Abstract
In anisotropic fluid-saturated porous solids, four waves can propagate along a general phase direction. However, solid particles in different waves may not vibrate in mutually orthogonal directions. In the propagation of each of these waves, the displacement of pore–fluid particles may not be parallel to that of solid particles. The polarization for a wave is the direction of aggregate displacement of the particles of the two constituents of a porous aggregate. These polarizations, for different waves, are not mutually orthogonal. Out of the four waves in anisotropic poroelastic medium, two are termed as quasi-longitudinal waves. The prefix ‘quasi’ refers to their polarization being nearly, but not exactly, parallel to the direction of propagation. The existence of purely longitudinal waves in an anisotropic poroelastic medium is ensured by the stationary characters of two expressions. These expressions involve the elastic (stiffness and coupling) coefficients of a porous aggregate and the components of phase direction. Necessary and sufficient conditions for the existence of longitudinal waves are discussed for different anisotropic symmetries. Conditions are also discussed for the existence of the apparent longitudinal waves, i.e., the propagation of wave motion with the particle displacement parallel to the ray direction instead of the phase direction. A graphical solution of a numerical example is shown to check the existence of these apparent longitudinal waves for general directions of phase propagation.
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References
Borgnis F.E.: Specific directions of longitudinal wave propagation in anisotropic media. Phys. Rev. 98, 1000–1005 (1955)
Brugger K.: Pure modes for elastic waves in crystals. J. Appl. Phys. 36, 759–768 (1965)
Truesdell C.: Existence of longitudinal waves. J. Acoust. Soc. Am. 40, 729–730 (1996)
Cazzani A., Rovati M.: Extrema of Young’s modulus for elastic solids with tetragonal symmetry. Int. J. Solids Struct. 42, 5057–5096 (2005)
Ting T.C.T.: Longitudinal and transverse waves in anisotropic elastic materials. Acta Mech. 185, 147–164 (2006)
Biot M.A.: The theory of propagation of elastic waves in a fluid-saturated porous solid, I. Low-frequency range, II. Higher frequency range. J. Acoust. Soc. Am. 28, 168–191 (1956)
Biot M.A.: Mechanics of deformation and acoustic propagation in porous media. J. Appl. Phys. 33, 1482–1498 (1962)
Biot M.A.: Generalized theory of acoustic propagation in porous dissipative media. J. Acoust. Soc. Am. 34, 1254–1264 (1962)
Mengi Y., McNiven H.D.: Propagation and decay of waves in porous media. J. Acoust. Soc. Am. 64, 1125–1131 (1978)
Schmitt D.P.: Acoustical multipole logging in transversely isotropic poroelastic formations. J. Acoust. Soc. Am. 86, 2397–2421 (1989)
Sharma M.D., Gogna M.L.: Wave propagation in liquid-saturated porous solids. J. Acoust. Soc. Am. 90, 1068–1073 (1991)
Thomsen L.: Elastic anisotropy due to aligned cracks in a porous rock. Geophys. Prosp. 43, 805–829 (1995)
Rathore J.S., Fjaer E., Holt R.M., Renlie L.: P- and S-wave anisotropy of a synthetic sandstone with controlled crack geometry. Geophys. Prosp. 43, 711–728 (1995)
Sharma M.D.: Surface wave propagation in a cracked poroelastic half-space lying under a uniform layer of fluid. Geophys. J. Int. 127, 31–39 (1996)
Hudson J.A., Liu E., Crampin S.: The mechanical properties of materials with interconnected cracks and pores. Geophys. J. Int. 124, 105–112 (1996)
Carcione J.M.: Wave Fields in Real Media: Wave propagation in anisotropic, anelastic and porous media. Pergamon Press, New York (2001)
Tod S.R.: The effects of stress and fluid pressure on the anisotropy of interconnected cracks. Geophys. J. Int. 149, 149–156 (2002)
Sharma M.D.: Three-dimensional wave propagation in a general anisotropic poroelastic medium: phase velocity, group velocity and polarization. Geophys. J. Int. 156, 329–344 (2004)
Sharma M.D.: Wave propagation in a general anisotropic poroelastic medium with anisotropic permeability: phase velocity and attenuation. Int. J. Solids Struct. 41, 4587–4597 (2004)
Johnson D.L., Koplik J., Dashen R.: Theory of dynamic permeability and tortuosity in fluid-saturated porous media. J. Fluid Mech. 176, 379–402 (1987)
Albert D.G.: A comparison between wave propagation in water-saturated and air-saturated porous materials. J. Appl. Phys. 73, 28–36 (1993)
Sharma M.D.: Group velocity along general direction in a general anisotropic medium. Int. J. Solids Struct. 39, 3277–3288 (2002)
Rasolofosaon P.N.J., Zinszner B.E.: Comparison between permeability anisotropy and elasticity anisotropy of reservoir rocks. Geophysics 67, 230–240 (2002)
Helbig K.: Foundations of Anisotropy for Exploration Seismics. Pergamon Press, New York (1994)
Synge J.L.: Flux of energy for elastic waves in anisotropic media. Proc. R.I.A. 58, 13–21 (1956)
Chadwick P., Whitworth A.M., Borejko P.: Basic theory of small-amplitude waves in a constrained elastic body. Arch. Rat. Mech. Anal. 87, 339–354 (1985)
Borejko P.: Inhomogeneous plane waves in a constrained elastic body. Q. J. Mech. Appl. Math. 40, 71–87 (1987)
Ben-Menahem A., Sena A.G.: Seismic source theory in stratified anisotropic media. J. Geophys. Res. 95, 15395–15427 (1990)
Crampin S., McGonigle R.: The variations of delays in stress induced polarisation anomalies. Geophys. J. R. Astro. Soc. 64, 115–131 (1981)
Aki K., Richards P.G.: Quantitative Seismology, Theory and Methods. Freeman, New York (1980)
Ben-Menahem A., Singh S.J.: Seismic Waves and Sources. Springer, New York (1981)
Ben-Menahem A., Gibson R.L. Jr., Sena A.G.: Green’s tensor and radiation patterns of point sources in general anisotropic inhomogeneous elastic media. Geophys. J. Int. 107, 297–308 (1991)
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Sharma, M.D. Existence of longitudinal waves in anisotropic poroelastic solids. Acta Mech 208, 269–280 (2009). https://doi.org/10.1007/s00707-009-0153-8
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DOI: https://doi.org/10.1007/s00707-009-0153-8