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欧洲环境样本中铯 - 135/铯 - 137同位素组成:环境迁移与源项排放应用

(135)Cs/(137)Cs isotopic composition of environmental samples across Europe: Environmental transport and source term emission applications.

作者信息

Snow Mathew S, Snyder Darin C

机构信息

Idaho National Laboratory, PO Box 1625, Idaho Falls, ID 83415-2805, USA.

Idaho National Laboratory, PO Box 1625, Idaho Falls, ID 83415-2805, USA.

出版信息

J Environ Radioact. 2016 Jan;151 Pt 1:258-263. doi: 10.1016/j.jenvrad.2015.10.025. Epub 2015 Nov 2.

Abstract

(135)Cs/(137)Cs isotopic analyses represent an important tool for studying the fate and transport of radiocesium in the environment; in this work the (135)Cs/(137)Cs isotopic composition in environmental samples taken from across Europe is reported. Surface soil and vegetation samples from western Russia, Ukraine, Austria, and Hungary show consistent aged thermal fission product (135)Cs/(137)Cs isotope ratios of 0.58 ± 0.01 (age corrected to 1/1/15), with the exception of one sample of soil-moss from Hungary which shows an elevated (135)Cs/(137)Cs ratio of 1.78 ± 0.12. With the exception of the outlier sample from Hungary, surface soil/vegetation data are in quantitative agreement with values previously reported for soils within the Chernobyl exclusion zone, suggesting that radiocesium at these locations is primarily composed of homogenous airborne deposition from Chernobyl. Seawater samples taken from the Irish Sea show (135)Cs/(137)Cs isotope ratios of 1.22 ± 0.11 (age corrected to 1/1/15), suggesting aged thermal fission product Cs discharged from Sellafield. The differences in (135)Cs/(137)Cs isotope ratios between Sellafield, Chernobyl, and global nuclear weapons testing fallout indicate that (135)Cs/(137)Cs isotope ratios can be utilized to discriminate between and track radiocesium transport from different nuclear production source terms, including major emission sources in Europe.

摘要

铯 - 135/铯 - 137同位素分析是研究放射性铯在环境中迁移转化的重要工具;本文报道了取自欧洲各地环境样品中的铯 - 135/铯 - 137同位素组成。来自俄罗斯西部、乌克兰、奥地利和匈牙利的表层土壤和植被样品显示,除匈牙利的一个土壤 - 苔藓样品铯 - 135/铯 - 137比值为1.78±0.12偏高外,其余样品的热裂变产物铯 - 135/铯 - 137同位素比值均一致,为0.58±0.01(年龄校正至2015年1月1日)。除匈牙利的异常样品外,表层土壤/植被数据与此前报道的切尔诺贝利禁区内土壤的值在数量上一致,这表明这些地点的放射性铯主要由切尔诺贝利的均匀大气沉降物组成。取自爱尔兰海的海水样品铯 - 135/铯 - 137同位素比值为1.22±0.11(年龄校正至2015年1月1日),表明是从塞拉菲尔德排放的老化热裂变产物铯。塞拉菲尔德、切尔诺贝利和全球核武器试验沉降物之间铯 - 135/铯 - 137同位素比值的差异表明,铯 - 135/铯 - 137同位素比值可用于区分和追踪来自不同核生产源项的放射性铯迁移,包括欧洲的主要排放源。

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