z-logo
open-access-imgOpen Access
Формирование ступенчатой поверхности Si(100) и ее влияние на рост островков Ge
Author(s) -
М.Ю. Есин,
А.И. Никифоров,
В.А. Тимофеев,
А.Р. Туктамышев,
В.И. Машанов,
И.Д. Лошкарев,
А.С. Дерябин,
О.П. Пчеляков
Publication year - 2018
Publication title -
fizika i tehnika poluprovodnikov
Language(s) - English
Resource type - Journals
eISSN - 1726-7315
pISSN - 0015-3222
DOI - 10.21883/ftp.2018.03.45630.8624
Subject(s) - monatomic gas , annealing (glass) , superstructure , condensed matter physics , nucleation , electron diffraction , materials science , silicon , crystallography , diffraction , growth rate , chemistry , optics , thermodynamics , physics , geometry , metallurgy , mathematics , organic chemistry
The transition from a two-domain to one-domain surface on a Si(100) substrate is investigated. It is demonstrated using reflection high-energy electron diffraction that at a temperature of 600°C and a deposition rate of 0.652 Å/s onto a Si(100) substrate pre-heated to 1000°C and inclined at an angle of 0.35°C to the plane, a series of reflections from the 1 × 2 superstructure completely vanishes at a constant flow of Si. This is attributed to the transition of the surface from monoatomic to diatomic steps. At growth rates lower than 0.652 Å/s, the transition from a two-domain to one-domain surface is also observed; with a decrease in the growth rate, the intensity ratio I _2 × 1/ I _1 × 2 decreases and the maximum of the dependences shifts toward lower temperatures. The complete vanishing of the series of superstructural reflections after preliminary annealing at a temperature of 700°C is not observed; this series only vanishes after annealing at 900 and 1000°C. The growth of Ge islands on a Si(100) surface preliminary annealed at a temperature of 800°C is studied. It is shown that the islands tend to nucleate at the step edges. A mechanism of Ge island ordering on the Si(100) surface is proposed.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here