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Control of lead solubility in soil contaminated with lead shot: Effect of soil pH

机译:控制铅丸污染的土壤中铅的溶解度:土壤pH的影响

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An incubation experiment was carried out to assess the rate of oxidation of Pb shot and subsequent transfer of Pb to the soil under a range of soil pH conditions. Lead shot corrosion was rapid, so that soil solution and fine earth ( < 1 mm) Pb concentrations increased rapidly within a few months. Corrosion products, dominated by hydrocerussite (Pb_3(CO_3)_2(OH)_2), developed in crusts surrounding individual Pb pellets. However, irrespective of pH, Pb~(2+) activities in the soil solutions, modelled using WHAM 6, were much lower than would be the case if they were controlled by the solubility of the dominant Pb compounds present in the Pb shot crust material. In contrast, modelling of soil solid-solution phase distribution of Pb, again using WHAM 6, suggested that, at least during the 24 months of the study, soil solution Pb concentrations were more likely to be controlled by sorption of Pb by the soil solid phase.
机译:进行了一个温育实验,以评估在一定范围的土壤pH条件下,Pb铅的氧化速率以及随后Pb向土壤的转移速率。铅丸腐蚀很快,因此土壤溶液和细土(<1 mm)中的Pb浓度在几个月内迅速增加。以水陶粒(Pb_3(CO_3)_2(OH)_2)为主的腐蚀产物在单个Pb颗粒周围的地壳中形成。但是,不管pH值如何,使用WHAM 6模拟的土壤溶液中的Pb〜(2+)活性均远低于由Pb抛壳材料中存在的主要Pb化合物的溶解度控制的情况。 。相比之下,再次使用WHAM 6对土壤铅的固溶相分布进行建模表明,至少在研究的24个月内,土壤溶液中铅的浓度更可能受到土壤固体对铅的吸附的控制。相。

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