1983
DOI: 10.1063/1.93992
|View full text |Cite
|
Sign up to set email alerts
|

Diffusion limited precipitation of oxygen in dislocation-free silicon

Abstract: The kinetics of oxygen precipitation in silicon have been determined from measurements of the IR 9-μm absorption band (4.2 K) and we obtain the time constant τ0 for the exponential approach to equilibrium for several temperatures. The density N of precipitate particles was measured directly by chemical etching, and inferred from IR scattering and cold neutron scattering. We use our values of τ0 and N to calculate the diffusion coefficient of oxygen in bulk silicon. This is the first time that this procedure ha… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2

Citation Types

1
1
0

Year Published

1998
1998
2013
2013

Publication Types

Select...
5
1

Relationship

0
6

Authors

Journals

citations
Cited by 44 publications
(2 citation statements)
references
References 12 publications
1
1
0
Order By: Relevance
“…The decrease of density at 1050 • C has to be attributed to a change of the Si lattice (softening). Similar phenomena have been observed in oxygen precipitation in Si [28]. The above model is further corroborated from the wider spread of densities at the temperatures for which the mean density is high (900-1000 • C) and the presence of the surface profile B (appearing only in some samples at 1000 and 1050 • C).…”
Section: Analysis Of the Nr Resultssupporting
confidence: 83%
See 1 more Smart Citation
“…The decrease of density at 1050 • C has to be attributed to a change of the Si lattice (softening). Similar phenomena have been observed in oxygen precipitation in Si [28]. The above model is further corroborated from the wider spread of densities at the temperatures for which the mean density is high (900-1000 • C) and the presence of the surface profile B (appearing only in some samples at 1000 and 1050 • C).…”
Section: Analysis Of the Nr Resultssupporting
confidence: 83%
“…The SiO 2 exhibits polymorphism even at atmospheric pressure and the pressure-temperature phase diagram is quite complex (for example, coesite and stishovite with densities 3 and 4.4 g cm −3 , respectively [27]). During oxide growth, especially at the initial stages studied here, most probably high pressures are created in the Si lattice as oxygen atoms are incorporated and Si interstitials emitted, if we assume a mechanism similar to that which takes place in the formation of SiO 2 precipitates in crystalline Si [28,29]. These high pressures would result in the formation of high pressure SiO 2 phases or mixture of low and high pressure phases.…”
Section: Analysis Of the Nr Resultsmentioning
confidence: 87%