Acoustic wave propagation simulation in a poroelastic medium saturated by two immiscible fluids using a staggered finite-difference with a time partition method

Article

Abstract

Based on the three-phase theory proposed by Santos, acoustic wave propagation in a poroelastic medium saturated by two immiscible fluids was simulated using a staggered high-order finite-difference algorithm with a time partition method, which is firstly applied to such a three-phase medium. The partition method was used to solve the stiffness problem of the differential equations in the three-phase theory. Considering the effects of capillary pressure, reference pressure and coupling drag of two fluids in pores, three compressional waves and one shear wave predicted by Santos have been correctly simulated. Influences of the parameters, porosity, permeability and gas saturation on the velocities and amplitude of three compressional waves were discussed in detail. Also, a perfectly matched layer (PML) absorbing boundary condition was firstly implemented in the three-phase equations with a staggered-grid high-order finite-difference. Comparisons between the proposed PML method and a commonly used damping method were made to validate the efficiency of the proposed boundary absorption scheme. It was shown that the PML works more efficiently than the damping method in this complex medium. Additionally, the three-phase theory is reduced to the Biot’s theory when there is only one fluid left in the pores, which is shown in Appendix. This reduction makes clear that three-phase equation systems are identical to the typical Biot’s equations if the fluid saturation for either of the two fluids in the pores approaches to zero.

Keywords

acoustic waves poroelastic media immiscible fluids staggered grids perfectly matched layers 

