Distribution of 28Si, 29Si, and 30Si isotopes under plastic deformation in subsurface layers of Si: B crystals


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The redistribution of 28Si, 29Si, and 30Si isotopes in subsurface layers of Si: B single crystals after their plastic deformation has been revealed. It has been found that the distribution profile of 28Si and 29Si isotopes becomes smoother after deformation, whereas the 30Si isotope distribution remains unchanged. A change in the subsurface profile of the 29SiO oxide is observed, which indicates the migration of the 29Si isotope in the composition of oxygen complexes during plastic deformation.

作者简介

O. Koplak

Institute of Problems of Chemical Physics; Taras Shevchenko National University of Kyiv

Email: morgunov2005@yandex.ru
俄罗斯联邦, ul. Akademika Semenova 1, Moscow oblast, Chernogolovka, 142432; ul. Volodymyrska 64/13, Kyiv, 01601

M. Vasil’ev

Kurdyumov Institute for Metal Physics

Email: morgunov2005@yandex.ru
乌克兰, Vernadsky Blvd. 36, Kiev, 03680

R. Morgunov

Institute of Problems of Chemical Physics

编辑信件的主要联系方式.
Email: morgunov2005@yandex.ru
俄罗斯联邦, ul. Akademika Semenova 1, Moscow oblast, Chernogolovka, 142432

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