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印度乔塔纳格布尔片麻岩杂岩延伸区地下水水质分类及健康风险评估。

Groundwater quality enumeration and health risk in the extended part of Chhotanagpur granite gneiss complex of India.

机构信息

Department of Geography, Sidho-Kanho-Birsha University, Ranchi Road, Purulia, West Bengal, India, 723104.

Department of Geography, Arsha College, Purulia, West Bengal, India, 723201.

出版信息

Environ Sci Pollut Res Int. 2024 Sep;31(41):54234-54261. doi: 10.1007/s11356-023-26397-4. Epub 2023 Mar 23.

DOI:10.1007/s11356-023-26397-4
PMID:36959399
Abstract

The majority of people on the earth bank largely on groundwater to quench their thirst. In the era of rapid population growth, the over-exploitation of groundwater gives rise to water scarcity, and people find themselves in distress to manage safe drinking water. In this backdrop, the present study is carried out in the terrain of Pre-Cambrian igneous and high- to low-graded metamorphic rocks, to assess the groundwater potential zones (GWPZs) and evaluation of groundwater quality. The map of GWPZ is produced employing the multi-criteria decision-making model and geospatial technology. It unveils that around 29% area of the watershed enjoys good GWPZ, whereas around 43% area experiences low GWPZ. The overall accuracy of the simulated model is 92%. The water quality index indicates that 68% of water samples belong to excellent to good water quality. A significant proportion of water samples (24%) are found to be unsuitable for drinking, which may be due to groundwater contamination by the process of leaching of mineral-rich weathered rocks. The presence of fluoride (F) beyond the maximum permissible limit (1.5 mg L) of WHO is recorded among 18% samples of the watershed, where 24,963 souls including 3457 children aged between 0 and 6 years lived and might have ingested F through drinking water. Hence, the health risk of those people is quite high. Children are at a more non-carcinogenic health risk of F than adults. The study also confirms no statistically significant difference (p ˃ 0.05) is observed between low and high GWPZ with respect to groundwater quality. The study recommends adopting a sustainable outlook to explore GWPZ, and an assessment of drinking water quality must be done before drinking.

摘要

地球上的大多数人主要依靠地下水来解渴。在人口快速增长的时代,地下水的过度开采导致了水资源短缺,人们发现自己难以管理安全饮用水。在此背景下,本研究在前寒武纪火成岩和高至低变质岩地形中进行,以评估地下水潜力区(GWPZ)和地下水质量评估。GWPZ 图是使用多准则决策模型和地理空间技术制作的。结果表明,流域约 29%的地区具有良好的 GWPZ,而约 43%的地区 GWPZ 较低。模拟模型的整体准确率为 92%。水质指数表明,68%的水样属于优良水质。相当一部分水样(24%)不适宜饮用,这可能是由于富含矿物质的风化岩石淋滤过程导致地下水受到污染。在流域的 18%的水样中检测到氟(F)超过世界卫生组织(WHO)规定的最大允许限值(1.5mg/L),其中包括 24963 名居民,包括 3457 名 0 至 6 岁的儿童,他们可能通过饮用水摄入了 F。因此,这些人的健康风险相当高。儿童比成年人更容易受到 F 的非致癌健康风险的影响。该研究还证实,低和高 GWPZ 之间的地下水质量没有统计学上的显著差异(p ˃ 0.05)。研究建议采用可持续的观点来探索 GWPZ,并在饮用之前必须对饮用水质量进行评估。

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