Comparative Study on the 2 Methods for Preparation of Sample Discs in XRFS Analysis of Carbonates
摘 要
在X射线荧光光谱法分析碳酸盐时,采用了两种样片的制法,即熔融法和超细粉末压片法,并对此两种方法进行了比较研究。结果表明:在所测定的15种组分中,采用超细粉末压片法所制样品的分析结果,其检出限有较大的改善,这是由于样品在制备过程中未被稀释;对测定的精密度而言,虽然在主、次组分方面不如熔融法好,但对于痕量组分,则超细粉末压片法占优。此外,在超细粉末压片制样过程中不存在二氧化碳的逃逸,而且粒度效应也基本消除,因此可定量测定碳酸盐中二氧化碳的含量。
Abstract
In the XRFS analysis of carbonates, a comparative study was made between the methods of preparation of sample discs by the fusion method and by the method of pressure-disking of super-fines (PDSF) in 3 aspects. As shown by the results: ① in the determination of 15 components in carbonate samples, values of detection limits were significantly improved with sample disc prepared by PDSF since no dilution of sample by additives was encountered; ② although higher precision of analytical results of major and minor components were obtained for sample disc prepared by the fusion method, but better precision of results was obtained for trace constituents with sample disc prepared by the PDSF method; and ③ as no escaping of CO2 was observed and the particls size effect was eliminated in the process of PDSF, quantitative determination of CO2 in carbonates was realized by using sample disc thus prepared.
中图分类号 O657.34 DOI 10.11973/lhjy-hx201606011
所属栏目 工作简报
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收稿日期 2015/5/20
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备注李小莉(1974-),女,河北廊坊人,高级工程师,主要 从事X射线荧光光谱分析及分析方法的建立。
引用该论文: LI Xiao-li,WU Liang-ying,WANG Li-qiang,WU Yan-tao. Comparative Study on the 2 Methods for Preparation of Sample Discs in XRFS Analysis of Carbonates[J]. Physical Testing and Chemical Analysis part B:Chemical Analysis, 2016, 52(6): 664~668
李小莉,吴良英,王力强,吴彦涛. X射线荧光光谱法分析碳酸盐时两种制样方法的比较[J]. 理化检验-化学分册, 2016, 52(6): 664~668
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参考文献
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【4】刘江斌,曹成东,赵峰,等.X射线荧光光谱法同时测定石灰石中主次痕量组分[J].岩矿测试, 2008,27(2):149-150.
【5】汪晓文.X射线荧光光谱法测定石灰石中SiO2、CaO、MgO的含量[J].分析仪器, 2004,26(4):29-31.
【6】袁秀茹,余宇,赵峰,等.X射线荧光光谱法同时测定白云岩中氧化钙和氧化镁等主次量组分[J].岩矿测试, 2009,28(4):376-378.
【7】李国会,樊守忠.X射线荧光光谱法直接测定碳酸盐岩石中主次痕量元素[J].岩矿测试, 1997,16(1):45-50.
【8】韩蔚,丁建军,梅一飞,等.X射线荧光光谱法测定石膏中11种元素的含量[J].理化检验-化学分册, 2015,51(2):188-191.
【9】MAREK L. A new approach to the particle-size effect correction in the X-Ray fluorescence analysis of multimetallic ore slurries[J]. X-Ray Spectrometry, 1988,17(2):161-165.
【10】HOLYNSKA B, MARKOWICZ A. Correction method of the particle-size effect in the X-ray fluorescence analysis of 'thin' and monolayer samples[J]. X-Ray Spectrometry, 1982,11(3):117-120.
【11】BRADNER D W. Analysis of limestones and dolomites by X-ray rluorescence[J]. The Rigaku Journal, 1999,16(1):16-24.
【12】GOTO A, HORIE T, OHBA T, et al. XRF analysis of major and trace elements for wide compositional ranges from silicate rocks to carbonate rocks using low dilution glass beads[J]. Japanese Magazine of Mineralogical and Petrological Sciences, 2002,33(2):162-173.
【13】MORI Y, MASHIMA H. X-ray fluorescence analysis of major and trace elements in silicate rocks using 1∶5 dilution glass beads[J]. Bulletin of the Kitakyushu Museum of Natural History and Human History, Ser A, 2005(3):1-12.
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