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²⁷Al and ²³Na NMR spectroscopy and structural modeling of aluminofluoride minerals

¹ Department of Geological Sciences, University of Manitoba, Winnipeg, Manitoba, Canada R3T 2N2
² Department of Chemistry, Brock University, St. Catharines, Ontario L2S 3A1, Canada
³ Department of Chemistry, Queen’s University, Kingston, Ontario K7L 3N6, Canada

Correspondence: ^* E-mail: sherriff{at}Ms.UManitoba.CA

Simulations of high-resolution ¹⁹F-decoupled ²⁷Al and ²³Na magic-angle spinning nuclear magnetic resonance (MAS NMR) spectra of the aluminofluoride minerals, cryolite, cryolithionite, thomsenolite, weberite, chiolite, prosopite, and ralstonite combined with theoretical modeling have given accurate values of chemical shift (_iso), and quadrupolar interaction parameters (C_q and ), thereby eliminating ambiguities incurred by the complex nuclear interactions. These NMR data have been correlated with local electronic environments in the minerals, which were calculated using Full Potential Linearized Augmented Plane Wave (FP LAPW) modeling based on the structures from X-ray diffraction (XRD) data. This combination of NMR, XRD, and modeling techniques allowed the analysis and optimization of the crystal structures.

The electronegativities and distances of neighboring ions, represented here by an environmental parameter , are shown to control _iso of both ²³Na and ²⁷Al. The calculations using , also show that the ions beyond the nearest neighbor play an important role in determining _iso of ²⁷Al and ²³Na in these aluminofluoride minerals, and the substitution of OH for F significantly affects the shielding around ²⁷Al in prosopite and ralstonite. There is a positive correlation between the site distortion at the Na and Al sites and the values of C_q in these aluminofluoride minerals.

Key Words: Cryolite • cryolithionite • elpasolite • weberite • thomsenolite • prosopite • chiolite • ralstonite • aluminofluoride minerals • ²³Na • ²⁷Al MAS NMR • FP LAPW calculations

This article has been cited by other articles:

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