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Spatio-temporal dynamics of heavy metals in sediments of the river estuarine system: Mahanadi basin (India)

机译:河口系统沉积物中重金属的时空动态:马哈纳迪盆地(印度)

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摘要

Dynamics of heavy metals in the surface sediments of Mahanadi river estuarine system were studied for three different seasons. This study demonstrates that the relative abundance of these metals follows in the order of Fe > Mn > Zn > Pb > Cr > Ni ≥ Co > Cu > Cd. The spatial pattern of heavy metals supported by enrichment ratio data, suggests their anthropogenic sources possibly from various industrial wastes and municipal wastes as well as agricultural runoff. The metal concentrations in estuarine sediments are relatively higher than in the river due to adsorption/accumulation of metals on sediments during saline mixing, while there is a decreasing trend of heavy metal concentrations towards the marine side. The temporal variations for metals, such as Fe, Mn, Zn, Ni and Pb exhibit higher values during monsoon season, which are related to agricultural runoff. Higher elemental concentrations are observed during pre-monsoon season for these above metals (except Ni) at the polluted stations and for metals, such as Cr, Co and Cd at all sites, which demonstrate the intensity of anthropogenic contribution. R-mode factor analysis reveals that "Fe-Mn oxy hydroxide", "organic matter", "CaCO_3", and "textural variables" factors are the major controlling geochemical factors for the enrichment of heavy metals in river estuarine sediment and their seasonal variations, though their intensities were different for different seasons. The relationships among the stations are highlighted by cluster analysis, represented in dendrograms to categorize different contributing sites for the enrichment of heavy metals in the river estuarine system.
机译:研究了三个不同季节马哈纳迪河河口系统表层沉积物中重金属的动力学。研究表明,这些金属的相对丰度依次为Fe> Mn> Zn> Pb> Cr> Ni≥Co> Cu> Cd。富集率数据支持的重金属的空间格局表明,它们的人为来源可能来自各种工业废物,市政废物以及农业径流。由于盐水混合过程中沉积物上金属的吸附/积累,河口沉积物中的金属浓度相对高于河流中的浓度,而重金属向海洋一侧的浓度却呈下降趋势。在季风季节,诸如Fe,Mn,Zn,Ni和Pb等金属的时间变化表现出较高的值,这与农业径流有关。在季风季节之前,这些受污染站的上述金属(镍除外)以及所有地点的诸如Cr,Co和Cd等金属的元素浓度均较高,这表明了人为贡献的强度。 R-模式因子分析表明,“ Fe-Mn氢氧化氧”,“有机物”,“ CaCO_3”和“结构变量”因子是河口沉积物中重金属富集及其季节变化的主要控制地球化学因子。 ,尽管它们的强度在不同季节有所不同。站间关系通过聚类分析突出显示,以树状图表示,对河口系统中重金属富集的不同贡献部位进行分类。

著录项

  • 来源
    《Environmental earth sciences》 |2014年第4期|1893-1909|共17页
  • 作者单位

    Faculty of Earth Systems and Environmental Science, Chonnam National University, Gwangju 500757, South Korea,Institute of Oceanography, National Taiwan University, Taipei 10617, Taiwan,Department of Chemistry, S.C.S. (Autonomous) College, Puri 752001, Orissa, India;

    Institute of Minerals and Materials Technology, Bhubaneswar 751013, Orissa, India;

    Faculty of Earth Systems and Environmental Science, Chonnam National University, Gwangju 500757, South Korea;

    Department of Chemistry, Utkal University, Bhubaneswar 751004, Orissa, India;

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

    Heavy metals; Sediments; River estuarine; Mahanadi; India;

    机译:重金属;沉积物;河口;Mahanadi;印度;

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