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首页> 外文期刊>Water, Air, and Soil Pollution >HEAVY METALS IN VERTICAL PROFILES OF THE MIDDLE ODRA RIVER OVERBANK SEDIMENTS: EVIDENCE FOR POLLUTION CHANGES
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HEAVY METALS IN VERTICAL PROFILES OF THE MIDDLE ODRA RIVER OVERBANK SEDIMENTS: EVIDENCE FOR POLLUTION CHANGES

机译:ODRA河中游沉积物垂直剖面中的重金属:污染变化的证据

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摘要

Heavy metal concentrations were investigated in the overbank sediments in the middle reach of the regulated Odra River, in south-west Poland. Samples of sediments were taken in 20 vertical profiles to a depth of 70 cm at 1-20 cm intervals. Regulation and lateral stability of the river channel for over 150 years enabled to follow the decrease in depth of the Cu and Pb concentration peaks across the floodplain. These peaks were recognised at different depth of the particular profiles: at about 40 cm in the inter-groin infills several meters from a river bank, at 25 cm in the levee at the edge of the floodplain, at several cm in crevasse splays and depressions parallel to flood-protection embankments. These peaks are correlated with maximum Cu and Pb emission and discharge of the mine effluents polluted with heavy metals in the Legnica Copper District at about 1980. Moreover, in profiles localised close to river banks, there are two peaks of Zn concentrations. The upper peak was dated at about 1987 and seems to be associated with the changes in amount of effluents discharged to surface waters in the upper and middle Odra River catchment. The lower one was dated at the first half of the 1940s and can be related to changes in industrial potential and population density after World War Ⅱ. Dates of sediment layers in different vertical profiles show that the highest rate of sediment accretion, 10-20 mm yr~(-1), has occurred in the inter-groin infills. Much lower rate, 3-6 mm yr , has typified the levee on the 3 m-high floodplain and the lowest one, up to 1-2 mm yr~(-1), is found in crevasse splays on the flood plain.
机译:在波兰西南部受管制的奥德拉河中游的过岸沉积物中调查了重金属浓度。在20个垂直剖面中以1-20 cm的间隔采集深度为70 cm的沉积物样品。 150多年来,河道的调节和横向稳定性使洪泛区铜和铅浓度峰值的深度减小。这些峰在特定剖面的不同深度处被识别:在距河岸几米的腹股沟间填充物约40 cm,在洪泛区边缘的堤防中约25 cm,在裂缝裂缝和凹陷处约数cm与防洪堤平行。这些峰值与Legnica铜区约1980年的重金属污染的矿山废水中最大的Cu和Pb排放量和排放量有关。此外,在靠近河岸的剖面中,有两个Zn浓度峰值。最高峰的日期约在1987年,似乎与奥德河上游和中流域地表水排放量的变化有关。较低的日期是在1940年代上半叶,可能与第二次世界大战后工业潜力和人口密度的变化有关。不同垂直剖面上的沉积物层日期显示,在腹股沟间填充物中出现了最高的沉积物沉积速率,为10-20 mm yr〜(-1)。低得多的比率是3-6毫米yr,代表了高3 m的洪泛区的堤防,而最低的比率是高达1-2 mm yr〜(-1),发生在洪泛平原的裂隙中。

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