叶卡捷琳堡市及其郊区泉水中氡和镭含量分析

V. Semenishchev, A. Voronina, L. A. Tomashova, Yulia I. Nasonova
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引用次数: 0

摘要

尽管发展了中央供水系统,但泉水仍然是饮用水的重要来源。本文对叶卡捷琳堡市及其居民点的泉水水质进行了辐射因素研究。测定了20个泉水中镭-226的活度浓度。方法。用平衡铋-214伽马线进行了氡-222活度的测定。为了测定镭-226,取5升水样,将镭预先浓缩在T-5吸附剂上;然后在薄层MnO2-PE吸附剂上分离镭,然后在α光谱仪上测量。结果。在绝大多数情况下,镭-226的活度浓度低于检测限(0.3 Bq/L);最大活性浓度为1.03±0.27,对应每日饮用该水的内剂量为0.21±0.05 μSv/y。镭-226的含量与氡-222、铀-238和碱土离子的浓度没有相关性。在2020年9月至2021年6月期间,对先前发现氡含量高的七个泉进行了氡活性监测。氡活度的季节变化显著;有些弹簧的最小活度与最大活度之差达到3。在大多数情况下,氡活度的增加发生在冬季,这可以解释为氡在冷水中的溶解度增加和流量减少。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analysis of radon and radium content in springs of the city of Ekaterinburg and its outskirts
Despite development of central water supply systems, springs still remain to be important sources of drinking water. In this work, the study of water quality in springs of Yekaterinburg city and its settlements was performed with the attention to radiological factor. Activity concentrations of radium-226 were determined in water of 20 springs. Methods. Determination of the radon-222 activities of was performed using gamma-spectrometry vis the equilibrium bismuth-214 gamma line. To determine radium-226, 5-liter water samples were taken, the radium was preconcentrated on a T-5 sorbent; then radium was separated on a thinlayer MnO2-PE sorbent followed by measurement on an alpha spectrometer. Results. In the vast majority of cases, activity concentrations of radium-226 were lower than the detection limit (0.3 Bq/L); the maximal activity concentration of 1.03 ± 0.27 was found that corresponded to the internal dose of 0.21 ± 0.05 μSv/y due to daily consumption of this water. No correlations were found between content of radium-226 and concentrations of radon-222, uranium-238 and alkaline earth ions. At the period of 09.2020 – 06.2021, monitoring of radon activity was performed in seven springs with previously found high radon content. Significant seasonal variations of radon activity were found; for some springs the difference between the minimal and the maximal activity reached 3. In the most cases, increase of radon activity occurred in water during winter that can be explained by both an increase of radon solubility in cold water and a decrease of flowrate.
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