Aarsand Aleksander Sverdrup, Mrdakovic Popic Jelena, Teien Hans-Christian
Faculty of Environmental Sciences and Natural Resource Management, Norwegian University of Life Sciences, Ås, Norway.
Norwegian Radiation and Nuclear Safety Authority, Østerås, Norway.
Front Public Health. 2025 Jul 9;13:1620899. doi: 10.3389/fpubh.2025.1620899. eCollection 2025.
Exposure to radon-222 (Rn) is a common problem in areas with high uranium-238 (U) content in the subsurface. The gas may enter dwellings through cracks and gaps in the foundation, or groundwater collected for household use. It is well documented that Rn poses a health risk, especially in high concentrations. In water, the gas often co-occurs with other naturally occurring radionuclides (NOR), such as radium-226 (Ra) and polonium-210 (Po). These may, in combination with chemically toxic elements, negatively affect water quality and consequently human health.
To investigate Rn content in drinking water and changes over time, water quality in six sampling points in western Norway were monitored over a period of 17 months. The majority of NORs, stable elements and general water parameters were found to be within accepted limits for drinking water quality in Norway. However, one of the sampling points, a drilled granite well, displayed high activity concentrations of Rn (up to 1,225 Bq/L), Pb (up to 41.7 mBq/L) and Po (up to 312 mBq/L). Water from other sampling points displayed low pH (5.8-6.5), which could affect mobility and bioavailability of toxic elements.
The magnitude of variation of Rn activity concentration was generally reflected in other parameters, such as Ca and U, but statistically significant correlation ( < 0.05) could only be found in three sampling points. Several water parameters, such as Ca, electrical conductivity, Rn and U displayed statistically significant correlation ( < 0.05) with temperature and precipitation, suggesting a seasonal dependence. Therefore, the variability was attributed to mineral weathering, recharge through rocks and regolith with different NOR-content, and dilution by rapid recharge. The findings of this study show that activity concentrations of Rn in different types of water sources is affected by recharge patterns, which should be considered for when assessing drinking water quality.
在地下铀 - 238(U)含量高的地区,接触氡 - 222(Rn)是一个常见问题。这种气体可能通过地基的裂缝和缝隙进入住宅,或者通过收集用于家庭使用的地下水进入。有充分的文献记载,Rn会带来健康风险,尤其是在高浓度情况下。在水中,这种气体常常与其他天然存在的放射性核素(NOR)共同出现,例如镭 - 226(Ra)和钋 - 210(Po)。这些物质可能与化学有毒元素一起,对水质进而对人类健康产生负面影响。
为了调查饮用水中的Rn含量及其随时间的变化,在挪威西部的六个采样点对水质进行了为期17个月的监测。发现大多数NOR、稳定元素和一般水质参数都在挪威饮用水水质的可接受范围内。然而,其中一个采样点,一口钻凿的花岗岩井,显示出高活度浓度的Rn(高达1225 Bq/L)、Pb(高达41.7 mBq/L)和Po(高达312 mBq/L)。其他采样点的水pH值较低(5.8 - 6.5),这可能会影响有毒元素的迁移性和生物可利用性。
Rn活度浓度的变化幅度通常反映在其他参数中(如Ca和U),但仅在三个采样点发现了具有统计学意义的相关性(<0.05)。几个水质参数,如Ca、电导率、Rn和U,与温度和降水量显示出具有统计学意义的相关性(<0.05),表明存在季节性依赖关系。因此,这种变异性归因于矿物风化、通过具有不同NOR含量的岩石和风化层的补给以及快速补给造成的稀释。本研究结果表明,不同类型水源中Rn的活度浓度受补给模式的影响,在评估饮用水水质时应予以考虑。