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A density functional theory study on the interaction mechanism between H2S and the α-Fe2O3(0001) surface

机译:H2S与α-Fe2O3(0001)表面相互作用机理的密度泛函理论研究

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摘要

The interaction mechanism of H2S and the α-Fe2O3(0001) surface during the desulfurization has been investigated by the density functional theory (DFT) method within a periodic slab model. Adsorptions of H2S, SH, S and H on the α-Fe2O3(0001) surface have been initially examined. Our results show that H2S, SH and atomic S favorably adsorb on the top of Fe site, and atomic H lies on the top of 0 site. Potential energy profiles have been constructed for the interactions of H2S with the α-Fe2O3(0001) surface along with two channels producing H2 and H2O. The calculations show that H2S firstly adsorbs on the α-Fe2O3(0001) surface in molecular mode, followed by two dehydroge-nation processes and forming surface sulfur species. Further, the processes of H-migration lead to the formation of H2 or H2O. Molecular-level calculations demonstrate that the pathways of H2-forming and H2O-forming are competitive kinetically. Two roles of the α-Fe2O3 during the interactions between H2S and the α-Fe2O3(0001) surface have also been discussed.
机译:在周期性平板模型中,通过密度泛函理论(DFT)方法研究了H2S与α-Fe2O3(0001)在脱硫过程中的相互作用机理。最初已经检查了H2S,SH,S和H在α-Fe2O3(0001)表面上的吸附。我们的结果表明,H2S,SH和原子S有利地吸附在Fe位点的顶部,原子H位于0位点的顶部。已经构造了用于H2S与α-Fe2O3(0001)表面以及产生H2和H2O的两个通道相互作用的势能曲线。计算表明,H2S首先以分子方式吸附在α-Fe2O3(0001)表面,然后经过两个脱氢过程并形成表面硫物种。此外,H迁移的过程导致形成H 2或H 2O。分子水平的计算表明,H2形成和H2O形成的途径在动力学上具有竞争性。还讨论了H2S和α-Fe2O3(0001)表面相互作用期间α-Fe2O3的两个作用。

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