To investigate the composition of oxygen-bearing species evaporated fr
om Sb-doped Si melts, a carefully designed deposit collector was used.
The collected deposits were analyzed by electron probe microanalysis
(EPMA), gas fusion analysis (GFA), X-ray diffraction, and diffuse refl
ectance infrared (DR-IR) spectroscopy. The results showed that the com
positions of the deposits depended on the temperatures of various regi
ons within the collector. Different deposits, with various amounts of
antimony oxide, silicon oxide, silicon, and antimony, were found in di
fferent temperature regions. In particular, it was discovered that ant
imony oxide was deposited only in the region where the temperature was
lower than 450 degrees C. Thus the present investigation gave evidenc
e showing that oxygen depletion from Sb-doped Si melt probably arose f
rom enhanced antimony oxide evaporation.