Xm. Tang et al., A DISPERSIVE-WAVE PROCESSING TECHNIQUE FOR ESTIMATING FORMATION SHEARVELOCITY FROM DIPOLE AND STONELEY WAVE-FORMS, Geophysics, 60(1), 1995, pp. 19-28
A model-guided dispersive-wave processing technique has been developed
to estimate formation shear-wave velocity from borehole acoustic logg
ing waveforms. These waveform data can be the Stoneley waves in monopo
le logging or the flexural waves in dipole logging. In this technique,
the waveform recorded on a given receiver is compared to the waveform
from a second receiver that is numerically propagated to the given re
ceiver's position using a trial formation shear-wave velocity. The num
erical propagation step uses the proper dispersion relation for the wa
ve mode (dipole or Stoneley). The phase difference between the two wav
eforms is minimized by varying the shear velocity. The velocity value
that minimizes the phase difference is chosen as the final shear veloc
ity at which the waveforms attain the optimum phase match. In this pro
cedure the dispersion effect is automatically accounted for by using t
he model theory and is demonstrated by a comparison with the results o
f the semblance method. Using this technique with a multiple-shot sche
me to process array acoustic logging data, formation shear velocity ca
n be estimated to the resolution of one receiver spacing [typically 0.
5 ft (0.1524 m)]. This result has been demonstrated by a field example
in which the improved resolution in the shear velocity log is convinc
ingly supported by the same character in the density log measured at o
ne receiver spacing intervals. Shear velocity logs obtained using fiel
d Stoneley and dipole sonic data are also compared to demonstrate the
ability of the technique to obtain high-resolution formation shear vel
ocity logs from the dispersive logging waveforms. The new technique ma
y find very useful applications in the determination of formation shea
r-wave properties using acoustic waveform logging.