Autor: |
E. E. Chaban, George W. Flynn, Joseph Eng, Yves J. Chabal, K. Radermacher, Krishnan Raghavachari, Gwyn P. Williams, Lisa M. Struck, Brian E. Bent, Siegfried Mantl, S. B. Christman |
Rok vydání: |
1997 |
Předmět: |
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Zdroj: |
Surface Science. 380:444-454 |
ISSN: |
0039-6028 |
DOI: |
10.1016/s0039-6028(97)00041-1 |
Popis: |
The vibrational spectrum of water dissociatively adsorbed on Si(100) surfaces is obtained with surface infrared absorption spectroscopy. Low frequency spectra ( −1 are acquired using a buried CoSi 2 layer as an internal mirror to perform external reflection spectroscopy. On clean Si(100), water dissociates into H and OH surface species as evidenced by EELS results [1] in the literature which show a SiH stretching vibration (2082 cm −1 ), and SiOH vibrations (OH stretch at 3660 cm −1 and the SiOH bend and SiO stretch of the hydroxyl group centered around 820 cm −1 ). In this paper, infrared (IR) measurements are presented which confirm and resolve the issue of a puzzling isotopic shift for the SiO mode of the surface hydroxyl group, namely, that the SiO stretch of the OH surface species formed upon H 2 O exposure occurs at 825 cm −1 , while the SiO stretch of the OD surface species formed upon D 2 O exposure shifts to 840 cm −1 , contrary to what is expected for simple reduced mass arguments. The higher resolution of IR measurements versus typical EELS measurements makes it possible to identify a new mode at 898 cm −1 , which is an important piece of evidence in understanding the anomalous frequency shift. By comparing the results of measurements for adsorption of H 16 2 O, H 18 2 O and D 2 O with the results from recently performed first-principles calculations, it can be shown that a strong vibrational interaction between the SiO stretching and SiOH bending functional group vibrations of the hydroxyl group accounts for the observed isotopic shifts. |
Databáze: |
OpenAIRE |
Externí odkaz: |
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