2022
DOI: 10.1016/j.compgeo.2022.104763
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Effect of flow-independent viscosity on the propagation behavior of Rayleigh wave in partially saturated soil based on the fractional standard linear solid model

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Cited by 16 publications
(8 citation statements)
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“…Employing the mixture theory and considering the FSLS model, the generalized governing equations for elastic waves propagation in three‐phase porous media are described as 36 trueμ¯()ωui,jjbadbreak+[]C11()ω+trueμ¯()ωuj,jigoodbreak+C12()ωwj,jigoodbreak+C13()ωvj,jigoodbreak=ρüigoodbreak+ρwẅigoodbreak+ρgv̈i$$\begin{equation}\bar \mu \left( \omega \right){u_{i,jj}} + \left[ {{C_{11}}\left( \omega \right) + \bar \mu \left( \omega \right)} \right]{u_{j,ji}} + {C_{12}}\left( \omega \right){w_{j,ji}} + {C_{13}}\left( \omega \right){v_{j,ji}} = \rho {\ddot u_i} + {\rho _w}{\ddot w_i} + {\rho _g}{\ddot v_i}\end{equation}$$ C21()ωuj,jibadbreak+C22()ωwj,jigoodbreak+C23()ωvj,jigoodbreak=ρwüigoodbreak+ρwẅi/0ptρwẅiϕSw0.0ptϕSwgoodbreak+μwẇi/0ptμwẇikrwk0.0ptkrwk$$\begin{equation}{C_{21}}\left( \omega \right){u_{j,ji}} + {C_{22}}\left( \omega \right){w_{j,ji}} + {C_{23}}\left( \omega \right){v_{j,ji}} = {\rho _w}{\ddot u_i} ...…”
Section: Computational Model and Basic Equationsmentioning
confidence: 99%
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“…Employing the mixture theory and considering the FSLS model, the generalized governing equations for elastic waves propagation in three‐phase porous media are described as 36 trueμ¯()ωui,jjbadbreak+[]C11()ω+trueμ¯()ωuj,jigoodbreak+C12()ωwj,jigoodbreak+C13()ωvj,jigoodbreak=ρüigoodbreak+ρwẅigoodbreak+ρgv̈i$$\begin{equation}\bar \mu \left( \omega \right){u_{i,jj}} + \left[ {{C_{11}}\left( \omega \right) + \bar \mu \left( \omega \right)} \right]{u_{j,ji}} + {C_{12}}\left( \omega \right){w_{j,ji}} + {C_{13}}\left( \omega \right){v_{j,ji}} = \rho {\ddot u_i} + {\rho _w}{\ddot w_i} + {\rho _g}{\ddot v_i}\end{equation}$$ C21()ωuj,jibadbreak+C22()ωwj,jigoodbreak+C23()ωvj,jigoodbreak=ρwüigoodbreak+ρwẅi/0ptρwẅiϕSw0.0ptϕSwgoodbreak+μwẇi/0ptμwẇikrwk0.0ptkrwk$$\begin{equation}{C_{21}}\left( \omega \right){u_{j,ji}} + {C_{22}}\left( \omega \right){w_{j,ji}} + {C_{23}}\left( \omega \right){v_{j,ji}} = {\rho _w}{\ddot u_i} ...…”
Section: Computational Model and Basic Equationsmentioning
confidence: 99%
“…The Kelvin-Voigt model has been reported to be weak in describing the instantaneous deformation of the soil skeleton and thus has some restrictions in the study on soil dynamic behaviors. 36 In light of the above, Liu et al 36 constructed a new viscoelastic dynamic governing equations for unsaturated soils utilizing the fractional-order standard linear solid (FSLS) model and studied the influence of model parameters on elastic wave propagation. Naturally, the utilization of more refined soil models for the study of pile-soil interactions is of great significance for practical engineering applications.…”
Section: Introductionmentioning
confidence: 99%
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