| 摘要 |
<p>The shear velocity of a formation traversed by a fluid-filled open or cased borehole is obtained. Waveforms are obtained from a dipole acoustic investigation of the formation relative to a common location in the borehole. In a direct technique, the bandwidth of the waveforms is substantially bounded by an upper frequency fu at and below which energy traveling at the shear velocity is dominant. Moreover, the bandwidth of the waveforms is concentrated near the frequency fu. The shear velocity of said earth formation is determined from waveforms obtained from a broadband dipole acoustic investigation. The waveforms are low-pass filtered, and an interim shear velocity vs is determined. Vs is first obtained for an initial fcut, and subsequently for additional decreasing values of fcut, until a preselected relationship between fcut and vs is satisfied. The last-determined vs is the shear velocity. In another embodiment the flexural mode phase velocity is determined as a function of frequency from the waveforms. If a low frequency asymptote is identifiable, it is reported as the shear velocity. If not, a plurality of additional curves of the flexural mode phase velocity as a function of frequency are theoretically determined, based on respective estimated shear velocities. These curves are respectively fitted to the curve determined from the waveforms, until a satisfactory least error fit is achieved. The last-estimated shear velocity is reported as a shear velocity of the formation.</p> |
