Free Pipe Effects On Guided Wave Propagation

The effects of free pipe on the pseudo-Rayleigh and Stoneley waves are studied by introducing a fluid annulus between the casing and cement layers of a cased borehole model. The existence of a fluid annulus region results in a second Stoneley mode being generated which propagates primarily in the...

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Main Authors: Burns, D. R., Cheng, C. H.
Other Authors: Massachusetts Institute of Technology. Earth Resources Laboratory
Format: Technical Report
Published: Massachusetts Institute of Technology. Earth Resources Laboratory 2019
Online Access:https://mit.atmire.com/handle/1721.1/121144
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author Burns, D. R.
Cheng, C. H.
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Burns, D. R.
Cheng, C. H.
author_sort Burns, D. R.
collection MIT
description The effects of free pipe on the pseudo-Rayleigh and Stoneley waves are studied by introducing a fluid annulus between the casing and cement layers of a cased borehole model. The existence of a fluid annulus region results in a second Stoneley mode being generated which propagates primarily in the annulus. The propagation and attenuation of this second mode are controlled by the fluid annulus, cement, and formation properties. The primary or central Stoneley mode becomes decoupled from the effects of formation when the free pipe situation exists, and its propagation and attenuation are controlled by the central fluid and casing properties only. The amplitude of the second Stoneley mode increases as the annulus thickness increases, but in most cases is an order of magnitude less than the primary mode amplitude. The pseudo-Rayleigh wave becomes more dispersive as the annulus region increases in thickness.
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spelling mit-1721.1/1211442019-04-11T07:12:34Z Free Pipe Effects On Guided Wave Propagation Burns, D. R. Cheng, C. H. Massachusetts Institute of Technology. Earth Resources Laboratory Burns, D. R. Cheng, C. H. The effects of free pipe on the pseudo-Rayleigh and Stoneley waves are studied by introducing a fluid annulus between the casing and cement layers of a cased borehole model. The existence of a fluid annulus region results in a second Stoneley mode being generated which propagates primarily in the annulus. The propagation and attenuation of this second mode are controlled by the fluid annulus, cement, and formation properties. The primary or central Stoneley mode becomes decoupled from the effects of formation when the free pipe situation exists, and its propagation and attenuation are controlled by the central fluid and casing properties only. The amplitude of the second Stoneley mode increases as the annulus thickness increases, but in most cases is an order of magnitude less than the primary mode amplitude. The pseudo-Rayleigh wave becomes more dispersive as the annulus region increases in thickness. Massachusetts Institute of Technology. Full Waveform Acoustic Logging Consortium 2019-04-04T10:09:02Z 2019-04-04T10:09:02Z 1986 Technical Report https://mit.atmire.com/handle/1721.1/121144 Earth Resources Laboratory Industry Consortia Annual Report;1986-03 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle Burns, D. R.
Cheng, C. H.
Free Pipe Effects On Guided Wave Propagation
title Free Pipe Effects On Guided Wave Propagation
title_full Free Pipe Effects On Guided Wave Propagation
title_fullStr Free Pipe Effects On Guided Wave Propagation
title_full_unstemmed Free Pipe Effects On Guided Wave Propagation
title_short Free Pipe Effects On Guided Wave Propagation
title_sort free pipe effects on guided wave propagation
url https://mit.atmire.com/handle/1721.1/121144
work_keys_str_mv AT burnsdr freepipeeffectsonguidedwavepropagation
AT chengch freepipeeffectsonguidedwavepropagation