1887
Volume 71, Issue 8
  • E-ISSN: 1365-2478

Abstract

Abstract

The elastic moduli of subsurface rocks saturated with geofluid often depend on the wave frequency and confining pressure due to the wave‐induced fluid flow and their significant intrinsic compressibility. Therefore, the knowledge of the pressure‐dependent dispersion of elastic moduli is usually used in broad practical scenarios such as geofluid discrimination and in situ abnormal pressure detection. We propose a simple dual‐porosity model to describe the pressure and frequency dependence of elastic moduli of fluid‐saturated rocks. First, we follow the idea of the Shapiro dual‐porosity model to yield more accurate formulas for pressure‐dependent stiff porosity and crack porosity. Then the new formulas for stiff and crack porosities are utilized to express the bulk and shear moduli of dry rocks as a function of pressure. Further, the bulk and shear moduli of a modified frame (i.e. a rock skeleton with the dry stiff pores and fluid‐saturated cracks) are formulated with the pressure‐dependent elastic moduli of dry rock. In order to consider the wave energy attenuation induced by fluid in cracks, the frequency‐independent fluid modulus imbedded in the formulas for bulk and shear moduli of a modified frame is replaced with a frequency‐dependent one incorporating the effect of viscoelastic relaxation. The effective bulk and shear moduli of entire fluid‐saturated body can be computed by inserting the pressure‐dependent stiff porosity and elastic moduli of a modified frame into the Gassmann equation. Moreover, appropriate simplification is performed on the central equations in the case of low porosity and weak deformation of stiff pores to yield an approximate model. Modelling results show that the proposed model can reasonably account for the nonlinear variation of bulk and shear moduli with the elevating effective pressure and cautiously predict the wave dispersion and attenuation. We validate our model by comparing the predicted elastic moduli with the corresponding results given by Shapiro model–based equations and with the laboratory measurements of five different fluid‐saturated rock samples.

Loading

Article metrics loading...

/content/journals/10.1111/1365-2478.13395
2023-09-22
2025-11-11
Loading full text...

Full text loading...

