Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.


Science 12 May 2000:
Vol. 288. no. 5468, pp. 1029 - 1033
DOI: 10.1126/science.288.5468.1029

Reports

Structure of the Hydrated alpha -Al2O3 (0001) Surface

Peter J. Eng, 1* Thomas P. Trainor, 2 Gordon E. Brown Jr., 23 Glenn A. Waychunas, 4 Matthew Newville, 1 Stephen R. Sutton, 1 Mark L. Rivers 15

The physical and chemical properties of the hydrated alpha -Al2O3 (0001) surface are important for understanding the reactivity of natural and synthetic aluminum-containing oxides. The structure of this surface was determined in the presence of water vapor at 300 kelvin by crystal truncation rod diffraction at a third-generation synchrotron x-ray source. The fully hydrated surface is oxygen terminated, with a 53% contracted double Al layer directly below. The structure is an intermediate between alpha -Al2O3 and gamma -Al(OH)3, a fully hydroxylated form of alumina. A semiordered oxygen layer about 2.3 angstroms above the terminal oxygen layer is interpreted as adsorbed water. The clean alpha -Al2O3 (0001) surface, in contrast, is Al terminated and significantly relaxed relative to the bulk structure. These differences explain the different reactivities of the clean and hydroxylated surfaces.

1 Consortium for Advanced Radiation Sources, The University of Chicago, Chicago, IL 60637, USA.
2 Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305-2115, USA.
3 Stanford Synchrotron Radiation Laboratory, Stanford, CA 94309, USA.
4 Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA.
5 Department of Geophysical Sciences, The University of Chicago, Chicago, IL 60637, USA.
*   To whom correspondence should be addressed. E-mail: eng{at}cars.uchicago.edu


Read the Full Text


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Structure, Chemistry, and Properties of Mineral Nanoparticles.
G. A. Waychunas and H. Zhang (2008)
Elements 4, 381-387
   Abstract »    Full Text »    PDF »
Scientific Advances Made Possible by User Facilities.
G. E. Brown Jr., G. Calas, and R. J. Hemley (2006)
Elements 2, 23-30
   Abstract »    Full Text »    PDF »
Molecular-Scale Processes Involving Nanoparticulate Minerals in Biogeochemical Systems.
B. Gilbert and J. F. Banfield (2005)
Reviews in Mineralogy and Geochemistry 59, 109-155
   Full Text »    PDF »
Laminar Growth of Ultrathin Metal Films on Metal Oxides: Co on Hydroxylated alpha -Al2O3(0001).
S. A. Chambers, T. Droubay, D. R. Jennison, and T. R. Mattsson (2002)
Science 297, 827-831
   Abstract »    Full Text »    PDF »
An Overview of Synchrotron Radiation Applications to Low Temperature Geochemistry and Environmental Science.
G. E. Brown Jr. and N. C. Sturchio (2002)
Reviews in Mineralogy and Geochemistry 49, 1-115
   Full Text »    PDF »
X-ray Reflectivity as a Probe of Mineral-Fluid Interfaces: A User Guide.
P. A. Fenter (2002)
Reviews in Mineralogy and Geochemistry 49, 149-221
   Full Text »    PDF »
Oxidation of Chromium(III) to (VI) by Manganese Oxides.
J. G. Kim, J. B. Dixon, C. C. Chusuei, and Y. Deng (2002)
Soil Sci. Soc. Am. J. 66, 306-315
   Abstract »    Full Text »    PDF »
Pb(II) distributions at biofilm-metal oxide interfaces.
A. S. Templeton, T. P. Trainor, S. J. Traina, A. M. Spormann, and G. E. Brown Jr. (2001)
PNAS
   Abstract »    Full Text »    PDF »
Pb(II) distributions at biofilm-metal oxide interfaces.
A. S. Templeton, T. P. Trainor, S. J. Traina, A. M. Spormann, and G. E. Brown Jr. (2001)
PNAS 98, 11897-11902
   Abstract »    Full Text »    PDF »



To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)