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坦桑尼亚辛吉达地区地下水中氟化物分布及健康风险评估:对饮用水水质和灌溉的影响

Fluoride distribution and health risk assessment in groundwater of Tanzania's Singida Region: implications for drinking water quality and irrigation.

作者信息

Banyikwa Andrew Toyi

机构信息

Department of Chemistry, College of Natural and Mathematical Sciences (CNMS), University of Dodoma, Dodoma, United Republic of Tanzania.

出版信息

Environ Geochem Health. 2025 Aug 28;47(10):417. doi: 10.1007/s10653-025-02696-2.

Abstract

Fluoride (F⁻) pollution poses a significant public health concern in the regions located in the fluoride belt of Tanzania which includes the Singida Region. Groundwater in this belt contains F⁻ that exceed the World Health Organization's recommended limit of 1.5 mg l. The hydrochemistry, distribution of F, and the non-carcinogenic health risk associated with F⁻ pollution in the fluoride belt of Tanzania remain largely unexplored. This study evaluated the hydrochemistry, F⁻ distribution in groundwater, assessed its regulation by major ions, estimated non-carcinogenic health risks, and examined the water's suitability for drinking and irrigation using 71 samples. The parameters analyzed included pH, electrical conductivity (EC), total hardness (TH), Ca⁺, Mg⁺, Na⁺, K⁺, Cl⁻, SO, HCO⁻, and F⁻. The results indicate that F⁻ pollution is prevalent in the Singida Region, with concentrations ranging from 0.17 to 13.00 mg l. Of the water samples analyzed, 56.34% were within the safe limits, while 43.66% exceeded the threshold. The percentage of water samples with a Hazard Quotient (HQ) > 1 for F⁻ was found to be 61.97% for infants, 60.56% for children, and 39.43% for adults, indicating a potential non-carcinogenic health risk from elevated F⁻ levels in drinking water particularly among infants and children. F exhibited a negative correlation with TH, and positive correlations with Na⁺, pH, and HCO⁻. The assessment of irrigation suitability using indices such as Sodium Adsorption Ratio (SAR), Kelly's Ratio (KR), Sodium Percentage (%Na), and Magnesium Adsorption Ratio (MAR) indicates that the groundwater is generally suitable for irrigation purposes.

摘要

在坦桑尼亚氟化物带所在地区,包括辛吉达地区,氟化物(F⁻)污染引发了重大的公共卫生问题。该地带的地下水中所含F⁻超过了世界卫生组织建议的1.5毫克/升的限值。坦桑尼亚氟化物带的水化学性质、F的分布以及与F⁻污染相关的非致癌健康风险在很大程度上仍未得到充分研究。本研究利用71个样本评估了水化学性质、地下水中F⁻的分布,评估了主要离子对其的调控作用,估计了非致癌健康风险,并检验了该水用于饮用和灌溉的适宜性。分析的参数包括pH值、电导率(EC)、总硬度(TH)、Ca⁺、Mg⁺、Na⁺、K⁺、Cl⁻、SO、HCO⁻和F⁻。结果表明,辛吉达地区普遍存在F⁻污染,浓度范围为0.17至13.00毫克/升。在所分析的水样中,56.34%在安全限值内,而43.66%超过了阈值。发现F⁻的危害商(HQ)>1的水样比例在婴儿中为61.97%,在儿童中为60.56%,在成人中为39.43%,这表明饮用水中F⁻水平升高存在潜在的非致癌健康风险,尤其是在婴儿和儿童中。F与TH呈负相关,与Na⁺、pH值和HCO⁻呈正相关。使用钠吸附比(SAR)、凯利比率(KR)、钠百分比(%Na)和镁吸附比(MAR)等指标对灌溉适宜性进行的评估表明,该地下水总体上适合用于灌溉目的。

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