Abstract
The thermal behavior of an ammonia-covered Si(100) surface is investigated by infrared spectroscopy and density functional methods. Upon adsorption at room temperature, and Si-H species are formed on the surface. Comparison of the vibrational studies with density functional calculations suggests that the structures are preferentially located on the same side along the silicon dimer row on a reconstructed Si(100) surface, although a mixture of different long-range configurations is likely formed. Decomposition of these species is observed to start at temperatures as low as . Theoretical predictions of the vibrational modes indicate that at this point, the spectrum is composed of a combination of and vibrational signatures, which result from insertion of N into Si-Si bonds. Our computational study of the formation of structures indicates that subsurface insertion is more feasible if the strain imposed during the insertion in a Si dimer is attenuated by a structure already inserted in the neighboring dimer along the same silicon dimer row. This cooperative reaction lowers the energetic requirements for subsurface insertion, providing a theoretical explanation for the mechanism of thermal decomposition of on Si(100) and for other systems where subsurface migration is observed experimentally.
3 More- Received 10 April 2007
DOI:https://doi.org/10.1103/PhysRevB.76.075348
©2007 American Physical Society