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印度卡纳塔克邦钦塔马尼村的地下水中铀的分布情况。

The distribution of groundwater uranium in Chintamani village, Karnataka, India.

作者信息

Rampur Sadashiva, V K Mahesh Kumar, Pelli Pavan R, Sarkar Senjuti, Pramanik Samayeta, Majumder Upama, S Shravanthi, Meenakshi T Bhavana, G Santhanakrishnan Srinidhi, Pendem Rushi, Ghosh Tanushree, Nagarajan Deepesh

机构信息

Department of Biotechnology, Faculty of Life and Allied Health Sciences, M.S. Ramaiah University of Applied Sciences, Bengaluru, Karnataka, 560054, India.

出版信息

F1000Res. 2025 Aug 21;14:321. doi: 10.12688/f1000research.162525.3. eCollection 2025.

Abstract

BACKGROUND

Chintamani village, Chikkaballapura district, Karnataka, India was found to possess high aquifer uranium concentrations. Geologically, Chintamani village is located on bedrock that is rich in elements like potassium (K) that naturally contain high levels of radioactive elements, such as uranium and thorium, due to the presence of alkali-feldspar granites and gneisses. Aquifer depletion has caused the concentration of these elements in groundwater to increase over time, posing a potential health hazard to the residents of Chintamani village.

METHODS

Here, we report the sampling of groundwater from 12 borewells located in Chintamani village in between the period of August 2024 to December 2024. We observed groundwater uranium concentrations of 0.018 ppm to 8.64 ppm. Data for borewell depth, the quantity of total dissolved solids (TDS), and the elemental composition of TDS is also reported. We observed a statistically significant spatial distribution of uranium concentrations in Chintamani village. Borewells possessing the highest observed concentrations of uranium were clustered towards the northwestern region of the village.

CONCLUSIONS

This dataset is expected to serve as a resource for guiding potential remediation efforts in these locations.

摘要

背景

印度卡纳塔克邦奇卡巴拉普拉区的钦塔马尼村被发现含水层铀浓度很高。从地质角度来看,钦塔马尼村位于富含钾(K)等元素的基岩上,由于存在碱长石花岗岩和片麻岩,这些元素天然含有高水平的放射性元素,如铀和钍。含水层枯竭导致这些元素在地下水中的浓度随时间增加,对钦塔马尼村的居民构成潜在健康危害。

方法

在此,我们报告了2024年8月至2024年12月期间对钦塔马尼村12口井的地下水采样情况。我们观察到地下水铀浓度在0.018 ppm至8.64 ppm之间。还报告了井深、总溶解固体(TDS)量以及TDS的元素组成数据。我们观察到钦塔马尼村铀浓度存在统计学上显著的空间分布。观测到铀浓度最高的井集中在村庄的西北部地区。

结论

该数据集有望作为指导这些地点潜在修复工作的资源。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b5af/12409395/d248a1271c1e/f1000research-14-185995-g0000.jpg

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