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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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Fundamental Solutions for a Class of Continuously Inhomogeneous, Isotropic, and Anisotropic Materialn-plane and anti-plane conditions in closed form using the Radon transform. Of course, there are alternative methods such as algebraic transforms, Fourier transforms, and Hankel transforms, but the Radon transform is quite general and versatile.
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Green’s Function for the Inhomogeneous Isotropic Half-Planef the inhomogeneous in-depth half-plane. The reader will notice that it is possible to reuse fundamental solutions instead, but the traction-free boundary condition at the horizontal free surface will have to materialize through numerical discretization in a BIE formulation.
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Wave Scattering in a Laterally Inhomogeneous, Cracked Poroelastic Finite Region is that the medium under consideration is a two-phase material, namely a poroelastic continuum. To simplify the representation, we replace the two-phase material by a single-phase one that exhibits viscoelastic behavior, which is a plausible representation for low-frequency vibrations.
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Solid Mechanics and Its Applicationshttp://image.papertrans.cn/s/image/863912.jpg
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https://doi.org/10.1007/978-3-319-45206-7Seismic mechanics; Functionally graded materials; Heterogeneities; Boundary integral equation method; St
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State-of-the-Art for the BIEMhquakes. A quantitative prediction of strong ground motion manifestation at a given site involves dealing with the source of seismic waves, their path to that site, and the effects of local conditions. A possible way of shedding some light on the understanding of the site-response phenomena and thei
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Book 2017undary 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
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George D. Manolis,Petia S. Dineva,Tsviatko V. Rangelov,Frank Wuttkeely different view from the authors, Wu Yujiang and Wang Deren [4] rewrited our algorithm in the language of interval analysis, and also suggested a new globally convergent scheme in the case that F is strongly monotone. It showed the authors that the RCA is almost Nickel‘s Ball Newton Method [1] (a
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