摘要
采用考虑弥散的数学模型计算272厂铀尾矿中^(238)U、^(230)Th、^(226)Ra、^(210)Pb和^(210)Po的释放和迁移过程。结果表明:在300年的时间尺度上,272厂铀尾矿中的^(210)Po、^(230)Th、^(210)Pb不能到达距离200m处的水井;水井中^(238)U和^(226)Ra的活度浓度和累积活度均呈指数增长;^(238)U、^(226)Ra的活度浓度将分别经过10、50a左右超过《生活饮用水卫生标准》(GB 5749—2006)的总α放射性≤0.5Bq/L的要求。
Mathematical model considering dispersion was used to calculate the nuclides of ^(238)U,^(230)Th,^(226)Ra,^(210)Pb and ^(210)Po liberated and transported by 272 uranium tailing.Results showed that:along 300 a,^(210)Po,^(230)Th and ^(210)Pb could not reach the well 200 maway;activity concentration and cumulative activity of ^(238)U and ^(226)Ra in the well expanded exponentially;activity concentration of ^(238)U and ^(226)Ra would exceed "Standards for drinking water quality"(GB 5749-2006) of totalαradioactivity≤0.5 Bq/L after about 10,50 years.
作者
李哲
丁志斌
富宝锋
司高华
刘东旭
LI Zhe;DING Zhibin;FU Baofeng;SI Gaohua;LIU Dongxu(College of Defense Engineering, PLA University of Science and Tech- nology, Nanjing Jiangsu 210007;Northwest Institute of Nuclear Technology, Xi 'an Shaanxi 710024)
出处
《环境污染与防治》
CAS
CSCD
北大核心
2017年第12期1375-1377,1383,共4页
Environmental Pollution & Control
关键词
铀尾矿
核素
238U
226RA
释放
迁移
弥散
uranium tailing
nuclide i ^238u
^226Ra
liberation
transport
dispersion