Is end member topaz easily synthesized (or available commercially)?
The topaz from the Thomas Range, Utah, USA, is very widely available in mm-scale gem-quality brown crystals, and is very close to the end-member Al2(SiO4)F2. F-quantities for this material are reported by Penfield & Minor (1894) - 20.37 wt%; Ribbe & Rosenberg (1971) - 20.4(6) wt%, specimen 2; and Barton et al. (1982) - 20.3 wt%. The theoretical maximum F content of Al2(SiO4)F2 is 20.646 wt%.
Unit cell refinement from powder diffraction data acquired for topaz from the Thomas Range gives b: 8.789 angstroms,
consistent with F = 20.1(5) wt% based on a quadratic regression of the b-cell dimension data of Alberico et al. (2003) and Diego Gatta et al. (2006). (One-sigma standard deviation of last decimal place in parentheses). This independent determination is in good agreement with the previously published data.
I would suggest that this topaz may be useful as a reference material.
References:
Alberico, A., Ferrando, S., Ivaldi, G. and Ferraris, G., 2003. X-ray single-crystal structure refinement of an OH-rich topaz from Sulu UHP terrane (Eastern China)–Structural foundation of the correlation between cell parameters and fluorine content. European Journal of Mineralogy, 15(5), pp.875-881.
Barton, M.D., Haselton, H.T., Hemingway, B.S., Kleppa, O.J. and Robie, R.A., 1982. The thermodynamic properties of fluor-topaz. American Mineralogist, 67(3-4), pp.350-355.
Gatta, G.D., Nestola, F., Bromiley, G.D. and Loose, A., 2006. New insight into crystal chemistry of topaz: A multi-methodological study. American Mineralogist, 91(11-12), pp.1839-1846.
Penfield, S.L. and Minor, J.C., 1894. On the chemical composition and related physical properties of topaz. American Journal of Science, (281), pp.387-396.
Ribbe, P.H. and Rosenberg, P.E., 1971. Optical and X-ray determinative methods for fluorine in topaz. American Mineralogist, 56(9-10), pp.1812-1821.