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Local Structure of Cationic Sites in Dehydrated Zeolites Inferred from 27Al Magic-Angle Spinning NMR and Density Functional Theory Calculations. A Study on Li-, Na-, and K-Chabazite

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    SYSNO ASEP0460633
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleLocal Structure of Cationic Sites in Dehydrated Zeolites Inferred from 27Al Magic-Angle Spinning NMR and Density Functional Theory Calculations. A Study on Li-, Na-, and K-Chabazite
    Author(s) Klein, Petr (UFCH-W) RID, ORCID
    Pashkova, Veronika (UFCH-W) RID, ORCID
    Thomas, Haunani M. (UFCH-W)
    Whittleton, Sarah R. (UFCH-W)
    Brus, Jiří (UMCH-V) RID, ORCID
    Kobera, Libor (UMCH-V) RID, ORCID
    Dědeček, Jiří (UFCH-W) RID, ORCID
    Sklenák, Štěpán (UFCH-W) RID, ORCID, SAI
    Source TitleJournal of Physical Chemistry C. - : American Chemical Society - ISSN 1932-7447
    Roč. 120, č. 26 (2016), s. 14216-14225
    Number of pages10 s.
    Languageeng - English
    CountryUS - United States
    Keywordszeolites ; density functional theory ; NMR spectroscopy
    Subject RIVCF - Physical ; Theoretical Chemistry
    Subject RIV - cooperationInstitute of Macromolecular Chemistry - Macromolecular Chemistry
    R&D ProjectsGA15-13876S GA ČR - Czech Science Foundation (CSF)
    GA15-14007S GA ČR - Czech Science Foundation (CSF)
    Institutional supportUFCH-W - RVO:61388955 ; UMCH-V - RVO:61389013
    UT WOS000379457000039
    EID SCOPUS84978027691
    DOI10.1021/acs.jpcc.6b04391
    AnnotationHigh-resolution 27Al magic-angle spinning (MAS) NMR spectroscopy of dehydrated M-forms (M = Li, Na, and K) of chabazite in tandem with density functional theory calculations are employed to study the quadrupolar interaction of 27Al nuclei in dehydrated zeolites and to understand the corresponding high-resolution 27Al MAS NMR spectra. We show that the broadening of the 27Al NMR signal in dehydrated zeolites occurs predominantly because of the deformation of the local structure of AlO4– tetrahedra caused by the binding of M+ to the zeolite framework. This deformation increases with the decreasing diameter of the cations from K+ to Li+. The influence of water in hydrated zeolites is limited only to prevent a strong coordination of the M+ cation to O atoms of the AlO4– tetrahedron, but there is no “averaging” effect concerning the local electrostatic field due to molecular motion of water molecules. Our results show that the 27Al NMR parameters in dehydrated zeolites can be calculated accurately enough to allow the description of the local structure of AlO4– tetrahedra in dehydrated zeolites and to infer the local structure of the sites accommodating the extraframework M+ cations.
    WorkplaceJ. Heyrovsky Institute of Physical Chemistry
    ContactMichaela Knapová, michaela.knapova@jh-inst.cas.cz, Tel.: 266 053 196
    Year of Publishing2017
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