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用径迹活化法测定了中国科学院原子能研究所地下水的铀含量,得到的结果为(5.38±0.67)×10~(-10)克/克。这一方法可以用来进行全国天然水的铀含量布点普查,作为铀矿资源普查方法之一。
The uranium content of groundwater in the Institute of Atomic Energy, Chinese Academy of Sciences, was determined by the track-activation method. The obtained results were (5.38 ± 0.67) × 10 -10 g / g. This method can be used to survey the national uranium content of natural water as one of the uranium resource census methods.