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首页> 外文期刊>International journal of mass spectrometry >Contribution of the Faraday cup coupled to 10(12) Omega current amplifier to uranium 235/238 and 234/238 isotope ratio measurements by thermal ionization mass spectrometry
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Contribution of the Faraday cup coupled to 10(12) Omega current amplifier to uranium 235/238 and 234/238 isotope ratio measurements by thermal ionization mass spectrometry

机译:热电离质谱法测量法拉第杯与10(12)欧米茄电流放大器的耦合对铀235/238和234/238同位素比测量的贡献

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摘要

This work highlights the possibility of improving, for given deposited quantities, the accuracy of uranium isotope ratio determination by Thermal Ionization Mass Spectrometry (TIMS) using Faraday cups coupled to a 10(12) Omega current amplifying system. This system improves the electronic sensitivity compared to the same Faraday cups coupled to 10(12) Omega current amplifiers. The analytical procedure developed in a previous work (Quemet et al., 2014) was applied in order to study the improvements in accuracy using the Faraday cups equipped with 10(12) Omega current amplifier. The U-234/U-238 and U-235/U-238 isotope ratios were measured on the Certified Reference Material IRMM 052 (natural uranium). Results were evaluated relying on NF T 90-210 norm regarding method validation. The U-234/U-238 and U-235/U-238 isotope ratios were studied by total evaporation using different configurations. First, U-234 or U-235 was measured with a Faraday cup coupled to a 10(12) Omega current amplifier and U-238 was measured with a Faraday cup coupled to a 10(12) Omega current amplifier. Then, 234U or U-235 was measured by discrete dynodes electron multiplier and U-238 was measured with a Faraday cup coupled to a 10(12) Omega current amplifier. In comparison to the configurations using the 10(12) Omega current amplifier, the analyzable quantity was reduced from 250 ng to 100 ng for the U-235/U-238 isotope ratio and from 50 ng to 3 ng for the U-234/U-238 isotope ratio with extended uncertainty below 0.28% for the U-235/U-238 isotope ratio, in compliance with the International Target Values (ITV 2010), and below 5% for the U-234/U-238 isotope ratio. (C) 2016 Elsevier B.V. All rights reserved.
机译:这项工作强调了对于给定的沉积量,通过使用法拉第杯和10(12)Omega电流放大系统耦合的热电离质谱(TIMS)来确定铀同位素比的准确性的可能性。与连接10(12)Omega电流放大器的相同法拉第杯相比,该系统提高了电子灵敏度。为了研究使用装有10(12)Omega电流放大器的法拉第杯的准确性提高,采用了先前工作中开发的分析程序(Quemet等,2014)。 U-234 / U-238和U-235 / U-238同位素比是通过认证参考材料IRMM 052(天然铀)测量的。根据有关方法验证的NF T 90-210规范对结果进行评估。使用不同的配置通过总蒸发研究了U-234 / U-238和U-235 / U-238同位素比。首先,使用耦合到10(12)Ω电流放大器的法拉第杯测量U-234或U-235,使用耦合到10(12)Ω电流放大器的法拉第杯测量U-238。然后,通过离散倍增极电子倍增器测量234U或U-235,并通过与10(12)Omega电流放大器耦合的法拉第杯测量U-238。与使用10(12)Omega电流放大器的配置相比,U-235 / U-238同位素比的可分析量从250 ng降低到100 ng,U-234 / U-235 / U-238的可分析量从50 ng降低到3 ng。符合国际目标值(ITV 2010)的U-235 / U-238同位素比率的U-238同位素比率具有扩展的不确定度,低于0.28%,而U-234 / U-238同位素比率的不确定度低于5% 。 (C)2016 Elsevier B.V.保留所有权利。

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