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DLTS study of oxygen precipitates in silicon annealed
at high pressure
I.V. Antonova a'*, A. Misiuk b, V.P. Popov a, L.I. Fedina a, S.S. Shaimeev a
aInstitute of Semiconductor Physics, Lavrent 'eva 13, 630090 Novosibirsk, Russian Federation
blnstitute of Electron Technology, Al.Lotnikow 32/46, 02-668 Warsaw, Poland
Received 9 December 1995; revised 19 March 1996
Abstract
The evolution of oxygen precipitates (OPs) created at 900-1000 K in Si-Cz with initial oxygen concentration
8 × 1017 cm -3 was studied by DLTS technique. The samples were subjected to high pressure (HP) treatment up to
1.3 GPa at high temperature (HT, 1230-1550 K) which caused a partial dissolution of OP. A new way of studying the
oxygen distribution is suggested. It is based on the investigation of an electrically active complex of the oxygen atom with
a vacancy (A-center, level E c- 0.18eV). A-centers were introduced by 3.0MeV electron irradiation with dose
1 x 10 t5 cm -2 and DLTS was used for A-center agglomerates detection. The analysis of data obtained allows one to
conclude that the irradiation dose used does not decompose OPs. It has been found that hydrostatic pressure retards OP
dissolution at HT treatment through a decrease in the migration energy o~a, coefficient D O and diffusion coefficient D. The
effect is explained on the assumption that oxygen diffuses in the form of connected pairs of the oxygen and self-
interstitials. |
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