Tube Waves, Seismic Waves And Effective Sources

A simple asymptotic analysis, based on the smallness of the ratio of the borehole radius to the wavelength, reveals the interaction between tube waves and seismic waves. The pressure field in a tube wave acts as a secondary source of seismic waves and conversely an incoming seismic wave excites a...

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Main Authors: Burridge, Robert, Kostek, Sergio, Kurkjian, Andrew L.
Other Authors: Massachusetts Institute of Technology. Earth Resources Laboratory
Format: Technical Report
Published: Massachusetts Institute of Technology. Earth Resources Laboratory 2012
Online Access:http://hdl.handle.net/1721.1/75206
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author Burridge, Robert
Kostek, Sergio
Kurkjian, Andrew L.
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Burridge, Robert
Kostek, Sergio
Kurkjian, Andrew L.
author_sort Burridge, Robert
collection MIT
description A simple asymptotic analysis, based on the smallness of the ratio of the borehole radius to the wavelength, reveals the interaction between tube waves and seismic waves. The pressure field in a tube wave acts as a secondary source of seismic waves and conversely an incoming seismic wave excites a tube wave. The asymptotic analysis leads to a characterization of these sources in terms of the solution to two-dimensional elastostatic problems. These may be solved exactly when the borehole has an elliptical cross-section even in an anisotropic formation. Also the borehole need not be straight provided that its radius of curvature is large compared with a wavelength.
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spelling mit-1721.1/752062019-04-11T04:49:19Z Tube Waves, Seismic Waves And Effective Sources Burridge, Robert Kostek, Sergio Kurkjian, Andrew L. Massachusetts Institute of Technology. Earth Resources Laboratory Burridge, Robert Kostek, Sergio A simple asymptotic analysis, based on the smallness of the ratio of the borehole radius to the wavelength, reveals the interaction between tube waves and seismic waves. The pressure field in a tube wave acts as a secondary source of seismic waves and conversely an incoming seismic wave excites a tube wave. The asymptotic analysis leads to a characterization of these sources in terms of the solution to two-dimensional elastostatic problems. These may be solved exactly when the borehole has an elliptical cross-section even in an anisotropic formation. Also the borehole need not be straight provided that its radius of curvature is large compared with a wavelength. 2012-12-04T16:51:38Z 2012-12-04T16:51:38Z 1993 Technical Report http://hdl.handle.net/1721.1/75206 Earth Resources Laboratory Industry Consortia Annual Report;1993-09 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle Burridge, Robert
Kostek, Sergio
Kurkjian, Andrew L.
Tube Waves, Seismic Waves And Effective Sources
title Tube Waves, Seismic Waves And Effective Sources
title_full Tube Waves, Seismic Waves And Effective Sources
title_fullStr Tube Waves, Seismic Waves And Effective Sources
title_full_unstemmed Tube Waves, Seismic Waves And Effective Sources
title_short Tube Waves, Seismic Waves And Effective Sources
title_sort tube waves seismic waves and effective sources
url http://hdl.handle.net/1721.1/75206
work_keys_str_mv AT burridgerobert tubewavesseismicwavesandeffectivesources
AT kosteksergio tubewavesseismicwavesandeffectivesources
AT kurkjianandrewl tubewavesseismicwavesandeffectivesources