A physical model for shear-wave velocity prediction
- Univ. of London (United Kingdom)
The clay-sand mixture model of Xu and White is shown to simulate observed relationships between S-wave velocity (or transit time), porosity and clay content. In general, neither S-wave velocity nor S-wave transit time is a linear function of porosity and clay content. For practical purposes, clay content is approximated by shale volume in well-log applications. In principle, the model can predict S-wave velocity from lithology and any pair of P-wave velocity, porosity and shale volume. Although the predictions should be the same if all measurements are error free, comparison of predictions with laboratory and logging measurements show that predictions using P-wave velocity are the most reliable. The robust relationship between S- and P-wave velocities is due to the fact that both are similarly affected by porosity, clay content and lithology. Because the model evaluates the bulk and shear moduli of the dry rock frame by a combination of Kuster and Toskoez` theory and differential effective medium theory, using pore aspect ratios to characterize the compliances of the sand and clay components, the relationship between P- and S-wave velocities is explicit and consistent. Numerical results from the model are confirmed by laboratory and logging data and demonstrate, for example, how the presence of gas has a more pronounced effect on P-wave velocity in shaly sands than in less compliant cleaner sandstones.
- Sponsoring Organization:
- USDOE
- OSTI ID:
- 277603
- Journal Information:
- Geophysical Prospecting, Journal Name: Geophysical Prospecting Journal Issue: 4 Vol. 44; ISSN GPPRAR; ISSN 0016-8025
- Country of Publication:
- United States
- Language:
- English
Similar Records
Prediction of P- and S-wave logs for seismic modeling
Ultrasonic velocities in sands--Revisited