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Changes in the surface structure of the heterogeneous body (diorite) under friction

  • Mechanical Properties, Physics of Strength, and Plasticity
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Abstract

Raman, infrared, and photoluminescent spectroscopy has been used to study changes in the surface structure of quartz diorite caused by friction. Before friction, the diorite surface layer has contained mainly quartz and feldspar crystals. After friction, some quartz and feldspar crystals have been destructed and replaced by a newly formed hydromica mineral with a low friction coefficient such as illite.

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Authors and Affiliations

  1. Ioffe Institute, Russian Academy of Sciences, St. Petersburg, 194021, Russia

    V. I. Vettegren, V. B. Kulik, R. I. Mamalimov & I. P. Shcherbakov

  2. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, 123995, Russia

    A. V. Ponomarev & G. A. Sobolev

  3. Peter the Great Saint Petersburg Polytechnic University, St. Petersburg, 195251, Russia

    A. Ya. Bashkarev

Authors
  1. V. I. Vettegren
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  2. A. V. Ponomarev
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  3. G. A. Sobolev
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  4. V. B. Kulik
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  5. R. I. Mamalimov
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  6. I. P. Shcherbakov
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  7. A. Ya. Bashkarev
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Corresponding author

Correspondence to V. I. Vettegren.

Additional information

Original Russian Text © V.I. Vettegren, A.V. Ponomarev, G.A. Sobolev, V.B. Kulik, R.I. Mamalimov, I.P. Shcherbakov, A.Ya. Bashkarev, 2018, published in Fizika Tverdogo Tela, 2018, Vol. 60, No. 1, pp. 127–131.

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Vettegren, V.I., Ponomarev, A.V., Sobolev, G.A. et al. Changes in the surface structure of the heterogeneous body (diorite) under friction. Phys. Solid State 60, 129–133 (2018). https://doi.org/10.1134/S1063783418010286

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  • DOI: https://doi.org/10.1134/S1063783418010286

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