摘要
236U是一种长寿命放射性核素,其半衰期为T1/2=2.342(3)×107a,在自然界的含量极微,天然铀中236U/238U的原子比约为~10-14。目前,对于236U及其测量的研究报道较少。首先介绍了236U的产生,并对地球中236U的总量进行了估算。概述了236U测定在亿年级中子注量率积分评估、核环境和核活动监测,以及地质学等领域中的重要应用。最后,对国内外加速器质谱(AMS)测量236U的状况进行了综述,报道了中国原子能科学研究院AMS小组通过对同位素干扰鉴别的多方面研究,初步建立了236U-AMS测量方法。
236U is a long-lived radionuclide with half-life of 2.342(3)×107 a.The ratio of 236U/238U is about 10-14 in the natural Uranium.The origin and production of 236U in globe are introduced and estimated in this paper,respectively.The major applicationsion of 236U as a 100-million year neutron flux integrator,as a "fingerprint" for monitoring nuclear environment and nuclear activity,and as a tracer in geological studies are briefly summarized.The accelerator mass spectrometry(AMS) measurement of 236U in the world and the research on HI-13 tandem accelerator at China Institute of Atomic Energy(CIAE) is also mentioned in this paper.
出处
《原子核物理评论》
CAS
CSCD
北大核心
2009年第4期312-318,共7页
Nuclear Physics Review
基金
国家自然科学基金委员会和中国工程物理研究院联合基金资助项目(10576040)~~
关键词
~236U
加速器质谱
环境监测
236U
accelerator mass spectrometry
environment monitor