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印度旁遮普邦北部卡普尔塔腊、贾朗达尔和霍希亚布尔地区铀的时空分布、地下水质量及其相关风险的定量评估。

Quantitative appraisal of spatiotemporal uranium distribution, quality of groundwater, and associated risks in Kapurthala, Jalandhar, and Hoshiarpur districts of northern Punjab, India.

机构信息

Department of Physics, Guru Nanak Dev University, Amritsar, Punjab, 143005, India.

Department of Chemistry, Centre for Advanced Studies, Guru Nanak Dev University, Amritsar, Punjab, 143005, India.

出版信息

Environ Sci Pollut Res Int. 2022 Jan;29(5):7225-7239. doi: 10.1007/s11356-021-16159-5. Epub 2021 Sep 1.

Abstract

Groundwater samples from Kapurthala (45), Jalandhar (70), and Hoshiarpur (70) districts from northern Punjab, India, were studied for seasonal variation (pre-monsoon and post-monsoon) of uranium distribution and physicochemical parameters, quality and suitability for drinking purposes, source apportionment, and health risks. The average uranium concentration (in μg L) in Kapurthala, Jalandhar, and Hoshiarpur districts was 12.7, 18.8, and 7.0, respectively, in pre-monsoon and 8.0, 17.3, and 5.6, respectively, in post-monsoon. In both seasons, uranium concentration was below WHO limit (30 μg L) in more than 90% of groundwater samples, and it was found to exhibit positive correlation majorly with TDS, EC, and total alkalinity. Principal component analysis revealed dissolution of rocks/minerals contributing to mineralization of associated aquifers in addition to some anthropogenic activities such as excessive application of fertilizers/pesticides and dumping of domestic waste followed by their seepage into the groundwater table. All groundwater samples fall in very good to good drinking groundwater quality and its quality is more improved in post-monsoon season owing to dilution of various inorganic salts during groundwater recharge in monsoon season. Average Hazard Index (HI) values due to ingestion of U, F, and NO via drinking water for both adults and children were found to be marginally greater than safe limit of 1 with major contribution from F. It is advisable to local government/public that regular monitoring of groundwater and proper management policies or strategies should be adopted followed by their implementation to control groundwater pollution in three districts.

摘要

从印度旁遮普邦北部的卡普尔塔腊(Kapurthala,45 个样本)、贾朗达尔(Jalandhar,70 个样本)和霍希亚布尔(Hoshiarpur,70 个样本)采集地下水样本,研究铀分布和理化参数的季节性变化(前季风期和后季风期)、水的质量和适宜性、来源分配和健康风险。卡普尔塔腊、贾朗达尔和霍希亚布尔地区的铀平均浓度(μg/L)分别为前季风期的 12.7、18.8 和 7.0,后季风期的 8.0、17.3 和 5.6。两个季节中,超过 90%的地下水样本铀浓度低于世界卫生组织(WHO)限值(30μg/L),且与 TDS、EC 和总碱度呈正相关。主成分分析显示,岩石/矿物的溶解作用除了一些人为活动(如过度使用化肥/农药和倾倒生活垃圾)之外,还导致相关含水层的矿化,这些人为活动随后渗透到地下水位。所有地下水样本均属于极好至良好的饮用水水质,且在后季风期由于雨季地下水补给过程中各种无机盐的稀释作用,水质得到进一步改善。由于饮用水中摄入 U、F 和 NO 导致的成人和儿童平均危害指数(HI)值略高于 1 的安全限值,主要贡献来自 F。建议当地政府/公众定期监测地下水,并采取适当的管理政策或策略,随后加以实施,以控制三个地区的地下水污染。

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