Stages of arc atomic emission spectrometry development as applied to the solid geological samples’ analysis

Q4 Chemistry Analitika i Kontrol Pub Date : 2021-01-01 DOI:10.15826/analitika.2021.25.4.007
I. E. Vasil’eva, E. Shabanova
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引用次数: 1

Abstract

The atomic emission spectrometry (AES) with arc discharge method evolution is inextricably linked with the fundamental scientific discoveries made in the 19th and 20th centuries, and it also reflects the change of scientific paradigms in a specific field of natural science – analytical chemistry. Theoretical comprehension and generalization of experimental data, along with the improving spectral equipment and methodological techniques for determining the elemental and material composition of solid geological samples, increased the accuracy of the analysis results i.e. the results were translated from qualitative to semi-quantitative and quantitative. Modern computerized equipment for direct AES with arc discharge provides minimal errors in measuring the spectral intensity due to the high stability of the excitation source of the spectra of atoms and molecules, the use of high-power polychromators and express digital recording of spectra by multi-channel detectors. However, in the commercial software of spectrometers, only the methods of manual spectra processing proposed in the 30s of the last century are programmed. That limits the possibilities of improving the analysis quality. The time has come to use the developed concept of computer processing of big spectral data, which is based on the information models of chemical analysis and the back propagation of error, in order to select the best models. Current article shows that the information models of computer spectra interpretation obtained from direct arc AES multi-element techniques of geological samples’ analysis using the injection-spillage method provide better quantitative results (category III of accuracy) due to a more complete account of spectral and matrix influences compared to the routine processing techniques.
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电弧原子发射光谱法在固体地质样品分析中的发展阶段
原子发射光谱法与电弧放电方法的演变与19、20世纪的基础科学发现有着密不可分的联系,它也反映了自然科学的一个特定领域——分析化学的科学范式的变化。对实验数据的理论理解和推广,以及测定固体地质样品元素和物质组成的光谱设备和方法技术的改进,提高了分析结果的准确性,即结果从定性转化为半定量和定量。由于原子和分子光谱激发源的高稳定性、高功率多色仪的使用以及多通道探测器对光谱的快速数字记录,用于电弧放电的直接AES的现代计算机化设备在测量光谱强度时提供了最小的误差。然而,在光谱仪的商业软件中,只编写了上世纪30年代提出的手工光谱处理方法。这限制了提高分析质量的可能性。利用基于化学分析信息模型和误差反向传播的计算机处理大光谱数据的成熟概念来选择最佳模型的时机已经到来。目前的文章表明,与常规处理技术相比,使用注入-溢出法分析地质样品的直接弧AES多元素技术获得的计算机光谱解释信息模型提供了更好的定量结果(精度为III类),因为它更完整地描述了光谱和矩阵的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Analitika i Kontrol
Analitika i Kontrol Chemistry-Analytical Chemistry
CiteScore
0.90
自引率
0.00%
发文量
15
期刊介绍: Analitika i Kontrol is a scientific journal covering theoretical and applied aspects of analytical chemistry and analytical control, published since autumn 1997. Founder and publisher of the journal is the Ural Federal University named after the first President of Russia Boris Yeltsin (UrFU, Ekaterinburg).
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