MECHANISTIC STUDIES OF THE PHOTODISSOCIATION OF PHYSISORBED O-2/GRAPHITE

We have investigated the vacuum ultra-violet photodissociation of molecular O2 physisorbed on graphite using synchrotron radiation with photon energies in the range 13-35 eV. The yield of desorbed O+ ions shows a threshold at nearly 19.5 eV and resonances at 24.5 eV and 28.5 eV, contrasting strongly...

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Main Authors: Bennett, R, Bennett, S, Siller, L, Macdonald, M, Palmer, R, Wright, H, Foord, J
Format: Journal article
Language:English
Published: 1994
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author Bennett, R
Bennett, S
Siller, L
Macdonald, M
Palmer, R
Wright, H
Foord, J
author_facet Bennett, R
Bennett, S
Siller, L
Macdonald, M
Palmer, R
Wright, H
Foord, J
author_sort Bennett, R
collection OXFORD
description We have investigated the vacuum ultra-violet photodissociation of molecular O2 physisorbed on graphite using synchrotron radiation with photon energies in the range 13-35 eV. The yield of desorbed O+ ions shows a threshold at nearly 19.5 eV and resonances at 24.5 eV and 28.5 eV, contrasting strongly with the gas phase photodissociation cross section. the principal mechanism of O+ production appears to be dipolar dissociation drive by photoelectrons generated in the substrate. An enchancement in the detection efficiency of low-energy ions, compared with previous measurements, has identified an additional dissociation mechanism leading to the desorption of O- ions. Specifically, the results support a channel for low-energy O- desorption, attributed to the dissociative attachment of photoelectrons, again generated in the graphite substrate, to the physisorbed O2 molecules.
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spelling oxford-uuid:09bdc33b-8ad9-4f88-930f-b35093e1a6e92022-03-26T09:19:55ZMECHANISTIC STUDIES OF THE PHOTODISSOCIATION OF PHYSISORBED O-2/GRAPHITEJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:09bdc33b-8ad9-4f88-930f-b35093e1a6e9EnglishSymplectic Elements at Oxford1994Bennett, RBennett, SSiller, LMacdonald, MPalmer, RWright, HFoord, JWe have investigated the vacuum ultra-violet photodissociation of molecular O2 physisorbed on graphite using synchrotron radiation with photon energies in the range 13-35 eV. The yield of desorbed O+ ions shows a threshold at nearly 19.5 eV and resonances at 24.5 eV and 28.5 eV, contrasting strongly with the gas phase photodissociation cross section. the principal mechanism of O+ production appears to be dipolar dissociation drive by photoelectrons generated in the substrate. An enchancement in the detection efficiency of low-energy ions, compared with previous measurements, has identified an additional dissociation mechanism leading to the desorption of O- ions. Specifically, the results support a channel for low-energy O- desorption, attributed to the dissociative attachment of photoelectrons, again generated in the graphite substrate, to the physisorbed O2 molecules.
spellingShingle Bennett, R
Bennett, S
Siller, L
Macdonald, M
Palmer, R
Wright, H
Foord, J
MECHANISTIC STUDIES OF THE PHOTODISSOCIATION OF PHYSISORBED O-2/GRAPHITE
title MECHANISTIC STUDIES OF THE PHOTODISSOCIATION OF PHYSISORBED O-2/GRAPHITE
title_full MECHANISTIC STUDIES OF THE PHOTODISSOCIATION OF PHYSISORBED O-2/GRAPHITE
title_fullStr MECHANISTIC STUDIES OF THE PHOTODISSOCIATION OF PHYSISORBED O-2/GRAPHITE
title_full_unstemmed MECHANISTIC STUDIES OF THE PHOTODISSOCIATION OF PHYSISORBED O-2/GRAPHITE
title_short MECHANISTIC STUDIES OF THE PHOTODISSOCIATION OF PHYSISORBED O-2/GRAPHITE
title_sort mechanistic studies of the photodissociation of physisorbed o 2 graphite
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