Please use this identifier to cite or link to this item: https://dspace.iiti.ac.in/handle/123456789/6645
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dc.contributor.authorManna, Santanuen_US
dc.date.accessioned2022-03-17T01:00:00Z-
dc.date.accessioned2022-03-21T10:50:02Z-
dc.date.available2022-03-17T01:00:00Z-
dc.date.available2022-03-21T10:50:02Z-
dc.date.issued2018-
dc.identifier.citationManna, S., Misra, J. C., Kundu, S., & Gupta, S. (2018). Surface wave propagation in an initially stressed heterogeneous medium having a sandy layer and a point source. Geomechanics and Engineering, 16(2), 169-176. doi:10.12989/gae.2018.16.2.169en_US
dc.identifier.issn2005-307X-
dc.identifier.otherEID(2-s2.0-85056340273)-
dc.identifier.urihttps://doi.org/10.12989/gae.2018.16.2.169-
dc.identifier.urihttps://dspace.iiti.ac.in/handle/123456789/6645-
dc.description.abstractAn attempt has been made here to study the propagation of SH-type surface waves in an elastic medium, which is initially stressed and heterogeneous and has a point source inside the medium. The upper portion of the composite medium is a sandy layer. It is situated on an initially stressed heterogeneous half-space, whose density, rigidity and internal friction are function of depth. The analysis has been carried out by using Fourier transform and Green’s function approach. The phase velocity has been investigated for several particular situations. It has been shown that the results of the study agree with those the case of Love wave propagation in a homogeneous medium in the absence of the sandy layer, when the initial stress is absent. In order to illustrate the validity of the analysis presented here, the derived analytical expression has been computed numerically, by considering an illustrative example and the variances of the concerned physical variables have been presented graphically. It is observed that the velocity of shear wave is amply influenced by the initial stress and heterogeneity parameters and the presence of the sandy layer. The study has an important bearing on investigations of different problems in the earth’s interior and also in seismological studies. © 2018 Techno-Press, Ltd.en_US
dc.language.isoenen_US
dc.publisherTechno Pressen_US
dc.sourceGeomechanics and Engineeringen_US
dc.subjectGeometryen_US
dc.subjectGreen's functionen_US
dc.subjectPhase velocityen_US
dc.subjectShear wavesen_US
dc.subjectSurface wavesen_US
dc.subjectAnalytical expressionsen_US
dc.subjectComposite mediumen_US
dc.subjectDispersion equationsen_US
dc.subjectHeterogeneityen_US
dc.subjectHeterogeneous mediumen_US
dc.subjectHomogeneous mediumen_US
dc.subjectInitially stresseden_US
dc.subjectPhysical variablesen_US
dc.subjectShear flowen_US
dc.titleSurface wave propagation in an initially stressed heterogeneous medium having a sandy layer and a point sourceen_US
dc.typeJournal Articleen_US
Appears in Collections:Department of Mathematics

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