Hydrogen oxidation on oxygen-rich IrO2(110)

Q1 Materials Science
Tao Li, Minkyu Kim, Zhu Liang, A. Asthagiri, J. Weaver
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引用次数: 11

Abstract

ABSTRACT We investigated the adsorption and oxidation of H2 on O-rich IrO2(110) using temperature programmed reaction spectroscopy (TPRS) and density functional theory (DFT) calculations. Our results show that H2 dissociation occurs efficiently on O-rich IrO2(110) at low temperature and initiates from an adsorbed H2 σ-complex on the coordinatively-unsaturated Ir atoms (Ircus). We find that on-top oxygen atoms (Oot), adsorbed on the Ircus sites, promote the desorption-limited evolution of H2O during subsequent oxidation of the adsorbed hydrogen on IrO2(110) while suppressing reaction-limited production of H2O via the recombination of bridging HO groups (HObr) (~500 to 750 K) during TPRS. The desorption-limited TPRS peak of H2O shifts from ~490 to 550 K with increasing Oot coverage, demonstrating that Oot atoms stabilize adsorbed OH and H2O species. DFT predicts that molecularly-adsorbed H2 dissociates on O-rich IrO2(110) at low temperature and that the resulting H-atoms redistribute to produce a mixture of HObr and HOot groups, with equilibrium favouring HOot groups. Our calculations further predict that subsequent H2O evolution occurs through the recombination of HObr/HOot and HOot/HOot pairs, and that these reactions represent desorption-limited pathways because the dissociative chemisorption of H2O is favoured over molecular adsorption on IrO2(110). The higher stability of HOot groups and their preferred formation causes the higher-barrier HOot/HOot recombination reaction to become the dominant pathway for H2O formation with increasing Oot coverage, consistent with the experimentally-observed upshift in the H2O TPRS peak temperature. Graphical abstract
富氧IrO2(110)上的氢氧化
摘要我们利用程序升温反应光谱(TPRS)和密度泛函理论(DFT)计算研究了富O IrO2(110)对H2的吸附和氧化。我们的结果表明,H2在低温下在富O的IrO2(110)上有效地发生离解,并由配位不饱和Ir原子(Ircus)上吸附的H2σ-络合物引发。我们发现,吸附在Ircus位点上的顶部氧原子(Oot)在随后吸附的氢在IrO2(110)上的氧化过程中促进了H2O的解吸受限释放,同时在TPRS过程中通过桥接HO基团(HObr)的重组(~500-750K)抑制了H2O的反应受限产生。随着Oot覆盖率的增加,H2O的解吸限制TPRS峰从~490 K移动到550K,表明Oot原子稳定了吸附的OH和H2O物种。DFT预测,分子吸附的H2在低温下在富含O的IrO2(110)上离解,并且所得的H原子重新分布以产生HObr和HOot基团的混合物,平衡有利于HOot基团。我们的计算进一步预测,随后的H2O进化是通过HObr/HOot和HOot/HOot对的重组发生的,并且这些反应代表了解吸受限的途径,因为H2O的离解化学吸附比IrO2上的分子吸附更有利(110)。HOot基团及其优选形成的更高稳定性导致随着Oot覆盖率的增加,更高的势垒HOot/HOot复合反应成为H2O形成的主要途径,这与实验观察到的H2O TPRS峰值温度的升高一致。图形摘要
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Catalysis Structure & Reactivity
Catalysis Structure & Reactivity CHEMISTRY, PHYSICAL-
CiteScore
4.80
自引率
0.00%
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0
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