In this work, we have prepared the buried SiC layers by a metal vapor vacuu
m are (MEVVA) ion source, respectively, on Si(100) and surface oxidized Si(
100) wafers. The Fourier transform infrared spectroscopy (FTIR) spectra of
the buried layers were found to be composed of two components, one assigned
to amorphous SiC (a-SiC) and the other one to cubic SiC (beta-SiC). It was
found that there is a critical dose at which the relative amount of beta-S
iC increase abruptly, and the silicon oxide thickness dependence of the fra
ction ratio (the relative amount of beta-SiC/the relative amount of a-SiC)
in the buried layers is of the shape similar to the distribution of the car
bon content. The results indicate that in the region of the maximum carbon
content the crystallized degree of the buried layers is higher. (C) 2000 El
sevier Science S.A. All rights reserved.