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Assessment of groundwater quality with special reference to arsenic in Nawalparasi district, Nepal using multiv ariate statistical techniques

机译:使用多元统计技术评估尼泊尔纳瓦尔帕拉西区的地下水水质,特别是砷

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摘要

Groundwater is a precious resource for humankind not only in Nepal but also across the globe due to its diverse functions. A total of 48 groundwater samples were collected from three villages of Nawalparasi district, Nepal, during pre-monsoon and monsoon to estimate the overall groundwater quality and to identify the sources of contamination with emphasis on arsenic (As). The average concentrations of all tested groundwater quality parameters (temp., pH, EC, ORP, Ca~(2+), Mg~(2+), Na~+, K~+, Cl~-, F~-,SO_4~(2-), PO_4~(3-), HCO_3~-, NO_3~-, Cu, Ni, Mn, Cd, Pb, Fe, Zn, Cr, and As) were well within permissible limits of WHO for drinking water, except for Ni, Cd, Pb, Cr, and As. Concentration of As ranged from 60 to 3,100 μg L~(-1) and 155 to 1,338 μg L~(-1) in pre-monsoon and monsoon, respectively. The Piper diagram of the groundwater chemistry showed groundwater of Nawalparasi belongs to Ca-Mg-HCO_3 and Mg-HCO_3 water type with HCO_3~- as dominant ions. As content in the study area was negatively correlated with Fe in pre-monsoon, while it was positively correlated in monsoon. Furthermore, As was negatively correlated with oxidation reduction potential suggesting reducing condition of groundwater. Principal component analysis revealed seven major factors that explained 81.996 and 83.763 % of total variance in water quality in pre-monsoon and monsoon, respectively. The variance of water quality was related mainly with the degree of water-rock interaction, mineralization, and anthropogenic inputs.
机译:地下水由于其多种功能,不仅在尼泊尔而且在全球都是人类宝贵的资源。在季风前和季风期间,从尼泊尔纳瓦尔帕拉西区的三个村庄收集了总共48个地下水样品,以估计总体地下水质量并确定砷(As)为污染源。所有测试的地下水水质参数(温度,pH,EC,ORP,Ca〜(2 +),Mg〜(2 +),Na〜+,K〜+,Cl〜-,F〜-,SO_4的平均浓度〜(2-),PO_4〜(3-),HCO_3〜-,NO_3〜-,Cu,Ni,Mn,Cd,Pb,Fe,Zn,Cr和As都在WHO饮用水允许的范围内,除了镍,镉,铅,铬和砷。季风前和季风中As的浓度分别为60〜3,100μgL〜(-1)和155〜1,338μgL〜(-1)。地下水化学反应的Piper图表明,Nawalparasi的地下水属于Ca-Mg-HCO_3和Mg-HCO_3水类型,其中HCO_3〜-为主要离子。由于研究区的含量在季风前与铁呈负相关,而在季风时呈正相关。此外,砷与氧化还原电位呈负相关,表明地下水的还原条件。主成分分析揭示了七个主要因素,分别解释了季风前和季风中水质总变化的81.996%和83.763%。水质的变化主要与水-岩相互作用,矿化和人为输入有关。

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  • 来源
    《Environmental earth sciences》 |2014年第1期|259-273|共15页
  • 作者单位

    Centre of Advanced Study in Botany, Banaras Hindu University, Varanasi 221005, UP, India;

    Centre for Environmental Sciences, Central University of Bihar, BIT Campus, Patna 800014, India;

    Department of Civil Engineering, Indian Institute of Technology, Banaras Hindu University, Varanasi 221005, India;

    School of Environmental Studies, State Key Laboratory of Bio-geology and Environmental Geology, China University of Geosciences, 388, Lumo Road, Wuhan 430074, China;

    Centre of Advanced Study in Botany, Banaras Hindu University, Varanasi 221005, UP, India;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Multivariate; Hierarchical; Groundwater; Arsenic; Terai; Nepal;

    机译:多变量分层地下水;砷;寺井尼泊尔;

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