Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5422704 | Surface Science | 2013 | 10 Pages |
Abstract
When glycine and water are co-adsorbed in UHV at low temperatures (<Â 170Â K) inter-layer diffusion is inhibited and the surface composition depends on the adsorption sequence. Water adsorbed on top of a glycine layer does not lead to significant changes in its chemical state. When glycine is adsorbed on top of a pre-adsorbed chemisorbed water layer or thick ice layer, however, it is found in its zwitterionic state, even at low coverage. No difference is seen in the chemical state of glycine when the layers are exposed to ambient water vapor pressure up to 0.2Â Torr at temperatures above 300Â K. Also the decomposition temperature stays the same, 360Â K, irrespective of the water vapor pressure. Only the reaction path of the decomposition products is affected by ambient water vapor.
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Authors
Andrey Shavorskiy, Tugce Eralp, Karina Schulte, Hendrik Bluhm, Georg Held,