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Effects of an off-centered tool on dipole and quadrupole logging

Authors
Byun, JoongmooToksoz, M. Nafi
Issue Date
Jul-2006
Publisher
SOC EXPLORATION GEOPHYSICISTS
Keywords
Data recording; Seismic waves; Well logging
Citation
GEOPHYSICS, v.71, no.4, pp.F91 - F100
Indexed
SCIE
SCOPUS
Journal Title
GEOPHYSICS
Volume
71
Number
4
Start Page
F91
End Page
F100
URI
https://scholarworks.bwise.kr/hanyang/handle/2021.sw.hanyang/181273
DOI
10.1190/1.2217368
ISSN
0016-8033
Abstract
An acoustic logging tool in inclined or horizontal boreholes may be placed apart from the center and produce additional complicated wavefields. We investigate the effects of an off-centered tool on monopole, dipole, and quadrupole logs due to off-centering of the tool. In recent logging tools, monopole, dipole, and quadrupole logs can be obtained by adding or subtracting responses at four monopole (pressure) receiver arrays at right angles. We examine the responses of the four monopole receiver array system for three directions of eccentricity: inline direction of the dipole source (Off 0 degrees case), crossline direction (Off 90 degrees case), and 45 degrees to the dipole source (Off 45 degrees case). To simulate responses at each receiver array, we use the discrete wavenumber method. In a dipole tool positioned on the borehole axis, the inline receiver arrays have only the flexural wave while the cross receiver arrays have zero response. However, an off-centered dipole source produces nondipole modes as well as the dipole mode. For all cases with a dipole source, the dipole mode was enhanced by subtracting responses at one of the inline receiver arrays from those of the other receiver array, and we could extract the formation shear velocity. Similar to the dipole source, an offcentered quadrupole source introduces additional nonquadrupole modes. The quadrupole mode was enhanced by subtracting the sum of responses at receiver arrays below negative poles of a quadrupole source from the sum of responses at receiver arrays below positive poles for all cases. In addition, the formation shear velocity was obtained from the time semblance calculation.
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COLLEGE OF ENGINEERING (DEPARTMENT OF EARTH RESOURCES AND ENVIRONMENTAL ENGINEERING)
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