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中国原子能科学研究院
收稿日期:1985-08-05,
纸质出版日期:1986-12
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郭士伦, 邓新绿, 孙盛芬, 等. 用裂变径迹法进行铀矿普查[J]. 核技术, 1986,09(12):11-14,26,54,55.
Shilun Guo, Xinlu Deng, Shengfen Sun, et al. Fission track method for uranium ore exploration[J]. Nuclear techniques, 1986, 09(12): 11-14,26,54,55.
用裂变径迹法测定了铀矿普查现场水样的铀含量,在10
-4
—10
-8
g/l范围内,所得结果与荧光比色法和激光荧光法基本符合;对低铀含量样品(≤10
-8
g/l),用其他方法不能给出确切数据,用裂变径迹法也能给出可供参考的铀含量数值。利用实测样品,对裂变径迹法的重复性进行了研究。最后,对水中杂质含量对测量结果的影响进行了分析和讨论。
The uranium concentrations in natural water collected in the fields of uranium ore exploration with fission track method have been determined. It shows that the results of fission track method are consistent with that of fluoro-colorimetry and laser fiuorometry for the same samples of water with uranium concentration in the region from 10
-4
to 10
-8
g/l. For water samples with lower uranium concentration (≤10
-8
g/l)
the fission track method can still give accurate or referential results. but the other two methods failed. The reproducibility of fission track method has been checked and discussed using samples collected in the same fields of uranium ore exploration. The effects of the concentration of the impurities in natural water on the determination of uranium concentration are analysed and discussed as well.
R. L. Fleischer et al . , Anal. Chem. , 48 , 642 ( 1976 ).
K. J. Wenrich-Verbeek et al . , Exploration for uranium ore deposite (Proceedings of symposium on exploration of uranium ore deposits) , 1976 .
郭士伦 和 孙盛芬 , 原子能科学技术 , 1 , 23 ( 1982 )。
高万林 等 , 放射性水文地球化学找矿 , 原子能出版社 , 1980 年。
曹宜锋 , 射线物理测量方法提要汇编 , 原子能出版社 , 1974 年,第 66 页。
郭士伦 等 , 原子能科学技术 , 1 , 65 ( 1976 )。
地球化学所 编译 , 简明地球化学手册 , 科学出版社 , 1977 年。
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