AB INITIO MOLECULAR DYNAMICS STUDY OF Fe-CONTAINING SMECTITES

被引:10
|
作者
Liu, Xiandong [1 ]
Meijer, Evert Jan [2 ,3 ]
Lu, Xiancai [1 ]
Wang, Rucheng [1 ]
机构
[1] Nanjing Univ, State Key Lab Mineral Deposit Res, Sch Earth Sci & Engn, Nanjing 210093, Peoples R China
[2] Univ Amsterdam, Vant Hoff Inst Mol Sci, NL-1018 WV Amsterdam, Netherlands
[3] Univ Amsterdam, Amsterdam Ctr Multiscale Modeling, NL-1018 WV Amsterdam, Netherlands
关键词
CPMD; Density Functional Theory; Hydroxyl Orientation; Iron; Smectite; Vibration Dynamics; DIOCTAHEDRAL; 2/1; PHYLLOSILICATES; 1ST PRINCIPLES CALCULATIONS; DENSITY-FUNCTIONAL THEORY; INFRARED-SPECTRUM; OXIDATION-STATE; VIBRATIONAL PROPERTIES; GARFIELD NONTRONITE; CLAY-MINERALS; STRUCTURAL FE; PYROPHYLLITE;
D O I
10.1346/CCMN.2010.0580109
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
In order to identify the influences imposed by Fe substitution, density functional theory-based Car-Parrinello molecular dynamics simulations were employed to study both oxidized and reduced Fe-bearing smectites. The following basic properties were investigated: local structures in the clay layer, hydroxyl on and the vibration dynamicos of H and Si. Structural analyses indicated that the average Fe-O bond lengths are similar to 2.08 angstrom and 2.02 angstrom in the reduced and oxidized models, respectively, and the Fe substitutions did not affect the coordination structures of the Al-O and Si-O polyhedra. For hydroxyl orientations, Fe(III) substitution had no obvious in but Fe(II) forces the coordinated hydroxyls to present a wide-angle distribution. Furthermore, the present work has shown that both substitutions can red-shift the hydroxyl in-plane bending mode. The analyses also revealed that Fe(III) substitution has no effect on the Si-O stretching, while Fe reduction causes a blue-shift of the out-of-plane stretching mode. The results provide quantitative constraints and clues for future research.
引用
收藏
页码:89 / 96
页数:8
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