_str_mv |
2003-12-01 |
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=S0102-261X2003000300006 |
url |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-261X2003000300006 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
10.1590/S0102-261X2003000300006 |
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.21 n.3 2003 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 |
_version_ |
1754820936342700032 |