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Shear instability in the subsurface layer of a material in friction

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Abstract

The shear instability in subsurface layers of a material in friction has been investigated. As the friction surface is approached, several characteristic regions can be distinguished in the bulk of the metal: the region of plastic deformation and texturing (I), the region of severe fragmentation (II), the region of turbulent flow (III), and the region of laminar flow (IV). Regions I and II can be referred to as regions of conventional plastic deformation, whereas regions III and IV correspond to regions of the development of shear instability of the Kelvin-Helmholtz type at the shear boundary. The possibility of implementing this phenomenon within the hydrodynamic approach has been evaluated.

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Authors and Affiliations

  1. Institute of Strength Physics and Materials Science, Siberian Branch, Russian Academy of Sciences, Akademicheskii pr. 2/4, Tomsk, 634021, Russia

    S. Yu. Tarasov & V. E. Rubtsov

Authors
  1. S. Yu. Tarasov
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  2. V. E. Rubtsov
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Correspondence to S. Yu. Tarasov.

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Original Russian Text © S.Yu. Tarasov, V.E. Rubtsov, 2011, published in Fizika Tverdogo Tela, 2011, Vol. 53, No. 2, pp. 336–340.

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Tarasov, S.Y., Rubtsov, V.E. Shear instability in the subsurface layer of a material in friction. Phys. Solid State 53, 358–362 (2011). https://doi.org/10.1134/S1063783411020302

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  • DOI: https://doi.org/10.1134/S1063783411020302

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