Complex F,Cl Apatite Solid Solution Investigated Using Multinuclear Solid-State NMR Methods
In this paper, a series of synthetic F,Cl apatites with low hydroxyl content was investigated using 31 P, 19 F, and 35 Cl solid-state magic angle spinning (MAS) NMR spectroscopic methods. 31 P single-pulse (SP) NMR spectra show that for each composition the phosphate 31 P chemical shift depends on occupancy of the nearest anion site for each composition. Overall the average chemical shift deviates from linear across the F/Cl series. For intermediate compositions 19 F SP NMR spectra reveal complex, broadened spectral profiles that are not correlated to composition. 19 F{ 35 Cl} TRAPDOR results indicate that the spectral profiles do not reflect occupancy of F and Cl in adjacent column anion sites. We propose that the complex 19 F lineshapes are principally due to broad distributions of 19 F–Ca distances arising from displacement of F along the anion channel. Finally, approximate fluorine atomic positions are estimated based on 19 F chemical shifts of alkaline earth fluoride salts, and the results are in good accord with those proposed for intermediate composition F,Cl apatites from XRD data.