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Acoustic response characteristics of unsaturated porous media

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  • Special Topics on Reservoir Acoustics
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Abstract

By employing the plane wave analysis method, the dispersion equations associated with compressional and shear waves using Santos’s three-phase poroelastic theory were driven. Considering the reservoir pressure, the high frequency corrections and the coupling drag of two fluids in pores, the influences of frequency and gas saturation on the phase velocities and the inverse quality factors of four body waves predicted by Santos’s theory were discussed in detail. The theoretical velocities of the fast compressional and shear waves were compared with the results of the low and high frequency experiments from open publications, respectively. The results showed that they are in good agreement in the low frequency case rather than in the high frequency case. In the latter case, several popular poroelastic models were considered and compared with the experimental data. In the models, the results of White’s theory fit the experimental data, but the parameter b in White’s model has a significant impact on the results. Under the framework of the linear viscoelasticity theory, the attenuation mechanism of Santos’s model was extended, and the comparisons between the experimental and theoretical results were also made with respect to attenuation. For the case of water saturation less than 90%, the extended model makes good predictions of the inverse quality factor of shear wave. There is a significant difference between the experimental and theoretical results for the compressional wave, but the difference can be explained by the experimental data available.

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References

  1. Brandt H. Factors affecting compressional wave velocity in unconsolidated marine sand sediments. J Acoust Soc Am, 1960, 32: 171–179

    Article  ADS  Google Scholar 

  2. Elliott S E, Wiley B F. Compressional velocities of partially saturate, unconsolidated sands. Geophysics, 1975, 40: 949–954

    Article  ADS  Google Scholar 

  3. Gregory A R. Fluid saturation effect on dynamic elastic properties of sedimentary rocks. Geophysics, 1976, 41: 895–921

    Article  MathSciNet  ADS  Google Scholar 

  4. Domenico S N. Effects of water saturation of sand reservoirs encased in shales. Geophysics, 1974, 29: 759–769

    Article  ADS  Google Scholar 

  5. Domenico S N. Effect of brine-gas mixture on velocity in unconsolidated sand reservoir. Geophysics, 1976, 41: 882–894

    Article  ADS  Google Scholar 

  6. Tittmann B R, Clark V A, Richardson J M, et al. Possible mechanism for seismic attenuation in rocks containing small amounts of volatiles. J Geophys Res, 1980, 85: 5199–5208

    Article  ADS  Google Scholar 

  7. Winker K, Nur A. Seismic attenuation: Effects of pore fluids and frictional sliding. Geophysics, 1982, 47: 1–15

    Article  ADS  Google Scholar 

  8. White J E. Computed seismic speeds and attenuation in rocks with partial gas saturation. Geophysics, 1975, 40: 224–232

    Article  ADS  Google Scholar 

  9. Pride S R, Berryman J G, Harris J M. Seismic attenuation due to wave-induced flow. J Geophys Res, 2004, 109: B01201

    Article  Google Scholar 

  10. Mavko G, Nur A. Wave attenuation in partially saturated rocks. Geophysics, 1979, 44: 161–178

    Article  ADS  Google Scholar 

  11. O’Connell R J, Budiansky B. Viscoelastic properties of fluid-saturated cracked solid. J Geophys Res, 1977, 82: 5719–5735

    Article  ADS  Google Scholar 

  12. Murphy W F. Effects of partial water saturation on attenuation in Massillon sandstone and Vycor porous glass. J Acoust Soc Am, 1982, 71: 1458–1468

    Article  MathSciNet  ADS  Google Scholar 

  13. Murhpy W F. Acoustic measures of partial gas saturation in tight sandsones. J Geophys Res B, 1984, 89: 11549–11559

    Article  Google Scholar 

  14. Knight R, Nolen-Hoeksema R. A laboratory study of the dependence of elastic wave velocities on pore scale fluid distribution. Geophys Res Lett, 1990, 17: 1529–1532

    Article  ADS  Google Scholar 

  15. Cadoret T, Mavko G, Zinszner B. Fluid distribution effect on sonic attenuation in partially saturated limestones. Geophysics, 1998, 63: 154–160

    Article  ADS  Google Scholar 

  16. Lo W C, Sposito G, Majer E. Wave propagation through elastic porous media containing two immiscible fluids. Water Resour Res, 2005, 41,W02025: 1–20

    Google Scholar 

  17. Wang D X, **n K F, Li Y M, et al. An experimental study of influence of water saturation on velocity and attenuation in sandstone under stratum conditions. Chin J Geophys, 2006, 49: 908–914

