New insight into crystal chemistry of topaz: A multi-methodological study

被引:28
作者
Gatta, G. Diego
Nestola, F.
Bromiley, G. D.
Loose, A.
机构
[1] Univ Milan, Dipartimento Sci Terra, I-20133 Milan, Italy
[2] Univ Padua, Dipartimento Mineral & Petrol, I-35137 Padua, Italy
[3] Univ Bayreuth, Bayer Geo Inst, D-95447 Bayreuth, Germany
[4] Univ Cambridge, Dept Earth Sci, Cambridge CB2 3WQ, England
[5] Forschungszentrum, D-52425 Julich, Germany
关键词
topaz; crystal chemistry; plasma mass spectroscopy; X-ray and neutron diffraction; infrared spectroscopy;
D O I
10.2138/am.2006.2223
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
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 degrees 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 center dot center dot center dot O/F interactions (distances < 2.38 A). 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.
引用
收藏
页码:1839 / 1846
页数:8
相关论文
共 57 条
  • [41] A COMPUTER-PROGRAM FOR REFINEMENT OF CRYSTAL ORIENTATION MATRIX AND LATTICE-CONSTANTS FROM DIFFRACTOMETER DATA WITH LATTICE SYMMETRY CONSTRAINTS
    RALPH, RL
    FINGER, LW
    [J]. JOURNAL OF APPLIED CRYSTALLOGRAPHY, 1982, 15 (OCT) : 537 - 539
  • [42] RIBBE PH, 1971, AM MINERAL, V56, P24
  • [43] Ribbe PH, 1971, AM MINERAL, V57, P168
  • [44] RIBBE PH, 1982, REV MINERAL, P215
  • [45] Rinne F, 1926, Z KRISTALLOGR, V63, P236
  • [46] THE INTENSITY OF FORBIDDEN REFLECTIONS OF PYROPE - UMWEGANREGUNG OR SYMMETRY REDUCTION
    ROSSMANITH, E
    ARMBRUSTER, T
    [J]. ZEITSCHRIFT FUR KRISTALLOGRAPHIE, 1995, 210 (09): : 645 - 649
  • [47] Schmidt MW, 1998, AM MINERAL, V83, P881
  • [48] IR active orientation of OH bending mode in topaz
    Shinoda, K
    Aikawa, N
    [J]. PHYSICS AND CHEMISTRY OF MINERALS, 1997, 24 (08) : 551 - 554
  • [49] On the space-group dispute of stibnite
    Sorensen, HO
    Lundegaard, LF
    [J]. JOURNAL OF APPLIED CRYSTALLOGRAPHY, 2004, 37 : 156 - 158
  • [50] Origin of low-symmetry growth sectors in edingtonite and yugawaralite, and crystal structure of the k{011} and v{120} sectors of yugawaralite
    Tanaka, T
    Kimura, R
    Akizuki, M
    Kudoh, Y
    [J]. MINERALOGICAL MAGAZINE, 2002, 66 (03) : 409 - 420