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

American Mineralogist; October; v. 93; no. 10; p. 1558-1567; DOI: 10.2138/am.2008.2849
© 2008 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
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
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 (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Sano-Furukawa, A.
Right arrow Articles by Ohtani, E.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Neutron diffraction study of {delta}-AlOOD at high pressure and its implication for symmetrization of the hydrogen bond

Asami Sano-Furukawa1,*, Kazuki Komatsu2,3, Carine B. Vanpeteghem4 and Eiji Ohtani1

1 Department of Earth and Planetary Materials Science, Tohoku University, Sendai 980-8578, Japan
2 Geochemical Laboratory, Graduate School of Science, University of Tokyo, Tokyo 113-0033, Japan
3 Centre for Science at Extreme Conditions, University of Edinburgh, Mayfield Road, Edinburgh, EH9 3JZ, U.K.
4 School of Chemistry and Biochemistry, Georgia Institute of Technology, Atlanta, Georgia 30332, U.S.A.

We have conducted a powder neutron diffraction study of the distorted rutile-type hydrous phase {delta}-AlOO(D0.74H0.26) at pressures up to 9.2 GPa. Rietveld refinement reveals that the observed diffraction data are best fitted by a model with an asymmetric hydrogen bond (space group P21nm). The Al-O2 bonds of the AlO6 octahedron remain longer than the Al-O1 bonds up to 9.2 GPa, reflecting the fact that O2 is the donor and O1 is the acceptor of the hydrogen bond of O2-D···O1. As pressure increases, the Al-O1 bond lengths remain almost constant or increase slightly, whereas the longer Al-O2 bonds are more compressible. The O···O distance of the shared edge of the octahedron is almost constant unlike the other O···O distances that decrease during compression. The bulk modulus of the AlO6 octahedron is determined to be 197.0(4) GPa, where K’ is fixed to 4. The AlO6 octahedron rotates about 1° during compression to 9.2 GPa. As pressure increases and the O2···O1 distance decreases, the D···O1 bond is shortened, whereas the O2-D bond becomes elongated, with pressure dependencies of –1.81(9) x 10–2 Å/GPa and 0.57(8) x 10–2 Å/GPa, respectively, implying the symmetrization of the hydrogen bond at high pressure. The decrease in intensity of the 120 reflection as pressure increases suggests that the transition from the structure with space group P21nm to that with Pnnm would take place in {delta}-AlOOD at high pressure. This transition could be attributed to the disorder of deuterium or symmetrization of the hydrogen bond.

Key Words: {delta}-AlOOD • neutron diffraction • hydrogen bond • symmetrization




This article has been cited by other articles:


Home page
American MineralogistHome page
A. Sano-Furukawa, H. Kagi, T. Nagai, S. Nakano, S. Fukura, D. Ushijima, R. Iizuka, E. Ohtani, and T. Yagi
Change in compressibility of {delta}-AlOOH and {delta}-AlOOD at high pressure: A study of isotope effect and hydrogen-bond symmetrization
American Mineralogist, August 1, 2009; 94(8-9): 1255 - 1261.
[Abstract] [Full Text] [PDF]


Home page
Mineral MagHome page
A. Suzuki
Compressibility of the high-pressure polymorph of AlOOH to 17 GPa
Mineralogical Magazine, June 1, 2009; 73(3): 479 - 485.
[Abstract] [Full Text] [PDF]




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