The use of monopole and dipole sources in crosswell surveying

Detalhes bibliográficos
Autor(a) principal: António, Julieta
Data de Publicação: 2004
Outros Autores: Tadeu, António
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10316/3983
https://doi.org/10.1016/S0926-9851(04)00053-9
Resumo: This paper implements a boundary element method (BEM) solution, formulated in the frequency domain, to simulate the crosswell S wave surveying technique. In this technique, one fluid-filled borehole hosts the source, and the other the receivers. The system is excited by a monopole or a dipole source placed near the first wall of the borehole wall, while the pressure field is recorded in the second borehole. The three-dimensional solution is computed as a summation of 2.5D solutions for different axial wave numbers.This model is used to assess the influence of the distance between boreholes and the material properties of the medium on the pressure field generated in the second borehole. Slow and fast formations are both simulated. It was found that the responses recorded the contribution of the non-dispersive body waves (the dilatational (P) and shear (S) waves) as well as the effect of dispersive waves associated with different wave modes. The final time solutions are thus intricate, exhibiting wave patterns that may make it difficult to interpret the arrival times of the refracted P and S waves.
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spelling The use of monopole and dipole sources in crosswell surveyingWave propagationMonopole and dipole sourcesCrosswell surveyingThis paper implements a boundary element method (BEM) solution, formulated in the frequency domain, to simulate the crosswell S wave surveying technique. In this technique, one fluid-filled borehole hosts the source, and the other the receivers. The system is excited by a monopole or a dipole source placed near the first wall of the borehole wall, while the pressure field is recorded in the second borehole. The three-dimensional solution is computed as a summation of 2.5D solutions for different axial wave numbers.This model is used to assess the influence of the distance between boreholes and the material properties of the medium on the pressure field generated in the second borehole. Slow and fast formations are both simulated. It was found that the responses recorded the contribution of the non-dispersive body waves (the dilatational (P) and shear (S) waves) as well as the effect of dispersive waves associated with different wave modes. The final time solutions are thus intricate, exhibiting wave patterns that may make it difficult to interpret the arrival times of the refracted P and S waves.http://www.sciencedirect.com/science/article/B6VFC-4D60GGB-2/1/08a72e22c052b611259a58399a80630a2004info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleaplication/PDFhttp://hdl.handle.net/10316/3983http://hdl.handle.net/10316/3983https://doi.org/10.1016/S0926-9851(04)00053-9engJournal of Applied Geophysics. 56:4 (2004) 231-245António, JulietaTadeu, Antónioinfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2020-11-06T16:59:55Zoai:estudogeral.uc.pt:10316/3983Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-19T20:57:12.460999Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv The use of monopole and dipole sources in crosswell surveying
title The use of monopole and dipole sources in crosswell surveying
spellingShingle The use of monopole and dipole sources in crosswell surveying
António, Julieta
Wave propagation
Monopole and dipole sources
Crosswell surveying
title_short The use of monopole and dipole sources in crosswell surveying
title_full The use of monopole and dipole sources in crosswell surveying
title_fullStr The use of monopole and dipole sources in crosswell surveying
title_full_unstemmed The use of monopole and dipole sources in crosswell surveying
title_sort The use of monopole and dipole sources in crosswell surveying
author António, Julieta
author_facet António, Julieta
Tadeu, António
author_role author
author2 Tadeu, António
author2_role author
dc.contributor.author.fl_str_mv António, Julieta
Tadeu, António
dc.subject.por.fl_str_mv Wave propagation
Monopole and dipole sources
Crosswell surveying
topic Wave propagation
Monopole and dipole sources
Crosswell surveying
description This paper implements a boundary element method (BEM) solution, formulated in the frequency domain, to simulate the crosswell S wave surveying technique. In this technique, one fluid-filled borehole hosts the source, and the other the receivers. The system is excited by a monopole or a dipole source placed near the first wall of the borehole wall, while the pressure field is recorded in the second borehole. The three-dimensional solution is computed as a summation of 2.5D solutions for different axial wave numbers.This model is used to assess the influence of the distance between boreholes and the material properties of the medium on the pressure field generated in the second borehole. Slow and fast formations are both simulated. It was found that the responses recorded the contribution of the non-dispersive body waves (the dilatational (P) and shear (S) waves) as well as the effect of dispersive waves associated with different wave modes. The final time solutions are thus intricate, exhibiting wave patterns that may make it difficult to interpret the arrival times of the refracted P and S waves.
publishDate 2004
dc.date.none.fl_str_mv 2004
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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status_str publishedVersion
dc.identifier.uri.fl_str_mv http://hdl.handle.net/10316/3983
http://hdl.handle.net/10316/3983
https://doi.org/10.1016/S0926-9851(04)00053-9
url http://hdl.handle.net/10316/3983
https://doi.org/10.1016/S0926-9851(04)00053-9
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Journal of Applied Geophysics. 56:4 (2004) 231-245
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eu_rights_str_mv openAccess
dc.format.none.fl_str_mv aplication/PDF
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