The structures of silicon native oxides formed in the SC-1, H2O2 and w
et ozone processes were characterized using X-ray photoelectron spectr
oscopy (XPS), transmission electron microscopy (TEM) and Fourier trans
form infrared spectroscopy (FT-IR). Spectral simulation was performed
to clarify the FT-IR spectra, assuming that the native oxide was pure
silicon dioxide. Effective medium theories were applied to understand
deviations of the observed spectra from the calculated ones. The devia
tions between the native oxide thickness evaluated by XPS and the abso
lute thickness obtained by TEM were also discussed. These deviations c
an be explained if the void is incorporated in the native oxides and t
he interface between the native oxide and the basal silicon-obtained b
y the wet ozone process has a relatively smooth surface and a structur
e more similar to that of pure silicon dioxide, compared with that obt
ained by SC-1 or H2O2 treatment.