Oxygen precipitates and the formation of thermal donors in silicon

1998 ◽  
Vol 32 (6) ◽  
pp. 640-641
Author(s):  
N. V. Vabishchevich ◽  
D. I. Brinkevich ◽  
V. S. Prosolovich
Keyword(s):  
2009 ◽  
Vol 156-158 ◽  
pp. 275-278
Author(s):  
Xiang Yang Ma ◽  
Yan Feng ◽  
Yu Heng Zeng ◽  
De Ren Yang

Oxygen precipitation (OP) behaviors in conventional and nitrogen co-doped heavily arsenic-doped Czocharalski silicon crystals subjected to low-high two-step anneals of 650 oC/8 h + 1000 oC/4-256 h have been comparatively investigated. Due to the nitrogen enhanced nucleation of OP during the low temperature anneal, much higher density of oxygen precipitates generated in the nitrogen co-doped specimens. With the extension of high temperature anneal, Oswald ripening of OP in the nitrogen co-doped specimens preceded that in the conventional ones. Moreover, due to the Oswald ripening effect, the oxygen precipitates in the conventional specimens became larger with a wider range of sizes. While, the sizes of oxygen precipitates in the nitrogen co-doped specimens distributed in a much narrower range with respect to the conventional ones.


1985 ◽  
Vol 59 ◽  
Author(s):  
P. Fraundorf

ABSTRACTThree separate “anomalous” effects in the precipitation of oxygen in silicon may be explained if typical poorly-crystallized platelet oxygen precipitates begin as tiny crystalline clusters. The first anomaly, sometimes referred to as the induction effect, may be explained if one postulates the existence of kinetically stable precipitate embryos (seeds) containing no more than one or two oxygen atoms. We show here that such a postulate, coupled with observations, places rather specific constraints on binding energy as a function of size for such tiny clusters. The second and third anomalies, arising in precipitate shape and retrogrowth behavior dependences, respectively, may be explained if one postulates the existence of a relatively dense precursor phase which undergoes first order phase transition, following otherwise classical rules, to the final-stage amorphous oxide normally found. In this case, both precipitate shape and strain field can be interpreted as a barometer of the interstitial ambient during key periods in a precipitate's history.


2004 ◽  
Vol 151 (12) ◽  
pp. G866 ◽  
Author(s):  
E. Leoni ◽  
L. Martinelli ◽  
S. Binetti ◽  
G. Borionetti ◽  
S. Pizzini

2016 ◽  
Vol 99 ◽  
pp. 231-235 ◽  
Author(s):  
D. Kot ◽  
G. Kissinger ◽  
M.A. Schubert ◽  
M. Klingsporn ◽  
A. Huber ◽  
...  

2013 ◽  
Vol 114 (4) ◽  
pp. 043520 ◽  
Author(s):  
V. V. Voronkov ◽  
R. Falster ◽  
TaeHyeong Kim ◽  
SoonSung Park ◽  
T. Torack

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