大气环境中的氚

N. Momoshima, T. Yamaguchi, T. Toyoshima, Y. Nagao, M. Takahashi, M. Takamura, Y. Nakamura
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引用次数: 13

摘要

在上层大气中,次级宇宙射线与氮或氧原子之间的核反应不断产生天然氚,估计其生成速率为0.2至0.25个氚原子厘米每秒,在世界上产生1-1.3 EBq氚库存。在以氢原子为组成元素的各种环境材料中都发现了天然存在的氚。20世纪50年代至60年代的核试验向环境中释放了大量人造氚,使环境中氚的浓度增加。核试验释放的氚量将达到240 EBq,在1963年禁止核试验条约签署40多年后,我们仍然可以在地下水等环境样本中检测到核弹氚。和平利用核能也增加了核电站和核燃料后处理工厂周围的环境氚浓度,因为氚作为空气和液体流出物的释放受到控制。氚以水蒸气、氢和碳氢化合物三种不同的化学形式存在于大气中。我们报告了在日本一般环境中测量的3种化学物质的大气氚浓度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tritium in the Atmospheric Environment
The production rate of natural tritium, produced constantly in the upper atmosphere by nuclear reactions between secondary cosmic rays and nitrogen or oxygen atoms, is estimated to be 0.2 to 0.25 tritium atom cm s which yields 1–1.3 EBq tritium inventory in the world. The naturally occurring tritium has been found in various environmental materials which contain hydrogen atom as a constituent element. The concentration of tritium in the environment had increased by nuclear tests in 1950s–1960s that had released a large amount of artificial tritium to the environment. The amount of tritium emitted from the nuclear tests would be 240 EBq and we can still detect the bomb tritium in environmental samples such as underground water more than 40 years after the test ban treaty in 1963. Peaceful use of nuclear energy has also increased environmental tritium concentrations such as around nuclear power stations and nuclear fuel reprocessing plants due to controlled release of tritium as airborne and liquid effluents. Tritium is found in the atmosphere as 3 different chemical forms that are water vapor, hydrogen, and hydrocarbon. We report atmospheric tritium concentrations of 3 chemical species measured in the general environment of Japan.
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