METAL ISLAND GROWTH AND DYNAMICS ON MOLYBDENITE SURFACES

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dc.contributor.author Becker U.
dc.contributor.author Rosso K.M.
dc.contributor.author Weaver R.
dc.contributor.author Hochella M.F.
dc.contributor.author Warren M.
dc.date.accessioned 2021-11-28T04:25:39Z
dc.date.available 2021-11-28T04:25:39Z
dc.date.issued 2003
dc.identifier https://www.elibrary.ru/item.asp?id=14278022
dc.identifier.citation Geochimica et Cosmochimica Acta, 2003, 67, 5, 923-934
dc.identifier.issn 0016-7037
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/32588
dc.description.abstract In order to understand the adsorption mechanism of metal atoms to semiconducting surfaces, we have studied, as a model system, the vapor phase adsorption of Ag, Au, and Cu on the (001) surface of molybdenite (MoS2) and the subsequent surface diffusion of these adsorbates. Our scanning tunneling microscopy (STM) images show that, depending on the type of metal atom that is adsorbed, islands of a characteristic size (2 nm for Ag, 8 to 10 nm for Cu, two distinct sizes of 2 nm and 8 to 10 nm for Au), shape (well rounded in the lateral extension) and thickness (one monolayer for Ag, 1 to 1.5 nm for Cu) are formed during the initial stages of deposition. Whole islands are observed to surface diffuse without loss of size or shape. Despite the relatively large size of the copper islands on molybdenite, these islands surface diffuse extensively, suggesting that the Cu-S interaction is weak. Surface diffusion is only hindered once individual islands start to coalesce. As copper islands accumulate, the size and shape of the original islands can still be recognized, supporting the conclusion that these characteristics are constant and that monolayer growth occurs by the aggregation of islands across the surface.
dc.subject Molybdenite
dc.title METAL ISLAND GROWTH AND DYNAMICS ON MOLYBDENITE SURFACES
dc.type Статья


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