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On the stress field in a half-plane covered by the pre-stretched layer under the action of arbitrary linearly located time-harmonic forces

dc.contributor.authorAkbarov, S. D.
dc.contributor.authorGuler, C.
dc.date.accessioned2026-06-27T13:04:55Z
dc.date.issued2007
dc.description.abstractWithin the framework of the piecewise homogeneous body model with the use of the Three-Dimensional Linearized Theory of Elastic Waves in Initially Stressed Bodies the stress field in a half-plane covered by the pre-stretched layer under the action of the inclined linearly located time-harmonic forces is investigated. The algorithm for obtaining numerical results is proposed. Concrete numerical results are presented for the pair of materials Aluminium, (layer) + Steel (halfplane) as well as for Steel (layer) + Aluminium (half-plane). These numerical results are involved in the normal stress acting on the interface plane. The dependencies between this stress and the frequency of the external force and the influence of the pre-stretching of the covering layer on these dependencies is analysed. (c) 2006 Elsevier Inc. All rights reserved.en
dc.description.urihttps://doi.org/10.1016/j.apm.2006.09.004
dc.identifier.doi10.1016/j.apm.2006.09.004
dc.identifier.eissn1872-8480
dc.identifier.endpage2390
dc.identifier.issn0307-904X
dc.identifier.issue11
dc.identifier.startpage2375
dc.identifier.urihttps://hdl.handle.net/20.500.14981/49445
dc.identifier.volume31
dc.identifier.wos000248968100001
dc.language.isoeng
dc.publisherELSEVIER SCIENCE INC
dc.relation.ispartofAPPLIED MATHEMATICAL MODELLING
dc.subjectLamb's problem
dc.subjectinitial stress
dc.subjecthalf-plane
dc.subjectcovered layer
dc.subjecttime-harmonic loading
dc.subjectfrequency
dc.subjectWAVE PROPAGATION
dc.subjectSURFACE
dc.subjectEngineering
dc.subjectMathematics
dc.subjectMechanics
dc.titleOn the stress field in a half-plane covered by the pre-stretched layer under the action of arbitrary linearly located time-harmonic forces
dc.typeArticle
dspace.entity.typePublication
local.import.sourceWOS

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