Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9567766 | Applied Surface Science | 2005 | 6 Pages |
Abstract
X-ray photoelectron spectroscopy (XPS), ultraviolet photoelectron spectroscopy (UPS) and work-function measurements have been used to investigate the Y/SiO2/Si(1Â 0Â 0) interfaces in situ as a function of annealing temperature. The results show that yttrium is very reactive with SiO2 and can react with SiO2 to form Y silicate and Y2O3 even at room temperature. Annealing leads to the continual growth of the Y silicate. Two distinctive reaction mechanisms are suggested for the annealing processes below and above 600Â K. The reaction between metallic yttrium and SiO2 dominates the annealing processes below 600Â K, while at annealing temperatures above 600Â K, a reaction between the new-formed Y2O3 and SiO2 becomes dominant. No Y silicide is formed during Y deposition and subsequent annealing processes. UPS valence-band spectra indicate the silicate layer is formed at the top surface. After 1050Â K annealing, a Y-silicate/SiO2/Si structure free of Y2O3 is finally formed.
Keywords
Related Topics
Physical Sciences and Engineering
Chemistry
Physical and Theoretical Chemistry
Authors
Z.M. Wang, J.X. Wu, Q. Fang, J.-Y. Zhang,