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首页> 外文期刊>Journal of the American Chemical Society >Carbonate Formation and Decomposition on Atomic Oxygen Precovered Au(111)
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Carbonate Formation and Decomposition on Atomic Oxygen Precovered Au(111)

机译:原子氧吸附的Au(111)的碳酸盐形成与分解

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The carbonate formation and decomposition (CO_3 ←→ CO_2 + O_a) reaction on gold is important from the point of view of low-temperature CO oxidation. Carbonate formation has been proposed as a possible reaction intermediate in CO oxidation in several investigations of supported and unsupported gold clusters. Therefore, an understanding of this reaction on Au(111) may provide additional insight. Carbonate formation and decomposition went undetected in previous studies on Au(110) and Au(111). However, a surface carbonate was readily formed when oxygen precovered Ag(110) was exposed to CO_2 at 300 K. This surface carbonate decomposes to produce CO_2 at 485 K and the remaining oxygen atoms recombinatively desorbed at 590 K. Owing to its similarity with silver, we would anticipate equally facile carbonate formation and decomposition reactions on gold. Similar reactions have also been reported on other surfaces.
机译:从低温CO氧化的观点来看,碳在金上的碳酸盐形成和分解(CO_3←→CO_2 + O_a)反应很重要。在对支持和不支持的金团簇的一些研究中,已提出碳酸盐的形成是CO氧化中可能的反应中间体。因此,对Au(111)上该反应的理解可能会提供其他见解。在先前关于Au(110)和Au(111)的研究中未发现碳酸盐的形成和分解。但是,当将预先覆盖了氧气的Ag(110)在300 K下暴露于CO_2时,很容易形成表面碳酸盐。该表面碳酸盐在485 K下分解产生CO_2,其余的氧原子在590 K下复合解吸。 ,我们预计在金上同样容易发生碳酸盐形成和分解反应。在其他表面上也有类似反应的报道。

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