Wave motion between two fluid-filled boreholes in an elastic medium

Bibliographic Details
Main Author: Tadeu, António
Publication Date: 2002
Other Authors: Godinho, Luís, Santos, Paulo
Format: Article
Language: eng
Source: Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
Download full: https://hdl.handle.net/10316/4024
https://doi.org/10.1016/S0955-7997(01)00088-1
Summary: The boundary element method (BEM) is used to fully simulate the propagation of waves between two fluid-filled boreholes. The sources are placed in one of the boreholes while the receivers are placed in the other. This model is frequently used in cross-hole seismic prospecting techniques to assess the characteristics of the elastic medium between the two boreholes. This work studies the dependence of the wave propagation patterns on the distance between the source and the receiver, their location and orientation relative to the axis of a circular borehole and type of elastic formation (fast and slow formations). In addition, this BEM model is used to compute the influence of the deformed boreholes whose cross-section is not circular. Both the spectra responses and the time-domain responses are computed to elucidate the main physical features of the problem solved.
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spelling Wave motion between two fluid-filled boreholes in an elastic mediumCross-hole seismic prospecting techniquesWave propagationBoundary element methodTwo-and-a-half-dimensional problemThe boundary element method (BEM) is used to fully simulate the propagation of waves between two fluid-filled boreholes. The sources are placed in one of the boreholes while the receivers are placed in the other. This model is frequently used in cross-hole seismic prospecting techniques to assess the characteristics of the elastic medium between the two boreholes. This work studies the dependence of the wave propagation patterns on the distance between the source and the receiver, their location and orientation relative to the axis of a circular borehole and type of elastic formation (fast and slow formations). In addition, this BEM model is used to compute the influence of the deformed boreholes whose cross-section is not circular. Both the spectra responses and the time-domain responses are computed to elucidate the main physical features of the problem solved.http://www.sciencedirect.com/science/article/B6V2N-44VDYFD-1/1/694be0b9fc1ef415b7449ec2defd9d082002info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleaplication/PDFhttps://hdl.handle.net/10316/4024https://hdl.handle.net/10316/4024https://doi.org/10.1016/S0955-7997(01)00088-1engEngineering Analysis with Boundary Elements. 26:2 (2002) 101-117Tadeu, AntónioGodinho, LuísSantos, Pauloinfo:eu-repo/semantics/openAccessreponame:Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)instname:FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiainstacron:RCAAP2020-11-06T16:59:55Zoai:estudogeral.uc.pt:10316/4024Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireinfo@rcaap.ptopendoar:https://opendoar.ac.uk/repository/71602025-05-29T05:17:11.516007Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) - FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiafalse
dc.title.none.fl_str_mv Wave motion between two fluid-filled boreholes in an elastic medium
title Wave motion between two fluid-filled boreholes in an elastic medium
spellingShingle Wave motion between two fluid-filled boreholes in an elastic medium
Tadeu, António
Cross-hole seismic prospecting techniques
Wave propagation
Boundary element method
Two-and-a-half-dimensional problem
title_short Wave motion between two fluid-filled boreholes in an elastic medium
title_full Wave motion between two fluid-filled boreholes in an elastic medium
title_fullStr Wave motion between two fluid-filled boreholes in an elastic medium
title_full_unstemmed Wave motion between two fluid-filled boreholes in an elastic medium
title_sort Wave motion between two fluid-filled boreholes in an elastic medium
author Tadeu, António
author_facet Tadeu, António
Godinho, Luís
Santos, Paulo
author_role author
author2 Godinho, Luís
Santos, Paulo
author2_role author
author
dc.contributor.author.fl_str_mv Tadeu, António
Godinho, Luís
Santos, Paulo
dc.subject.por.fl_str_mv Cross-hole seismic prospecting techniques
Wave propagation
Boundary element method
Two-and-a-half-dimensional problem
topic Cross-hole seismic prospecting techniques
Wave propagation
Boundary element method
Two-and-a-half-dimensional problem
description The boundary element method (BEM) is used to fully simulate the propagation of waves between two fluid-filled boreholes. The sources are placed in one of the boreholes while the receivers are placed in the other. This model is frequently used in cross-hole seismic prospecting techniques to assess the characteristics of the elastic medium between the two boreholes. This work studies the dependence of the wave propagation patterns on the distance between the source and the receiver, their location and orientation relative to the axis of a circular borehole and type of elastic formation (fast and slow formations). In addition, this BEM model is used to compute the influence of the deformed boreholes whose cross-section is not circular. Both the spectra responses and the time-domain responses are computed to elucidate the main physical features of the problem solved.
publishDate 2002
dc.date.none.fl_str_mv 2002
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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dc.identifier.uri.fl_str_mv https://hdl.handle.net/10316/4024
https://hdl.handle.net/10316/4024
https://doi.org/10.1016/S0955-7997(01)00088-1
url https://hdl.handle.net/10316/4024
https://doi.org/10.1016/S0955-7997(01)00088-1
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Engineering Analysis with Boundary Elements. 26:2 (2002) 101-117
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