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非晶态氧化铁簇的排列:磁铁矿形成的非经典机制。

Alignment of Amorphous Iron Oxide Clusters: A Non-Classical Mechanism for Magnetite Formation.

机构信息

State Key Laboratory for Modification of Chemical Fibers and Polymer Materials, College of Chemistry, Chemical Engineering and Biotechnology, Center for Advanced Low-Dimension Materials, Donghua University, Shanghai, 201620, China.

Physical Chemistry, University of Konstanz, Universitätsstrasse 10, 78457, Konstanz, Germany.

出版信息

Angew Chem Int Ed Engl. 2017 Mar 27;56(14):4042-4046. doi: 10.1002/anie.201610275. Epub 2017 Mar 2.

Abstract

Despite numerous studies on the nucleation and crystallization of iron (oxyhydr)oxides, the roles of species developing during the early stages, especially primary clusters and intermediate amorphous particles, are still poorly understood. Herein, both ligand-free and ligand-protected amorphous iron oxide (AIO) clusters (<2 nm) were synthesized as precursors for magnetite formation. Thermal annealing can crystallize the clusters into magnetite particles, and AIO bulk phases with domains of pre-aligned clusters are found to be direct precursors to crystals, suggesting a non-classical aggregation-based pathway that differs from the reported oriented attachment or particle accretion mechanisms.

摘要

尽管已经有许多关于铁(氧)氢氧化物成核和结晶的研究,但对于早期形成的物种(特别是初级团簇和中间非晶颗粒)的作用仍了解甚少。在此,我们合成了无配体和配体保护的非晶氧化铁(AIO)团簇(<2nm)作为磁铁矿形成的前体。热退火可以使这些团簇结晶成磁铁矿颗粒,而具有预对准团簇畴的 AIO 体相被发现是晶体的直接前体,这表明存在一种非经典的基于聚集的路径,与报道的定向附着或颗粒 accretion 机制不同。

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