    ADS  Google Scholar 

  18. Nie J X, Yang D H, Yang H Z. Wave dispersion and attenuation in partially saturated sandstones. Chin Phys Lett, 2004, 21: 572–575

    Article  ADS  Google Scholar 

  19. King M S, Marsden J R, Dennis J W. Biot dispersion for P- and S-waves velocities in partially and fully saturated sandstones. Geophys Prospecting, 2000, 48: 1075–1089

    ADS  Google Scholar 

  20. Tuncay K, Corapcioglu M Y. Body waves in poroelastic media saturated by two immiscible fluids. J Geophys Res B, 1996, 101: 25149–25159

    Article  Google Scholar 

  21. Wei C F, Muraleetharan K K. A continuum theory of porous media saturated by multiple immiscible fluids: I. Linear poroelasticity. Int J Eng Sci, 2002, 40: 1807–1833

    Article  MathSciNet  Google Scholar 

  22. Cai Y Q, Li B Z, Xu C J. Analysis of elastic wave propagation in sandstone saturated by two immiscible fluids. Chin J Rock Mech Eng, 2006, 25: 2009–2016

    Google Scholar 

  23. Santos J E, Corberó J M, Douglas J. Static and dynamic behavior of a porous solid saturated by a two-phase fluid. J Acoust Soc Am A, 1990, 87: 1428–1438

    Article  ADS  Google Scholar 

  24. Santos J E, Douglas J, Corberó J M, et al. A model for wave propagation in a porous medium saturated by a two-phase fluid. J Acoust Soc Am B, 1990, 87: 1439–1448

    Article  ADS  Google Scholar 

  25. Santos J E, Ravazzoli C L, Gauzellino R M, et al. Simulation of waves in poro-viscoelastic rocks saturated by immiscible fluids: Numerical evidence of a second slow wave. J Comput Acoust, 2004, 12: 1–21

    Article  MATH  Google Scholar 

  26. Zhao H B, Wang X M. Acoustic wave propagation simulation in a poroelastic medium saturated by two immiscible fluids using a staggered finite-difference with a time partition method. Sci China Ser G-Phys Mech Astron, 2008, 51: 723–744

    Article  ADS  Google Scholar 

  27. Berryman J G. Confirmation of Biot’s theory. Appl Phys Lett, 1980, 37: 382–384

    Article  ADS  Google Scholar 

  28. Douglas J, Furtado F, Pereira F. On the numerical simulation of waterflooding of heterogeneous petroleum reservoirs. Comput Geosci, 1997, 1: 155–190

    Article  MATH  MathSciNet  Google Scholar 

  29. Carcione J M, Cavallini F, Santos J E, et al. Wave propagation in partially saturated porous media: Simulation of a second slow wave. Wave Motion, 2004, 39: 227–240

    Article  MATH  MathSciNet  Google Scholar 

  30. Carcione J M. Wave fields in real media: wave propagation in anisotropic, anelastic and porous media. London: Elsevier Sciences, 2001. 65–73

    Google Scholar 

  31. Yin C S, Batzle M L, Smith B J. Effects of partial liquid/gas saturation on extensional wave attenuation in Berea sandstone. Geophys Res Lett, 1992, 19: 1399–1402

    Article  ADS  Google Scholar 

  32. Bourbié T, Zinszner B. Saturation methods and attenuation versus saturation relationships in Fontainebleau sandstone. In: 54th SEG meeting, Atlanta, 1984. 344–347

  33. Diallo M S, Appel E. Acoustic wave propagation in saturated porous media: Reformulation of the Biot/Squirt (BISQ) flow theory. J Appl Geophys, 2000, 44: 313–325

    Article  Google Scholar 

  34. Pham N H, Carcione J M, Helle H B, et al. Wave velocities and attenuation of shaley sandstones as a function of pore pressure and partial saturation. Geophys prospecting, 2002, 50: 615–627

    Article  ADS  Google Scholar 

  35. Biot M A. Theory of propagation of elastic waves in a fluid-saturated porous solid. II. High frequency range. J Acoust Soc Am, 1956, 28: 179–191

    Article  MathSciNet  ADS  Google Scholar 

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Correspondence to HaiBo Zhao.

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Zhao, H., Wang, X., Chen, S. et al. Acoustic response characteristics of unsaturated porous media. Sci. China Phys. Mech. Astron. 53, 1388–1396 (2010). https://doi.org/10.1007/s11433-010-4056-4

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  • DOI: https://doi.org/10.1007/s11433-010-4056-4

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