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American Mineralogist; November 2006; v. 91; no. 11-12; p. 1839-1846; DOI: 10.2138/am.2006.2223
© 2006 Mineralogical Society of America
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New insight into crystal chemistry of topaz: A multi-methodological study

G. Diego Gatta1,*, F. Nestola2,3, G.D. Bromiley4 and A. Loose5

1 Dipartimento di Scienze della Terra, Università degli Studi di Milano, Via Botticelli 23, I-20133 Milano, Italy
2 Dipartimento di Mineralogia e Petrologia, Università degli Studi di Padova, Corso Garibaldi 37, I-35137 Padova, Italy
3 Bayerisches Geoinstitut, Universität Bayreuth, Universitätsstrasse 30, D-95447 Bayreuth, Germany
4 Department of Earth Sciences, Cambridge University, Downing Street, Cambridge CB2 3EQ, U.K.
5 Forschungszentrum Jülich, D-52425 Jülich, Germany

Correspondence: * E-mail: diego.gatta{at}unimi.it

The crystal chemistry of a natural topaz [with OH/(OH + F) < 0.5] was reinvestigated by means of laser ablation inductively coupled plasma mass spectroscopy, single-crystal X-ray diffraction (at 298 K) and neutron diffraction (at 298 and 10 K), and polarized infrared spectroscopy to define unambiguously the real symmetry of topaz, the location of the proton and its thermal displacement parameters at room and low temperatures, the hydrogen-bonding and the vibration modes (stretching and bending) of the OH dipole. X-ray and neutron structural refinements allow us to infer that the crystal structure of natural topaz with OH/(OH + F) < 0.5 can be described with the Pbnm space group. Violating reflections, found in the previous investigations and in this study, are likely due to Renninger effect (double diffraction phenomenon). The nuclear density Fourier map shows that the proton is located at Wyckoff 8d position and the refined coordinates are: x = 0.495(2), y = 0.252(1), z = 0.1629(7). The O-H bond lies on the (010)-plane and forms an angle of about 28.9° with the c-axis. Neutron structural refinements at 298 and 10 K show that the displacement ellipsoid of the proton is highly anisotropic. The H-bonding arrangement appears to be complex, with at least four potential H···O/F interactions (distances < 2.38 Å). The topological configuration of the O-H group described by the neutron structural refinements is confirmed by the infrared investigation: the OH stretching mode (at 3640 cm–1) has no component of vibration parallel to the b axis (i.e., the O-H direction is perpendicular to [010]). The OH bending mode (at 1161 cm–1) shows components along the three crystallographic axes, which appear to be more prominent along the a and b-axes. The possible distribution into the crystal structure of topaz of the minor/trace elements found (Na, Ca, Fe Cr, V, Ti, B), and the implied topological effects, is discussed.

Key Words: Topaz • crystal chemistry • plasma mass spectroscopy • X-ray and neutron diffraction • infrared spectroscopy




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K. Komatsu, H. Kagi, W.G. Marshall, T. Kuribayashi, J.B. Parise, and Y. Kudoh
Pressure dependence of the hydrogen-bond geometry in topaz-OD from neutron powder diffraction
American Mineralogist, January 1, 2008; 93(1): 217 - 227.
[Abstract] [Full Text] [PDF]




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