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Dynamic Instability in Geomaterials Associated with the Presence of Negative Stiffness Elements

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Part of the book series: Springer Series in Geomechanics and Geoengineering ((SSGG))

Abstract

One of the mechanisms of instability in geomaterials is associated with the descending branch of stress-strain curve caused by internal fracturing. The descending stress-strain curve can also be produced by negative stiffness elements, one of the mechanisms of negative stiffness being the rotation of non-spherical grains. The presence of negative stiffness elements can cause dynamic instability in the geomaterials. We investigate a simple elastic model of dynamic instability consisting of chains of oscillators some with negative stiffness springs. We show that in a stable chain only one oscillator can have negative stiffness spring and formulate the criterion of stability.

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Acknowledgments

The authors acknowledge the financial support through ARC Discovery Grant DP120102434.

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Correspondence to Elena Pasternak .

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© 2015 Springer International Publishing Switzerland

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Pasternak, E., Dyskin, A. (2015). Dynamic Instability in Geomaterials Associated with the Presence of Negative Stiffness Elements. In: Chau, KT., Zhao, J. (eds) Bifurcation and Degradation of Geomaterials in the New Millennium. IWBDG 2014. Springer Series in Geomechanics and Geoengineering. Springer, Cham. https://doi.org/10.1007/978-3-319-13506-9_23

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  • DOI: https://doi.org/10.1007/978-3-319-13506-9_23

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  • Publisher Name: Springer, Cham

  • Print ISBN: 978-3-319-13505-2

  • Online ISBN: 978-3-319-13506-9

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