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首页> 外文期刊>The journal of physical chemistry, C. Nanomaterials and interfaces >Comparison of Multilayer Water Adsorption on the Hydrophobic Galena (PbS) and Hydrophilic Pyrite (FeS2) Surfaces: A DFT Study
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Comparison of Multilayer Water Adsorption on the Hydrophobic Galena (PbS) and Hydrophilic Pyrite (FeS2) Surfaces: A DFT Study

机译:疏水方铅矿(PbS)和亲水性黄铁矿(FeS2)表面上多层水吸附的比较:DFT研究

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摘要

To investigate the essential difference in the water adsorption on the hydrophobic galena (PbS) and hydrophilic pyrite (FeS2) surfaces, a single, mono-, and multilayer water adsorptions on the PbS and FeSz(100) surfaces have been simulated by means of density functional theory. The calculated results show that the water molecule adsorption on the hydrophobic PbS surface is via a hydrogen bond between the S and H atom and on the hydrophilic FeS2 surface is mainly via the interaction between surface Fe and the water O atom. On the galena surface, the hydrogen bond effect of multilayer water weakens the S···H bond interaction and leads to the galena surface being hydrophobic. For the pyrite surface, the hydrogen bond effect of the multilayer water enhances the activity of the O 2p orbital and favors the interaction of the O 2p and Fe 3d e_g orbital, which results in the pyrite surface being hydrophilic and undergoing a greater relaxation. These variations may have a great influence on the subsequent mterfacial reactions on the galena and pyrite surfaces.
机译:为了研究疏水方铅矿(PbS)和亲水性黄铁矿(FeS2)表面上水吸附的本质区别,已通过密度模拟了PbS和FeSz(100)表面上的单,单和多层水吸附功能理论。计算结果表明,疏水性PbS表面的水分子吸附是通过S和H原子之间的氢键,而亲水FeS2表面的水分子吸附主要是通过表面Fe和水O原子之间的相互作用。在方铅矿表面,多层水的氢键作用减弱了S··H键的相互作用,并导致方铅矿表面疏水。对于黄铁矿表面,多层水的氢键作用增强了O 2p轨道的活性,并有利于O 2p和Fe 3d e_g轨道的相互作用,这导致黄铁矿表面具有亲水性,并具有更大的松弛度。这些变化可能会对方铅矿和黄铁矿表面的后续界面反应产生重大影响。

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