The effect of stresses on the sound velocity in rocks: Theory of Acoustoelasticity and Experimental Measurements

The theory of acoustoelasticity provides direct link between the change of elastic wave velocities and residual stresses in solids. The general theory of acoustoelasticity is reviewed. A number of experimental measurements of the effect of stresses on the sound velocities in various types of rocks a...

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Main Authors: Huang, Xiaojun, Burns, Daniel R., Toksoz, M. Nafi
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/1721.1/68599
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author Huang, Xiaojun
Burns, Daniel R.
Toksoz, M. Nafi
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Huang, Xiaojun
Burns, Daniel R.
Toksoz, M. Nafi
author_sort Huang, Xiaojun
collection MIT
description The theory of acoustoelasticity provides direct link between the change of elastic wave velocities and residual stresses in solids. The general theory of acoustoelasticity is reviewed. A number of experimental measurements of the effect of stresses on the sound velocities in various types of rocks are compiled and compared to the acoustoelastic theory. The theory of acoustoelasticity agrees within 1% of error with experiments for stress levels that are representative for in-situ reservior conditions. With the measurements of Nur and Simmons, acoustoelastic theory is found to agree with Sayers's microcrack model within 2% of error, much smaller than experimental error which was 10%. We may safely conclude that the theory of acoustoelasticity is a macroscopic version of the microcrack model and applicable to in-situ rocks.
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spelling mit-1721.1/685992019-04-11T06:24:51Z The effect of stresses on the sound velocity in rocks: Theory of Acoustoelasticity and Experimental Measurements Huang, Xiaojun Burns, Daniel R. Toksoz, M. Nafi Massachusetts Institute of Technology. Earth Resources Laboratory Huang, Xiaojun Burns, Daniel R. Toksoz, M. Nafi The theory of acoustoelasticity provides direct link between the change of elastic wave velocities and residual stresses in solids. The general theory of acoustoelasticity is reviewed. A number of experimental measurements of the effect of stresses on the sound velocities in various types of rocks are compiled and compared to the acoustoelastic theory. The theory of acoustoelasticity agrees within 1% of error with experiments for stress levels that are representative for in-situ reservior conditions. With the measurements of Nur and Simmons, acoustoelastic theory is found to agree with Sayers's microcrack model within 2% of error, much smaller than experimental error which was 10%. We may safely conclude that the theory of acoustoelasticity is a macroscopic version of the microcrack model and applicable to in-situ rocks. 2012-01-17T17:49:00Z 2012-01-17T17:49:00Z 2001 Technical Report http://hdl.handle.net/1721.1/68599 Earth Resources Laboratory Industry Consortia Annual Report;2001-09 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle Huang, Xiaojun
Burns, Daniel R.
Toksoz, M. Nafi
The effect of stresses on the sound velocity in rocks: Theory of Acoustoelasticity and Experimental Measurements
title The effect of stresses on the sound velocity in rocks: Theory of Acoustoelasticity and Experimental Measurements
title_full The effect of stresses on the sound velocity in rocks: Theory of Acoustoelasticity and Experimental Measurements
title_fullStr The effect of stresses on the sound velocity in rocks: Theory of Acoustoelasticity and Experimental Measurements
title_full_unstemmed The effect of stresses on the sound velocity in rocks: Theory of Acoustoelasticity and Experimental Measurements
title_short The effect of stresses on the sound velocity in rocks: Theory of Acoustoelasticity and Experimental Measurements
title_sort effect of stresses on the sound velocity in rocks theory of acoustoelasticity and experimental measurements
url http://hdl.handle.net/1721.1/68599
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