Rooney Corinne P, McLaren Ronald G, Condron Leo M
Centre for Soil and Environmental Quality, Agriculture and Life Sciences Division, P.O. Box 84 Lincoln University, Canterbury, New Zealand.
Environ Pollut. 2007 Sep;149(2):149-57. doi: 10.1016/j.envpol.2007.01.009. Epub 2007 Mar 13.
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 (<1mm) 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.
进行了一项培养实验,以评估在一系列土壤pH条件下铅丸的氧化速率以及随后铅向土壤中的转移情况。铅丸腐蚀迅速,因此在几个月内土壤溶液和细土(<1mm)中的铅浓度迅速增加。腐蚀产物以白铅矿(Pb(3)(CO(3))(2)(OH)(2))为主,在单个铅丸周围的硬壳中形成。然而,无论pH值如何,使用WHAM 6模拟的土壤溶液中的Pb(2+)活性都远低于如果由铅丸硬壳材料中存在的主要铅化合物的溶解度控制时的情况。相比之下,再次使用WHAM 6对土壤中铅的固溶相分布进行模拟表明,至少在研究的24个月内,土壤溶液中的铅浓度更可能受土壤固相吸附铅的控制。