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Mnemonic Rutile–Rutile Interfaces Triggering Spontaneous Dissociation of Water

机译:助记金红石-金红石界面触发水的自发解离

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Water interaction with mineral surfaces is a complex living system decisive forany photocatalytic process. Resolving the atomistic structure ofmineral–water interfaces is thus crucial for understanding these processes.Fibrous rutile TiO_2, grown hydrothermally on twinned rutile seeds underacidic conditions, is studied in terms of interface translation, atomic structure,and surface chemistry in the presence of water, by means of advancedmicroscopy and spectroscopy methods combined with structure modelingand density functional theory calculations. It is shown that fibers whilestaying in stable separation during their growth, adopt a specialcrystallographic registry that is controlled by repulsion forces between fullyhydroxylated and protonated (110) surfaces. During relaxation, a turbulentproton transfer and cracking of O-H bonds is observed, generating a strongacidic character via proton jump from bridge -OH~b to terminal -OH~t groups,and spontaneous dissociation of interfacial water via a transient protonationof the -OH~t groups. It is shown, that this specific interface structure can beimplemented to induce acidic response in an initially neutral medium whenre-immersed. This is thought to be the first demonstration ofquantum-confined mineral–water interface, capable of memorizing its pastand conveying its structurally encoded properties into a new environment.
机译:水与矿物表面的相互作用是一个复杂的生命系统,对任何光催化过程都具有决定性作用。因此,解析矿水界面的原子结构对于理解这些过程至关重要。采用先进的显微镜和光谱学方法,结合结构建模和密度泛函理论计算,从界面平移、原子结构和水存在下的表面化学等方面研究了在酸性条件下双生金红石种子的纤维性金红石TiO_2。结果表明,纤维在生长过程中保持稳定分离的同时,采用了一种特殊的晶体学登记,该登记由完全羟基化和质子化(110)表面之间的排斥力控制。在弛豫过程中,观察到湍流质子转移和O-H键的破裂,通过质子从桥-OH~b跃升到末端-OH~t基团产生强酸性,并通过-OH~t基团的瞬态质子化产生界面水的自发解离。结果表明,当重新浸入时,可以实现这种特定的界面结构以在初始中性介质中诱导酸性响应。这被认为是量子限制矿泉水界面的首次演示,能够记住其过去并将其结构编码特性传达到新环境中。

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