References

  1. Biot, M. A. (1956) Thermoelasticity and irreversible thermodynamics. Journal of Applied Physics, 27, 240–253. https://doi.org/10.1063/1.1722351.
    [Google Scholar]
  2. Biot, M. A. (1962) Mechanics of deformation and acoustic propagation in porous media. Journal of Applied Physics, 33, 1482–1498. https://doi.org/10.1063/1.1728759.
    [Google Scholar]
  3. Borgomano, J.V.M., Pimienta, L.X., Fortin, J. & Guéguen, Y. (2019) Seismic dispersion and attenuation in fluid‐saturated carbonate rocks: effect of microstructure and pressure. Journal of Geophysical Research: Solid Earth, 124, 12498–12522. https://doi.org/10.1029/2019JB018434.
    [Google Scholar]
  4. Carcione, J.M. (2014) Wave fields in real media. Theory and numerical simulation of wave propagation in anisotropic, anelastic, porous and electromagnetic media, 3rd edition, extended and revised. Amsterdam, The Netherlands: Elsevier.
    [Google Scholar]
  5. Chen, F., Zong, Z. & Yin, X. (2022) Acoustothermoelasticity for joint effects of stress and thermal fields on wave dispersion and attenuation. Journal of Geophysical Research: Solid Earth, 127, e2021JB023671. https://doi.org/10.1029/2021JB023671.
    [Google Scholar]
  6. Chen, F. & Zong, Z. (2022) PP wave reflection coefficient in stress‐induced anisotropic media and amplitude variation with incident angle and azimuth inversion. Geophysics, 87, C155–C172. https://doi.org/10.1190/geo2021‐0706.1.
    [Google Scholar]
  7. Chen, F.B., Zong, Z.Y. & Yin, X.Y. (2023) Monitoring the change in horizontal stress with multi‐wave time‐lapse seismic response based on nonlinear elasticity theory. Petroleum Science, 20, 815–826. https://doi.org/10.1016/j.petsci.2022.09.022.
    [Google Scholar]
  8. Coyner, K.B. (1984) Effect of stress, pore pressure, and pore fluids on bulkstrain, velocity, and permeability of rocks. (PhD thesis). Massachusetts Institute of Technology.
  9. David, E.C. & Zimmerman, R.W. (2012) Pore structure model for elastic wave velocities in fluid‐saturated sandstones. Journal of Geophysical Research, 117, 7210. https://doi.org/10.1029/2012JB009195
    [Google Scholar]
  10. Detournay, E. & Cheng, A.H.D. (1993) Fundamentals of poroelasticity, In: Hudson, J. A. (Ed.) Comprehensive rock engineering: principles, practice and projects. Oxford, UK: Pergamon Press, pp. 113–171.
    [Google Scholar]
  11. Dvorkin, J. & Nur, A. (1993) Dynamic poroelasticity: a unified model with the squirt and the Biot mechanisms. Geophysics, 58, 524–533. https://doi.org/10.1190/1.1443435.
    [Google Scholar]
  12. Dvorkin, J., Nolen‐Hoeksema, R. & Nur, A. (1994) The squirt‐flow mechanism: macroscopic description. Geophysics, 59, 428–438. https://doi.org/10.1190/1.1443605.
    [Google Scholar]
  13. Glubokovskikh, S., Gurevich, B. & Saxena, N. (2016) A dual‐porosity scheme for fluid/solid substitution. Geophysical Prospecting, 64, 1112–1121. https://doi.org/10.1111/1365‐2478.12389.
    [Google Scholar]
  14. Gurevich, B., Makarynska, D. & Pervukhina, M. (2009) Ultrasonic moduli for fluid‐saturated rocks: Mavko‐Jizba relations rederived and generalized. Geophysics, 74, N25–N30. https://doi.org/10.1190/1.3123802.
    [Google Scholar]
  15. Gurevich, B., Makarynska, D., De Paula, O.B. & Pervukhina, M. (2010) A simple model for squirt flow dispersion and attenuation in fluid‐saturated granular rocks. Geophysics, 75, N109–N120. https://doi.org/10.1190/1.3509782.
    [Google Scholar]
  16. Han, T., Gurevich, B., Pervukhina, M., Clennell, M.B. & Zhang, J. (2016) Linking the pressure dependency of elastic and electrical properties of porous rocks by a dual porosity model. Geophysical Journal International, 205, 378–388. https://doi.org/10.1093/gji/ggw019.
    [Google Scholar]
  17. Mavko, G.M. & Nur, A. (1979) Wave attenuation in partially saturated rocks. Geophysics, 44, 161–178. https://doi.org/10.1190/1.1440958.
    [Google Scholar]
  18. Mavko, G. & Jizba, D. (1991) Estimating grain‐scale fluid effects on velocity dispersion in rocks. Geophysics, 56, 1940–1949. https://doi.org/10.1190/1.1443005.
    [Google Scholar]
  19. Plona, T.J. (1980) Observation of a second bulk compressional wave in a porous medium at ultrasonic frequencies. Applied Physics Letters, 36, 259–261. https://doi.org/10.1063/1.91445.
    [Google Scholar]
  20. Shapiro, S.A. (2003) Elastic piezosensitivity of porous and fractured rocks. Geophysics, 68, 482–486. https://doi.org/10.1190/1.1567215.
    [Google Scholar]
  21. Sun, Y. & Gurevich, B. (2020) Modeling the effect of pressure on the moduli dispersion in fluid‐saturated rocks. Journal of Geophysical Research: Solid Earth, 125, e2019JB019297. https://doi.org/10.1029/2019JB019297.
    [Google Scholar]
  22. Tsai, H.C. & Lee, C.C. (1998) Compressive stiffness of elastic layers bonded between rigid plates. International Journal of Solids and Structures, 35, 3053–3069. https://doi.org/10.1016/S0020‐7683(97)00355‐7
    [Google Scholar]
  23. Zimmerman, R.W., Somerton, W.H. & King, M.S. (1986) Compressibility of porous rocks. Journal of Geophysical Research, 91, 12765–12777. https://doi.org/10.1029/JB091iB12p12765.
    [Google Scholar]
  24. Zong, Z.Y, Chen, F.B., Yin, X.Y. & Li, K. (2023) Effect of stress on wave propagation in fluid‐saturated porous thermoelastic media. Surveys in Geophysics, 44, 425–462. https://doi.org/10.1007/s10712‐022‐09743‐y.
    [Google Scholar]
/content/journals/10.1111/1365-2478.13395
Loading
/content/journals/10.1111/1365-2478.13395
Loading

Data & Media loading...

  • Article Type: Research Article
Keyword(s): acoustics; attenuation; elastics; modelling; rock physics

Most Cited This Month Most Cited RSS feed

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error