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; July 2001; v. 86; no. 7-8; p. 910-914
© 2001 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 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 (7)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Balan, E.
Right arrow Articles by Calas, G.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

First principles study of water adsorption on the (100) surface of zircon: Implications for zircon dissolution

Etienne Balan1,*, Francesco Mauri1, Jean-Pierre Muller1,2 and Georges Calas1

1 Laboratoire de Minéralogie-Cristallographie, UMR CNRS 7590, Universités Paris 6 et 7, IPGP, Case 115, 4 Place Jussieu, 75252 Paris Cedex 05, France
2 IRD, 213 Rue Lafayette, 75480 Paris Cedex 10, France

Correspondence: * E-mail: Etienne.Balan{at}lmcp.jussieu.fr

We have studied the interaction of aqueous species with the (100) face of zircon using first-principles quantum mechanical calculations. Adsorption energy of molecular water on the Zr Lewis site is 1.27 eV per molecule, whereas the energy of dissociative adsorption is only 0.84 eV per molecule. Thus, the non-dissociative adsorption of water is strongly preferred with respect to the dissociative adsorption on the (100) face of zircon. Such behavior, which is related to the weak ability of the surface structure to relax, is changed by a 5% increase of the surface cell parameters. From our theoretical results, we propose that the exceptional resistance of zircon to dissolution may be related to the strong acidity of the Zr-O-Si bridging O atoms, which promotes the associative adsorption of water on the (100) surface of zircon.




This article has been cited by other articles:


Home page
American MineralogistHome page
M. Zhang, L. A. Boatner, E. K.H. Salje, S. Honda, and R. C. Ewing
Pb+ irradiation of synthetic zircon (ZrSiO4): Infrared spectroscopic investigation
American Mineralogist, August 1, 2008; 93(8-9): 1418 - 1423.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
S. Delattre, S. Utsunomiya, R. C. Ewing, J.-L. Boeglin, J.-J. Braun, E. Balan, and G. Calas
Dissolution of radiation-damaged zircon in lateritic soils
American Mineralogist, November 1, 2007; 92(11-12): 1978 - 1989.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
E. Balan, E. Balan, F. Mauri, C. J. Pickard, I. Farnan, and G. Calas
The aperiodic states of zircon: an ab initio molecular dynamics study
American Mineralogist, November 1, 2003; 88(11-12): 1769 - 1777.
[Abstract] [Full Text] [PDF]


Home page
American MineralogistHome page
T. Geisler, T. Geisler, R. T. Pidgeon, R. Kurtz, W. van Bronswijk, and H. Schleicher
Experimental hydrothermal alteration of partially metamict zircon
American Mineralogist, October 1, 2003; 88(10): 1496 - 1513.
[Abstract] [Full Text] [PDF]




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