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水溶液中形成的铁(III)-氧低聚物电子结构的检测。

Detection of the electronic structure of iron-(iii)-oxo oligomers forming in aqueous solutions.

作者信息

Seidel Robert, Kraffert Katrin, Kabelitz Anke, Pohl Marvin N, Kraehnert Ralph, Emmerling Franziska, Winter Bernd

机构信息

Helmholtz-Zentrum Berlin für Materialien und Energie, Institute for Material Development, Albert-Einstein-Strasse 15, D-12489 Berlin, Germany.

出版信息

Phys Chem Chem Phys. 2017 Dec 13;19(48):32226-32234. doi: 10.1039/c7cp06945f.

Abstract

The nature of the small iron-oxo oligomers in iron-(iii) aqueous solutions has a determining effect on the chemical processes that govern the formation of nanoparticles in aqueous phase. Here we report on a liquid-jet photoelectron-spectroscopy experiment for the investigation of the electronic structure of the occurring iron-oxo oligomers in FeCl aqueous solutions. The only iron species in the as-prepared 0.75 M solution are Fe monomers. Addition of NaOH initiates Fe hydrolysis which is followed by the formation of iron-oxo oligomers. At small enough NaOH concentrations, corresponding to approximately [OH]/[Fe] = 0.2-0.25 ratio, the iron oligomers can be stabilized for several hours without engaging in further aggregation. Here, we apply a combination of non-resonant as well as iron 2p and oxygen 1s resonant photoelectron spectroscopy from a liquid microjet to detect the electronic structure of the occurring species. Specifically, the oxygen 1s partial electron yield X-ray absorption (PEY-XA) spectra are found to exhibit a peak well below the onset of liquid water and OH (aq) absorption. The iron 2p absorption gives rise to signal centered between the main absorption bands typical for aqueous Fe. Absorption bands in both PEY-XA spectra are found to correlate with an enhanced photoelectron peak near 20 eV binding energy, which demonstrates the sensitivity of resonant photoelectron (RPE) spectroscopy to mixing between iron and ligand orbitals. These various signals from the iron-oxo oligomers exhibit maximum intensity at [OH]/[Fe] = 0.25 ratio. For the same ratio, we observe changes in the pH as well as in complementary Raman spectra, which can be assigned to the transition from monomeric to oligomeric species. At approximately [OH]/[Fe] = 0.3 we begin to observe particles larger than 1 nm in radius, detected by small-angle X-ray scattering.

摘要

铁(III)水溶液中小的铁氧低聚物的性质对控制水相中纳米颗粒形成的化学过程具有决定性影响。在此,我们报告了一项用于研究FeCl水溶液中存在的铁氧低聚物电子结构的液体喷射光电子能谱实验。在制备的0.75 M溶液中,唯一的铁物种是铁单体。加入NaOH引发铁水解,随后形成铁氧低聚物。在足够小的NaOH浓度下,对应于大约[OH]/[Fe]=0.2 - 0.25的比例,铁低聚物可以稳定几个小时而不发生进一步聚集。在此,我们应用非共振以及来自液体微喷射的铁2p和氧1s共振光电子能谱的组合来检测所存在物种的电子结构。具体而言,发现氧1s部分电子产率X射线吸收(PEY - XA)光谱在液态水和OH(aq)吸收起始点以下有一个明显的峰。铁2p吸收产生的信号集中在水溶液中铁典型的主要吸收带之间。发现两个PEY - XA光谱中的吸收带都与结合能接近20 eV处增强的光电子峰相关,这证明了共振光电子(RPE)光谱对铁和配体轨道之间混合的敏感性。来自铁氧低聚物的这些各种信号在[OH]/[Fe]=0.25比例时表现出最大强度。对于相同比例,我们观察到pH以及互补拉曼光谱的变化,这可以归因于从单体物种到低聚物种的转变。在大约[OH]/[Fe]=0.3时,我们开始观察到通过小角X射线散射检测到的半径大于1 nm的颗粒。

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