Abstract

Solid-state nuclear magnetic resonance (NMR) was used to characterize porous silicon (PS) surfaces. On freshly prepared samples, the range of hydrogen content measured by 1H NMR was equivalent to 0.5−3 monolayers, while fluorine concentrations were below the 19F NMR detection limit. The 1H nuclei were used to selectively cross-polarize (CP) 29Si near the hydrogen passivation. This method was used to study the passivation of an as-prepared, thick (116 μm), high surface area (893 m2/g), photoluminescent (700 nm) PS sample. CP followed by polarization inversion (CPPI) provided some spectral editing. Changes resulting from low-temperature annealing in air and an HF soak were followed by both NMR and infrared spectroscopy. The features of the 29Si NMR spectra are assigned as (O)2(Si)Si−H (−50 ppm), (O)3Si−H (−84 ppm), (Si)3Si−H (−91 ppm), (Si)2Si−H2 (−102 ppm), and (O)4Si (−109 ppm). These assignments are discussed in relationship to experimental measurements and correlations of 29Si NMR chemical shifts for other materials. The 29Si NMR line widths for PS fall between those for crystalline silicon and those for amorphous hydrogenated silicon (a-Si:H), suggesting that disorder near the PS surface is intermediate between these extremes. However, comparision of the isotropic chemical shift values shows that the bonding in the disordered regions of PS differs from that found in a-Si:H. In addition, the sharp 29Si NMR resonance observed in the bulk single crystal starting material cannot be resolved in the spectra of PS. Thus, well-ordered silicon nanocrystallites in the PS are several bond lengths removed from hydrogen or comprise only a small fraction of the PS layer.

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