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

American Mineralogist; November 2007; v. 92; no. 11-12; p. 1827-1832; DOI: 10.2138/am.2007.2382
© 2007 Mineralogical Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
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 (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Fechtelkord, M.
Right arrow Articles by Bismayer, U.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Proton dynamics in letovicite: Part II. Static 2H NMR experiments and lineshape simulations

Michael Fechtelkord1,*, Astrid Diekmann2 and Ulrich Bismayer3

1 Institut für Geologie, Mineralogie und Geophysik der Ruhr-Universität Bochum, Universitätsstrasse 150, 44780 Bochum, Germany
2 Institut für Mineralogie der Universität Hannover, Welfengarten 1, 30167 Hannover, Germany
3 Mineralogisch-Petrographisches Institut der Universität Hamburg, Grindelallee 48, 20146 Hamburg, Germany

Correspondence: * E-mail: Michael.Fechtelkord{at}ruhr-uni-bochum.de

Synthetic deuterated letovicite (ND4)3D(SO4)2 has been investigated using static 2H NMR spectroscopy acquired with a quadrupolar echo sequence. Subsequently, the experimental signals were fitted with theoretical quadrupolar lineshapes to extract the quadrupolar coupling parameters. Experiments were carried out in the temperature range of 102–425 K. Two different signals were distinguished due to ammonium and free acidic deuterons. The ammonium deuterons show only small quadrupolar interaction at room temperature, which can be described best by a fast anisotropic dynamic reorientation of the tetrahedra leading to residual quadrupolar interaction. The dynamically averaged "static" quadrupolar coupling constant is CQ = 2.4 kHz at room temperature. The development of CQ as a function of temperature clearly indicates three phase transitions at 160, 260, and 400 K (triclinic P1 -> monoclinic P2/n or Pn -> monoclinic C2/c -> rhombohedral RFormulam). The asymmetry parameter {eta} shows a similar behavior. It indicates strongest the monoclinic -> monoclinic phase transition at 260 K. The lineshape corresponding to the free acidic protons is difficult to simulate because it is strongly superimposed by the dominant ammonium proton resonance. However, the decrease of the quadrupolar coupling constant of the signal from CQ = 108 kHz at 130 K to 31.5 kHz above 370 K can be assigned to a time-averaging of the quadrupolar interaction due to the increased motion of the sulfate tetrahedra about their threefold axis, so that CQ amounts to only 1/3 of the static quadrupolar coupling constant of the static spectrum at low temperatures.

Key Words: Letovicite • proton conduction • ferroelastic • 2H • lineshape analysis • simulation • reorientation • solid state NMR • quadrupole echo




This article has been cited by other articles:


Home page
American MineralogistHome page
M. Fechtelkord, A. Diekmann, and U. Bismayer
Proton dynamics in letovicite: Part I. Static 1H and 15N NMR MAS experiments and lineshape simulations
American Mineralogist, November 1, 2007; 92(11-12): 1821 - 1826.
[Abstract] [Full Text] [PDF]




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