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References

  1. 1.
    Domenico S N. Effect of brine-gas mixture on velocity in unconsolidated sand reservoir. Geophysics, 1976, 41: 882–894CrossRefADSGoogle Scholar
  2. 2.
    Mochizuki S. Attenuation in partially saturated rocks. J Geophys Res, 1982, 87: 8598–8604CrossRefADSGoogle Scholar
  3. 3.
    Murphy W F. Effects of partial water saturation on attenuation in Massillon sandstone and Vycor porous glass. J Acoust Soc Am, 1982, 71: 1458–1468CrossRefADSMathSciNetGoogle Scholar
  4. 4.
    Murhpy W F. Acoustic measures of partial gas saturation in tight sandsones. J Geophys Res, 1984, 89(B13): 11549–11559CrossRefADSGoogle Scholar
  5. 5.
    Mavko G, Nolen-Hoeksema R. Estimating seismic velocities at ultrasonic frequencies in partially saturated rocks. Geophysics, 1994, 59(2): 252–258CrossRefADSGoogle Scholar
  6. 6.
    Lee M W. Elastic velocities of partially saturated unconsolidated sediments. Mar Petrol Geol, 2004, 21: 641–650CrossRefGoogle Scholar
  7. 7.
    Wang Z, Nur A. Effects of CO2 flooding on wave velocities in rocks with hydrocarbons. Soc Petrol Engrs Reservoir Eng, 1989, 3: 429–439Google Scholar
  8. 8.
    Xue Z, Ohsumi T, Koide H. Laboratory measurements of seismic wave velocity by CO2 injection in two porous sandstones: In Gale and Kaya. In: Proceedings of the 6th International Conference on Greenhouse Gas Control Technologies 2002. Kyoto: Elsevier, 2003. 359–364CrossRefGoogle Scholar
  9. 9.
    Xue Z, Ohsumi T. Seismic wave monitoring of CO2 migration in water-saturated porous sandstone. Explor Geophys, 2004, 35: 25–32CrossRefGoogle Scholar
  10. 10.
    Tuncay K, Corapcioglu M Y. Body waves in poroelastic media saturated by two immiscible fluids. J Geophys Res B, 1996, 101(11): 149–159Google Scholar
  11. 11.
    Tuncay K, Corapcioglu M Y. Wave propagation in poroelastic media saturated by two fluids. J Appl Mech, 1997, 64: 313–320MATHCrossRefGoogle Scholar
  12. 12.
    Berryman J G, Thigpen L, Chin R. Bulk elastic wave propagation in partially saturated porous solids. J Acoust Soc Am, 1988, 84(1): 360–373CrossRefADSGoogle Scholar
  13. 13.
    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: 1807–1833CrossRefMathSciNetGoogle Scholar
  14. 14.
    Lo W C, Sposito G, Majer E. Immiscible two-phase fluid flows in deformable porous media. Adv Water Res, 2002, 25:1105–1117CrossRefGoogle Scholar
  15. 15.
    Lo W C, Sposito G, Majer E. Wave propagation through elastic porous media containing two immiscible fluids. Water Res Res, 2005, 41, W02025: 1–20CrossRefGoogle Scholar
  16. 16.
    Lu J F, Hanyga A. Linear dynamic model for porous media saturated by two immiscible fluids. Int J Solids Struct, 2005, 42:2689–2709MATHCrossRefGoogle Scholar
  17. 17.
    White J E. Computed seismic speeds and attenuation in rocks with partial gas saturation. Geophysics, 1975, 40(2): 224–323CrossRefADSGoogle Scholar
  18. 18.
    Dutta N C, Odé H. Attenuation and dispersion of compressional wave in fluid-filled porous rocks with partial gas saturation (White model) (I): Biot theory. Geophysics, 1979, 44(11): 1777–1788CrossRefADSGoogle Scholar
  19. 19.
    Dutta N C, Odé H. Attenuation and dispersion of compressional wave in fluid-filled porous rocks with partial gas saturation (White model) (II): Results. Geophysics, 1979, 44(11): 1789–1805CrossRefADSGoogle Scholar
  20. 20.
    Dutta N C, Seriff A J. On White’s model of attenuation in rocks with partial saturation. Geophysics, 1979, 44(11): 1806–1812CrossRefADSGoogle Scholar
  21. 21.
    Norris A N. Low-frequency dispersion and attenuation in partially saturated rocks. J Acoust Soc Am, 1993, 94: 359–370CrossRefADSMathSciNetGoogle Scholar
  22. 22.
    Johnson D L. Theory of frequency dependent acoustics in patchy-saturated porous media. J Acoust Soc Am, 2001, 110(2): 682–694CrossRefADSGoogle Scholar
  23. 23.
    Ciz R, Gurevich B. Amplitude of Biot’s slow wave scattered by a spherical inclusion in a fluid-saturated poroelastic medium. Geophys J Int, 2005, 160: 991–1005CrossRefADSGoogle Scholar
  24. 24.
    Carcione J M, Helle H B, Pham N H. White’s model for wave propagation in partially saturated rocks: Comparison with poroelastic numerical experiments. Geophysics, 2003, 68: 1389–1398CrossRefADSGoogle Scholar
  25. 25.
    Wang D, Zhang H L, Wang X M. A numerical study of acoustic wave propagation in partially saturated poroelastic rock. Chin J Geophys, 2006, 49(2): 465–473Google Scholar
