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Study of partitioning and dynamics of metals in contaminated soilusing modified four-step BCR sequential extraction procedure

机译:改进的四步BCR顺序萃取程序研究污染土壤中金属的分配和动力学

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The modified four-step BCR sequential extraction procedure (exchangeable and weak acid avail-able species, reducible, oxidisable and residual fractions) was used to examine the distribution of As, Cd, Cr, Cu, Pb, and Zn with soil depth in an area (Baia Mare - Bozanta, Romania) with both high natural level of elements considered as toxic and historical pollution resulting from non-ferrous metallurgy. The BCR approach proved a high metal input of anthropogenic origin down to 40 cm, while at lower depths the naturally elevated metal content must be considered. Results of the partitioning study and XRD analysis of solid matrix showed the greatest potential for chemical remobilisation of Cd, Zn, and Cu in weak acidic medium as well as their affinity for the oxidisable fraction (organic matter/sulphide). The tendency of Cr, Pb, and As to be immobilised as residual or reducible species on Fe-Mn oxides was evident. Although the partitioning of As in chemically inactive forms such as scorodite (FeAsO_4 · 2H_2O) soluble under reducible conditions and beudantite (PbFe_3(AsO_4) (SO_4) (OH)_2)), a residual species soluble in acid media, chemical mobilisation from soil in groundwater was confirmed. Dynamic processes of metal retention in soil under different conditions, namely acidic, reducing or oxidisable, were predicted from the Pearson's correlation analysis of element species with soil characteristics and components such as Fe, Mn, organic matter content, pH, and total element content, respectively. At the moment of the study, soil and groundwater in the area were found to be polluted with As, Cd, Cu, Pb and Zn.
机译:改进的四步BCR顺序萃取程序(可交换和弱酸可利用的种类,可还原的,可氧化的和残留的馏分)用于检查土壤中As,Cd,Cr,Cu,Pb和Zn在土壤深度的分布。该地区(拜亚马雷-博赞塔,罗马尼亚)具有很高的天然元素含量,并被有色冶金业造成历史污染。 BCR方法证明人为来源的金属输入量低至40 cm,而在较低深度时,必须考虑自然增加的金属含量。固体基质的分配研究和XRD分析结果表明,在弱酸性介质中Cd,Zn和Cu的化学固定潜力最大,并且它们对可氧化级分(有机物/硫化物)具有亲和力。 Cr,Pb和As被固定为Fe-Mn氧化物上残留或可还原物种的趋势很明显。尽管砷以化学惰性形式(例如可在可还原条件下溶解的臭葱石(FeAsO_4·2H_2O)和膨润土(PbFe_3(AsO_4)(SO_4)(OH)_2))分配,但残留物可溶于酸性介质,可从土壤化学迁移在地下水中被证实。根据皮尔森对元素种类与土壤特征和成分(例如铁,锰,有机质含量,pH和总元素含量)的相关性进行的皮尔逊相关分析,可以预测金属在不同条件下(酸性,还原性或可氧化性)在土壤中的动态保留过程,分别。在研究之时,该地区的土壤和地下水被砷,镉,铜,铅和锌污染。

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