印度西北方邦Bagpat地区Yamuna-Hindon交汇区地球化学过程及地下水质量评价。

IF 1.8 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
Gautam Chandra Mondal, Abhishek Pandey Bharat, Abhay Kumar Singh
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引用次数: 0

摘要

本研究旨在了解印度西北方邦Bagpat地区Yamuna-Hindon交界区地下水资源的地球化学特征。该地区是印度恒河带的一部分,是世界上最肥沃和农业密集的地区之一。为了研究控制地下水质量的地球化学过程,在季风前收集了105个地下水样本,并根据美国公共卫生协会(APHA)概述的方法,分析了各种物理化学参数,即pH,电导率(EC),总溶解固形物(TDS),总硬度(TH),浊度,主要阴离子(HCO3-, SO42-, F-, Cl-, NO3-),阳离子(Ca2+, Mg2+, Na+, K+)。采用ICP-MS法对地下水中溶解重金属(Fe、Mn、Zn、Pb、Cu、Cr、Ni、As、Se、Co、Cd、Al)进行了分析。分析结果表明,地下水以中性至轻度碱性为主。主要阳离子化学主要遵循Na+ > Mg2+ > Ca2+ > K+的出现规律,阴离子主要遵循HCO3- > Cl- > SO42- > NO3- > F-的出现规律。Piper三角图数据表明,Ca2+- mg2 +- hco3 -和Na+- k +- hco3 -Cl-是主要的水文地球化学相。虽然与Cl-、F-和NO3-有关的阳离子可能部分来源于人为来源,但该地区地下水地球化学主要由造岩矿物风化作用控制。TDS、TH、浊度和F-是饮用水中主要超标参数。除铁、锰、铝、硒外,其余重金属均在饮用水规定标准范围内。在某些地点,较高的盐度、%Na和镁危害(MH)限制了其对农业用途的适用性。对5个样品中选定的有机氯和有机磷农药的评价表明,在少数样品中存在林丹、β-硫丹和滴滴涕异构体。然而,在得出任何最终结论之前,需要对这一集约化农业地区可能存在的农药污染进行详细调查。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geochemical processes and groundwater quality assessment in the Yamuna-Hindon interfluve region of Bagpat district, Western Uttar Pradesh, India

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 (HCO3, SO42−, F, Cl, NO3), cations (Ca2+, Mg2+, 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+ > Mg2+ > Ca2+ > K+, while for anions it was HCO3 > Cl > SO42− > NO3 > F. The data plotted on Piper triangular diagram indicated that Ca2+-Mg2+-HCO3 and Na+-K+-HCO3-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 NO3 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.

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来源期刊
Geochemical Transactions
Geochemical Transactions 地学-地球化学与地球物理
CiteScore
3.70
自引率
4.30%
发文量
2
审稿时长
>12 weeks
期刊介绍: Geochemical Transactions publishes high-quality research in all areas of chemistry as it relates to materials and processes occurring in terrestrial and extraterrestrial systems.
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