光州地区地下水铀、氡浓度分布特征

Heejeong Seo, Kyoungwoo Min, Jiyoung Park, Juhyun Park, Hoyeon Hwang, Se-il Park, SeonJeong Kim, Suk-kyung Jeong, Seok-jin Bae, S. Kim
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引用次数: 0

摘要

背景:由于在韩国一些地区检测到高浓度的铀和氡,因此有必要对光州地区的天然放射性物质进行调查。目的:了解光州地区地下水水化学特征,探讨天然放射性物质铀和氡的分布特征。方法:根据光州地区的地质情况,对62口地下水进行了铀、氡浓度测定。为此制作了铀、氡含量的地质分布图。结果:地下水类型以ca - hco3为主。地下水中铀的浓度范围为0 ~ 29.3µg/L,平均值为3.3µg/L,中位数为0.9µg/L。地下水中铀的中位数浓度依次为冲积层、花岗质片麻岩和黑云母花岗岩(按地质单元划分)。地下水氡浓度范围为4.8 ~ 313.2 Bq/L,平均值为75.6 Bq/L,中位数为59.6 Bq/L。地下水中氡的中位浓度依次为黑云母花岗岩、冲积层和花岗片麻岩。对研究区地下水进行相关性分析,发现铀与氡的相关性不显著。结论:在本研究区,铀的浓度远远低于饮用水水质标准允许的浓度,但在11%的样本中,氡的浓度超过了饮用水水质监测标准。据判断,在对研究地区的高浓度氡探测点进行彻底审查后,将需要采取适当的措施,例如安装减少氡的设施。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Distribution Characteristics of Uranium and Radon Concentrations of Groundwater in Gwangju Area
ABSTRACT Background: As high concentrations of uranium and radon have been detected in some areas in Korea, it is considered necessary to investigate natural radioactive materials in the Gwangju area. Objectives: This study aimed to identify the hydrochemical characteristics of groundwater in Gwangju and investigate the distribution characteristics of uranium and radon, which are naturally radioactive substances. Methods: To determine the uranium and radon concentrations in groundwater according to the geology of the Gwangju area, we measured 62 groundwater wells. A geological distribution map of uranium and radon content was prepared for this study. Results: The groundwater type, defined using a Piper diagram, was mainly Ca-HCO 3 . The concentration of uranium in the groundwater ranged from 0 to 29.3 µg/L, with a mean of 3.3 µg/L and a median of 0.9 µg/L. The median concentration of uranium in groundwater was highest in alluvium, granitic gneiss, and biotite granite (classified by geological unit), in that order. The concentration of radon in the groundwater ranged from 4.8 to 313.2 Bq/L, with a mean of 75.6 Bq/L and a median of 59.6 Bq/L. The median concentration of radon in groundwater was highest in biotite granite, alluvium, and granitic gneiss, in that order. As a result of the correlation analysis of groundwater in the study area, there was no significant correlation between uranium and radon. Conclusions: In this study area, uranium was shown to be far below the concentrations allowed by drinking water quality standards, but radon concentrations exceeded drinking water quality monitoring standards in 11% of the samples. It was judged that appropriate measures, such as the installation of radon reduction facilities, will be required after a thorough review of high-concentration radon detection sites of in the research area.
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