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Investigating Depth of Mode Waves in the Borehole Surrounded by Transversely Isotropic Elastic Formation

CHEN Xue-lian1,WANG Rui-jia2   

  1. 1.College of Geo-Resources and Information, China University of Petroleum, Dongying,Shandong 257061,China;2.Faculty of Natural Resources & Information Technology, China University of Petroleum, Beijing 102249,China
  • Received:2007-09-27 Revised:1900-01-01 Online:2008-05-26 Published:2008-05-26
  • Contact: CHEN Xue-lian

Abstract: The curves of the dispersion and sensitivity for the mode waves in the borehole surrounded by a transversely isotropic elastic solid are numerically simulated. The results show that the flexural wave is sensitive to the velocity of the vertically propagating shear wave (vSV), while the Stoneley wave is sensitive to the velocity of the horizontally propagating shear wave (vSH). In the slow formation, the investigating depth of the Stoneley wave is about 1.5 radius of the borehole to the wall for the full calculating frequency range; the flexural wave exhibits frequencydependent characteristic of the radial depth of investigation, and the investigating depth is deep (about 4 radius of the borehole) with low wavenumbers and shallow (about 1.5 radius of the borehole) with high wavenumbers. In the fast formation, the sensitivity of the flexural wave to the vSV diminishes slightly, but the sensitivity of the Stoneley wave to the vSH diminishes significantly due to the influence of the fluid filled in the borehole.

Key words: transversely isotropic elastic formation, flexural wave, Stoneley wave, investigating depth, sensitivity

CLC Number: 

  • P631.8
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