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Using a discrete wavenumber method, we examine the effects on Logging-While-Drilling (LWD) logs when a
mismatch exists between the amplitudes or generating times of the signals from individual monopoles in a LWD multipole
source. An amplitude-mismatched LWD dipole/quadrupole source produces non-dipole/non-quadrupole modes as well as
flexural and screw modes. The strongest of non-dipole/non-quadrupole modes is the Stoneley mode, whose amplitude
increases with increasing mismatch. However, we can recover the flexural mode signals by A-C processing, and the screw
mode by A-B+C-D processing, respectively. The Stoneley mode, which has the same amplitude at the same radial
distance from the borehole axis, is cancelled out by A-C and A-B+C-D processing as long as the tool is placed at the
centre of the borehole. The responses from a time-mismatchedLWDmultipole source look like the summation of responses by
two or four monopole sources off the borehole axis. However, we can avoid the misinterpretation of the formation velocities
by referring to the computed dispersion curves, which are independent of the arrival times of the modes, on the frequency
semblance plot.
Using a discrete wavenumber method, we examine the effects on Logging-While-Drilling (LWD) logs when a
mismatch exists between the amplitudes or generating times of the signals from individual monopoles in a LWD multipole
source. An amplitude-mismatched LWD dipole/quadrupole source produces non-dipole/non-quadrupole modes as well as
flexural and screw modes. The strongest of non-dipole/non-quadrupole modes is the Stoneley mode, whose amplitude
increases with increasing mismatch. However, we can recover the flexural mode signals by A-C processing, and the screw
mode by A-B+C-D processing, respectively. The Stoneley mode, which has the same amplitude at the same radial
distance from the borehole axis, is cancelled out by A-C and A-B+C-D processing as long as the tool is placed at the
centre of the borehole. The responses from a time-mismatchedLWDmultipole source look like the summation of responses by
two or four monopole sources off the borehole axis. However, we can avoid the misinterpretation of the formation velocities
by referring to the computed dispersion curves, which are independent of the arrival times of the modes, on the frequency
semblance plot.
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- Publisher :Korean Society of Earth and Exploration Geophysicists
- Publisher(Ko) :한국지구물리물리탐사학회
- Journal Title :Geophysics and Geophysical Exploration
- Journal Title(Ko) :지구물리와 물리탐사
- Volume : 12
- No :1
- Pages :143~153


Geophysics and Geophysical Exploration






