Structure of the hydrated α-Al2O3 (0001) surface

被引:473
|
作者
Eng, PJ [1 ]
Trainor, TP
Brown, GE
Waychunas, GA
Newville, M
Sutton, SR
Rivers, ML
机构
[1] Univ Chicago, Consortium Adv Radiat Sources, Chicago, IL 60637 USA
[2] Stanford Univ, Dept Geol & Environm Sci, Stanford, CA 94305 USA
[3] Stanford Synchrotron Radiat Lab, Stanford, CA 94309 USA
[4] Univ Calif Berkeley, Lawrence Berkeley Lab, Div Earth Sci, Berkeley, CA 94720 USA
[5] Univ Chicago, Dept Geophys Sci, Chicago, IL 60637 USA
关键词
D O I
10.1126/science.288.5468.1029
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
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.
引用
收藏
页码:1029 / 1033
页数:5
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