Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.14279/1116
DC FieldValueLanguage
dc.contributor.authorEfstathiou, Angelos M.-
dc.contributor.authorSavva, Petros G.-
dc.date.accessioned2013-01-21T08:53:46Zen
dc.date.accessioned2013-05-16T06:25:17Z-
dc.date.accessioned2015-12-02T08:49:51Z-
dc.date.available2013-01-21T08:53:46Zen
dc.date.available2013-05-16T06:25:17Z-
dc.date.available2015-12-02T08:49:51Z-
dc.date.issued2008-07-
dc.identifier.citationJournal of Catalysis, 2008, vol. 257, iss. 2, pp. 324–333en_US
dc.identifier.issn00219517-
dc.identifier.urihttps://hdl.handle.net/20.500.14279/1116-
dc.description.abstractSteady-state isotopic transient kinetic analysis (SSITKA), transient isothermal, and temperature-programmed surface reaction in H2 (H2-TPSR) techniques coupled with online mass spectroscopy (MS) and in situ diffuse reflectance infrared Fourier transform spectroscopy (DRIFTS) were used to study essential mechanistic and kinetic aspects of the selective catalytic reduction (SCR) of NO with the use of H2 under strongly oxidizing conditions (H2-SCR) over a novel Pt/MgO{single bond}CeO2 catalyst. The main focus was to study and report for the first time the effects of reaction temperature on the chemical structure and surface concentration of the active NOx intermediate species thereby formed. The information obtained is essential to understanding the volcano-type profile of the catalyst activity versus reaction temperature observed here and also reported previously. In the present work, two active NOx intermediate species identified by SSITKA-DRIFTS were found in the nitrogen-reaction path toward N2 and N2O formation, one species located in the vicinity of the Pt{single bond}CeO2 support interface region (nitrosyl [NO+] coadsorbed with a nitrate [NO-3] species on an adjacent Ce4+{single bond}O2- site pair) and the second located in the vicinity of the Pt{single bond}MgO support interface region. The chemical structure of the second kind of active NOx species was found to depend on reaction temperature. In particular, the chemical structure was that of bidentate or monodentate nitrate (NO-3) at T < 200 ° C and that of chelating nitrite (NO-2) at T > 200 ° C. The concentration of the active NOx intermediates that lead to N2 formation was found to be practically independent of reaction temperature (120-300 °C) and significantly larger than 1 equivalent monolayer of surface Pt (θNOx = 2.4 - 2.6). The former result cannot be used to explain the volcano-type behavior of the catalytic activity versus the reaction temperature observed; alternative explanations are explored. The H-spillover process involved in the H2-SCR mechanism was found to be limited within a support region of about a 4-5 Å radius around the Pt nanoparticles (dPt = 1.2 - 1.5 nm).en_US
dc.formatpdfen_US
dc.language.isoenen_US
dc.relation.ispartofJournal of Catalysisen_US
dc.rights© Elsevieren_US
dc.subjectAddition reactionsen_US
dc.subjectIsotopesen_US
dc.subjectSurfacesen_US
dc.titleThe influence of reaction temperature on the chemical structure and surface concentration of active nox in h2-scr over pt/mgo{single bond}ceo2: ssitka-drifts and transient mass spectrometry studiesen_US
dc.typeArticleen_US
dc.collaborationUniversity of Cyprusen_US
dc.subject.categoryChemical Sciencesen_US
dc.journalsSubscriptionen_US
dc.countryCyprusen_US
dc.subject.fieldNatural Sciencesen_US
dc.publicationPeer Revieweden_US
dc.identifier.doi10.1016/j.jcat.2008.05.010en_US
dc.dept.handle123456789/54en
dc.relation.issue2en_US
dc.relation.volume257en_US
cut.common.academicyear2008-2009en_US
dc.identifier.spage324en_US
dc.identifier.epage333en_US
item.languageiso639-1en-
item.cerifentitytypePublications-
item.fulltextNo Fulltext-
item.grantfulltextnone-
item.openairetypearticle-
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
crisitem.author.deptDepartment of Chemical Engineering-
crisitem.author.facultyFaculty of Geotechnical Sciences and Environmental Management-
crisitem.author.orcid0000-0001-6390-315X-
crisitem.author.parentorgFaculty of Geotechnical Sciences and Environmental Management-
crisitem.journal.journalissn0021-9517-
crisitem.journal.publisherElsevier-
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