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孟加拉国全新世和更新世含水层的水文地球化学评估、来源、质量和潜在健康风险评估。

Hydrogeochemical appraisal, sources, quality and potential health risk assessment in Holocene and Pleistocene aquifers in Bangladesh.

机构信息

Isotope Hydrology Division, Institute of Nuclear Science and Technology, Atomic Energy Research Establishment, Bangladesh Atomic Energy Commission, Ganakbari, Savar, Dhaka, 1349, Bangladesh.

Department of Chemistry, Mawlana Bhashani Science & Technology University, Santosh, Tangail, 1902, Bangladesh.

出版信息

Environ Sci Pollut Res Int. 2024 Aug;31(38):50261-50282. doi: 10.1007/s11356-024-34510-4. Epub 2024 Aug 1.

Abstract

This study integrated hydrochemical analysis, isotopic analysis, the integrated water quality index (IWQI), and the health risk assessment model to analyze hydrochemical characteristics, quality, and nitrate health risks in a typical agricultural and industrial (i.e., Holocene and Pleistocene) simultaneously affected by anthropogenic activities, as well as to explore the recharge mechanisms of the groundwater. The shallow groundwater is mainly Ca-HCO and deep groundwater is mainly Na-HCO types. In shallow and intermediate aquifers (Holocene), rainfall recharge is seen, but in deep aquifers (Holocene) and the Madhupur tract (Pleistocene), there is no evidence of recent recharge from the stable isotopic (δH‰ and δO‰) composition of groundwater. Anthropogenic sources significantly impacted the groundwater chemistry of shallow and intermediate aquifers more than geogenic sources. Most metalloids, and metals (As, and Cr, Fe, Ni, Pb, and Mn) and NO exceed the WHO-2011 and BD acceptable limit from shallow and intermediate groundwater. PCA analysis revealed the contamination of shallow and intermediate aquifers by metalloids, metals and from various anthropogenic activities. Based on the IWQI, HPI, HEI, and DC, groundwater samples from shallow and intermediate aquifers are unsuitable for oral consumption. The NPI shows that the metalloids, and metals are responsible for groundwater pollution in a descending order of As > Fe > Pb > Ni > Cr > Mn. Health risk assessment indicates oral and dermal consumption of contaminated water from shallow and intermediate aquifers can pose carcinogenic and non-carcinogenic health risks for both the adults and the children. The HQ and HI values of shallow and intermediate groundwater indicates higher non-carcinogenic risk. Carcinogenic risk through oral and dermal consumption follows an order of As > Ni > Cr > Pb and Ni > Cr > As > Pb, respectively. Compared to adults, children are more susceptible to both carcinogenic and non-carcinogenic risks. Potential threats to the health of people living in the study region need immediate attention from the public, government, and the scientific community.

摘要

本研究综合运用水化学分析、同位素分析、综合水质指数(IWQI)和健康风险评估模型,分析了受人为活动同时影响的典型农业和工业地区(全新世和更新世)的水化学特征、水质和硝酸盐健康风险,并探讨了地下水的补给机制。浅层地下水主要为 Ca-HCO 型,深层地下水主要为 Na-HCO 型。在浅层和中层含水层(全新世)中可见到降雨补给,但在深层含水层(全新世)和 Madhupur 地带(更新世)中,从地下水稳定同位素(δH‰和δO‰)组成来看,没有最近的补给证据。人为源对浅层和中层含水层的地下水化学影响大于地球化学源。大多数类金属、金属(As、Cr、Fe、Ni、Pb 和 Mn)和硝酸盐超过了 WHO-2011 标准和 BD 可接受限值。主成分分析(PCA)表明,浅层和中层含水层受到类金属、金属和各种人为活动的污染。根据 IWQI、HPI、HEI 和 DC,浅层和中层地下水样本不适合口服。NPI 表明,类金属和金属对地下水污染的责任程度依次为 As>Fe>Pb>Ni>Cr>Mn。健康风险评估表明,浅层和中层含水层受污染的水通过口服和皮肤接触,会对成人和儿童造成致癌和非致癌健康风险。浅层和中层地下水的 HQ 和 HI 值表明存在更高的非致癌风险。通过口服和皮肤接触摄入浅层和中层地下水的致癌风险依次为 As>Ni>Cr>Pb 和 Ni>Cr>As>Pb。与成人相比,儿童更容易受到致癌和非致癌风险的影响。生活在研究区域的人们的健康受到的潜在威胁需要引起公众、政府和科学界的关注。

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