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原子氢与过渡金属表面的相互作用:一项高通量计算研究。

Atomic Hydrogen Interaction with Transition Metal Surfaces: A High-Throughput Computational Study.

作者信息

Allés Miquel, Meng Ling, Beltrán Ismael, Fernández Ferran, Viñes Francesc

机构信息

Departament de Ciència de Materials i Química Física and Institut de Química Teòrica i Computacional (IQTCUB), Universitat de Barcelona, c/Martí i Franquès 1-11, Barcelona 08028, Spain.

出版信息

J Phys Chem C Nanomater Interfaces. 2024 Nov 16;128(47):20129-20139. doi: 10.1021/acs.jpcc.4c06194. eCollection 2024 Nov 28.

Abstract

Hydrogen adatoms are involved in many reactions catalyzed by Transition Metal (TM) surfaces, such as the Haber-Bosch process or the reverse water gas shift reaction, key to our modern society. Any rational improvement on such a catalyst requires an atomistic knowledge of the metal↔hydrogen interaction, only attainable from first-principles calculations on suited, realistic models. The present thorough density functional theory study evaluates such H interaction at a low coverage on most stable surfaces of , , and TMs. These are (001), (011), and (111) for and TMs and (0001), (101̅0), and (112̅0) for , covering 27 TMs and 81 different TM surfaces in total. In general terms, the results validate, while expanding, previous assessments, revealing that TM surfaces can be divided into two main groups, one in the majority where H would be thermodynamically driven to dissociate into H adatoms, located at heights of ∼0.5 or ∼1.0 Å, and another for late TMs, generally with a electronic configuration, where H adsorption with no dissociation would be preferred. No trends in H adsorption energies are found down the groups, but yes along the series, with a best linear adjustment found for the -band center descriptor, especially suited for close-packed and TMs surfaces, with a mean absolute error of 0.15 eV. Gibbs free adsorption energies reveal a theoretical volcano plot where TMs are best suited, but with peak Pt performance displaced due to dispersive force inclusion in the method. Still, the volcano plot with respect to the experimental logarithm of the exchanged current density polycrystalline data is far from being valid for a quantitative assessment, although useful for a qualitative screening and to confirm the trends computationally observed.

摘要

氢原子参与了许多由过渡金属(TM)表面催化的反应,如哈伯-博施法或逆水煤气变换反应,这些反应对现代社会至关重要。对这种催化剂进行任何合理的改进都需要对金属与氢的相互作用有原子层面的了解,而这只有通过对合适的、现实的模型进行第一性原理计算才能实现。目前这项全面的密度泛函理论研究评估了氢在铁、钴、镍过渡金属最稳定表面上低覆盖度时的相互作用。对于铁和钴过渡金属,这些表面是(001)、(011)和(111);对于镍过渡金属,这些表面是(0001)、(101̅0)和(112̅0),总共涵盖27种过渡金属和81个不同的过渡金属表面。一般来说,研究结果在扩展先前评估的同时进行了验证,表明过渡金属表面可分为两大类,一类占多数,氢在热力学作用下会解离成氢原子,氢原子位于约0.5或约1.0 Å的高度;另一类是晚期过渡金属,通常具有d电子构型,更倾向于不发生解离的氢吸附。在族中未发现氢吸附能的趋势,但在周期系列中存在趋势,对于能带中心描述符发现了最佳线性拟合,特别适用于密排的铁和钴过渡金属表面,平均绝对误差为0.15 eV。吉布斯自由吸附能揭示了一个理论火山图,其中镍过渡金属最适合,但由于方法中包含色散力,铂的峰值性能发生了偏移。尽管如此,相对于实验测得的多晶交换电流密度对数数据的火山图,对于定量评估远非有效,不过对于定性筛选以及确认计算观察到的趋势还是有用的。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7747/11613584/5e3ac4ddf29f/jp4c06194_0001.jpg

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