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首页> 外文期刊>The Analyst: The Analytical Journal of the Royal Society of Chemistry: A Monthly International Publication Dealing with All Branches of Analytical Chemistry >ANALYSIS OF SILICATE ROCKS USING FIELD-PORTABLE X-RAY FLUORESCENCE INSTRUMENTATION INCORPORATING A MERCURY(II) IODIDE DETECTOR - A PRELIMINARY ASSESSMENT OF ANALYTICAL PERFORMANCE
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ANALYSIS OF SILICATE ROCKS USING FIELD-PORTABLE X-RAY FLUORESCENCE INSTRUMENTATION INCORPORATING A MERCURY(II) IODIDE DETECTOR - A PRELIMINARY ASSESSMENT OF ANALYTICAL PERFORMANCE

机译:掺汞(II)碘化物探测器的现场便携式X射线荧光仪分析硅质岩-分析性能的初步评估

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摘要

An assessment is reported of the performance of a field-portable energy dispersive X-ray fluorescence analysis system using Fe-55, Cd-109 and Am-241 excitation sources and a high resolution mercury(II) iodide detector, Seventy international reference materials, mainly of silicate composition, were analysed as compressed powder pellets. Results from spectra recorded for live times of 200 s (per source) showed that the major elements K, Ca, Ti, Mn and Fe and the trace elements Ba, Nb, Rb, Sr, Y and Zr could be determined routinely in 'normal' silicate rocks and in addition Co, Cr, Cu, Ga, La, Nd, Ni, V and Zn at higher concentrations or in mineralized samples, Detection limits for the most sensitively measured trace elements (Rb, Sr, Y, Zr, Nb) were found to be in the range 6-14 mu g g(-1) and for Ba (K-line), 21 mu g g(-1) Precision in the determination of the major elements was generally in the range 0.45-2% (relative standard deviation) and a high degree of accuracy was achieved when judged from a self-consistent comparison of analysed values with the expected compositions of the 70 reference materials, Having characterized performance in the laboratory with 'ideal' control over sample presentation, work is now in progress to evaluate additional discrepancies that will be encountered in the analysis of geological and archaeological samples in the field. [References: 24]
机译:报告了使用Fe-55,Cd-109和Am-241激发源以及高分辨率碘化汞(II)检测器的现场便携式能量色散X射线荧光分析系统的性能评估,七十种国际参考材料,主要由硅酸盐组成的粉末被分析为压缩粉末颗粒。记录的200 s(每个信号源)的实时光谱结果表明,可以正常测定主要元素K,Ca,Ti,Mn和Fe以及痕量元素Ba,Nb,Rb,Sr,Y和Zr。较高浓度或矿化样品中的硅酸盐岩石以及Co,Cr,Cu,Ga,La,Nd,Ni,V和Zn,最敏感测量的痕量元素(Rb,Sr,Y,Zr,Nb )被发现在6-14 mu gg(-1)的范围内,而对于Ba(K线),在21 mu gg(-1)的范围内主要元素的测定精度通常在0.45-2%的范围内通过将分析值与70种参考物质的预期成分进行自洽比较来判断时,可以达到(相对标准偏差)和高度准确性,具有在实验室中表现出的“理想”控制样品呈现,工作表现的特点目前正在进行评估地质和地质分析中会遇到的其他差异的工作。 d野外考古样品。 [参考:24]

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