磁铁矿
碳纤维
反应性(心理学)
共晶体系
氧化物
碳热反应
金属
钨铁矿
还原气氛
无机化学
大气温度范围
氧化钙
氧化铁
化学
材料科学
相(物质)
冶金
有机化学
微观结构
复合数
气象学
复合材料
病理
物理
替代医学
医学
作者
Shiyong Wu,Xiao Zhang,Jing Gu,Youqing Wu,Jinsheng Gao
出处
期刊:Energy & Fuels
[American Chemical Society]
日期:2007-06-09
卷期号:21 (4): 1827-1831
被引量:19
摘要
Under the nitrogen atmosphere, carbothermal reactions of calcium oxide and magnetite began at about 900 and 820 °C, respectively. Above about 1200 °C, CaO reacted with carbon to form CaC2, and the interaction between carbon and CaO was dominant. At the temperature range of 820−920 °C, Fe3O4 was reduced quickly to Fe. After the process, with the increase of the heat-treatment temperature, Fe reacted with carbon to produce the eutectic compound of Fe and carbon (FexCy) and the mole ratio of C and Fe in FexCy became larger and larger but no Fe3C was presented. At the low-temperature range of 950−1100 °C, calcium oxide and magnetite separately presented a catalytic action on the reactivity of carbon and the mixture of calcium oxide and magnetite had a cocatalytic effect on the carbon reaction with CO2. Under the CO2 atmosphere, the carbothermal reactions of metal oxides were restrained in the temperature range (950−1100 °C) above the point, at which the carbothermal reaction of metal oxides started to take place under the N2 atmosphere.
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