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Assessment of sediment and porewater after one year of subaqueous capping of contaminated sediments in Hamilton Harbour, Canada

机译:在加拿大汉密尔顿港对被污染的沉积物进行水下水下封盖一年后,评估沉积物和孔隙水

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In this manuscript, we present data from a demonstration in situ capping site (100 m x 100 m) in Hamilton Harbour, Lake Ontario, Canada. A layer of clean medium to coarse sand with the average thickness of 35 cm was placed at the site in the summer of 1995. Concentration of Zn, Cr, and Cd in the original sediments reached values over 6000, 300 and 15 mu g/g, respectively. The predicted consolidation of the uppermost one meter of sediment was about 14 cm, which was in good agreement with values obtained from comparisons of moisture content values of pre-capping and post-capping cores. A thin layer of fresh moderately contaminated sediments has started to develop on the top of the cap. In general, the concentrations of elements were greater in porewater than in the overlying water, e.g., the concentration of Fe and soluble reactive phosphorus were 1000 times, and those of Mn 100 times greater. There was a significant reduction in the vertical fluxes of all the trace elements after the capping of the contaminated sediments. (C) 1998 IAWQ. Published by Elsevier Science Ltd. [References: 17]
机译:在这份手稿中,我们提供了加拿大安大略湖汉密尔顿港一个示范性封盖现场(100 m x 100 m)的数据。 1995年夏季,在现场放置了一层清洁的中等至粗砂,平均厚度为35 cm。原始沉积物中的Zn,Cr和Cd浓度达到6000、300和15μg / g以上的值, 分别。最高的一米沉积物的预计固结约为14厘米,这与从封顶前和封顶后岩心的水分含量值比较中获得的值非常吻合。盖子顶部开始形成一层薄薄的新鲜,中等污染的沉积物。通常,孔隙水中的元素浓度比上覆水中的要高,例如,Fe和可溶性活性磷的浓度是1000倍,Mn的浓度是100倍。污染的沉积物封盖后,所有微量元素的垂直通量显着降低。 (C)1998 IAWQ。由Elsevier Science Ltd.发布[参考:17]

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