Please use this identifier to cite or link to this item: https://scholarbank.nus.edu.sg/handle/10635/94983
DC FieldValue
dc.titleSurface reactions at 300-750 K in the iron-oxygen-water system studied by SIMS
dc.contributor.authorHultquist, G.
dc.contributor.authorSeo, M.
dc.contributor.authorLu, Q.
dc.contributor.authorChuah, G.K.
dc.contributor.authorTan, K.L.
dc.date.accessioned2014-10-16T08:42:28Z
dc.date.available2014-10-16T08:42:28Z
dc.date.issued1992
dc.identifier.citationHultquist, G.,Seo, M.,Lu, Q.,Chuah, G.K.,Tan, K.L. (1992). Surface reactions at 300-750 K in the iron-oxygen-water system studied by SIMS. Applied Surface Science 59 (2) : 135-145. ScholarBank@NUS Repository.
dc.identifier.issn01694332
dc.identifier.urihttp://scholarbank.nus.edu.sg/handle/10635/94983
dc.description.abstractSecondary ion mass spectroscopy, SIMS, has been applied to the surface study of the iron-oxygen-water system in the 300-750 K temperature range in order to gain insight into the initial stages of wet oxidation of iron. During sputtering with Ar+ ions the emission of OH-containing ions was strongly dependent on temperature. In situ X-ray photoelectron spectrometry experiments were conducted in order to support this observation. In experiments where the metal was exposed simultaneously to H2 18O and 16O2, the source of O in the reaction product could be determined by analysis of the ions emitted at different temperatures. This analysis showed that a coupled reaction. 2Fe + H2O + 1 3O2 → 2FeOH, is operating at room temperature. At higher temperatures iron reacts preferentially with water as can be seen from the abundance of 18O in the emitted ions. © 1992.
dc.sourceScopus
dc.typeArticle
dc.contributor.departmentCHEMISTRY
dc.contributor.departmentPHYSICS
dc.description.sourcetitleApplied Surface Science
dc.description.volume59
dc.description.issue2
dc.description.page135-145
dc.description.codenASUSE
dc.identifier.isiutNOT_IN_WOS
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