Department of Environmental Sciences, COMSATS University Islamabad, Vehari Campus, Vehari, 61100, Pakistan.
Department of Sanitary Engineering, Faculty of Civil and Environmental Engineering, Gdansk University of Technology, 1/12 Narutowicza Str., Gdańsk, 80-233, Gdańsk, Poland.
Environ Sci Pollut Res Int. 2024 Oct;31(50):59990-60003. doi: 10.1007/s11356-024-35210-9. Epub 2024 Oct 4.
Groundwater from alluvial fan plains is the prevailing water source, especially for arid/semiarid regions, but its contamination poses substantial risks to water supply and public health. The recent study aims to assess the hydro-geochemistry, distribution, and potential health risks of NO, NO, and F concentrations in the groundwater of previously unexplored health facilities in District Vehari, Punjab, Pakistan. In total, 75 groundwater samples were evaluated for NO, NO, and F levels as well as pH, EC, TDS, CO, HCO, Cl, Na, Fe, K, Ca, Mg, taste, odor, color, and turbidity. The Durav graph shows that the water type is Na-HCO-Ca, with Na and HCO dominant, weak acids > strong acids, and alkaline ions > alkalis. Results revealed that drinking water samples (21.73% and 20%) taken from Tehsil Mailsi, and the Basic Health Unit (BHU) exceeded the WHO standard (1.5 mg/L) for F concentration, respectively. Moreover, the mean chronic daily intake (CDI) of F was 0.044, 0.018, and 0.02 mg/kg/day in children, men, and women, respectively. Similarly, the average CDI of NO was 0.113, 0.046, and 0.050 in children, men, and women, respectively, and the respective values of NO were 0.004, 0.001, and 0.001. The NO shows a significant range of hazard quotient (HQ) (0.0-1.172) in children. The range of HQ for F was 0.0-3.114, 0.0-1.290, and 0.0-1.389 in children, men, and women, respectively. Additionally, the health risks analysis revealed an HQ > 1.0 for children in groundwater, indicating a potential carcinogenic risk from the F. Pearson correlation and PCA analysis found a significant positive correlation (0.8) between NO and NO and a negative correlation (0.3) between F and HCO. These findings highlight the need for groundwater treatment in healthcare facilities prior to water consumption. Enforcing international and national drinking water standards in healthcare units is vital to strengthening services and providing equitable access to safe drinking water. Legislative and efficient water management measures must be taken for the protection of public health.
地下水是冲积扇平原的主要水源,特别是在干旱/半干旱地区,但地下水的污染对供水和公共健康构成了重大风险。最近的研究旨在评估巴基斯坦旁遮普省Vehari 地区以前未勘探的卫生设施中地下水的 NO、NO 和 F 浓度的水文地球化学、分布和潜在健康风险。共评估了 75 个地下水样本的 NO、NO 和 F 水平以及 pH、EC、TDS、CO、HCO、Cl、Na、Fe、K、Ca、Mg、味道、气味、颜色和浊度。Durav 图显示,水的类型为 Na-HCO-Ca,以 Na 和 HCO 为主,弱酸>强酸,碱性离子>碱性。结果表明,从 Tehsil Mailsi 和基本卫生单位(BHU)采集的饮用水样本(分别为 21.73%和 20%)中 F 浓度超过了世界卫生组织(1.5 mg/L)的标准。此外,儿童、男性和女性的 F 平均慢性日摄入量(CDI)分别为 0.044、0.018 和 0.02 mg/kg/天。同样,NO 的平均 CDI 分别为 0.113、0.046 和 0.050,NO 的相应值分别为 0.004、0.001 和 0.001。NO 在儿童中显示出显著的危害商(HQ)范围(0.0-1.172)。F 的 HQ 范围分别为 0.0-3.114、0.0-1.290 和 0.0-1.389,儿童、男性和女性的 HQ 范围分别为 0.0-3.114、0.0-1.290 和 0.0-1.389。此外,健康风险分析显示,儿童的地下水 HQ>1.0,表明 F 存在潜在的致癌风险。Pearson 相关性和 PCA 分析发现,NO 和 NO 之间存在显著的正相关(0.8),F 和 HCO 之间存在负相关(0.3)。这些发现突出表明,在医疗保健设施中,必须在饮用水之前进行地下水处理。在医疗单位执行国际和国家饮用水标准对于加强服务和提供公平获得安全饮用水至关重要。必须采取立法和有效的水管理措施来保护公众健康。