Department of Environment Studies, Panjab University, Chandigarh, India.
Department of Environment Studies, Post Graduate Government College-11, Chandigarh, India.
Environ Geochem Health. 2020 Jul;42(7):1833-1862. doi: 10.1007/s10653-019-00449-6. Epub 2019 Nov 5.
Groundwater quality in the alluvial plains of Punjab has special significance and needs great attention since it is the foremost source of drinking, irrigation and industrial uses. The present research work emphasizes the integrated hydrogeochemical and chemometric statistical approaches to appraise the geochemical processes and source apportionment of the groundwater in the alluvial plains of Jalandhar district, Punjab, India. The human health risk assessment was also performed to quantify the potential non-carcinogenic impacts of nitrate and fluoride on human health through ingestion of groundwater. For this purpose, 41 groundwater samples were collected from different groundwater abstraction units and analysed for pH, electrical conductivity, total dissolved solids, total hardness, total alkalinity and major ions (Ca, Mg, Na, K, HCO, CO, SO, NO, F, Cl and PO) using standard protocols. Drinking water quality index and Revelle index showed that groundwater samples fall under poor to unfit water class and salinization along the south-western portion of the study region shows poor water quality. The results of the hazard index (HI) show 68% and 46.34% of the groundwater samples have HI > 1 for children and adults. The non-carcinogenic health risk assessment of nitrate (NO) and fluoride (F) on the local population indicated that the children are more vulnerable through direct ingestion of drinking water than adults. Piper diagram and saturation index reveal that Ca-Mg-HCO is the dominant hydrochemical facies and oversaturated with calcite, dolomite and aragonite minerals in the groundwater. Gibbs diagrams, chloro-alkaline indices and scatter plots show that the hydrochemistry of the groundwater is mainly governed by aquifer material interaction such as weathering of silicate, carbonate rock, halite dissolution and cation exchange process. Chemometric statistical techniques revealed that the source identification of parameters such as Ca, Mg, Na, K, HCO, CO and F is originated from geogenic factors, whereas NO, SO, Cl and PO are from the anthropogenic origin. Therefore, urgent and efficient measures must be taken to combat groundwater pollution and reduce human health risk in the study area.
旁遮普冲积平原的地下水质量具有特殊意义,需要高度关注,因为它是饮用水、灌溉和工业用途的首要来源。本研究工作强调了综合水文地球化学和化学计量统计方法,以评估印度旁遮普杰朗达尔地区冲积平原地下水的地球化学过程和来源分配。还进行了人类健康风险评估,以通过摄入地下水量化硝酸盐和氟化物对人类健康的潜在非致癌影响。为此,从不同地下水抽取单元采集了 41 个地下水样本,并使用标准协议分析了 pH 值、电导率、总溶解固体、总硬度、总碱度和主要离子(Ca、Mg、Na、K、HCO、CO、SO、NO、F、Cl 和 PO)。饮用水质量指数和雷维尔指数表明,地下水样本属于差到不适用水类,研究区域西南部的盐化表明水质较差。危害指数(HI)的结果显示,68%和 46.34%的地下水样本的 HI 值儿童和成人均大于 1。当地居民的硝酸盐(NO)和氟化物(F)的非致癌健康风险评估表明,儿童通过直接饮用饮用水比成年人更容易受到伤害。Piper 图和饱和度指数表明,Ca-Mg-HCO 是主要的水文地球化学相,地下水中的方解石、白云石和文石矿物过饱和。Gibbs 图、氯-堿指数和散点图表明,地下水的水化学主要受含水层物质相互作用的控制,如硅酸盐、碳酸盐岩的风化、岩盐溶解和阳离子交换过程。化学计量统计技术表明,Ca、Mg、Na、K、HCO、CO 和 F 等参数的来源识别是由地球成因因素引起的,而 NO、SO、Cl 和 PO 则是由人为因素引起的。因此,必须采取紧急和有效的措施来防治地下水污染,降低研究区域的人类健康风险。