Abstract
The proposition is supported that the influence of ultrahigh pressure leads to the creation of a convective crystal state in which the entire ensemble of atoms is divided into strongly and weakly excited atoms. The first of these are found in a delocalized state, achieving the convective mass transfer regime, and the second are responsible for crystal structure.
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Translated from Izvestiya Vysshikh Uchebnikh Zavedenii, Fizika, No. 6, pp. 34–40, June, 1986.
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Olemskoi, A.I., Naumov, I.I. & Panin, V.E. Nature of the convective state of crystals in “ultrahigh pressure + shear” conditions. Soviet Physics Journal 29, 454–459 (1986). https://doi.org/10.1007/BF00898011
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DOI: https://doi.org/10.1007/BF00898011