1887
ASEG2007 - 19th Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

Seismic prospecting and evaluation of the rock mechanical properties require knowledge of shear-wave (S-wave) velocity. However, frequently the S-wave logs are not available, especially in past years. Prediction of Swave velocity is still attracting researchers’ attention because of its importance in petroleum exploration and engineering application.

A new rock physics model of clay-sand mixture is developed based on Self-Consistent Approximations (SCA) and Gassmann model. The model assumes that total pore space consists of two parts: (1) pores from sand grains and (2) pores from clays. The elastic moduli of clay-fluid mixture and sand-pore mixture are obtained by SCA. The clay-fluid mixture first fills up the total porosity, then replace the matrix (sand grains), taking the form of structure clay. The model can explain the distinctive changing relations between clay content and compressional velocity of the sand-clay mixture observed by Marion.

The model can be applied to predict compressional and shear wave velocities of the rock using conventional logs such as acoustic velocity, density and gamma ray logs. Parameters of the sand clay mixture model are chosen according to the fitness between predicted and measured compressional wave velocity. After that, we use the improved model to predict shear wave velocity, and the computational results indicate that the predicted shear wave velocities agree well with the measured velocities. The reliability of the shear wave velocity estimation can be validated by the predicted and measured compressional wave velocities fitness.

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/content/journals/10.1071/ASEG2007ab145
2007-12-01
2026-01-23
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References

  1. Berryman, J.G., 1980, Long-wavelength propagation in composite elastic media: Journal of Acoustic Society of America, 68, 1809-1831.
  2. Han, D. H., Nur, A., and Morgan, D., 1986, Effects of porosity and clay content on wave velocities in sandstones: Geophysics, 51, 2093-2107.
  3. Gassmann, F., 1951, Über die Elastizität poröser Medien: Vier. der Natur.Gesellschaft in Zürich, 96, 1-23.
  4. Kuster, G. T. and Toksöz, M. N., 1974, Velocity and attenuation of seismic waves in two phase media: Geophysics, 39, 587-606.
  5. Marion, D., Nur, A., Yin, H., and Han, D., 1992, Compressional velocity and porosity in sand-clay mixtures: Geophysics, 57, 554-563.
  6. Sams, M.S. and Andra, M., 2001, The effect of clay distribution on the elastic properties of sandstones: Geophysical Prospecting, 49, 1128-149.
  7. Xu, S. Y. and White, R. E., 1995, A new velocity model for clay-sand mixtures: Geophysical Prospecting, 43, 687-717.
/content/journals/10.1071/ASEG2007ab145
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  • Article Type: Research Article
Keyword(s): Effective Medium Model; Self-Consistent Approximations; Shear Wave Velocity
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