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首页> 外文期刊>Journal of Materials Science >Characterization of ultrafine gamma-Fe(C), alpha-Fe(C) and Fe3C particles synthesized by arc-discharge in methane
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Characterization of ultrafine gamma-Fe(C), alpha-Fe(C) and Fe3C particles synthesized by arc-discharge in methane

机译:甲烷中电弧放电合成的超细γ-Fe(C),α-Fe(C)和Fe3C颗粒的表征

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Ultrafine gamma-Fe(C), alpha-Fe(C) and Fe3C particles were prepared by arc-discharge synthesis in a methane atmosphere. The phases, morphology, structure and surface layer of the particles were studied by means of X-ray diffraction (XRD), transmission electron microscopy (TEM) techniques and X-ray photoelectron spectroscopy (XPS). It was found that the mean particle size ranged from 9.8 to 12.8 nm. The surface of particles mostly consisted of a carbon layer and a little oxide. Phase transformation from gamma-Fe(C) to alpha-Fe(C) was studied by annealing in vacuum and by differential thermal analysis and thermogravimetry (DTA-TGA) measurement. The abundance of gamma-Fe( C) was determined by a magnetization measurement to be approximately 30%. Phase transformation occurred between 300 and 500 degrees C in a flowing argon atmosphere. The Fe3C particles oxidized to alpha-Fe2O3 and carbon dioxide at 610 degrees C or so. (C) 1998 Chapman & Hall. [References: 17]
机译:超细γ-Fe(C),α-Fe(C)和Fe3C颗粒是通过在甲烷气氛中进行电弧放电合成制备的。通过X射线衍射(XRD),透射电子显微镜(TEM)技术和X射线光电子能谱(XPS)研究了颗粒的相,形态,结构和表面层。发现平均粒径为9.8-12.8nm。颗粒表面主要由碳层和少量氧化物组成。通过真空退火,差热分析和热重分析(DTA-TGA)测量研究了从γ-Fe(C)到α-Fe(C)的相变。通过磁化测量确定γ-Fe(C)的丰度约为30%。在流动的氩气气氛中,相变发生在300到500摄氏度之间。 Fe3C颗粒在610摄氏度左右氧化为α-Fe2O3和二氧化碳。 (C)1998查普曼和霍尔。 [参考:17]

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