NMR Characteristics of Possible Oxygen Sites in Aluminosilicate Glasses and Melts: An ab Initio Study

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Abstract

Ab initio molecular orbital calculations have been carried out for silicate, aluminosilicate, and aluminate clusters in order to study the NMR characteristics of oxygen sites that are possibly present in the structure of aluminosilicate glasses and melts. Of particular interest are the different types of bridging oxygens (oxygens bonded to two tetrahedrally coordinated Si and/or Al) and tricluster oxygens (oxygens linked to three tetrahedrally coordinated Si and/or Al). The calculated values for the 17O quadrupolar coupling constants (QCC) of Si-O-Si, Si-O-Al, and Al-O-Al bridging oxygens agree reasonably well with experimental NMR data for similar oxygen sites in crystalline silicates, aluminosilicates, or aluminates, and do not show significant dependence on the basis set and theory (Hartree-Fock vs density functional theory) of calculations. The calculated values for the 17O isotropic chemical shift (δiO), on the other hand, show large dependence on the basis set and method of calculations, although the relative differences in δiO for the clusters of interest do not vary as much. Our calculations indicate that bridging oxygens give progressively larger 17O QCC and larger, but overlapping, δiO from Al-O-Al to Si-O-Al to Si-O-Si. Coordination of Si-O-Al or Al-O-Al bridging oxygens to Ca2+, a network-modifying cation, tends to decrease their 17O QCC and increase their δiO, consistent with experimental NMR data. Tricluster oxygens give progressively larger 17O QCC and larger δiO values from O(Al3), to O(SiAl2), to O(Si2Al), to O(Si3). The O(Al3) and O(SiAl2) tricluster oxygens have 17O NMR characteristics overlapping with those of Si-O-Al bridging oxygens, and the O(Si2Al) tricluster oxygen overlapping with those of Si-Q-Si bridging oxygens. Our calculations suggest that it may be difficult to distinguish O(Al3), O(SiAl2), or O(Si2Al) tricluster oxygens from bridging oxygens in aluminosilicate glasses on the basis of 17O NMR data alone, although it should be possible to distinguish O(Al3) tricluster oxygen from Al-O-Al bridging oxygen in aluminates using 17O NMR. The O(Si3) tricluster have larger 17O QCC and larger δiO values than all types of bridging oxygens and thus may be unambiguously identified on the basis of 17O NMR data, if present in the structure of aluminosilicates or silicates.

Original languageEnglish
Pages (from-to)10816-10830
Number of pages15
JournalJournal of Physical Chemistry B
Volume103
Issue number49
DOIs
Publication statusPublished - Dec 9 1999

ASJC Scopus subject areas

  • Physical and Theoretical Chemistry
  • Surfaces, Coatings and Films
  • Materials Chemistry

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