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用穆斯堡尔谱仪分析焙烧铁矿石样品中的含铁矿物的相态变化
The analysis of the phase changes of the iron minerals in roasted iron ore samples by Mossbauer spectrometer
【摘要】 <正> 本文用穆斯堡尔效应,分析了在400℃、500℃、600℃、700℃、800℃及900℃的温度下,在还原、中性、氧化气氛中,分别焙烧40分钟后,铁矿石样品中各含铁矿物的铁的相对含量,在最佳磁化焙烧温度(650~700℃)下磁性矿相(Fe3O4+γ-Fe2O3)的相对含量达80~90%,从而为选矿工艺提供了有价值的数据。
【Abstract】 This paper has systematically analysed the relative contents of the iron in the iron-containing minerals of iron ore samples by Mossbauer spectrometer. The iron ore samples were roasted in reductive atmosphere, neutral atmosphere and oxidation atmosphere at 400℃, 500℃, 600℃, 700℃, 800℃ and 900℃ for forty minutes, respectively. This work has provided valuable data for some iron-steel companies.
- 【文献出处】 核技术 ,Nuclear Techniques , 编辑部邮箱 ,1982年06期
- 【被引频次】1
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