Dispersion-Corrected Density Functional Theory and Classical Force Field Calculations of Water Loading on a Pyrophyllite(001) Surface

被引:42
作者
Zhang, Guozhen [1 ,2 ,3 ]
Al-Saidi, W. A. [1 ,2 ,4 ]
Myshakin, Evgeniy M. [3 ,5 ]
Jordan, Kenneth D. [1 ,2 ,3 ]
机构
[1] Univ Pittsburgh, Dept Chem, Pittsburgh, PA 15260 USA
[2] Univ Pittsburgh, Ctr Mol & Mat Simulat, Pittsburgh, PA 15260 USA
[3] Natl Energy Technol Lab, Pittsburgh, PA 15236 USA
[4] Univ Pittsburgh, Dept Chem & Petr Engn, Pittsburgh, PA 15261 USA
[5] URS, Pittsburgh, PA 15236 USA
关键词
INITIO MOLECULAR-DYNAMICS; AB-INITIO; SMECTITE CLAY; TOTAL-ENERGY; ADSORPTION; MONTMORILLONITES; SIMULATION; COMPLEXES; HYDRATION; HEXAMER;
D O I
10.1021/jp305801d
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070305 [高分子化学与物理];
摘要
Water adsorption on the (001) surface of pyrophyllite [Al(OH)(Si2O5)] was investigated using density functional theory (DFT) with dispersion corrections and force field calculations. The DFT calculations show that a water molecule can bind either to one or to two basal oxygen atoms of the surface, with adsorption energies varying from -0.10 to -0.19 eV depending on the binding configuration and binding site. Because the water-water interactions are stronger than the water-surface interactions, the energetically preferred structures with two or more molecules on the surface are clusters reminiscent of their gas-phase counterparts. The trend in water-surface binding energies with the number of water molecules obtained from force field calculations qualitatively agrees with that predicted by the dispersion-corrected DFT calculations. However, the force field calculations give a low-energy structural motif with a water molecule coordinated to a hydroxyl group associated with the octahedral layer of the pyrophyllite surface. This binding motif is found to be unstable in the DFT calculations.
引用
收藏
页码:17134 / 17141
页数:8
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