An Electron Spectroscopic Study of the Cobalt(101̄2)-Oxygen Interaction: Chemisorption Properties, Oxide Growth and Oxidation States of the Surface Metal Ions

The interaction of oxygen with the stepped (101̄2) surface of cobalt has been investigated over a range of temperature (300–800 K) and pressure (10 −7 −10 +1 Torr) by XPS, UPS and LEED. After completion of a layer of chemisorbed atoms, oxygen uptake proceeds by the nucleation and growth of CoO. An e...

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Main Authors: E. G. Scott, K. A. Prior, R. M. Lambert
Format: Article
Language:English
Published: Hindawi - SAGE Publishing 1984-06-01
Series:Adsorption Science & Technology
Online Access:https://doi.org/10.1177/026361748400100204
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spelling doaj-af8892712dff4f62a76548ca5d11fcdb2021-04-02T09:52:10ZengHindawi - SAGE PublishingAdsorption Science & Technology0263-61742048-40381984-06-01110.1177/026361748400100204An Electron Spectroscopic Study of the Cobalt(101̄2)-Oxygen Interaction: Chemisorption Properties, Oxide Growth and Oxidation States of the Surface Metal IonsE. G. ScottK. A. PriorR. M. LambertThe interaction of oxygen with the stepped (101̄2) surface of cobalt has been investigated over a range of temperature (300–800 K) and pressure (10 −7 −10 +1 Torr) by XPS, UPS and LEED. After completion of a layer of chemisorbed atoms, oxygen uptake proceeds by the nucleation and growth of CoO. An examination of the satellite intensities associated with the Co(2p) levels yields no evidence for the formation of the higher oxide, and valence band UP spectra point to the same conclusion. However, the LEED results indicate that poorly ordered domains of the (100) plane of the Co 3 O 4 spinel lattice are formed after extensive oxidation. A model is proposed which accounts for these observations; it also provides a basis for reconciling a number of conflicting reports in the literature.https://doi.org/10.1177/026361748400100204
collection DOAJ
language English
format Article
sources DOAJ
author E. G. Scott
K. A. Prior
R. M. Lambert
spellingShingle E. G. Scott
K. A. Prior
R. M. Lambert
An Electron Spectroscopic Study of the Cobalt(101̄2)-Oxygen Interaction: Chemisorption Properties, Oxide Growth and Oxidation States of the Surface Metal Ions
Adsorption Science & Technology
author_facet E. G. Scott
K. A. Prior
R. M. Lambert
author_sort E. G. Scott
title An Electron Spectroscopic Study of the Cobalt(101̄2)-Oxygen Interaction: Chemisorption Properties, Oxide Growth and Oxidation States of the Surface Metal Ions
title_short An Electron Spectroscopic Study of the Cobalt(101̄2)-Oxygen Interaction: Chemisorption Properties, Oxide Growth and Oxidation States of the Surface Metal Ions
title_full An Electron Spectroscopic Study of the Cobalt(101̄2)-Oxygen Interaction: Chemisorption Properties, Oxide Growth and Oxidation States of the Surface Metal Ions
title_fullStr An Electron Spectroscopic Study of the Cobalt(101̄2)-Oxygen Interaction: Chemisorption Properties, Oxide Growth and Oxidation States of the Surface Metal Ions
title_full_unstemmed An Electron Spectroscopic Study of the Cobalt(101̄2)-Oxygen Interaction: Chemisorption Properties, Oxide Growth and Oxidation States of the Surface Metal Ions
title_sort electron spectroscopic study of the cobalt(101̄2)-oxygen interaction: chemisorption properties, oxide growth and oxidation states of the surface metal ions
publisher Hindawi - SAGE Publishing
series Adsorption Science & Technology
issn 0263-6174
2048-4038
publishDate 1984-06-01
description The interaction of oxygen with the stepped (101̄2) surface of cobalt has been investigated over a range of temperature (300–800 K) and pressure (10 −7 −10 +1 Torr) by XPS, UPS and LEED. After completion of a layer of chemisorbed atoms, oxygen uptake proceeds by the nucleation and growth of CoO. An examination of the satellite intensities associated with the Co(2p) levels yields no evidence for the formation of the higher oxide, and valence band UP spectra point to the same conclusion. However, the LEED results indicate that poorly ordered domains of the (100) plane of the Co 3 O 4 spinel lattice are formed after extensive oxidation. A model is proposed which accounts for these observations; it also provides a basis for reconciling a number of conflicting reports in the literature.
url https://doi.org/10.1177/026361748400100204
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