Abstract
The effect of ultrathin oxides on nanocrystallites of luminescent porous silicon is studied using infrared, optical, and Auger spectroscopy. Room-temperature oxidation is performed using H2O2 immersion and UV ozone interactions, producing oxides of ∼5 and ∼10 Å, respectively. The H2O2 oxidized sample is optically active, while the ozone oxidized sample is not active. UV-ozone produces a transverse optical Si-O-Si mode blueshifted by ∼90cm-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 samples. 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.
Original language | English (US) |
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Pages (from-to) | 841-843 |
Number of pages | 3 |
Journal | Applied Physics Letters |
Volume | 73 |
Issue number | 6 |
DOIs | |
State | Published - 1998 |
ASJC Scopus subject areas
- Physics and Astronomy (miscellaneous)