Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves

In Vertical Seismic Profiling tube waves are generated by compressional waves impinging on subsurface fractures or permeable zones. The amplitude of tube waves is dependent upon the formation permeability, the length of the fracture, and on the source frequency. The generation of tube waves is f...

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Main Authors: Beydoun, W. B., Cheng, C. H., Toksoz, M. N.
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/1721.1/75049
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author Beydoun, W. B.
Cheng, C. H.
Toksoz, M. N.
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Beydoun, W. B.
Cheng, C. H.
Toksoz, M. N.
author_sort Beydoun, W. B.
collection MIT
description In Vertical Seismic Profiling tube waves are generated by compressional waves impinging on subsurface fractures or permeable zones. The amplitude of tube waves is dependent upon the formation permeability, the length of the fracture, and on the source frequency. The generation of tube waves is formulated theoretically and the relative effects of these parameters are studied individually. Field examples are shown for open fractures in granite. From tube wave amplitudes normalized to P-wave amplitudes, calculated permeabilities are on the order of 400 millidarcys.
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spelling mit-1721.1/750492019-04-09T16:14:41Z Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves Beydoun, W. B. Cheng, C. H. Toksoz, M. N. Massachusetts Institute of Technology. Earth Resources Laboratory Beydoun, W. B. Cheng, C. H. Toksoz, M. N. In Vertical Seismic Profiling tube waves are generated by compressional waves impinging on subsurface fractures or permeable zones. The amplitude of tube waves is dependent upon the formation permeability, the length of the fracture, and on the source frequency. The generation of tube waves is formulated theoretically and the relative effects of these parameters are studied individually. Field examples are shown for open fractures in granite. From tube wave amplitudes normalized to P-wave amplitudes, calculated permeabilities are on the order of 400 millidarcys. 2012-11-27T20:28:07Z 2012-11-27T20:28:07Z 1983 Technical Report http://hdl.handle.net/1721.1/75049 Earth Resources Laboratory Industry Consortia Annual Report;1983-10 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle Beydoun, W. B.
Cheng, C. H.
Toksoz, M. N.
Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves
title Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves
title_full Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves
title_fullStr Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves
title_full_unstemmed Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves
title_short Detection Of Subsurface Fractures And Permeable Zones By The Analysis Of Tube Waves
title_sort detection of subsurface fractures and permeable zones by the analysis of tube waves
url http://hdl.handle.net/1721.1/75049
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