Nanosecond dynamics of destruction of the surface layer of a heterogeneous nanocrystalline solid (sandstone) under the friction


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It has been found that the friction of a heterogeneous material, namely, sandstone, leads to the appearance of triboluminescence. The phenomenon of triboluminescence corresponds to luminescence of ≡Si–O free radicals and Fe3+ ions. These radicals and ions are formed as a result of the breaking of Si–O–Si bonds in nanocrystals of quartz and feldspar entering into the composition of the sandstone. The time dependence of the triboluminescence intensity represents a set of flashes, each having the duration of a few nanoseconds. It has been assumed that triboluminescence flashes correspond to the appearances of cracks in the material. Сrack opening is found to be approximately 180 nm. The size distribution of the cracks is exponential.

Sobre autores

G. Sobolev

Schmidt Institute of Physics of the Earth

Email: Victor.Vettegren@mail.ioffe.ru
Rússia, ul. Bol’shaya Gruzinskaya 10–1, Moscow, 123242

A. Ponomarev

Schmidt Institute of Physics of the Earth

Email: Victor.Vettegren@mail.ioffe.ru
Rússia, ul. Bol’shaya Gruzinskaya 10–1, Moscow, 123242

I. Shcherbakov

Ioffe Institute

Email: Victor.Vettegren@mail.ioffe.ru
Rússia, Politekhnicheskaya ul. 26, St. Petersburg, 194021

R. Mamalimov

Ioffe Institute

Email: Victor.Vettegren@mail.ioffe.ru
Rússia, Politekhnicheskaya ul. 26, St. Petersburg, 194021

V. Vettegren’

Ioffe Institute

Autor responsável pela correspondência
Email: Victor.Vettegren@mail.ioffe.ru
Rússia, Politekhnicheskaya ul. 26, St. Petersburg, 194021

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