Propagation and attenuation characteristics of Rayleigh waves in the irregular bottom of the ocean in porous half-spaces

References

• Biot MA. Theory of propagation of elastic waves in a fluid-saturated porous solid. I. Low-frequency range. J Acoust Soc Am. 1956;28(2):168–178.
   Web of Science ®Google Scholar
• Biot MA. Theory of propagation of elastic waves in a fluid-saturated porous solid. II. Higher frequency range. J Acoust Soc Am. 1956;28(2):179–191.
   Web of Science ®Google Scholar
• Deresiewicz H, Rice JT. The effect of boundaries on wave propagation in a liquid-filled porous solid: V. Transmission across a plane interface. Bull Seismol Soc Am. 1964;54(1):409–416.
   Google Scholar
• Deresiewicz H, Levy A. The effect of boundaries on wave propagation in a liquid-filled porous solid: X. Transmission through a stratified medium. Bull Seismol Soc Am. 1967;57(3):381–391.
   Web of Science ®Google Scholar
• Corapcioglu MY. Wave propagation in porous media—a review. Transport Porous Med. 1991: 373–469.
   Google Scholar
• Berryman JG, Thigpen L, Chin RCY. Bulk elastic wave propagation in partially saturated porous solids. J Acoust Soc Am. 1988;84(1):360–373.
   Web of Science ®Google Scholar
• Berryman JG. Seismic wave attenuation in fluid-saturated porous media. Pure Appl Geophys. 1995;128(1-2):423–432.
   Google Scholar
• Zienkiewicz OC, Chang CT, Bettess P. Drained, undrained, consolidating and dynamic behaviour assumptions in solis. Géotechnique. 1980;30(4):385–395.
   Web of Science ®Google Scholar
• Zienkiewicz OC, Shiomi T. Dynamic behavior of saturated porous media: the generalized Biot formulation and its numerical solution. Int J Numer Anal Methods Geomech. 1984;8(1):71–96.
   Web of Science ®Google Scholar
• Huang M, Zienkiewicz OC. New unconditionally stable staggered solution procedures for coupled soil-pore fluid dynamic problems. Int J Numer Methods Eng. 1998;43:1029–1052.
   Web of Science ®Google Scholar
• Kumar R, Hundal BS. Surface wave propagation in a fluid saturated incompressible porous half-space lying under two layers of different liquids. Earth Planets Space. 2007;59(8):929–936.
   Web of Science ®Google Scholar
• Alam P, Kundu S, Gupta S, et al. Study of torsional wave in a poroelastic medium sandwiched between a layer and a half-space of heterogeneous dry sandy media. Waves Random Complex Media. 2018;28(1):182–201.
   Web of Science ®Google Scholar
• Kundu S, Alam P, Gupta S, et al. Impacts on the propagation of SH-waves in a heterogeneous viscoelastic layer sandwiched between an anisotropic porous layer and an initially stressed isotropic half-space. J Mech. 2017;33(1):13–22.
   Web of Science ®Google Scholar
• Eringen AC, Suhubi ES. Nonlinear theory of simple micro-elastic solids—I. Int J Eng Sci. 1964;2(2):189–203.
   Google Scholar
• Eringen C. Theory of micropolar fluids. J Math Mech. 1966;1(16):1–18.
   Google Scholar
• Tomar SK, Kumar R, Kaushik VP. Wave propagation of micropolar elastic medium with stretch. Int J Eng Sci. 1998;36(5):683–698.
   Web of Science ®Google Scholar
• Kumari A, Kundu S, Gupta S. Propagation and attenuation characteristics of Rayleigh waves induced due to irregular surface in liquid-saturated micropolar porous half-space. European Phys J Plus. 2019;134(11):1–12.
   Web of Science ®Google Scholar
• Mahmoodian M, Eskandari-Ghadi M, Nikkhoo A. Rayleigh, Love and Stoneley waves in a transversely isotropic saturated poroelastic media by means of potential method. Soil Dyn Earthq Eng. 2020;134:106139.
   Web of Science ®Google Scholar
• Zorammuana C, Singh SS. Elastic waves in thermoelastic saturated porous medium. Meccanica. 2016;51(3):593–609.
   Web of Science ®Google Scholar
• Singh SS, Tochhawng L. Stoneley and Rayleigh waves in thermoelastic materials with voids. J Vib Control. 2019;25(2):2053–2062.
   Google Scholar
• Lalvohbika J, Singh SS. Scattering of qSH-waves from a corrugated interface between two dissimilar nematic elastomers. Waves Random Complex Media. 2020: 1–24.
   Web of Science ®Google Scholar
• Paul P, Kundu S, Mandal D. Study of Rayleigh type surface wave in the initial stressed irregular bottom of ocean due to point source. Waves Random Complex Media. 2018;28(1):76–95.
   Web of Science ®Google Scholar
• Singh B, Kaur B. Propagation of Rayleigh waves in an incompressible rotating orthotropic elastic solid half-space with impedance boundary conditions. J Mech Behav Mater. 2017;26(3):73–78.
   Google Scholar
• Saha S, Singh AK, Chattopadhyay A. Impact of curved boundary on the propagation characteristics of Rayleigh-type wave and SH-wave in a prestressed monoclinic media. Mech Adv Mater Struct. 2019: 1–14.
   Web of Science ®Google Scholar
• Singh AK, Das A, Mistri KC, et al. Effect of corrugation on dispersion of Love-type wave in a layer with monoclinic symmetry, overlying an initially stressed transversely isotropic half-space. Multidiscip Model Mater Struct. 2017;13(2):308–325.
   Web of Science ®Google Scholar
• Asano S. Reflection and refraction of elastic waves at a corrugated interface. Bull Seismol Soc Am. 1966;56(1):201–221.
   Web of Science ®Google Scholar
• Gogna ML. Analysis of seismological data. Cambridge: Cambridge University; 1969.
   Google Scholar
• Vashisth AK, Gogna ML. The effect of loose boundaries on wave propagation in a porous solid: reflection and refraction of seismic waves across a plane interface. Int J Solids Struct. 1993;30(18):2485–2499.
   Web of Science ®Google Scholar
• Men F-l. Water propagation in porous, water-saturated viscoelastic media. Chin Sci Bull. 1966;11(3):142–142.
   Google Scholar
• Men F-l. One dimensional wave propagation in fluid-saturated porous elastic media. Acta Mathematica Scientia. 1984;04:467–476.
   Google Scholar
• Yew CH, Jogi PN. Study of wave motions in fluid-saturated porous rocks. J Acoust Soc Am. 1976;60(1):2–8.
   Web of Science ®Google Scholar
• Gubbins D. Seismology and plate tectonics. Space Technology. 1990.
   Google Scholar