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Does soil water saturation mobilize metals from riparian soils to adjacent surface water? A field monitoring study in a metal contaminated region

机译:土壤含水饱和度是否能将金属从河岸土壤迁移到邻近的地表水?金属污染区域的现场监测研究

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In the Noorderkempen (NW Belgium), a large area (about 280 km~2) is contaminated with cadmium (Cd) and zinc (Zn) due to historical pollution by the Zn smelters. Direct aquatic emissions of metals have diminished over time, however the surface water metal concentration largely exceeds quality standards, mainly during winter periods. Monitoring data were analyzed to reveal whether these fluctuations are related to seasonal redox reactions in associated contaminated riparian soils that drain into the rivers. A field survey was set up with soil pore-water and groundwater monitored for three years in transects of soil monitoring points perpendicular to rivers at contaminated and non-contaminated sites. Site averaged surface water concentrations of a 15 year dataset exceeded local quality standards 4 to 200-fold. Winter averaged metal concentrations significantly exceeded the corresponding summer values 1.3-1.8 (Zn) and 1.5-2.4 fold (Cd). Zinc and Cd concentrations in water were positively related to Fe and Mn but not to Ca, K or Na suggesting that redox reactions and not dilution processes are involved. In ground- and pore-water of the associated riparian soils, the concentrations of Zn fluctuate by the same order of magnitude as in surface water but were generally smaller than in the corresponding contaminated rivers. In addition, correlations of dissolved Zn with Fe and Mn were lacking. This analysis suggests that redox reactions in streams, and not in riparian soils, explain the seasonal trends of Zn and Cd in surface water. Hence, river sediments and not riparian soils may be the cause of the winter peaks of Zn and Cd in these rivers.
机译:在Noorderkempen(比利时西北部),由于锌冶炼厂的历史性污染,大面积(约280 km〜2)被镉(Cd)和锌(Zn)污染。随着时间的推移,金属的水生直接排放量有所减少,但是主要在冬季,地表水金属的浓度大大超过了质量标准。分析监测数据以揭示这些波动是否与排入河流的相关污染河岸土壤中的季节性氧化还原反应有关。建立了一个野外调查,在垂直于受污染和未受污染地点的河流的土壤监测点的样面中对土壤孔隙水和地下水进行了三年监测。 15年数据集的站点平均地表水浓度超过了当地质量标准的4到200倍。冬季的平均金属浓度大大超过了相应的夏季值1.3-1.8(锌)和1.5-2.4倍(镉)。水中的锌和镉浓度与铁和锰呈正相关,但与钙,钾或钠无正相关,这表明氧化还原反应而不涉及稀释过程。在相关河岸土壤的地下水和孔隙水中,锌的浓度波动与地表水中的数量级相同,但通常小于相应的受污染河流中的锌。另外,缺乏溶解的锌与铁和锰的相关性。该分析表明,溪流而不是河岸土壤中的氧化还原反应解释了地表水中锌和镉的季节性趋势。因此,河流沉积物而不是河岸土壤可能是这些河流中锌和镉冬季峰值的原因。

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