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Journal ArticleDOI

Stiffness matrices for layered soils

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TLDR
In this article, the Haskell-Thompson transfer matrix method is used to derive layer stiffness matrices which may be interpreted and applied in the same way as stiffness matrix in conventional structural analysis, and the exact expressions are given for the matrices, as well as approximations for thin layers.
Abstract
The Haskell-Thompson transfer matrix method is used to derive layer stiffness matrices which may be interpreted and applied in the same way as stiffness matrices in conventional structural analysis These layer stiffness matrices have several advantages over the more usual transfer matrices: (1) they are symmetric; (2) fewer operations are required for analysis; (3) there is an easier treatment of multiple loadings; (4) substructuring techniques are readily applicable; and (5) asymptotic expressions follow naturally from the expressions (very thick layers; high frequencies, etc) While the technique presented is not more powerful than the original Haskell-Thompson scheme, it is nevertheless an elegant complement to it The exact expressions are given for the matrices, as well as approximations for thin layers Also, simple examples of application are presented to illustrate the use of the method

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Citations
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Proceedings ArticleDOI

Measurement and Modeling of Scholte Wave Dispersion in Coastal Waters

TL;DR: In this paper, a numerical model based on the dynamic stiffness matrix approach was developed to model the phase velocity dispersion of Scholte waves in the bottom of Narragansett Bay, Rhode Island.
Journal ArticleDOI

Geometric Seismic-Wave Inversion by the Boundary Element Method

TL;DR: In this article, a new class of geometric inverse models for a full waveform inversion (FWI) based on the boundary element method (BEM) is presented. And the proposed approach enables an effective identification of 2D subsurface geometries by directly estimating the shape of laterally varying interfaces from raw measurements.
Journal ArticleDOI

Ground response analysis using non-recursive matrix implementation of hybrid frequency-time domain (HFTD) approach

TL;DR: In this article, a Hybrid Frequency-Time Domain (HFTD) method was proposed for the solution of nonlinear ground response problem using non-recursive matrix approach, the displacements, caused by the bedrock acceleration, at the surface of layered soil are calculated while pseudo-forces due to nonlinear behavior of soil are obtained iteratively using an appropriate transformation scheme.
Journal ArticleDOI

On free wave propagation in anisotropic layered media

TL;DR: In this paper, the reverberation-ray matrix (MRRM) is extended and modified for the analysis of free wave propagation in anisotropic layered elastic media, and a general, numerically stable formulation is established within the state space framework.
References
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Book ChapterDOI

The Dispersion of Surface Waves on Multilayered Media

TL;DR: In this paper, a matrix formalism developed by W. T. Thomson is used to obtain the phase velocity dispersion equations for elastic surface waves of Rayleigh and Love type on multilayered solid media.
Journal ArticleDOI

Transmission of Elastic Waves through a Stratified Solid Medium

TL;DR: In this article, the transmission of a plane elastic wave at oblique incidence through a stratified solid medium consisting of any number of parallel plates of different material and thickness is studied theoretically.
Journal ArticleDOI

Shear Waves in Plane Infinite Structures

TL;DR: In this paper, a numerical procedure is developed for the dynamic analysis of plane, linearly elastic systems consisting of an irregular zone joined to semi-infinite layered zones, where all exciting forces are assumed to be harmonic and perpendicular to the plane of the structure.
Journal ArticleDOI

Lumped mass method for Rayleigh waves

TL;DR: In this paper, a simple numerical method is developed for the analysis of generalized Rayleigh waves in multilayered elastic media, which completely avoids the use of displacement potentials and leads to a simple eigenvalue problem which may be solved by generally available effective computer codes.