Finite-difference time-domain method for modelling of seismic wave propagation in viscoelastic media

DOI10.1016/J.AMC.2014.03.029zbMath1334.74089OpenAlexW2005714538MaRDI QIDQ274955

F. Blanchet-Sadri, M. Dambrine

Publication date: 25 April 2016

Published in: Applied Mathematics and Computation (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/j.amc.2014.03.029

zbMATH Keywords

modellingfinite difference methodpropagationSH wavesviscoelastic medium

Mathematics Subject Classification ID

Soil and rock mechanics (74L10) Seismology (including tsunami modeling), earthquakes (86A15) Finite difference methods for initial value and initial-boundary value problems involving PDEs (65M06) Linear constitutive equations for materials with memory (74D05) Linear waves in solid mechanics (74J05) Finite volume methods applied to problems in solid mechanics (74S10)

Related Items (5)

A piecewise partitioning scaled boundary finite element algorithm to solve viscoelastic problems with cyclic symmetry ⋮ A Diagonalization-Based Parallel-in-Time Algorithm for Crank-Nicolson’s Discretization of the Viscoelastic Equation ⋮ Perfectly matched layer and infinite element coupled with finite elements for SH waves in an imperfect piezoelectric viscoelastic structure ⋮ Schemes in generalized finite differences for seismic wave propagation in Kelvin-Voight viscoelastic media ⋮ Direct Sturm-Liouville problem for surface love waves propagating in layered viscoelastic waveguides

Cites Work

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• Transmission of shear waves through a self-reinforced layer sandwiched between two inhomogeneous viscoelastic half-spaces
• Viscoelastic surface waves of an assigned wavelength
• Reflection and refraction of \(SH\)-waves at a corrugated interface between two laterally and vertically heterogeneous viscoelastic solid half-spaces
• Random wave propagation in a viscoelastic layered half space

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