Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
American Mineralogist Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

American Mineralogist; July 2003; v. 88; no. 7; p. 996-1002
© 2003 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 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 Web of Science (10)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Dinnebier, R. E.
Right arrow Articles by Jansen, M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Bulk moduli and high-pressure crystal structures of minium, Pb3O4, determined by X-ray powder diffraction

Robert E. Dinnebier1, Stefan Carlson2, Michael Hanfland3 and Martin Jansen1,*

1 Max-Planck-Institute for Solid State Research, Heisenbergstrasse 1, D-70569 Stuttgart, Germany
2 MAX-lab, Lund University, P.O. Box 118, SE-22100 Lund, Sweden
3 Experiments Division High Pressure Group, European Synchrotron Radiation Facility, B.P. 220, F-38043 Grenoble CEDEX, France

Correspondence: * E-mail: m.jansen{at}fkf.mpg.de

We report the pressure dependence of the crystal structure of lead tetroxide (p ≤ 41.05 GPa, T = 298 K) using high-resolution angle-dispersive X-ray powder diffraction. Pb3O4 shows two reversible phase transitions in the measured pressure range. The crystal structures of the modifications identified have in common frameworks of Pb+4O6 octahedra and irregular Pb+2O4+1 respectively Pb2+O6+1 polyhedra. At ambient conditions, Pb3O4 crystallizes in space group P42/mbc (phase I). Between 0.11 and 0.3 GPa it exhibits a displacive second order phase transition to a structure with space group Pbam (phase II). A second displacive phase transition occurs between 5.54 and 6.6 GPa to another structure with space group Pbam (phase III) but halved c dimension. A non-linear compression behavior over the entire pressure range is observed, which can be described by two Vinet relations in the ranges from 0.28 to 5.54 GPa and from 6.6 to 41.05 GPa. The extrapolated bulk moduli of the high-pressure phases were determined to be K0 = 21(2) GPa for phase II and K0 = 91(3) GPa for phase III. The crystal structures of all phases were refined from X-ray diffraction powder data collected at several pressures between 0.06 and 41.05 GPa. Except for their cell dimensions, phases I and II were found to be isostructural to the corresponding phases at low temperatures, whereas phase III can be derived from the Sr2PbO4 aristotype. With increasing pressure, the lone pair which is localized at Pb2+ adopts increasingly pure s-character, which is reflected by the similar coordination polyhedra of Pb2+ in Pb3O4 (phase III) and of Sr2+ in Sr2PbO4.




This article has been cited by other articles:


Home page
American MineralogistHome page
L. B. Railsback
Patterns in the compositions of oxysalt and sulfosalt minerals, and the paradoxical nature of quartz
American Mineralogist, February 1, 2007; 92(2-3): 356 - 369.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Mineralogical Society of America