The mode of attack of oxygen atoms on the basal plane of graphite
- 15 March 1983
- journal article
- research article
- Published by AIP Publishing in The Journal of Chemical Physics
- Vol. 78 (6) , 3325-3328
- https://doi.org/10.1063/1.445198
Abstract
Gold decoration of the basal lattice plane of graphite etched by atomic oxygen has been made possible by first desorbing the surface oxide layer on the basal plane. The formation of monolayer pits, as revealed by gold decoration, shows that anisotropy does exist, i.e., carbon atoms are preferentially attacked by atomic oxygen in the direction of a axes, rather than the direction of c axis. The monolayer pits are initiated from lattice vacancies which are continually formed by atomic oxygen. The monolayer pits created by atomic oxygen are, unlike the pits by O2 which are circular, hexagonal in shape, the sides of which are composed of 〈101̄l〉 lattice planes.Keywords
This publication has 10 references indexed in Scilit:
- Etch decoration—scanning electron microscopy technique for measuring carbon gasification ratesReview of Scientific Instruments, 1982
- Kinetics and mechanism of oxidation of basal plane on graphiteThe Journal of Chemical Physics, 1981
- Kinetics of Single-Layer Graphite Oxidation: Evaluation by Electron MicroscopyScience, 1971
- Graphite oxidation—the mobile surface-oxide intermediateCarbon, 1969
- Oxidation of carbons and graphites by atomic oxygen kinetic studiesTransactions of the Faraday Society, 1965
- Oxidation of carbons and graphites by atomic oxygen an electron microscope study of surface changesTransactions of the Faraday Society, 1965
- Determination of Lattice Vacancies in GraphiteThe Journal of Chemical Physics, 1964
- Variations in orientation of etch pits on graphite surfacesPhilosophical Magazine, 1963
- The oxidation of graphite I. The observation of oxidation on synthetic graphite before and after irradiationProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1963
- Reaction of Atomic Oxygen with CarbonNature, 1963