Wang Chongmin, Baer Donald R, Amonette James E, Engelhard Mark H, Antony Jiji, Qiang You
Environmental Molecular Sciences Laboratory, Pacific Northwest National Laboratory, P.O. Box 999, Richland, Washington 99352, USA.
J Am Chem Soc. 2009 Jul 1;131(25):8824-32. doi: 10.1021/ja900353f.
An iron (Fe) nanoparticle exposed to air at room temperature will be instantly covered by an oxide shell that is typically approximately 3 nm thick. The nature of this native oxide shell, in combination with the underlying Fe(0) core, determines the physical and chemical behavior of the core-shell nanoparticle. One of the challenges of characterizing core-shell nanoparticles is determining the structure of the oxide shell, that is, whether it is FeO, Fe(3)O(4), gamma-Fe(2)O(3), alpha-Fe(2)O(3), or something else. The results of prior characterization efforts, which have mostly used X-ray diffraction and spectroscopy, electron diffraction, and transmission electron microscopic imaging, have been framed in terms of one of the known Fe-oxide structures, although it is not necessarily true that the thin layer of Fe oxide is a known Fe oxide. In this Article, we probe the structure of the oxide shell on Fe nanoparticles using electron energy loss spectroscopy (EELS) at the oxygen (O) K-edge with a spatial resolution of several nanometers (i.e., less than that of an individual particle). We studied two types of representative particles: small particles that are fully oxidized (no Fe(0) core) and larger core-shell particles that possess an Fe core. We found that O K-edge spectra collected for the oxide shell in nanoparticles show distinct differences from those of known Fe oxides. Typically, the prepeak of the spectra collected on both the core-shell and the fully oxidized particles is weaker than that collected on standard Fe(3)O(4). Given the fact that the origin of this prepeak corresponds to the transition of the O 1s electron to the unoccupied state of O 2p hybridized with Fe 3d, a weak pre-edge peak indicates a combination of the following four factors: a higher degree of occupancy of the Fe 3d orbital; a longer Fe-O bond length; a decreased covalency of the Fe-O bond; and a measure of cation vacancies. These results suggest that the coordination configuration in the oxide shell on Fe nanoparticles is defective as compared to that of their bulk counterparts. Implications of these defective structural characteristics on the properties of core-shell structured iron nanoparticles are discussed.
在室温下暴露于空气中的铁(Fe)纳米颗粒会立即被一层通常约3纳米厚的氧化壳所覆盖。这种天然氧化壳的性质,与下面的Fe(0)核相结合,决定了核壳纳米颗粒的物理和化学行为。表征核壳纳米颗粒的挑战之一是确定氧化壳的结构,即它是FeO、Fe₃O₄、γ-Fe₂O₃、α-Fe₂O₃,还是其他物质。先前表征工作的结果,大多使用X射线衍射和光谱、电子衍射以及透射电子显微镜成像,是以已知的铁氧化物结构之一来描述的,尽管铁氧化物的薄层不一定是已知的铁氧化物这一点并不一定正确。在本文中,我们使用电子能量损失谱(EELS)在氧(O)K边以几纳米的空间分辨率(即小于单个颗粒的分辨率)探测铁纳米颗粒上氧化壳的结构。我们研究了两种类型的代表性颗粒:完全氧化的小颗粒(无Fe(0)核)和具有铁核的较大核壳颗粒。我们发现,纳米颗粒中氧化壳收集的O K边光谱与已知铁氧化物的光谱有明显差异。通常,在核壳颗粒和完全氧化颗粒上收集的光谱的预峰比在标准Fe₃O₄上收集的预峰弱。鉴于这个预峰的起源对应于O 1s电子向与Fe 3d杂化的O 2p未占据态的跃迁,一个弱的预边峰表明以下四个因素的综合作用:Fe 3d轨道的占有率较高;Fe - O键长较长;Fe - O键的共价性降低;以及一定程度的阳离子空位。这些结果表明,与它们的块状对应物相比,铁纳米颗粒上氧化壳中的配位构型是有缺陷的。讨论了这些有缺陷的结构特征对核壳结构铁纳米颗粒性质的影响。