2014
DOI: 10.1061/(asce)em.1943-7889.0000706
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Transient Dynamic Analysis of Gradient-Saturated Viscoelastic Porous Media

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Cited by 5 publications
(4 citation statements)
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“…Based on this theory, the complex dispersion equation for Love waves is derived for transversely isotropic fluid-saturated porous media with exponential and linear variation of shear modulus [23][24]. The dispersion behaviour of plane wave [25], Rayleigh wave [26] and transient response of viscoelastic porous medium [27], are analysed in the inhomogeneous saturated soil with gradient variation of mechanical properties along the depth. However, it should be noted that none of these studies examine the problem of amplification of the porous soil response.…”
Section: Introductionmentioning
confidence: 99%
“…Based on this theory, the complex dispersion equation for Love waves is derived for transversely isotropic fluid-saturated porous media with exponential and linear variation of shear modulus [23][24]. The dispersion behaviour of plane wave [25], Rayleigh wave [26] and transient response of viscoelastic porous medium [27], are analysed in the inhomogeneous saturated soil with gradient variation of mechanical properties along the depth. However, it should be noted that none of these studies examine the problem of amplification of the porous soil response.…”
Section: Introductionmentioning
confidence: 99%
“…Analytical methods are usually based on the wave function expansion . Numerical methods include the finite element method, the finite difference method, spectral element method, boundary element method (BEM), discrete wave number method, and other boundary types or hybrid methods . The literature reviews summarized more studies in this field.…”
Section: Introductionmentioning
confidence: 99%
“…In reality, the soil is a porous medium and often saturated with fluid, especially in coastal areas; however, because of the substantial computational effort required to obtain the seismic behavior of inhomogeneous saturated poroviscoelastic soil profile, very few studies applying Biot’s theory (Biot 1956a, 1956b, 1962) can be found; Ke et al (2005, 2006) assumed an exponential and linear variations of the shear modulus and derived the complex dispersion equation of Love waves in transversely isotropic fluid saturated porous media. Moreover, the dispersion behavior of plane wave (Zhou et al , 2013) and Rayleigh wave (Zhou and Ma, 2016) and the transient response (Zhou, 2013) are analyzed in inhomogeneous saturated soil with gradient variation of mechanical properties with depth; it should be noted that the formulas proposed to describe the inhomogeneous shear modulus of saturated porous soil profile are not realistic models and don’t take into account the geotechnical soil properties, which can change the free-field ground motion.…”
Section: Introductionmentioning
confidence: 99%