Formation and Decomposition of Iron Nitrides Observed by in situ Powder Neutron Diffraction and Thermal Analysis

热分解 分析化学(期刊) 中子衍射 无定形固体 材料科学 粉末衍射 大气温度范围 氮化铁 氮化物 氮气 结晶学 化学 晶体结构 热力学 图层(电子) 有机化学 复合材料 物理 色谱法
作者
Marc Widenmeyer,Thomas C. Hansen,Elke Meißner,Rainer Niewa
出处
期刊:Zeitschrift für anorganische und allgemeine Chemie [Wiley]
卷期号:640 (7): 1265-1274 被引量:48
标识
DOI:10.1002/zaac.201300676
摘要

Abstract In order to gain more information on the formation and decomposition behavior of various iron nitrides from different starting materials in situ neutron diffraction and thermal analysis under application of different gas atmospheres and heating rates were carried out. The following phases were observed during these investigations: crystalline α‐Fe, γ‐FeN z , γ′‐Fe 4 N y , ϵ‐Fe 3 N 1+ x , ζ‐Fe 2 N, FeCl 2 , [Fe(NH 3 ) 6 ]Cl 2 , Fe(NH 3 ) 2 Cl 2 , and amorphous Fe(NH 3 )Cl 2 . In situ neutron diffraction data were collected in high quality, due to an optimized experimental setup with a time resolution of two minutes on D20 (Institut Laue‐Langevin) allowing for detailed Rietveld analyses. For all phase transitions, decomposition and formation temperatures a strong dependency from the heating rate, thermal history of the sample, gas flow conditions, and particle size exists. The nitrogen contents observed during thermal decomposition of ζ‐Fe 2 N were related to the binary phase diagram Fe‐N. At low temperatures (< 400 °C) ϵ‐ and ζ‐phase are non‐equilibrated. However, through annealing equilibrium state is reached. For γ′‐Fe 4 N y formed in situ at higher temperatures an expansion of the homogeneity range towards lower nitrogen content is observed above 600 °C. For the formation of ϵ‐Fe 3 N 1+ x from FeCl 2 and NH 3 a previously proposed reaction sequence involving different ammoniates was confirmed. This reaction occurs via formation of amorphous Fe(NH 3 )Cl 2 . The therein observed in situ formed ammoniates were additionally characterized by IR spectroscopy.

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