Mondal Gautam Chandra, Bharat Abhishek Pandey, Singh Abhay Kumar
Water Resource Management Group, CSIR-Central Institute of Mining and Fuel Research, Dhanbad, 826001, Jharkhand, India.
Academy of Scientific and Innovative Research (AcSIR), Ghaziabad, 201002, Uttar Pradesh, India.
Geochem Trans. 2025 Aug 1;26(1):7. doi: 10.1186/s12932-025-00102-5.
The present research work aims to understand the geochemistry of groundwater resources of the Yamuna-Hindon interfluve region of Bagpat district, Western Uttar Pradesh, India. The region is a part of Indo-Gangetic belt, one of the world's most fertile and intensely farmed areas. To investigate the geochemical processes governing groundwater quality, a total of 105 groundwater samples were collected during pre-monsoon season and analyzed for various physico-chemical parameters, namely, pH, electrical conductivity (EC), total dissolved solid (TDS), total hardness (TH), turbidity, major anions (HCO, SO, F, Cl, NO) cations (Ca, Mg, Na, K) following the methods outlined in the American Public Health Association (APHA). The dissolved heavy metals (Fe, Mn, Zn, Pb, Cu, Cr, Ni, As, Se, Co, Cd and Al) in groundwater were analyzed by ICP-MS following the instrument manual. The analysis results revealed that the groundwater is pre-dominantly neutral to mildly alkaline in nature. The major cation chemistry majorly followed the occurrence pattern of Na > Mg > Ca > K, while for anions it was HCO > Cl > SO > NO > F. The data plotted on Piper triangular diagram indicated that Ca-Mg-HCO and Na-K-HCO-Cl were major hydrogeochemical facies. Weathering of rock-forming minerals mainly governed the groundwater geochemistry in this region, although part of the cations associated with Cl, F and NO may originate from anthropogenic sources. TDS, TH, turbidity and F were identified as the major parameters that violated the prescribed limits for drinking water. Most of the heavy metals were found within the drinking water prescribed limits except for Fe, Mn, Al and Se. Elevated salinity, %Na, and magnesium hazard (MH) at certain sites limit its suitability for agricultural use. The assessment of selected organochlorine and organophosphorus pesticides in five samples indicated presence of lindane, β-endosulfan and DDT isomers in few samples. However, a detailed investigation of possible pesticide contamination in this intensive agriculture area is required before drawing any final conclusions.
本研究旨在了解印度北方邦西部巴格帕特地区亚穆纳河与欣登河间地区地下水资源的地球化学特征。该地区是印度河—恒河平原的一部分,是世界上最肥沃且农业集约化程度最高的地区之一。为研究控制地下水水质的地球化学过程,在季风来临前采集了105份地下水样本,并按照美国公共卫生协会(APHA)规定的方法分析了各种物理化学参数,即pH值、电导率(EC)、总溶解固体(TDS)、总硬度(TH)、浊度、主要阴离子(HCO、SO、F、Cl、NO)和阳离子(Ca、Mg、Na、K)。按照仪器手册,采用电感耦合等离子体质谱法(ICP-MS)分析了地下水中溶解的重金属(Fe、Mn、Zn、Pb、Cu、Cr、Ni、As、Se、Co、Cd和Al)。分析结果表明,该地区地下水主要呈中性至弱碱性。主要阳离子化学组成大致遵循Na>Mg>Ca>K的分布模式,而阴离子则为HCO>Cl>SO>NO>F。绘制在派珀三角图上的数据表明,Ca-Mg-HCO和Na-K-HCO-Cl是主要的水文地球化学相。尽管与Cl、F和NO相关的部分阳离子可能来自人为源,但该地区地下水地球化学主要受造岩矿物风化控制。TDS、TH、浊度和F被确定为超出饮用水规定限值的主要参数。除Fe、Mn、Al和Se外,大多数重金属含量均在饮用水规定限值内。某些地点盐度、钠百分比和镁危害(MH)升高,限制了其农业用途。对五个样本中选定的有机氯和有机磷农药进行的评估表明,少数样本中存在林丹、β-硫丹和滴滴涕异构体。然而,在得出任何最终结论之前,需要对这个集约化农业地区可能存在的农药污染进行详细调查。