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郝樊华, 刘雪梅, 胡思得, 龙开明. 热表面电离质谱法测定贫化铀样品痕量铀同位素比值及含量[J]. 岩矿测试, 2010, 29(4): 373-376.
引用本文: 郝樊华, 刘雪梅, 胡思得, 龙开明. 热表面电离质谱法测定贫化铀样品痕量铀同位素比值及含量[J]. 岩矿测试, 2010, 29(4): 373-376.
HAO Fan-hua, LIU Xue-mei, HU Si-de, LONG Kai-ming. Determinationof Isotope Ratios and Concentration of Trace Uranium in Depleted Uranium Samples by Thermal Ionization Mass Spectrometry[J]. Rock and Mineral Analysis, 2010, 29(4): 373-376.
Citation: HAO Fan-hua, LIU Xue-mei, HU Si-de, LONG Kai-ming. Determinationof Isotope Ratios and Concentration of Trace Uranium in Depleted Uranium Samples by Thermal Ionization Mass Spectrometry[J]. Rock and Mineral Analysis, 2010, 29(4): 373-376.

热表面电离质谱法测定贫化铀样品痕量铀同位素比值及含量

Determinationof Isotope Ratios and Concentration of Trace Uranium in Depleted Uranium Samples by Thermal Ionization Mass Spectrometry

  • 摘要: 选用磷酸为离子流发射剂,热表面电离质谱法分析纳克量级贫化铀样品的铀同位素比值,方法最大相对标准偏差<2.9%。以233U为稀释剂,采用同位素稀释法对铀的含量进行测定,扩展不确定度为2.4%(K=2)。研究表明,在纳克量级的铀同位素比值测定中,来自铼带等铀本底的干扰影响不容忽视,需要进一步研究并扣除。

     

    Abstract: With H3PO4 as the ionization intensifier, the isotope ratios of uranium in the depleted uranium samples with uranium concentration at nanogram-level were determined by thermal ionization mass spectrometry (TIMS) with the precision of <2.9%RSD. With 233U as the diluent, the concentration of uranium in the samples were also determined by isotope dilution mass spectrometry (IDMS) with the expanded uncertainty of 2.4% .The research results showed that in uranium isotope ratio determination for the samples with nanogram-level of uranium, uranium background interference from rhenium filament and other sources should not be ignored, which is needed for further study to remove the background interference.

     

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