The effect of ultrathin oxides on nanocrystallites of luminescent poro
us silicon is studied using infrared, optical, and Auger spectroscopy.
Room-temperature oxidation is performed using H2O2 immersion and UV o
zone interactions, producing oxides of similar to 5 and similar to 10
Angstrom, respectively. The H2O2 oxidized sample is optically active,
while the ozone oxidized sample is not active. UV-ozone produces a tra
nsverse optical Si-O-Si mode blueshifted by similar to 90 cm(-1) from
bulk oxide, which H2O2 does not produce. Auger Si LVV spectra show an
oxidelike signal for UV/ozone samples and a Si-like signal for H2O2 sa
mples. We discuss this in terms of different oxidation behaviors that
either preserve or break Si-Si dimers that may be responsible for the
optical behavior. (C) 1998 American Institute of Physics.