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Titlebook: Seismic Wave Propagation in Non-Homogeneous Elastic Media by Boundary Elements; George D. Manolis,Petia S. Dineva,Frank Wuttke Book 2017 S

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发表于 2025-3-21 18:43:47 | 显示全部楼层 |阅读模式
书目名称Seismic Wave Propagation in Non-Homogeneous Elastic Media by Boundary Elements
编辑George D. Manolis,Petia S. Dineva,Frank Wuttke
视频video
概述Offers a step-by-step tutorial on the application of boundary integral equation methods in mechanics.Includes a methodology for the numerical modeling of elastic wave propagation problems.Presents tes
丛书名称Solid Mechanics and Its Applications
图书封面Titlebook: Seismic Wave Propagation in Non-Homogeneous Elastic Media by Boundary Elements;  George D. Manolis,Petia S. Dineva,Frank Wuttke Book 2017 S
描述.This book focuses on the mathematical potential and computational efficiency of the Boundary Element Method (BEM) for modeling seismic wave propagation in either continuous or discrete inhomogeneous elastic/viscoelastic, isotropic/anisotropic media containing multiple cavities, cracks, inclusions and surface topography. BEM models may take into account the entire seismic wave path from the seismic source through the geological deposits all the way up to the local site under consideration..The general presentation of the theoretical basis of elastodynamics for inhomogeneous and heterogeneous continua in the first part is followed by the analytical derivation of fundamental solutions and Green‘s functions for the governing field equations by the usage of Fourier and Radon transforms. The numerical implementation of the BEM is for antiplane in the second part as well as for plane strain boundary value problems in the third part. Verification studies and parametric analysis appearthroughout the book, as do both recent references and seminal ones from the past..Since the background of the authors is in solid mechanics and mathematical physics, the presented BEM formulations are valid f
出版日期Book 2017
关键词Seismic mechanics; Functionally graded materials; Heterogeneities; Boundary integral equation method; St
版次1
doihttps://doi.org/10.1007/978-3-319-45206-7
isbn_softcover978-3-319-83238-8
isbn_ebook978-3-319-45206-7Series ISSN 0925-0042 Series E-ISSN 2214-7764
issn_series 0925-0042
copyrightSpringer International Publishing Switzerland 2017
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发表于 2025-3-21 22:20:39 | 显示全部楼层
Anti-plane Strain Wave Motion in Unbounded Inhomogeneous Mediaterest. Furthermore, numerical results are given for the heterogeneous, orthotropic half-plane. The BIEM formulation computes the scattered wave field, gives the incident wave field, and further determines displacements and stresses at select points of the boundary-value problem at hand.
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Book 2017on in either continuous or discrete inhomogeneous elastic/viscoelastic, isotropic/anisotropic media containing multiple cavities, cracks, inclusions and surface topography. BEM models may take into account the entire seismic wave path from the seismic source through the geological deposits all the w
发表于 2025-3-22 14:25:56 | 显示全部楼层
Site Effects in Finite Geological Region Due to Wavepath Inhomogeneityese studies are useful within the context of earthquake engineering and the design of infrastructure in seismically prone regions. The complexity of these problems necessitates the use of hybrid computational techniques, where the BIEM accounts for the vast bulk of the geological medium surrounding the near site region.
发表于 2025-3-22 20:36:38 | 显示全部楼层
State-of-the-Art for the BIEMiscussed, together with applications to seismic wave propagation problems. More specifically, a closer look with scales of hundreds of . reveals the Earth is both strongly inhomogeneous with a sharp gradient of variation of its material properties and also heterogeneous due to the existence of free
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Wave Propagations in Inhomogeneous Isotropic/Orthotropic Half-Planescally, quadratic and exponential variations of the inhomogeneity in terms of the depth coordinate are considered for both the isotropic and the orthotropic half-plane, and wave motion in these media is mathematically reconstructed.
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