Fachgebiet Bodenchemie mit Pedologie, Institut für Bodenkunde und Standortslehre, Universität Hohenheim, 70593, Stuttgart, Germany.
Fachgebiet Boden- und Grundwassermanagement, Institut für Grundbau, Abfall- und Wasserwesen, Fakultät für Architektur und Bauingenieurwesen, Bergische Universität Wuppertal, Pauluskirchstr. 7, 42285, Wuppertal, Germany.
Environ Geochem Health. 2017 Dec;39(6):1291-1304. doi: 10.1007/s10653-017-9988-4. Epub 2017 May 24.
European floodplain soils are frequently contaminated with potentially toxic inorganic substances. We used a multi-surface model to estimate the aqueous concentrations of Cd, Cu, Ni, Pb and Zn in three Mollic Fluvisols from the Central Elbe River (Germany). The model considered complexation in solution and interactions with soil organic matter (SOM), a clay mineral and hydrous Al, Fe and Mn oxides. The amounts of reactive metals were derived from extraction with 0.43 M HNO. Modelling was carried out as a function of pH (soil pH ± 1.4) because it varies in floodplain soils owing to redox processes that consume or release protons. The fraction of reactive metals, which were dissolved according to the modelling, was predominantly <1%. Depending on soil properties, especially pH and contents of SOM and minerals of the clay fraction, the modelled concentrations partially exceeded the trigger values for the soil-groundwater pathway of the German soil legislation. This differentiation by soil properties was given for Ni, Pb and Zn. On the other hand, Cd was more mobile, i.e., the trigger values were mostly exceeded. Copper represented the opposite, as the modelling did not predict exceeding the trigger values in any horizon. Except for Pb and partially Zn (where oxides were more important), SOM was the most important adsorbent for metals. However, given the special composition and dynamics of SOM in mollic horizons, we suggest further quantitative and qualitative investigations on SOM and on its interaction with metals to improve the prediction of contaminant dynamics.
欧洲洪泛区土壤经常受到潜在有毒无机物质的污染。我们使用多表面模型来估算来自易北河中部(德国)的三种软土中 Cd、Cu、Ni、Pb 和 Zn 的水相浓度。该模型考虑了溶液中的络合作用以及与土壤有机质(SOM)、粘土矿物和水合 Al、Fe 和 Mn 氧化物的相互作用。反应性金属的数量是根据 0.43 M HNO3 的提取得出的。建模是作为 pH 的函数进行的(土壤 pH ± 1.4),因为由于消耗或释放质子的氧化还原过程,洪泛区土壤中的 pH 值会发生变化。根据建模溶解的反应性金属部分 <1%。取决于土壤特性,特别是 pH 值以及 SOM 和粘土部分矿物的含量,模型预测的浓度部分超过了德国土壤法规中土壤-地下水途径的触发值。这种由土壤特性引起的分化适用于 Ni、Pb 和 Zn。另一方面,Cd 更具迁移性,即触发值大多被超过。铜则相反,因为在任何层次上建模都没有预测超过触发值。除了 Pb 和部分 Zn(其中氧化物更为重要)外,SOM 是金属的最重要吸附剂。然而,鉴于 SOM 在软土层中的特殊组成和动态,我们建议对 SOM 及其与金属的相互作用进行进一步的定量和定性研究,以提高污染物动态的预测能力。