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Torsional surface waves in a gradient-elastic half-space

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dc.contributor.author Georgiadis, HG en
dc.contributor.author Vardoulakis, I en
dc.contributor.author Lykotrafitis, G en
dc.date.accessioned 2014-03-01T01:15:56Z
dc.date.available 2014-03-01T01:15:56Z
dc.date.issued 2000 en
dc.identifier.issn 0165-2125 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/13841
dc.subject Dispersion Curve en
dc.subject Exponential Decay en
dc.subject Free Surface en
dc.subject hankel transform en
dc.subject Layered Structure en
dc.subject Linear Elasticity en
dc.subject Material Properties en
dc.subject Surface Acoustic Wave en
dc.subject Surface Wave en
dc.subject Wave Propagation en
dc.subject Electric and Magnetic Fields en
dc.subject Shear Horizontal en
dc.subject.classification Acoustics en
dc.subject.classification Mechanics en
dc.subject.classification Physics, Multidisciplinary en
dc.subject.other ENERGY en
dc.title Torsional surface waves in a gradient-elastic half-space en
heal.type journalArticle en
heal.identifier.primary 10.1016/S0165-2125(99)00035-9 en
heal.identifier.secondary http://dx.doi.org/10.1016/S0165-2125(99)00035-9 en
heal.language English en
heal.publicationDate 2000 en
heal.abstract The present work deals with torsional wave propagation in a linear gradient-elastic half-space. More specifically, we prove that torsional surface waves (i.e. waves with amplitudes exponentially decaying with distance from the free surface) do exist in a homogeneous gradient-elastic half-space. This finding is in contrast with the well-known result of the classical theory of linear elasticity that torsional surface waves do not exist in a homogeneous half-space. The weakness of the classical theory, at this point, is only circumvented by modeling the half-space as having material properties variable with depth (E. Meissner, Elastische Oberflachenwellen mit Dispersion in einem inhomogenen Medium, Vierteljahrsschrift der Naturforschenden Gesellschaft in Zurich 66 (1921) 181-195; I. Vardoulakis, Torsional surface waves in inhomogeneous elastic media, Internat. J. Numer. Anal. Methods Geomech. 8 (1984) 287-296; G.A. Maugin, Shear horizontal surface acoustic waves on solids, in: D.E Parker, G.A. Maugin (Eds.), Recent Developments in Surface Acoustic Waves, Springer Series on Wave Phenomena, vol. 7, Springer, Berlin, 1988, pp. 158-172), as a layered structure (Maugin, 1988; E. Reissner, Freie und erzwungene Torsionsschwingungen des elastischen Halbraumes, Ingenieur-Archiv 8 (1937) 229-245) or by considering couplings with electric and magnetic fields for different types of materials (Maugin, 1988). The theory employed here is the simplest possible version of Mindlin's (R.D. Mindlin, Micro-structure in linear elasticity, Arch. Rat. Mech. Anal. 16 (1964) 51-78) generalized linear elasticity. A simple wave-propagation analysis based on Hankel transforms and complex-variable theory was done in order to determine the conditions for the existence of the torsional surface motions and to derive dispersion curves and cut-off frequencies. Also, we notice that, up to date, no other generalized linear continuum theory (including the integral-type non-local theory) has successfully been proposed to predict torsional surface waves in a homogeneous half-space. (C) 2000 Elsevier Science B.V. All rights reserved. en
heal.publisher ELSEVIER SCIENCE BV en
heal.journalName WAVE MOTION en
dc.identifier.doi 10.1016/S0165-2125(99)00035-9 en
dc.identifier.isi ISI:000086536400003 en
dc.identifier.volume 31 en
dc.identifier.issue 4 en
dc.identifier.spage 333 en
dc.identifier.epage 348 en


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