X-ray fluorescence determination of magnetite iron in iron ores after preliminary magnetic separation

被引:0
作者
V. A. Simakov
V. E. Isaev
机构
[1] Fedorovsky All-Russia Research Institute of Mineral Resources,
来源
Inorganic Materials | 2015年 / 51卷
关键词
magnetite iron; magnetic separation; X-ray fluorescence analysis; iron ores;
D O I
暂无
中图分类号
学科分类号
摘要
The technique for determining the magnetite iron content in iron ores by X-ray fluorescence after preliminary extraction of magnetic fraction by using a magnetic separator is proposed. Separation of the magnetic and nonmagnetic fractions occurs with sufficient completeness and accuracy at a particle size in the sample in the range of–0.074 to +0.044 mm. At smaller grain size, the quality of separation sharply worsens. Mixing of a weighed sample with nonmagnetic powder before separation provides satisfactory accuracy of recovery of the magnetic fraction even in the case of a very finely powdered sample. Application of an X-ray fluorescence energy dispersion spectrometer makes it possible to perform a qualitative assessment of separation by comparison of spectra of scattered and fluorescent radiation after each separation cycle.
引用
收藏
页码:1438 / 1441
页数:3
相关论文
共 4 条
[1]  
Lenin S.S.(1969)Fluorescence X-Ray spectral analysis of geological powdered samples by standard-background technique with the use of noncoherent scatter Appar. Metody Rentgenovskogo Anal. 4 161-164
[2]  
Serikov I.V.(1970)On a technique of defining the background value when fluorescence X-Ray spectral analysis of geological samples Appar. Metody Rentgenovskogo Anal. 7 172-178
[3]  
Lenin S.S.(undefined)undefined undefined undefined undefined-undefined
[4]  
Serikov I.V.(undefined)undefined undefined undefined undefined-undefined