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首页> 外文期刊>Journal of Enviromental Quality >Zinc Fractionation in Contaminated Soils by Sequential and Single Extractions: Influence of Soil Properties and Zinc Content
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Zinc Fractionation in Contaminated Soils by Sequential and Single Extractions: Influence of Soil Properties and Zinc Content

机译:顺序和单次萃取分离污染土壤中的锌:对土壤性质和锌含量的影响

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摘要

We studied the fractionation of zinc (Zn) in 49 contaminated soils as influenced by Zn content and soil properties using a seven-step sequential extraction procedure (F1: NH4NO3; F2: NH4–acetate, pH 6; F3: NH3OHCl, pH 6; F4: NH4–EDTA, pH 4.6; F5: NH4–oxalate, pH 3; F6: NH4–oxalate/ascorbic acid, pH 3; F7: residual). The soils had developed from different geologic materials and covered a wide range in soil pH (4.0–7.3), organic C content (9.3–102 g kg–1), and clay content (38–451 g kg–1). Input of aqueous Zn with runoff water from electricity towers during 26 to 74 yr resulted in total soil Zn contents of 3.8 to 460 mmol kg–1. In acidic soils (n = 24; pH <6.0), Zn was mainly found in the mobile fraction (F1) and the last two fractions (F6 and F7). In neutral soils (n = 25; pH 6.0), most Zn was extracted in the mobilizable fraction (F2) and the intermediate fractions (F4 and F5). The extractability of Zn increased with increasing Zn contamination of the soils. The sum of mobile (F1) and mobilizable (F2) Zn was independent of soil pH, the ratio of Zn in F1 over F1+F2 plotted against soil pH, exhibited the typical shape of a pH sorption edge and markedly increased from pH 6 to pH 5, reflecting the increasing lability of mobilizable Zn with decreasing soil pH. In conclusion, the extractability of Zn from soils contaminated with aqueous Zn after decades of aging under field conditions systematically varied with soil pH and Zn content. The same trends are expected to apply to aqueous Zn released from decomposing Zn-bearing contaminants, such as sewage sludge or smelter slag. The systematic trends in Zn fractionation with varying soil pH and Zn content indicate the paramount effect of these two factors on molecular scale Zn speciation. Further research is required to characterize the link between the fractionation and speciation of Zn and to determine how Zn loading and soil physicochemical properties affect Zn speciation in soils.
机译:我们使用七步顺序萃取程序(F1:NH4NO3; F2:NH4–乙酸盐,pH 6; F3:NH3OHCl,pH 6; F6:NH4NO3),研究了受锌含量和土壤性质影响的49种受污染土壤中锌(Zn)的分离。 F4:NH4-EDTA,pH 4.6; F5:NH4-草酸酯,pH 3; F6:NH4-草酸酯/抗坏血酸,pH 3; F7:残留)。土壤是从不同的地质材料发育而来的,涵盖了广泛的土壤pH(4.0-7.3),有机碳含量(9.3-102 g kg-1)和粘土含量(38-451 g kg-1)。在26至74年间,电力塔中的径流水输入了Zn水溶液,导致土壤总Zn含量为3.8至460 mmol kg-1。在酸性土壤(n = 24; pH <6.0)中,锌主要存在于流动部分(F1)和最后两个部分(F6和F7)中。在中性土壤(n = 25; pH 6.0)中,大部分锌都从可移动部分(F2)和中间部分(F4和F5)中提取。锌的可提取性随着土壤中锌污染的增加而增加。流动性(F1)和可移动性(F2)锌的总和与土壤pH无关,F1中F1 + F2上Zn的比例与土壤pH的关系曲线图显示了典型的pH吸附边缘形状,并且从pH 6显着增加到pH 5,反映了随着土壤pH值的降低,可迁移锌的不稳定性增加。总之,在田间条件下老化数十年后,从被含水锌污染的土壤中提取锌的能力随土壤pH和锌含量的变化而系统地变化。从分解含锌污染物(如污水污泥或冶炼炉渣)中释放出的含水锌,预计也会出现同样的趋势。随着土壤pH和锌含量的变化,锌分离的系统趋势表明,这两个因素对分子尺度的锌形态具有至关重要的作用。需要进一步的研究来表征锌的分离和形态之间的联系,并确定锌含量和土壤理化性质如何影响土壤中锌的形态。

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