A fast modeling method is formulated for low-frequency Stoneley-wave p
ropagation in an irregular borehole. This fast modeling method provide
s synthetic waveforms which include the effects of two borehole irregu
larities, diameter changes (washout), and formation property changes.
The essential physics of the low-frequency Stoneley waves are captured
with a simple 1-D model. A mass-balance boundary condition and a prop
agator matrix are used to express Stoneley-wave interactions with the
borehole irregularities. The accuracy of the proposed method was confi
rmed through comparison with existing finite-difference and boundary i
ntegral modeling methods that yielded cross-correlations greater than
0.98, Comparison of synthetic records calculated for an actual borehol
e with field records showed qualitative agreement in the major reflect
ions because of the washout zones, but showed some disagreements in th
e reflections caused by the fractures; Since the synthetic records inc
lude only information relating to the borehole geometry and the elasti
c properties of formation, the reflection caused by the fracture will
appear only in the field record. These results suggest the possibility
of distinguishing Stoneley-wave reflections caused by fractures from
those caused by borehole irregularities. Further, the fast computation
al speed of this method-over 300 times faster than either boundary int
egral or finite-difference methods-makes it quite suitable for field a
pplication.