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The crystal structure of voggite, a new hydrated Na–Zr hydroxide–phosphate–carbonate mineral*

Published online by Cambridge University Press:  05 July 2018

Jan T. Szymański  and
Andrew C. Roberts
Jan T. Szymański
Affiliation:
CANMET, 555 Booth Street, Ottawa, Ontario, Canada, K1A 0G1
Andrew C. Roberts
Affiliation:
Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, K1A 0E8
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Abstract

The crystal structure of the new mineral voggite, Na2Zr(PO4)(CO3)(OH).2H2O , from the Francon quarry, Montreal, Quebec, Canada, has been solved in order to determine the correct chemical formula, as conventional electron microprobe methods were found unreliable. The unit cell is monoclinic, I2/m, with a = 12.261(2), b = 6.561(1), c = 11.757(2)Å, β = 116.19(2)°. The structure consists of layers of edge-sharing Zr-O pentagonal bipyramids, separated by layers of Na-(O,H2O) octahedra. The carbonate ion acts as a bidentate ligand in the Zr-O polyhedron, the third oxygen atom being bonded to the Na atom. The phosphate group is bonded to three different Zr atoms and to a Na atom. The Zr-O bond lengths vary from 2.067 to 2.283 (mean 2.140Å), while Na-O are between 2.304 and 2.773, (σ = 0.006Å, mean 2.480Å). The carbonate and phosphate bonds are normal. It is inferred from the structure that the columns of octahedrally coordinated Na atoms can easily be broken apart when subjected to the heat generated by the electron microprobe beam, with the subsequent expulsion of water. This gives rise to ‘mobile’ Na atoms, which make quantitative electron microprobe analysis extremely difficult. The structure allows the ‘liberated’ Na atoms to move freely within planes parallel to .

Keywords

voggitehydrated Na–Zr hydroxide-phosphate-carbonatecrystal structureNa-ion mobilityFrancon quarryMontrealQuebecCanada
Type
Crystal Structures
Information
Mineralogical Magazine , Volume 54 , Issue 376 , September 1990 , pp. 495 - 500
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1990

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References

Brown, I. D. and Wu, Kang Kun (1976) Empirical Parameters for calculating cation-oxygen bond valences. Acta Cryst. B32, 1957-9.CrossRefGoogle Scholar
Ermer, O. and Dunitz, J. D. (1970) Least-squares refinement of centrosymmetric trial structures in non-centro symetric space groups. A warning. Ibid. A24, 163.Google Scholar
Gabe, E. J., LePage, Y., Charland, J.-P., Lee, F. L. and White, P. S. (1989) NRCVAX—an interactive program system for structure analysis. J. Appl. Cryst. 22, 384-7.CrossRefGoogle Scholar
Hargreaves, A. (1955) Some observations on the probability distribution of X-ray intensities. Acta Cryst. 8, 12-14.CrossRefGoogle Scholar
Howells, E. R., Philips, D. C. and Rogers, D. (1950) The probability distribution of X-ray intensities, II. Experimental investigation and the X-ray detection of centres of symmetry. Ibid. 3, 210-4.CrossRefGoogle Scholar
International Tables for X-ray Crystallography, Vol IV (1974) The Kynoch Press, Birmingham, England. (Ibers, J. A. and Hamilton, W. C., eds.).Google Scholar
Roberts, A. C., Sabina, A. P., Ercit, S. T., Grice, J. D., Szymafiski, J. T. and Ramik, R. A. (1990) Voggite, a new hydrated Na-Zr hydroxide-phosphatecarbonate from the Francon quarry, Montreal, Quebec. Can. Mineral. 28, 155-9.Google Scholar
Szymański, J. T. (1982) The crystal structure of hydrodresserite, BaAl2(CO3)2(OH)4.3H2O. Ibid. 20, 253-62.Google Scholar