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水质指数和化学计量学方法在印度恒河流域浅层含水层污染评估中的应用。

Application of water quality index and chemometric methods on contamination assessment in the shallow aquifer, Ganges River basin, India.

作者信息

Rajmohan Natarajan

机构信息

Water Research Center, King Abdulaziz University, Jeddah, 21598, Kingdom of Saudi Arabia.

出版信息

Environ Sci Pollut Res Int. 2021 May;28(18):23243-23257. doi: 10.1007/s11356-020-12270-1. Epub 2021 Jan 13.

Abstract

Water quality index and chemometric methods were employed to assess the groundwater quality and contamination sources in the upper Ganges basin (UGB) and lower Ganges basin (LGB) as groundwater is a sole source for drinking, domestic and agricultural uses. Groundwater samples were collected from UGB (n = 44) and LGB (n = 26) and analysed for physicochemical parameters. Groundwater in this basin is desirable (51%) to permissible (TDS < 1000 mg/l, 96%) classes for drinking. Chemical constituents in the groundwater are lower than the maximum allowable limit recommended by the WHO for drinking except K. Drinking water quality index (DWQI) values reveal that groundwater belongs to excellent (89%) and good (10%) classes. However, the high concentrations of Fe and Mn in 61 and 77% of samples, respectively, restrict the usage for drinking according to USEPA recommendations. Both LGB and UGB groundwater in shallow wells have elevated concentration of TDS, EC and other ions (Ca, Cl and SO in LGB; major ions, NO, PO, F, Fe and Mn in UGB) and imply the influences of anthropogenic activities. Principal component analysis and hierarchical cluster analysis reiterated that groundwater quality is affected by the anthropogenic activities as well as mineral dissolutions (carbonate and silicate minerals). This study highlighted that the infiltration of wastewater from various contamination sources likely triggered the dissolution of the minerals in the vadose zone that resulted in the accumulation of ions in the shallow aquifer. An effective management plan is essential to protect this shallow aquifer.

摘要

由于地下水是该地区唯一的饮用水、生活用水及农业用水来源,故采用水质指数和化学计量学方法对恒河上游流域(UGB)和恒河下游流域(LGB)的地下水水质及污染源进行评估。从UGB(n = 44)和LGB(n = 26)采集了地下水样本,并对其理化参数进行分析。该流域的地下水水质适宜饮用(占51%)至允许饮用(总溶解固体含量<1000 mg/l,占96%)。除钾元素外,地下水中的化学成分均低于世界卫生组织推荐的饮用最大允许限值。饮用水水质指数(DWQI)值表明,地下水属于优良(占89%)和良好(占10%)等级。然而,分别有61%和77%的样本中含有高浓度的铁和锰,根据美国环境保护局的建议,这限制了其作为饮用水的用途。LGB和UGB浅井中的地下水,其总溶解固体、电导率及其他离子(LGB中的钙、氯和硫酸根;UGB中的主要离子、硝酸根、磷酸根、氟、铁和锰)浓度均有所升高,这意味着受到了人为活动的影响。主成分分析和层次聚类分析再次表明,地下水水质受人为活动以及矿物溶解(碳酸盐和硅酸盐矿物)的影响。该研究强调,来自各种污染源的废水渗入可能引发了包气带中矿物的溶解,从而导致浅含水层中离子的积累。制定有效的管理计划对于保护该浅含水层至关重要。

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