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The effect of catchment soils on heavy metal concentrations in a brook situated in the historic mining region of Braubach, Germany

机译:在德国布劳巴赫历史悠久的采矿区中的一条小溪中,集水区土壤对重金属浓度的影响

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Forest soils located in the region of Braubach (Rhineland-Palatinate, Germany) are characterized by elevated concentrations of cadmium (Cd), copper (Cu), and lead (Pb), resulting from local heavy metal emissions. The regional geomorphology is dominated by the low mountain range of the Rhenish Massif and the frequent occurrence of V-shaped valleys crossed by small tributaries of the Rhine River. The frequent occurrence of steep valley slopes should theoretically facilitate the influence of polluted forest soils on brooks of the valley bottoms by intensified processes of slope water influx and soil erosion. To investigate pollution state and soil-water interactions in a heavy metal enriched catchment, concentrations of Cd, Cu, and Pb were determined for catchment soils, sediment, suspended matter, and surface water of a brook situated close to a former smelter area. Heavy metal binding was characterized by BCR sequential extraction method. Total concentrations of Cd increased with the transition from catchment soils to brook sediments and suspended matter, while the proportions of the analyzed binding fractions partially changed. The concentrations of Cu and Pb in soils were marked by a higher heterogeneity and exceeded the concentrations found in sediments and suspended matter. For Pb, the proportions of binding fractions were relatively static, whereas the Cu binding fractions in suspended matter clearly differed in comparison with soils and sediments. For all studied heavy metals, an increase in the concentration of the respective dissolved fraction was found along the course of the brook.
机译:位于布劳巴赫地区(莱茵兰-普法尔茨州,德国)的森林土壤的特征在于局部重金属的排放导致镉(Cd),铜(Cu)和铅(Pb)的浓度升高。该地区的地貌学主要由莱茵山脉的低山山脉和莱茵河的小支流交叉形成的V形山谷所致。从理论上讲,频繁发生的陡峭山谷坡应通过加剧坡面水涌入和水土流失的过程来促进受污染的森林土壤对山谷底部溪流的影响。为了调查富集重金属的流域的污染状态和土壤-水之间的相互作用,确定了靠近原冶炼厂区域的一条流域土壤,沉积物,悬浮物和地表水的镉,铜和铅的浓度。重金属结合通过BCR顺序萃取法进行了表征。 Cd的总浓度随着从集水区土壤到溪沉积物和悬浮物的过渡而增加,而分析的结合部分的比例则部分改变。土壤中铜和铅的浓度具有较高的异质性,超过了沉积物和悬浮物中的浓度。对于Pb,结合部分的比例相对固定,而悬浮物质中的Cu结合部分与土壤和沉积物相比明显不同。对于所有研究的重金属,沿着溪流的过程发现各自溶解部分的浓度增加。

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