Abstract

The structure of a synthetic fluoromica has been investigated and elucidated by complementary 29Si, 1H, 19F, 23Na, and 27Al single and double resonance experiments. The phyllosilicate possesses a charge heterogeneity arising from the presence of different charged sites in the octahedral sheets of the T-O-T layers. Part of the magnesium atoms in the octahedral sheets is missing, creating vacancies. Charge balancing proceeds mostly by incorporation of sodium ions into the interlayer space and substitution of Mg by sodium in the lattice. The latter process produces a nonexchangeable fraction of sodium ions (∼20% of the total inventory) and creates multiple sites for the fluoride ions, as evidenced from 19F NMR spectroscopy. Detailed quantitative information about the sodium–fluoride distance geometries were obtained from 19F/23Na double rotational echo double resonance (REDOR) experiments; furthermore, different types of fluoride sites could be discriminated on the basis of 19F/23Na double resonance experime...

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