Please use this identifier to cite or link to this item: https://dspace.iiti.ac.in/handle/123456789/6559
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dc.contributor.authorManna, Santanuen_US
dc.date.accessioned2022-03-17T01:00:00Z-
dc.date.accessioned2022-03-21T10:49:48Z-
dc.date.available2022-03-17T01:00:00Z-
dc.date.available2022-03-21T10:49:48Z-
dc.date.issued2021-
dc.identifier.citationManna, S., Halder, T., & Althobaiti, S. N. (2022). Dispersion of love-type wave and its limitation in a nonlocal elastic model of nonhomogeneous layer upon an orthotropic extended medium. Soil Dynamics and Earthquake Engineering, 153 doi:10.1016/j.soildyn.2021.107117en_US
dc.identifier.issn0267-7261-
dc.identifier.otherEID(2-s2.0-85121673276)-
dc.identifier.urihttps://doi.org/10.1016/j.soildyn.2021.107117-
dc.identifier.urihttps://dspace.iiti.ac.in/handle/123456789/6559-
dc.description.abstractThis research paper investigates the Love-type surface wave dispersion in a nonlocal elastic nonhomogeneous medium over a nonlocal orthotropic semi-infinite medium under the effect of interior initial stress component. A generalized linear elasticity theory with the nonlocal effect in the fundamental stress-strain relation is adopted to address the equation of motion in layered media. In the case of time-harmonic plane wave propagation, PDEs (cf. equations of motion) of the nonlocal elasticity are reduced to closed-form singular differential equations. The equation of dispersive wave is derived using appropriate plane stress-displacement-continuity conditions of the model. The dispersion of Love-type wave and its limitation in a nonlocal elastic media are analysed graphically using MATLAB software. For the specific model, it is observed that the attenuation of the dispersion of Love-type wave depends on a nonlocal parameter. Also, the dispersive wave becomes nondispersive with zero attenuation for large values (∼0.4) of the nonlocal parameter. In the case of dispersive wave, variation of the phase velocity of the fundamental wave mode for different values of nonlocality, nonhomogeneity, wave number and initial stress parameters are shown graphically. Some special cases are deduced from the original dispersion equation and validated with the published literature. © 2021 Elsevier Ltden_US
dc.language.isoenen_US
dc.publisherElsevier Ltden_US
dc.sourceSoil Dynamics and Earthquake Engineeringen_US
dc.subjectDispersion (waves)en_US
dc.subjectEquations of motionen_US
dc.subjectMATLABen_US
dc.subjectStress-strain curvesen_US
dc.subjectSurface wavesen_US
dc.subjectWave propagationen_US
dc.subjectDispersive wavesen_US
dc.subjectElastic modelsen_US
dc.subjectEquation of motionen_US
dc.subjectInitial stressen_US
dc.subjectLove waveen_US
dc.subjectLove-type wavesen_US
dc.subjectNon-local elasticitiesen_US
dc.subjectNonhomogeneityen_US
dc.subjectNonlocalen_US
dc.subjectOrthotropicen_US
dc.subjectElasticityen_US
dc.titleDispersion of Love-type wave and its limitation in a nonlocal elastic model of nonhomogeneous layer upon an orthotropic extended mediumen_US
dc.typeJournal Articleen_US
Appears in Collections:Department of Mathematics

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