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236U及其加速器质谱(AMS)测量
引用本文:王祥高,何明,李朝历,王伟,张大伟,黄春堂,石国柱,沈洪涛,吴绍雷,贺国珠,龚杰,陆丽燕,武绍勇,姜山. 236U及其加速器质谱(AMS)测量[J]. 原子核物理评论, 2009, 26(4): 312-318. DOI: 10.11804/NuclPhysRev.26.04.312
作者姓名:王祥高  何明  李朝历  王伟  张大伟  黄春堂  石国柱  沈洪涛  吴绍雷  贺国珠  龚杰  陆丽燕  武绍勇  姜山
作者单位:1 中国原子能科学研究院核物理所, 北京 102413; 2 广西大学物理科学与工程技术学院, 广西 南宁 530004
基金项目:国家自然科学基金-中国工程物理研究院联合基金(NSAF基金) 
摘    要:236U是一种长寿命放射性核素, 其半衰期为T1/2=2.342(3)×107 a, 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236UAMS测量方法。 236U is a longlived 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.

关 键 词:236U   加速器质谱   环境监测
收稿时间:1900-01-01

~(236)U and Its Measurement with Accelerator Mass Spectrometry
WANG Xiang-gao,HE Ming,LI Chao-li,WANG Wei,ZHANG Da-wei,HUANG Chun-tang,SHI Guo-zhu,SHEN Hong-tao,WU Shao-lei,HE Guo-zhu,GONG Jie,LU Li-yuan,WU Shao-yong,JIANG Shan. ~(236)U and Its Measurement with Accelerator Mass Spectrometry[J]. Nuclear Physics Review, 2009, 26(4): 312-318. DOI: 10.11804/NuclPhysRev.26.04.312
Authors:WANG Xiang-gao  HE Ming  LI Chao-li  WANG Wei  ZHANG Da-wei  HUANG Chun-tang  SHI Guo-zhu  SHEN Hong-tao  WU Shao-lei  HE Guo-zhu  GONG Jie  LU Li-yuan  WU Shao-yong  JIANG Shan
Affiliation:1 China Institute of Atomic Energy, Beijing 102413, China;2 College of Physics Science and Technology, Guangxi University, Nanning 530004, China
Abstract:~(236)U is a long-lived radionuclide with half-life of 2.342(3)×10~7 a.The ratio of ~(236)U/~(238)U is about 10~(-14) in the natural Uranium.The origin and production of ~(236)U in globe are introduced and esti-mated in this paper,respectively.The major applicationsion of ~(236)U as a 100-million year neutron flux in-tegrator.as a"fingerprint"for monitoring nuclear environment and nuclear activity,and as a tracer in geo-logical studies are briefly summarized.The accelerator mass spectrometry(AMS)measurement of ~(236)U in the world and the research on HI-13 tandem accelerator at China Institute of Atomic Energy(CIAE)is also mentioned in this paper.
Keywords:~(236)U  ~(236)U  accelerator mass spectrometry  environment monitor
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