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Unusual redox behaviour of the magnetite/hematite core-shell structures processed by the laser floating zone method

机译:激光浮区法处理磁铁矿/赤铁矿芯壳结构的异常氧化还原行为

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摘要

Magnetite (Fe3O4) offers unique physical and chemical properties, being an important material for many industrial applications. Certain limitations on the application conditions are, however, imposed by the redox stability issue. Fine control of the iron oxidation states represents a challenge for materials engineering. The present work explores relevant redox processes in iron oxides, processed under highly non equilibrium laser floating zone (LFZ) conditions under atmospheres with different oxygen activities. The as-grown fibres showed a structure composed of the Fe3O4 core and the Fe2O3 shell. This study uncovers unexpectedly lower hematite content and shell thickness for the fibres processed under more oxidizing conditions. Combined structural and microstructural studies, supported by the analysis of the existing literature data, strongly suggest that the redox processes during the LFZ process can be rather determined by kinetics of melt crystallization, nuclei formation and heat transfer than by the oxygen content in the gas phase. The proposed mechanisms are further confirmed by electrical and magnetic studies of the composite fibres.
机译:磁铁矿(FE3O4)提供独特的物理和化学性质,是许多工业应用的重要材料。然而,对申请条件的某些限制由氧化还原稳定性问题施加。铁氧化态的精细控制是材料工程的挑战。本作者探讨了在高度平衡激光浮区(LFZ)条件下的氧化铁中的相关氧化还原过程,在大气下具有不同的氧气活性。生长的纤维显示由Fe3O4核和Fe 2 O 3壳组成的结构。本研究发现在更氧化条件下加工的纤维的含纤维含量和壳体厚度揭示。通过分析现有文献数据的组合结构和微观结构研究强烈建议在LFZ过程中的氧化还原过程可以通过熔融结晶,核形成和传热而不是通过气相中的氧含量来确定的氧化还原过程。通过复合纤维的电和磁性研究进一步证实了所提出的机制。

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