Surface Waves in Anisotropic and Laminated Bodies and Defects Detection by Rober

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The Nile on eBay FREE SHIPPING UK WIDE Surface Waves in Anisotropic and Laminated Bodies and Defects Detection by Robert V. Goldstein, Gérard A. Maugin Among the variety of wave motions one can single out surface wave pr- agation since these surface waves often adjust the features of the energy transfer in the continuum (system), its deformation and fracture. FORMAT Hardcover LANGUAGE English CONDITION Brand New Publisher Description Among the variety of wave motions one can single out surface wave pr- agation since these surface waves often adjust the features of the energy transfer in the continuum (system), its deformation and fracture. Predicted by Rayleigh in 1885, surface waves represent waves localized in the vicinity ofextendedboundaries(surfaces)of?uidsorelasticmedia. Intheidealcase of an isotropic elastic half-space while the Rayleigh waves propagate along the surface, the wave amplitude (displacement) in the transverse direction exponentially decays with increasing distance away from the surface. As a resulttheenergyofsurfaceperturbationsislocalizedbytheRayleighwaves within a relatively narrow layer beneath the surface. It is this property of the surface waves that leads to the resonance phenomena that accompany the motion of the perturbation sources (like surface loads) with velocities close to the Rayleigh one; (see e. g. , R. V. Goldstein. Rayleigh waves and resonance phenomena in elastic bodies. Journal of Applied Mathematics and Mechanics (PMM), 1965, v. 29, N 3, pp. 608-619). It is essential to note that resonance phenomena are also inherent to the elastic medium in the case where initially there are no free (unloaded) surfaces. However, they occur as a result of an external action accompanied by the violation of the continuity of certain physical quantities, e. g. , by crack nucleation and dynamic propagation. Note that the aforementioned resonance phenomena are related to the nature of the surface waves as homogeneous solutions (eigenfunctions) of the dynamic elasticity equations for a half-space (i. e. nonzero solutions at vanishing boundary conditions). Table of Contents On the Role of Anisotropy in Crystalloacoustics.- Surface Waves of Non-Rayleigh Type.- Nonlinearity in Elastic Surface Waves Acts Nonlocally.- Explicit Secular Equations for Surface Waves in an Anisotropic Elastic Half-Space from Rayleigh to Today.- "Nongeometrical Phenomena" in Propagation of Elastic Surface Waves.- Complex Rays and Internal Diffraction at the Cusp Edge.- Edge Waves in the Fluid Beneath an Elastic Sheet with Linear Nonhomogeneity.- On Continuum Modelling of Wave Propagation in Layered Medium; Bending Waves.- Edge Localised Bending Waves in Anisotropic Media: Energy and Dispersion.- Surface Electromagnetic Perturbations Induced by Unsteady-State Subsurface Flow.- Resonant Waves in a Structured Elastic Halfspace.- Numerical Analysis of Rayleigh Waves in Anisotropic Media.- Guided Waves in Anisotropic Media: Applications.- A General Purpose Computer Model for Calculating Elastic Waveguide Properties, with Application to Non-Destructive Testing.- The Influence of the Initial Stresses on the Dynamic Instability of an Anisotropic Cone.- Embedding Theorem and Mutual Relation for the Interface and Shear Wavespeeds.- The Non-Uniqueness of Constant Velocity Crack Propagation.- Embedding Formulae for Planar Cracks.- Wave Propogation and Crack Detection in Layered Structures. Long Description Among the variety of wave motions one can single out surface wave pr- agation since these surface waves often adjust the features of the energy transfer in the continuum (system), its deformation and fracture. Predicted by Rayleigh in 1885, surface waves represent waves localized in the vicinity ofextendedboundaries(surfaces)of'uidsorelasticmedia. Intheidealcase of an isotropic elastic half-space while the Rayleigh waves propagate along the surface, the wave amplitude (displacement) in the transverse direction exponentially decays with increasing distance away from the surface. As a resulttheenergyofsurfaceperturbationsislocalizedbytheRayleighwaves within a relatively narrow layer beneath the surface. It is this property of the surface waves that leads to the resonance phenomena that accompany the motion of the perturbation sources (like surface loads) with velocities close to the Rayleigh one; (see e. g. , R. V. Goldstein. Rayleigh waves and resonance phenomena in elastic bodies. Journal of Applied Mathematics and Mechanics (PMM), 1965, v. 29, N 3, pp. 608-619). It is essential to note that resonance phenomena are also inherent to the elastic medium in the case where initially there are no free (unloaded) surfaces. However, they occur as a result of an external action accompanied by the violation of the continuity of certain physical quantities, e. g. , by crack nucleation and dynamic propagation. Note that the aforementioned resonance phenomena are related to the nature of the surface waves as homogeneous solutions (eigenfunctions) of the dynamic elasticity equations for a half-space (i. e. nonzero solutions at vanishing boundary conditions). Details ISBN 1402023855 Short Title SURFACE WAVES IN ANISOTROPIC & Language English ISBN-10 1402023855 ISBN-13 9781402023859 Media Book Format Hardcover DEWEY 530.416 Series Number 163 Edited by Gérard A. Maugin Affiliation Institute for Problems in Mechanics Imprint Springer-Verlag New York Inc. Place of Publication New York, NY Country of Publication United States Pages 321 DOI 10.1023/b131128;10.1007/1-4020-2387-1 AU Release Date 2004-09-15 NZ Release Date 2004-09-15 US Release Date 2004-09-15 UK Release Date 2004-09-15 Author Gérard A. Maugin Publisher Springer-Verlag New York Inc. Edition Description 2004 ed. Series NATO Science Series II: Mathematics, Physics and Chemistry Year 2004 Edition 2004th Publication Date 2004-09-15 Alternative 9781402023866 Illustrations XI, 321 p. Audience Professional & Vocational Country of Origin NL Product Class Description Physics We've got this At The Nile, if you're looking for it, we've got it. With fast shipping, low prices, friendly service and well over a million items - you're bound to find what you want, at a price you'll love! 30 DAY RETURN POLICY No questions asked, 30 day returns! 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