001     57967
005     20240619091034.0
024 7 _ |2 DOI
|a 10.2138/am.2006.1896
024 7 _ |2 WOS
|a WOS:000234527900004
037 _ _ |a PreJuSER-57967
041 _ _ |a eng
082 _ _ |a 550
084 _ _ |2 WoS
|a Geochemistry & Geophysics
084 _ _ |2 WoS
|a Mineralogy
100 1 _ |0 P:(DE-HGF)0
|a Gatta, G. D.
|b 0
245 _ _ |a The real topological configuration of the extra-framework content in alkali-poor beryl: a multi methodological study
260 _ _ |a Washington, DC
|b Soc.
|c 2006
300 _ _ |a 29 - 34
336 7 _ |a Journal Article
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336 7 _ |a ARTICLE
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336 7 _ |a JOURNAL_ARTICLE
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336 7 _ |a article
|2 DRIVER
440 _ 0 |0 17581
|a American Mineralogist
|v 91
|x 1945-3027
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a The crystal structure of alkali/water-poor beryl (1120 + Na2O + Cs2O < 1.2 wt%) was reinvestigated by means of laser ablation inductively coupled plasma mass spectroscopy, thermogravimetric analysis, neutron diffraction, and polarized infrared spectroscopy to determine the real topological configuration of the extra-framework content in the six-membered ring channels. Analysis of the nuclear density Fourier map suggests that the (water) oxygen is located along the sixfold axis at the 2a site (0,0, 1/4), whereas the (water) protons are at -0.028(7), -0.071(3), 0.332(1). The hydrogen atoms are distributed in 6 x 2 equivalent positions, above and below the oxygen site. Geometrical configuration of the water molecule is well defined: the O-H bond distance is 0.949(18) angstrom and the H-O-H bond angle is 106.9(2.2)degrees. The (HH)-H-... vector is oriented at similar to 4 degrees from [001]. This configuration is completely different from that found in alkali-rich beryl, where the (HH)-H-... vector is perpendicular to [00 1]. Na is probably located, with the H2O oxygen, at the 2a site. According to the chemical analysis, which shows that the amounts of other alkali and earth-alkali cations are negligible (Rb, K, Mg, Mn <= 110 ppm, Ca <= 225 ppm, Cs <= 430 ppm), no effect of other cations on the extra-framework population was observed in the structural refinement. The final agreement index (R-1) of the structural refinement was 0.037 for 34 refined parameters and 160 unique reflections with F-0 > 4 sigma(F-0). The topological configuration of the H2O molecule into the channel is confirmed by the spectroscopic investigation. Polarized single-crystal IR spectra show that the H2O molecule is oriented with the molecular symmetry axis perpendicular to the hexagonal axis and (HH)-H-... vector parallel (or quasi-parallel) to [001].
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653 2 0 |2 Author
|a chemical mineral analysis
653 2 0 |2 Author
|a L-A-ICP-MAS
653 2 0 |2 Author
|a crystal structure
653 2 0 |2 Author
|a single-crystal neutron diffraction
653 2 0 |2 Author
|a water-poor beryl
653 2 0 |2 Author
|a polarized IR-spectra
653 2 0 |2 Author
|a trace elements
653 2 0 |2 Author
|a REE
700 1 _ |0 P:(DE-HGF)0
|a Nestola, F.
|b 1
700 1 _ |0 P:(DE-HGF)0
|a Bromiley, G. D.
|b 2
700 1 _ |0 P:(DE-Juel1)130821
|a Mattauch, S.
|b 3
|u FZJ
773 _ _ |0 PERI:(DE-600)2045960-9
|a 10.2138/am.2006.1896
|g Vol. 91, p. 29 - 34
|p 29 - 34
|q 91<29 - 34
|t American mineralogist
|v 91
|x 1945-3027
|y 2006
909 C O |o oai:juser.fz-juelich.de:57967
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914 1 _ |a Nachtrag
|y 2006
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
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