Number of the records: 1  

Mechanism of Framework Oxygen Exchange in Fe-Zeolites: A Combined DFT and Mass Spectrometry Study

  1. 1.
    SYSNO ASEP0389992
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleMechanism of Framework Oxygen Exchange in Fe-Zeolites: A Combined DFT and Mass Spectrometry Study
    Author(s) Andrikopoulos, Prokopis C. (UFCH-W) RID, ORCID
    Sobalík, Zdeněk (UFCH-W) RID
    Nováková, Jana (UFCH-W) RID
    Sazama, Petr (UFCH-W) RID, ORCID
    Sklenák, Štěpán (UFCH-W) RID, ORCID, SAI
    Source TitleChemPhysChem. - : Wiley - ISSN 1439-4235
    Roč. 14, č. 3 (2013), s. 520-531
    Number of pages11 s.
    Languageeng - English
    CountryDE - Germany
    Keywordsdensity functional theory ; iron ; zeolites
    Subject RIVCF - Physical ; Theoretical Chemistry
    R&D ProjectsIAA400400812 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    GA203/09/1627 GA ČR - Czech Science Foundation (CSF)
    Institutional supportUFCH-W - RVO:61388955
    UT WOS000315142900009
    EID SCOPUS84874055020
    DOI10.1002/cphc.201200900
    AnnotationThe role of framework oxygen atoms in N2O decomposition [N2O(g)!N2(g) and 1=2O2(g)] over Fe-ferrierite is investigated employing a combined experimental (N2 18O decomposition in batch experiments followed by mass spectroscopy measurements) and theoretical (density functional theory calculations) approach. The occurrence of the isotope exchange indicates that framework oxygen atoms are involved in the N2O decomposition catalyzed by Fe-ferrierite. Our study, using an Fe-ferrierite sample with iron exclusively present as FeII cations accommodated in the cationic sites, shows that the mobility of framework oxygen atoms in the temperature range: 553 to 593 K is limited to the four framework oxygen atoms of the two AlO4- tetrahedra forming cationic sites that accomodate FeII. They exchange with the Fe extra-framework 18O atom originating from the decomposed N2 18O. We found, using DFT calculations, that O2 molecules facilitate the oxygen exchange. However, the corresponding calculated energy barrier of 87 kcalmol-1 is still very high and it is higher than the assumed experimental value based on the occurrence of the sluggish oxygen exchange at 553 K.
    WorkplaceJ. Heyrovsky Institute of Physical Chemistry
    ContactMichaela Knapová, michaela.knapova@jh-inst.cas.cz, Tel.: 266 053 196
    Year of Publishing2014
Number of the records: 1  

  This site uses cookies to make them easier to browse. Learn more about how we use cookies.