当前位置: X-MOL 学术Inorg. Mater. › 论文详情
Our official English website, www.x-mol.net, welcomes your feedback! (Note: you will need to create a separate account there.)
X-Ray Fluorescence Determination of Ore Elements in Ferromanganese Formations
Inorganic Materials ( IF 0.8 ) Pub Date : 2020-12-29 , DOI: 10.1134/s0020168520140046
V. M. Chubarov , A. A. Amosova , A. L. Finkelshtein

Abstract

Elemental analysis of ferromanganese formations (first of all, the determination of ore elements) is a necessary stage in the development of ore deposits. A technique for X-ray fluorescence quantitative analysis was proposed for the determination of iron, manganese, cobalt, nickel, copper, and zinc in oceanic ferromanganese formations (nodules and crusts). The studies were performed using a S4 Pioneer wavelength-dispersive spectrometer equipped with a LiF (200) crystal and a scintillation detector. In order to plot the calibration curves, sets of certified reference materials such as ferromanganese nodules, cobalt-bearing ferromanganese crusts, and pelagic sediments previously dried at 105°C for 24 h to remove hygroscopic moisture were used. Two sample preparation techniques were compared: pressing of powder samples with the use a boric acid substrate and homogenizing via fusion with lithium tetraborate at a ratio of 1 : 30 in an electric furnace at 1050°C. For each sample preparation technique, spectral overlaps and matrix correction methods (theoretical and empirical) were considered, and optimal calibration curves for determining ore elements were chosen. The accuracy of the X-ray fluorescence technique was assessed via analyzing a reference material FeMn-1 with a certified content of ore elements and a reference ferromanganese nodule sample preliminarily analyzed using a PerkinElmer M403 atomic absorption spectrometer. Both homogenization via fusion and analysis of pressed samples provide quantitative X-ray fluorescence determination of the main ore elements and can be used to assess the industrial significance of oceanic ferromanganese formations.



中文翻译:

X射线荧光法测定锰铁矿中矿石元素

摘要

铁锰形成的元素分析(首先是确定矿石元素)是矿床开发中的必要阶段。提出了一种用于X射线荧光定量分析的技术,用于测定海洋锰铁地层(结核和结壳)中的铁,锰,钴,镍,铜和锌。使用配备有LiF(200)晶体和闪烁检测器的S4 Pioneer波长色散光谱仪进行研究。为了绘制校准曲线,使用了一组经过认证的参考材料,例如锰铁结核,含钴的锰铁结壳和预先在105°C下干燥24小时以去​​除吸湿性的浮游沉积物。比较了两种样品制备技术:使用硼酸基质压制粉末样品,并在1050°C的电炉中通过以1:30的比例与四硼酸锂熔融而均质化。对于每种样品制备技术,均应考虑光谱重叠和基质校正方法(理论和经验),并选择确定矿石元素的最佳校准曲线。X射线荧光技术的准确性是通过使用PerkinElmer M403原子吸收光谱仪分析具有矿物质含量的参考材料FeMn-1和参考的锰铁结核样品进行初步评估的。

更新日期:2020-12-29
down
wechat
bug