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使用离子交换色谱分离后,通过扇形场电感耦合等离子体质谱法测定淡水湖沉积物中的钚同位素。

Determination of plutonium isotopes in freshwater lake sediments by sector-field ICP-MS after separation using ion-exchange chromatography.

作者信息

Liao Haiqing, Zheng Jian, Wu Fengchang, Yamada Masatoshi, Tan Mingguang, Chen Jianmin

机构信息

State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guanshui Road 46, Guiyang 550002, China.

出版信息

Appl Radiat Isot. 2008 Aug;66(8):1138-45. doi: 10.1016/j.apradiso.2008.01.001. Epub 2008 Jan 12.

Abstract

The determination of Pu isotopes in lake sediments is important for many studies, such as Pu pollution source identification, sediment mixing estimation, erosion evaluation and establishment of deposition chronology in lakes. In this paper, a simple analytical method using sector field inductively coupled plasma mass spectrometry (ICP-MS) combined with two-stage chromatographic separation and purification of Pu was developed based on the optimization and adaptation of the previously published method for marine samples with an emphasis on the study of the elimination of interferences for the analysis of freshwater lake sediments. A strong base anion-exchange resin (AG MP-1M) was used to purify Pu isotopes with concentrated HBr as the final eluent for Pu elution. The chemical yields were ca. 64% and the decontamination factor for U was ca. 10(5). The developed method was validated using a freshwater lake sediment reference material (SRM-4354) and a marine sediment reference material (IAEA-368), and applied to the determination of Pu isotopes in sediment samples of Lake Poyang, East China. For the analysis of certified reference materials, both 239+240Pu activity of 31.6 mBq g(-1) and 240Pu/239Pu atom ratio of 0.033 for IAEA-368 were comparable to the certified value and/or literature values. As for SRM-4354, 239+240Pu activity of 3.90 mBq g(-1) agreed well with the certified value. However, the mean 240Pu/239Pu atom ratio of 0.144 was lower than those reported by other laboratories. This difference suggested that this material may be isotopically inhomogeneous. 240Pu/239Pu atom ratios of Poyang Lake sediment samples ranged from 0.185 to 0.192 with a mean value of 0.187+/-0.004, indicating that plutonium pollution originated from global fallout.

摘要

湖泊沉积物中钚同位素的测定对于许多研究都很重要,例如钚污染源识别、沉积物混合估算、侵蚀评估以及湖泊沉积年代学的建立。本文基于对先前发表的海洋样品方法的优化和调整,开发了一种使用扇形场电感耦合等离子体质谱(ICP-MS)结合钚的两级色谱分离和纯化的简单分析方法,重点研究了消除淡水湖沉积物分析中的干扰。使用强碱性阴离子交换树脂(AG MP-1M)纯化钚同位素,以浓氢溴酸作为钚洗脱的最终洗脱剂。化学产率约为64%,铀的去污因子约为10⁵。所开发的方法通过使用淡水湖沉积物标准物质(SRM-4354)和海洋沉积物标准物质(IAEA-368)进行了验证,并应用于中国东部鄱阳湖沉积物样品中钚同位素的测定。对于有证标准物质的分析,IAEA-368的²³⁹ + ²⁴⁰Pu活度为31.6 mBq g⁻¹,²⁴⁰Pu/²³⁹Pu原子比为0.033,均与认证值和/或文献值相当。至于SRM-4354,²³⁹ + ²⁴⁰Pu活度为3.90 mBq g⁻¹与认证值吻合良好。然而,²⁴⁰Pu/²³⁹Pu原子比的平均值为0.144,低于其他实验室报告的值。这种差异表明该物质可能在同位素上不均匀。鄱阳湖沉积物样品的²⁴⁰Pu/²³⁹Pu原子比范围为0.185至0.192,平均值为0.187±0.004,表明钚污染源自全球沉降物。

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