  26. 26.
    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, 1990a, 87: 1428–1438CrossRefADSGoogle Scholar
  27. 27.
    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, 1990b, 87: 1439–1448CrossRefADSGoogle Scholar
  28. 28.
    Ravazzoli C L, Santos J E, Carcione J M. Acoustic and mechanical response of reservoir rocks under variable saturation and effective pressure. J Acous Soc Am, 2003, 113(4): 1801–1811CrossRefADSGoogle Scholar
  29. 29.
    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): 1–21MATHCrossRefMathSciNetGoogle Scholar
  30. 30.
    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: 227–240MATHCrossRefMathSciNetGoogle Scholar
  31. 31.
    Wang X M, Dodds K, Zhao H B. An improved high-order rotated staggered finite-difference algorithm for simulating elastic waves in heterogeneous viscoelastic/anisotropic media. Explor Geophys, 2006, 37(2): 160–174CrossRefGoogle Scholar
  32. 32.
    Douglas J, Furtado F, Pereira F. On the numerical simulation of waterflooding of heterogeneous petroleum reservoirs. Comput Geosci, 1997, 1: 155–190MATHCrossRefMathSciNetGoogle Scholar
  33. 33.
    Berryman J G. Confirmation of Biot’s theory. Appl Phys Lett, 1980, 37: 382–384CrossRefADSGoogle Scholar
  34. 34.
    Carcione J M, Quiroga-Goode G. Some aspects of the physics and numerical modeling of Biot’s compressional waves. J Comput Acoust, 1996, 3: 261–280CrossRefGoogle Scholar
  35. 35.
    Zhao H B, Wang X M, Chen H. A method solving the stiffness problem in Biot’s poroelastic equations using a staggered high-order finite-difference. Chin Phys, 2006, 12: 2819–2827ADSGoogle Scholar
  36. 36.
    Wang X M, Zhang H L, Wang D. Modeling of seismic wave propagation in Heterogeneous poroelastic media using a high-order staggered finite-difference method. Chin J Geophys, 2003, 46(6): 842–849Google Scholar
  37. 37.
    Putzer E J. Avoiding the Jordan canonical form in the discussion of linear systems with constant coefficients. Am Math Month, 1966, 73(1): 2–6MATHCrossRefMathSciNetGoogle Scholar
  38. 38.
    Zhao H B, Wang X M, Zhang H L. Studies on effective and stable absorbing boundary conditions in ultrasonic wave modeling. Ultrason Symp IEEE, 2005, 3: 1472–1475CrossRefGoogle Scholar
  39. 39.
    Collino F, Tsogka C. Application of the perfectly matched absorbing layer model to the linear elastodynamic problem in anisotropic heterogeneous media. Geophysics, 2001, 66(1): 294–307CrossRefADSGoogle Scholar
  40. 40.
    Zeng Y Q, He J Q, Liu Q H. The application of the perfectly matched layer in numerical modeling of the perfectly matched layer in numerical modeling of wave propagation in poroelastic media. Geophysics, 2001, 66(4): 1258–1266CrossRefADSGoogle Scholar
  41. 41.
    Zhao H B, Wang X M, Wang D, et al. Applications of the boundary absorption using a perfectly matched layer for elastic wave simulation in poroelastic media. Chin J Geophys, 2007, 50(2): 581–591Google Scholar
  42. 42.
    Arntsen B, Carcione J M. Numerical simulation of the Biot slow wave in water-saturated Nivelsteiner sandstone. Geophysics, 2001, 66: 890–896CrossRefADSGoogle Scholar
  43. 43.
    Cerjan C, Kosloff D, Kosloff R. A nonreflecting boundary condition for discrete acoustic and elastic wave equations. Geophysics, 1985, 50(4): 705–708CrossRefADSGoogle Scholar
  44. 44.
    Cacione J M, Quiroga-Goode G. Full frequency-range transient solution for compresional waves in a fluid-saturated viscoacoustic porous medium. Geophys Prosp, 1996, 44: 99–129CrossRefGoogle Scholar
  45. 45.
    Plona T J. Acoustics of fluid-saturated porous media. Ultrason Symp IEEE, 1982, 2: 1044–1048Google Scholar
  46. 46.
    Biot M A. Theory of propagation of elastic waves in a fluid-saturated porous solid (I): Low-frequency range. J Acoust Soc Am, 1956, 28: 168–178CrossRefADSMathSciNetGoogle Scholar
  47. 47.
    Biot M A. Generalized theory of acoustic propagation in porous dissipative media. J Acoust Soc Am, 1962, 34: 1254–1264CrossRefADSMathSciNetGoogle Scholar
  48. 48.
    Berryman J G. Elastic wave propagation in fluid-saturated porous media. J Acoust Soc Am, 1981, 69: 416–424MATHCrossRefADSGoogle Scholar

Copyright information

© Science in China Press and Springer-Verlag GmbH 2008

Authors and Affiliations

  1. 1.Institute of AcousticsChinese Academy of SciencesBeijingChina

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