Journal
JOURNAL OF VIBRATION AND CONTROL
Volume 28, Issue 3-4, Pages 396-409Publisher
SAGE PUBLICATIONS LTD
DOI: 10.1177/1077546320977716
Keywords
Elastic-plastic; anisotropic; orthotropic; transversely isotropic; voids; dislocation
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Funding
- Council of Scientific and Industrial Research, New Delhi [09/135(0817)/2018-EMR-1]
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A dispersion equation is derived for the propagation of one-dimensional plane waves in a general linear anisotropic isothermal elastic-plastic material with voids. The plasticity of the material is defined through the dislocation of a single slip plane and direction. It is found that there are four basic waves traveling at different speeds in these specific anisotropic elastic-plastic materials with voids. A new wave appears due to the presence of plasticity in the material. Out of the four waves in orthotropic/transversely isotropic materials with voids, one wave is independent of plasticity and voids, while the remaining three waves depend on plasticity and voids.
Dispersion equation is derived for the propagation of one-dimensional plane waves in a general linear anisotropic isothermal elastic-plastic material with voids. The plasticity of the considered material is defined through the dislocation of a single slip plane and direction. The derived dispersion equation is then reduced for the relevant wave propagation in particular media, namely, monoclinic, orthotropic, transversely isotropic, and isotropic elastic-plastic material with voids. In general, it is found that there exist four basic waves traveling with distinct speeds in these specific anisotropic elastic-plastic materials with voids. A new wave is found to appear because of the presence of plasticity in the material. Out of the four basic waves traveling in an orthotropic/transversely isotropic material with voids, a wave travels independent of plasticity and void parameters, whereas the remaining three waves depend on plasticity as well as on the presence of voids. The one which is traveling independent of plasticity and voids is nondispersive and nonattenuating, whereas the other waves are dispersive in nature. The speeds of all the existing waves are computed numerically for a specific model, displayed graphically, and discussed.
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