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arXiv 2209.04205cond-mat.mtrl-sci
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赤铁矿与水蒸气的快速氧交换

Rapid oxygen exchange between hematite and water vapor

Zdenek Jakub, Matthias Meier, Florian Kraushofer, Jan Balajka, Jiri Pavelec, Michael Schmid, Cesare Franchini, Ulrike Diebold, Gareth S. Parkinson

摘要:

氧化物/液体和氧化物/气体界面的氧交换在技术和环境研究中非常重要,因为它与催化活性和材料降解密切相关。然而,原子尺度的细节大多是未知的,并且通常归因于晶格中定义不清的缺陷。在这里,我们表明,即使是化学稳定的,有序的表面可以令人惊讶的反应。具体来说,我们发现,在70 °C以下的温度下,赤铁矿(α-Fe 2 O3)无缺陷单晶r切割(1-102)表面上的所有3重配位晶格氧原子在几分钟内与周围水蒸气中的氧交换,而原子尺度的表面结构未受该过程的干扰。在液态水暴露后观察到类似的行为,但实验数据清楚地表明,大多数交换发生在最终单层的解吸过程中,而不是在浸泡过程中。密度泛函理论计算表明,交换可以发生在表面扩散,其中晶格氧提取的成本是由HO-HOH-OH复合物的稳定性补偿。这种对晶格氧稳定性的见解与许多研究领域高度相关,从催化和制氢到地球化学和古气候学。

英文摘要:

Oxygen exchange at oxide/liquid and oxide/gas interfaces is important in technology and environmental studies, as it is closely linked to both catalytic activity and material degradation. The atomic-scale details are mostly unknown, however, and are often ascribed to poorly defined defects in the crystal lattice. Here we show that even thermodynamically stable, well-ordered surfaces can be surprisingly reactive. Specifically, we show that all the 3-fold coordinated lattice oxygen atoms on a defect-free single-crystalline r-cut (1-102) surface of hematite (α-Fe2O3) are exchanged with oxygen from surrounding water vapor within minutes at temperatures below 70 °C, while the atomic-scale surface structure is unperturbed by the process. A similar behavior is observed after liquid water exposure, but the experimental data clearly show most of the exchange happens during desorption of the final monolayer, not during immersion. Density functional theory computations show that the exchange can happen during on-surface diffusion, where the cost of the lattice oxygen extraction is compensated by the stability of an HO-HOH-OH complex. Such insights into lattice oxygen stability are highly relevant for many research fields ranging from catalysis and hydrogen production to geochemistry and paleoclimatology.

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