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Direct Observation of Oxygen Dissociation on Non-Stoichiometric Metal Oxide Catalysts

机译:直接观察非化学计量金属氧化物催化剂上的氧离解

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摘要

Oxygen dissociation on metal oxides is a key reaction step, limiting the efficiency of numerous technologies. The complexity of the multi-step oxygen reduction reaction (ORR) makes it difficult to investigate the oxygen dissociation step independently. Direct observation of the oxygen dissociation process is described, quantitatively, on perovskites La0.6Sr0.4Co0.2Fe0.8O3- and (La0.8Sr0.2)(0.95)MnO3 +/-, using gas-phase isotope-exchange with a 1:1 O-16(2):O-18(2) ratio. Oxygen transport mechanisms between gas-surface reactions and surface-bulk exchange are deconvoluted. Our findings show that regardless of participation of lattice oxygen, La0.6Sr0.4Co0.2Fe0.8O3- is better at oxygen dissociation than (La0.8Sr0.2)(0.95)MnO3 +/-. Heteroexchange, involving lattice oxygen, dominates on La0.6Sr0.4Co0.2Fe0.8O3-. In contrast, (La0.8Sr0.2)(0.95)MnO3 +/- shows both homoexchange and heteroexchange, with the latter only happening above 600 degrees C. Using a 1:1 isotope mixture, a simple method is presented for separation of the oxygen dissociation step from the overall ORR.
机译:金属氧化物上的氧离解是关键的反应步骤,限制了许多技术的效率。多级氧还原反应(ORR)的复杂性使得难以独立研究氧解离步骤。定量描述了钙钛矿La0.6Sr0.4Co0.2Fe0.8O3-和(La0.8Sr0.2)(0.95)MnO3 +/-上氧解离过程的直接观察,使用气相同位素交换为1 1:1 O-16(2):O-18(2)比率。消除了气体-表面反应与表面-本体交换之间的氧气传输机制。我们的发现表明,无论晶格氧的参与如何,La0.6Sr0.4Co0.2Fe0.8O3-的氧离解性能均优于(La0.8Sr0.2)(0.95)MnO3 +/-。涉及晶格氧的异质交换在La0.6Sr0.4Co0.2Fe0.8O3-上占主导地位。相比之下,(La0.8Sr0.2)(0.95)MnO3 +/-表现出均质交换和异质交换,后者仅在600摄氏度以上发生。使用1:1同位素混合物,提出了一种简单的分离方法氧离解步骤从整体ORR开始。

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