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Surface phase diagram of hematite pseudocubes in hydrous environments

机译:含水环境中赤铁矿假立方体的表面相图

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摘要

Hematite nanoparticles often display the pseudocubic morphology enclosed exclusively by the (012) surface. The surface chemistry on these facets is important to understand the formation and properties of these nanoparticles in varying chemical environments. The surface is typically terminated by hydroxyl groups in water or humid atmospheres, and the various terminations differ largely in composition, structure, thermodynamic stability, and chemical reactivity. When we compare a large variety of chemical configurations, we find that three specific terminations are thermodynamically stable under aerobic conditions. The termination by singly and triply coordinated hydroxyl groups (S-, T-OH) is stable at low temperatures and in hydrous environments, the stoichiometric clean termination is stable at high temperatures and in dry environments, and the termination by doubly coordinated hydroxyl groups (D-OH) is stable under intermediate conditions. The S-,T-OH termination can convert topologically to the clean surface by dissociative adsorption of water, whereas the conversion from these two terminations to the D-OH termination requires re-organization of several atomic layers at the surface. Therefore, the surface may reversibly change between S-,T-OH and the clean surface depending on the temperature and humidity. Based on these findings we have constructed surface phase diagrams to predict the termination types in different hydrous and humid environments.
机译:赤铁矿纳米粒子通常显示仅由(012)表面包围的假立方形态。这些方面的表面化学对于了解这些纳米粒子在变化的化学环境中的形成和性质非常重要。该表面通常在水或潮湿的气氛中被羟基封端,并且各种封端在组成,结构,热力学稳定性和化学反应性上有很大不同。当我们比较各种各样的化学构型时,我们发现三个特定的末端在有氧条件下是热力学稳定的。在低温和含水环境中,单和三配位羟基(S-,T-OH)终止是稳定的,在高温和干燥环境中,化学计量的干净终止是稳定的,而在双配位羟基(S-,T-OH)终止稳定( D-OH)在中间条件下稳定。 S-,T-OH末端可以通过水的解离吸附从拓扑上转换为干净的表面,而从这两个末端到D-OH末端的转换需要在表面重新组织几个原子层。因此,表面可能会根据温度和湿度在S-,T-OH和清洁表面之间可逆地变化。基于这些发现,我们构建了表面相图,以预测不同含水和潮湿环境下的终端类型。

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