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Sediment-borne Contaminants in Rivers Discharging into the Humber Estuary, UK

机译:河流中的沉积物污染物排入英国的亨伯河口

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As part of a project to characterise and quantify the volume of sediments which comprise the Holocene (10,000 years to present) fill of the Humber Estuary, a study was undertaken to determine the geochemistry and heavy mineralogy of bed sediments in the river systems that discharge into the estuary. A total of 19 sediment samples in the Trent and Ouse river systems were taken for analysis. Contamination was evaluated by comparison of the sample geochemistry with that of the appropriate catchment (using existing data), and by evaluation of the proportion of anthropogenic heavy minerals (including natural minerals which have been mobilised by mining) in the sediment sample. Heavy metals fall into two groups with different patterns of distribution. Pb-Zn concentrations are greatest in catchments and rivers draining the Pennine orefields. Levels of these metals remain high between source areas and the Humber Estuary suggesting that large quantities are trapped in sediments stored within the fluvial systems. By way of contrast other heavy metals, associated with manufacturing industry, such as Cu and Co, have high concentrations near source cities, but decrease rapidly in amount down the river systems because of dilution by other sediments. The differing behaviour of mining and industrial related contaminants is generally reflected by the heavy minerals. Concentrations of gangue minerals, such as barytes and fluorite, are generally highest in rivers draining mining areas; 'furnace' materials, such as slags are highest in industrialised rivers such as the Aire and the Don. The anthropogenic origin of all the contaminants is illustrated by comparison of the catchment and river sediment geochemistry and heavy mineralogy with that of early Holocene fluvially-derived sediments cored in boreholes drilled in the present Humber Estuary. The findings of the study corroborate those of others focused on water chemistry and floodplain sediments (Neal et al., 1996, 1997; Macklin et al., 1997). However, the comparison of pre-existing data on catchment geochemistry with a limited number of river samples, as demonstrated here, provides a fast and cost effective tool for the determination of contamination characteris- tics in river systems.
机译:作为表征和量化包括亨伯河口全新世(迄今10,000年)填充物的沉积物数量的项目的一部分,进行了一项研究,以确定河流系统中向河床排放的河床沉积物的地球化学和重矿物学。河口。在特伦特河和乌斯河系统中总共采集了19个沉积物样本进行分析。通过将样品的地球化学与适当的流域的地球化学进行比较(使用现有数据),并通过评估沉积物中的人为重矿物(包括已开采的天然矿物)的比例来评估污染。重金属分为两种不同的分布模式。铅矿田的流域和河流中铅锌的浓度最高。在源区和亨伯河口之间,这些金属的含量仍然很高,这表明大量金属被困在河流系统内存储的沉积物中。相比之下,与制造业相关的其他重金属,例如Cu和Co,在源城市附近的浓度很高,但是由于其他沉积物的稀释,其在河系中的含量迅速下降。重金属矿物通常反映出采矿和工业相关污染物的不同行为。在流向矿区的河流中,重矿物和萤石等石矿物的浓度通常最高。炉渣等“炉子”材料在艾尔河和唐河等工业化河流中含量最高。通过对流域和河流沉积物地球化学以及重矿物学与目前在亨伯河口钻探的岩心中早期全新世河流相衍生的沉积物进行比较,可以说明所有污染物的人为起源。该研究的结果证实了其他研究的重点是水化学和洪泛区沉积物(Neal等,1996,1997; Macklin等,1997)。但是,如此处所示,将流域地球化学的现有数据与有限数量的河流样本进行比较,为确定河流系统的污染特征提供了一种快速且经济高效的工具。

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