Improvement of Electrode of Tritium Enrichment Cell and Application to Tritium Monitoring in Environmental Surface Water at South Osaka Area

Syojiro Kimura, A. Iwamoto, M. Inagaki
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Abstract

The experimental studies on the improvement of electrode materials used for the electrolytic enrichment of tritium and on the establishment of rapid procedure for the analysis of tritium and its application to tritium monitoring in environmental surface water at south Osaka area were carried out. The more efficient recovery rate and reappearance of tritium were obtained by the trial of the exchange of the electrode material from nickel (Ni) to iron (Fe) at high current condition. However, by considering the electrolytic corrosiveness of iron, a combined multi plate electrode of Fe (-)-Ni (+) (an effective surface area ; 63cm2) was adopted. In the case of such operational conditions that a current density ; 180 mA/cm2 and a cooling temperature ; 5°C using a 100 ml glass cell inserted into the electrode, time required for decreasing the volume of sample solution from 100 ml to 15 ml was more than 22 h. In addition the recovery rate and the concentration ratio of tritium were 90% and 6 times respectively. Then, the tritium activity of the water sample could be counted rapidly with a relative counting error of ±20% for 4 h in a low level liquid scintillation counter. By the trial using the above mentioned method for the tritium monitoring in environmental surface water at south Osaka area from 1986 to 1992, it was proved that the tritium activities decreased to the naturally producing level of tritium (BG) during this term and the decreasing half times of tritium concentration in this area by dilution were about 4 years.
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氚富集电池电极的改进及其在大阪南部地表水环境氚监测中的应用
对电解富集氚电极材料的改进、氚快速分析程序的建立及其在大阪南部地区环境地表水氚监测中的应用进行了实验研究。通过在大电流条件下将电极材料由镍(Ni)交换为铁(Fe)的试验,获得了更高的氚回收率和重现率。然而,考虑到铁的电解腐蚀性,Fe (-)- ni(+)组合多极板电极(有效表面积;采用63cm2)。在这样的操作条件下,电流密度;180 mA/cm2和冷却温度;在5°C下使用100 ml玻璃电池插入电极,将样品溶液的体积从100 ml减少到15 ml所需时间超过22 h。此外,氚的回收率和浓度比分别为90%和6倍。然后在低液位液体闪烁计数器中快速计数水样的氚活度,相对计数误差为±20%,持续4 h。1986 ~ 1992年对大阪南部地区环境地表水氚监测的试验证明,在此期间,该地区氚活度下降到氚的自然产生水平(BG),稀释后该地区氚浓度下降一半的时间约为4年。
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