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首页> 外文期刊>Journal of Geochemical Exploration: Journal of the Association of Exploration Geochemists >The relationship between WRB soil units and heavy metals content in soils of Catamarca (Argentina)
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The relationship between WRB soil units and heavy metals content in soils of Catamarca (Argentina)

机译:卡塔马卡(阿根廷)土壤中的RBB土壤单位与重金属含量的关系

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摘要

Trace element content in soils is mainly dependent on the nature of parent rocks from which the soil material is derived,as well as weathering and soil forming processes.Despite the close relationship between soil and rock,the soil forming processes modify the regolith and redistribute the content of heavy metals in the soil horizons.The World Reference Base (WRB) is a morphogenetic system of soil classification strongly based in soil genesis at the level of Reference Soil Groups (RSG).Present differences in trace elements content between different RSG may reflect the impact of pedogenic pathways of each RSG on the original trace element distribution.The natural variation of heavy metal content is a preliminary step in assessing heavy metal contamination in soils.Therefore,the term geochemical background became an important reference with increasing environmental awareness.The concentration and distribution of Cd,Cr,Cu,Ni,Pb,and Zn were investigated in thirty profiles of Catamarca in the municipal district of Fray Mamerto Esquiu,Argentina.The heavy metals content,except for Cd,is highly dependent on RSG according to WRB.Occasional or continuous contribution of sediments as in alluvial soils becomes the soil forming processes that acquires greater importance in the distribution of heavy metals.The organic matter content is the soil property that comes out as relevant at lower levels of Fluvisols when Humic or Mollihumic qualifiers apply.All studied soils show extremely high Pb in relation to the surrounding bedrock.This confirms that the infilling of the alluvial valley is not derived from the surrounding bedrock but it must come from a different source.The increase in the silt content of soils in the southern part of the alluvial valley are well reflected by Ni content.Therefore,pedogenic processes have had little influence in regional Ni distribution.The upper limit of the background,which allows distinguishing between natural element and anomalous concentrations are presented.The heavy metal showing the greatest number of samples with slight enrichment anomalies is Cd.Slight enrichment anomalies in Cd,Cr,Cu,Pb and Zn were detected in profile 29 confirming an anthropogenic pollution.
机译:土壤中的微量元素含量主要取决于衍生土壤材料的母岩的性质以及风化和成土过程。尽管土壤与岩石之间存在着密切的关系,但成土过程却改变了go石并重新分布了土壤。世界参考基准(WRB)是土壤分类的形态发生系统,强烈基于土壤起源于参考土壤组(RSG)的水平。不同RSG之间的痕量元素含量存在差异可能反映出重金属含量的自然变化是评估土壤中重金属污染的一个初步步骤。因此,地球化学背景一词随着环境意识的增强而成为重要的参考。在t的30个剖面中研究了Cd,Cr,Cu,Ni,Pb和Zn的浓度和分布根据WRB,重金属含量(镉除外)高度依赖于RSG。由于在冲积土壤中,沉积物的偶然性或持续性成为土壤形成过程,在分配过程中越来越重要当腐殖质或莫利腐质定性剂应用时,有机质含量是在氟维索醇含量较低时相关的土壤性质。所有研究的土壤相对于周围基岩均显示出极高的Pb含量,这证实了土壤的填充性。冲积谷不是来自周围的基岩,而必须来自不同的来源。冲积谷南部土壤的泥沙含量的增加可以很好地反映在镍的含量上。因此,成岩作用几乎没有影响。镍的局部分布。背景的上限,可以区分自然元素和异常浓度样品中重金属含量最高,重金属含量稍有异常,重金属Cd含量最高。在29号剖面中检测到Cd,Cr,Cu,Pb和Zn的轻含量异常,证实了人为污染。

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