1887
ASEG2012 - 22nd Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

Knowledge of the pressure dependencies of rock properties in unconsolidated sands is important for accurate time-lapse feasibility studies, pore pressure prediction, and reservoir characterization. A key problem that arises in determining such pressure dependencies is an accurate model at low effective stress. We propose a double exponential model to describe the pressure sensitivity of the bulk modulus (K) or shear modulus (G) for unconsolidated sands. The physical basis for our model relies on observed porosity-depth trends in unconsolidated sands, and the concept of critical porosity. Our new model matches laboratory measurements on unsaturated sand samples that have a range of grain size distributions and compositions. Grain size distribution data is first used to estimate critical porosity, which is then used as a zero effective pressure constraint in the data fitting process. We show that our new model more accurately predicts pressure sensitivity near zero-effective pressure compared to current methods, and is thus more accurate for situations in which core measurements at low effective stresses are not available.

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/content/journals/10.1071/ASEG2012ab119
2012-12-01
2026-01-18
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References

  1. Athy, L. F., 1930, Compaction and oil migration: AAPG Bulletin 14, 25-35.
  2. Beard, D. C., and Weyl, P. K., 1973, Influence of texture on porosity and permeability of unconsolidated sand: AAPG Bulletin 57, 349-369.
  3. Berner, R. A., 1980, Early Diagenesis -- A Theoretical Approach, Princeton, Princeton University Press.
  4. Dutta, T., Mavko, G., Mukerji, T., and Lane, T., 2009, Compaction trends for shale and clean sandstone in shallow sediments, Gulf of Mexico: The Leading Edge 28, 590-596.
  5. Eberhart-Phillips, D., Han, D.-H., and Zoback, M. D., 1989, Empirical relationships among seismic velocity, effective pressure, porosity, and clay content in sandstone: Geophysics 54, 82-89.
  6. Gassmann, F., 1951, Elastic waves through a packing of spheres: Geophysics 16, 673-685.
  7. Marion, D., West, C., and Nur, A., 1988, Model of unconsolidated marine sediments, Part I: Sand-clay model and Part II: Applications in seismic processing: SEG Technical Program Expanded Abstracts 7, 916-921.
  8. Mavko, G., Mukerji, T., and Dvorkin, J., 1998, The Rock Physics Handbook, Cambridge University Press.
  9. Nur, A. M., Mavko, G., Dvorkin, J., and Gal, D., 1995, Critical porosity: The key to relating physical properties to porosity in rocks: SEG Technical Program Expanded Abstracts 14, 878-881.
  10. Prasad, M., 2002, Acoustic measurements in unconsolidated sands at low effective pressure and overpressure detection: Geophysics 67, 405-412.
  11. Scherer, M., 1987, Parameters influencing porosity in sandstones: a model for sandstone porosity prediction: AAPG Bulletin 71, 485-491.
  12. Shapiro, S. A., 2003, Elastic piezosensitivity of porous and fractured rocks: Geophysics 68, 482-486.
  13. Trask, P. D., 1931, Compaction of sediments: AAPG Bulletin 15, 271-276.
  14. Woods, A. W., 1955, A textbook of sound, New York, McMillan Co.
  15. Yan, F., and Han, D.-H., 2009, Modeling of effective pressure effect on porous reservoir rocks: SEG Technical Program Expanded Abstracts 28, 2025-2029.
  16. Zimmer, M., 2003, Seismic velocities in unconsolidated sands: Measurements of pressure, sorting, and compaction effects: Ph.D. dissertation, Stanford University.
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