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Concentrations of inorganic arsenic in groundwater, agricultural soils and subsurface sediments from the middle Gangetic plain of Bihar, India

机译:印度比哈尔邦中部恒河平原地下水,农业土壤和地下沉积物中无机砷的浓度

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摘要

Concentrations of inorganic forms [arsenite, As(Ⅲ) and arsenate, As(Ⅴ) of arsenic (As) present in groundwater, agricultural soils and subsurface sediments located in the middle Gangetic plain of Bihar, India were determined. Approximately 73% of the groundwater samples (n = 19) show As(Ⅲ) as the dominant species while 27% reveals As(Ⅴ) was the dominant species. The concentration of As(Ⅲ) in agricultural soil samples varies from not detectable to 40 μg/kg and As(Ⅴ) was observed as the major species (ranging from 1050 to 6835 μg/kg) while the total As concentration varied from 3528 to 14,690 μg/kg. Total extracted concentration of As was higher in the subsurface sediments (range 9119-20,056 μg/kg in Methrapur and 4788-19,681 μg/kg in Harail Chapar) than the agricultural soil, indicating the subsurface sediment as a source of As. Results of X-ray diffraction (XRD) and environmental scanning electron microscope (ESEM) revealed the presence of hematite and goethite throughout the vertical section below while magnetite was observed only in the upper oxidized layer at Methrapur and Harail Chapar. Alteration of Fe-ox-ides and presence of fibrous goethite indicating presence of diagenetic sediment. Siderite plays a crucial role as sinks to the As in subsurface sediments. The study also concluded that decomposition of organic matter present in dark and grey sections promote the redox conditions and trigger mobilization of As into groundwater.
机译:测定了印度比哈尔邦中部恒河平原的地下水,农业土壤和地下沉积物中无机形态的砷(砷),砷(Ⅲ)和砷酸盐,砷(Ⅴ)的无机形态的浓度。大约73%(n = 19)的地下水样品中砷(Ⅲ)为优势种,而27%的地下水样品中砷(Ⅴ)为优势种。农业土壤样品中As(Ⅲ)的浓度从不可检测到40μg/ kg不等,以As(Ⅴ)为主要种类(从1050到6835μg/ kg不等),而总As的浓度在3528到200μg/ kg之间。 14,690微克/千克地下沉积物中As的总提取浓度高于农业土壤(Methrapur中为9119-20,056μg/ kg,Harail Chapar中为4788-19,681μg/ kg),表明地下沉积物是As的来源。 X射线衍射(XRD)和环境扫描电子显微镜(ESEM)的结果显示,在下面的垂直区域中均存在赤铁矿和针铁矿,而仅在Methrapur和Harail Chapar的上部氧化层中观察到了磁铁矿。铁-氧-氧化物的变化和纤维针铁矿的存在表明成岩沉积物的存在。菱铁矿在地下沉积物中向砷的下沉起关键作用。该研究还得出结论,深色和灰色部分中存在的有机物的分解促进了氧化还原条件并触发了砷向地下水中的迁移。

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  • 来源
    《The Science of the Total Environment》 |2016年第15期|1103-1114|共12页
  • 作者单位

    Global Centre for Environmental Remediation (GCER), Faculty of Science and Information Technology, University of Newcastle, University Drive, Callaghan, NSW 2308, Australia ,Cooperative Research Centre for Contamination Assessment and Remediation of the Environment (CRC-CARE), University of Newcastle, ATC Building, University Drive, Callaghan, NSW 2308, Australia ,School of Environmental Sciences, Jawaharlal Nehru University, New Delhi 110067, India;

    School of Environmental Sciences, Jawaharlal Nehru University, New Delhi 110067, India;

    Global Centre for Environmental Remediation (GCER), Faculty of Science and Information Technology, University of Newcastle, University Drive, Callaghan, NSW 2308, Australia ,Cooperative Research Centre for Contamination Assessment and Remediation of the Environment (CRC-CARE), University of Newcastle, ATC Building, University Drive, Callaghan, NSW 2308, Australia;

    Global Centre for Environmental Remediation (GCER), Faculty of Science and Information Technology, University of Newcastle, University Drive, Callaghan, NSW 2308, Australia ,Cooperative Research Centre for Contamination Assessment and Remediation of the Environment (CRC-CARE), University of Newcastle, ATC Building, University Drive, Callaghan, NSW 2308, Australia;

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

    Inorganic arsenic; Agricultural soil; Subsurface sediments; Extractable arsenic; Middle Gangetic plain;

    机译:无机砷农业土壤;地下沉积物;可萃取砷;中恒河平原;

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