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SPECIATION OF Pb IN INDUSTRIALLY POLLUTED SOILS

机译:工业污染土壤中铅的形态

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This study was aimed at elucidating the importance of original Pb-speciation versus soil-characteristics to mobility and distribution of Pb in industrially polluted soils. Ten industrially polluted Danish surface soils were characterized and Pb speciation was evaluated through SEM-EDX studies, examination of pH-dependent desorption, distribution in grain-size fractions and sequential extraction. Our results show that the first factors determining the speciation of Pb in soil are: (1) the stability of the original speciation and (2) the contamination level, while soil characteristics are of secondary importance. In nine of ten soils Pb was concentrated strongly in the soil fines (< 0.063 mm). In all soils, particles with a highly concentrated Pb-content were observed during SEM-EDX. In eight of the soils, the particles contained various Pb-species with aluminum/iron, phosphate, sulfate and various metals (in solder and other alloys) as important associates. In the one soil, where Pb was not concentrated in the soil fines, Pb was precipitated solely as PbCrO_4, while pure (metallic) Pb was repeatedly observed in the last soil. Pb was bound strongly to the soils with >50% extracted in step Ⅲ (oxidizing) and Ⅳ (residual) of sequential extraction for all soils but one. A significant amount of exchangeable Pb existed only in severely contaminated soils, where the bonding capacity of organic matter and oxides was exceeded. Among soil constituents, Pb was observed to adsorb preferentially to feldspars and organic matter while presence of phosphate increased the strength of the Pb-bonding in phosphate-rich soils.
机译:这项研究旨在阐明原始铅形态与土壤特征对工业污染土壤中铅的迁移和分布的重要性。对十种工业污染的丹麦表层土壤进行了表征,并通过SEM-EDX研究,pH依赖的解吸检查,粒度级分的分布和顺序萃取对铅的形态进行了评估。我们的结果表明,决定土壤中Pb形态的首要因素是:(1)原始形态的稳定性和(2)污染水平,而土壤特性次要。在十个土壤中的九个中,Pb集中在土壤细粉中(<0.063 mm)。在所有土壤中,SEM-EDX期间都观察到了高浓度Pb含量的颗粒。在八种土壤中,这些颗粒包含各种Pb物种,其中铝/铁,磷酸盐,硫酸盐和各种金属(在焊料和其他合金中)是重要的缔合物。在一种Pb不集中在土壤细粉中的土壤中,Pb仅以PbCrO_4的形式沉淀,而在最后一种土壤中反复观察到纯(金属)Pb。铅与土壤牢固结合,对于除一种土壤外的所有土壤,在步骤Ⅲ(氧化)和Ⅳ(残余)中依次提取的> 50%。仅在严重污染的土壤中存在大量可交换的Pb,那里的有机物和氧化物的结合能力超过了。在土壤成分中,观察到Pb优先吸附到长石和有机质上,而磷酸盐的存在则增加了富含磷酸盐的土壤中Pb结合的强度。

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