Measuring fluorine in uranium oxyfluoride particles using secondary ion mass spectrometry for nuclear forensics

Kips Ruth, M. Kristo, Hutcheon Ian, Z. Wang, Johnson Tim, Gerlach David, Amonette Jim, Olsen Khris, Stefaniak Elzbieta
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引用次数: 5

Abstract

Abstract Gaseous uranium hexafluoride (UF6) is used for the enrichment of uranium and is known to be a very reactive and volatile gas. When a small amount of UF6 is released in the environment, it forms uranium oxyfluoride (UO2F2) particles and hydrogen fluoride from the reaction with atmospheric moisture. The UO2F2 particles settle on various surfaces within the enrichment facility where they are collected by safeguards organizations such as the International Atomic Energy Agency (IAEA) through a technique called environmental sampling. Despite their small size, the uranium isotopic composition of these particles is used to determine whether an enrichment facility is compliant with its declarations. Additional and complementary information on the particles' source, formation process and exposure history can be obtained from elemental, molecular and morphological analysis. As fluorine is not always detected in uranium particles originating from enrichment facilities, it is assumed that UO2F2 is unstable under certain environmental conditions. This study aims to determine how those environmental conditions affect the relative amount of fluorine in UO2F2 particles. Expressly for the purpose of this work, we prepared a set of UO2F2 particle samples from the hydrolysis of UF6 and stored these samples in environmental chambers at different temperature, humidity and lighting conditions. The NanoSIMS secondary ion mass spectrometer, with a nanometer-scale spatial resolution, was used to measure the F+/U+ secondary ion ratio of individual particles immediately after sample preparation, and at different time intervals. NanoSIMS analyses on single particles stored up to 7 months in dry air did not detect a significant decrease in the relative amount of fluorine. The exposure to high humidity however, resulted in a much lower F+/U+ ratio, up to 2 orders of magnitude below that of the particles stored in dry air. It should be noted that fluorine was still detected in these samples, even after 7 months of high humidity exposure.
核取证用二次离子质谱法测量氟化铀氧颗粒中的氟
气态六氟化铀(UF6)用于铀浓缩,是一种非常活跃和易挥发的气体。当少量UF6释放到环境中时,它与大气水分反应形成氟化铀氧(UO2F2)颗粒和氟化氢。UO2F2粒子沉降在浓缩设施的不同表面,由国际原子能机构(IAEA)等保障组织通过一种称为环境采样的技术收集。尽管这些颗粒的体积很小,但它们的铀同位素组成可以用来确定一个浓缩设施是否符合其申报。通过元素分析、分子分析和形态分析,可以获得有关颗粒来源、形成过程和暴露历史的附加和补充信息。由于并非总能在源自浓缩设施的铀颗粒中检测到氟,因此假定UO2F2在某些环境条件下是不稳定的。本研究旨在确定这些环境条件如何影响UO2F2颗粒中氟的相对含量。为此,我们从UF6水解中制备了一套UO2F2颗粒样品,并将这些样品存放在不同温度、湿度和光照条件下的环境室中。采用纳米尺度空间分辨率的NanoSIMS二次离子质谱仪,在样品制备后立即和不同时间间隔测量单个颗粒的F+/U+二次离子比。对在干燥空气中储存长达7个月的单个颗粒进行的NanoSIMS分析未发现氟的相对含量显著减少。然而,暴露在高湿度下,导致F+/U+比低得多,比储存在干燥空气中的颗粒低2个数量级。应该指出的是,即使在高湿度暴露7个月后,这些样品中仍检测到氟。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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