Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
American Mineralogist Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

American Mineralogist; January 2006; v. 91; no. 1; p. 29-34; DOI: 10.2138/am.2006.1896
© 2006 Mineralogical Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Deposit data for Gatta et al.
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (4)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Gatta, G. D.
Right arrow Articles by Mattauch, S.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

The real topological configuration of the extra-framework content in alkali-poor beryl: A multi-methodological study

G. Diego Gatta1,2,*, F. Nestola2, G.D. Bromiley2,3 and S. Mattauch4

1 Dipartimento di Scienze della Terra, Universita’ degli Studi di Milano, Via Botticelli 23, I-20133 Milano, Italy
2 Bayerisches Geoinstitut, Universitaet Bayreuth, Universitaet Str. 30, D-95447 Bayreuth, Germany
3 Department of Earth Sciences, Cambridge University, Downing Street, Cambridge CB2 3EQ, U.K.
4 Forschungszentrum Jülich, D-52425 Jülich, Germany

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

The crystal structure of alkali/water-poor beryl (H2O + 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) Å and the H-O-H bond angle is 106.9(2.2)°. The H···H vector is oriented at ~4° from [001]. This configuration is completely different from that found in alkali-rich beryl, where the H···H vector is perpendicular to [001]. 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 (R1) of the structural refinement was 0.037 for 34 refined parameters and 160 unique reflections with Fo > 4{sigma}(Fo). 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 H···H vector parallel (or quasi-parallel) to [001].

Key Words: Chemical mineral analysis • L-A-ICP-MAS • crystal structure • single-crystal neutron diffraction • water-poor beryl • polarized IR-spectra • trace elements • REE




This article has been cited by other articles:


Home page
American MineralogistHome page
G. D. Gatta, F. Nestola, G.D. Bromiley, and A. Loose
New insight into crystal chemistry of topaz: A multi-methodological study
American Mineralogist, November 1, 2006; 91(11-12): 1839 - 1846.
[Abstract] [Full Text] [PDF]


Home page
Reviews in Mineralogy and GeochemistryHome page
E. Libowitzky and A. Beran
The Structure of Hydrous Species in Nominally Anhydrous Minerals: Information from Polarized IR Spectroscopy
Reviews in Mineralogy and Geochemistry, January 1, 2006; 62(1): 29 - 52.
[Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Mineralogical Society of America