University of Maryland Energy Research Center, University of Maryland, College Park, MD, 20742, USA.
Angew Chem Int Ed Engl. 2016 Dec 5;55(49):15268-15271. doi: 10.1002/anie.201607700. Epub 2016 Nov 9.
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 La Sr Co Fe O and (La Sr ) MnO , using gas-phase isotope-exchange with a 1:1 O : O ratio. Oxygen transport mechanisms between gas-surface reactions and surface-bulk exchange are deconvoluted. Our findings show that regardless of participation of lattice oxygen, La Sr Co Fe O is better at oxygen dissociation than (La Sr ) MnO . Heteroexchange, involving lattice oxygen, dominates on La Sr Co Fe O . In contrast, (La Sr ) MnO shows both homoexchange and heteroexchange, with the latter only happening above 600 °C. Using a 1:1 isotope mixture, a simple method is presented for separation of the oxygen dissociation step from the overall ORR.
氧化物上的氧离解是一个关键的反应步骤,限制了许多技术的效率。多步骤氧还原反应 (ORR) 的复杂性使得难以独立研究氧离解步骤。使用气相同位素交换(1:1 O:O 比),对钙钛矿 La Sr Co Fe O 和 (La Sr ) MnO 进行了定量描述,直接观察了氧离解过程。在气-固表面反应和表面-体相交换之间的氧传输机制被解卷积。我们的研究结果表明,无论晶格氧的参与与否,La Sr Co Fe O 比 (La Sr ) MnO 更有利于氧离解。涉及晶格氧的异质交换在 La Sr Co Fe O 上占主导地位。相比之下,(La Sr ) MnO 表现出同型交换和异型交换,后者仅在 600°C 以上发生。使用 1:1 的同位素混合物,提出了一种从整体 ORR 中分离氧离解步骤的简单方法。