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Heavy Metal Contamination in the Surface Layer of Bottom Sediments in a Flow-Through Lake: A Case Study of Lake Symsar in Northern Poland

机译:直通湖泊底部沉积物表层的重金属污染:以波兰北部Symsar湖为例

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River-lake systems most often behave as hydrographic units, which undergo complex interactions, especially in the contact zone. One such interaction pertains to the role of a river in the dispersal of trace elements carried into and out of a lake. In this study, we aimed to assess the impact of rivers on the accumulation of heavy metals in bottom sediments of natural lakes comprised in postglacial river-lake systems. The results showed that a river flowing through a lake is a key factor responsible for the input of the majority of available fraction of heavy metals (Zn, Mn, Cd and Ni) into the water body and for their accumulation along the flow of river water in the lake. The origin of other accumulated elements were the linear and point sources in catchments. In turn, the Pb content was associated with the location of roads in the direct catchment, while the sediment structure (especially size of fraction and density) could have affected the accumulation of Cr and Zn, which indicated correlations between these metals and fine fraction. Our results suggest that lakes act as filters and contribute to the self-purification of water that flows through them. As a result, the content of most metals in lake sediments showed a decrease by approx. 75% between the upstream (inflow) and downstream (outflow) sections. The increased content of two metals only, such as chromium and cadmium (higher by 2.0 and 2.5 times, respectively, after passing through the lake), was due to the correlation of the metals with fine sand. Both the content and distribution pattern of heavy metals in lake sediments are indicative of the natural response of aquatic ecosystems to environmental stressors, such as pollutant import with river water or climate change. The complex elements creating the water ecosystem of each lake can counteract stress by temporarily removing pollutants such as toxic metals form circulation and depositing them mostly around the delta.
机译:河湖系统最常表现为水文单位,它们会经历复杂的相互作用,尤其是在接触区。一种这样的相互作用涉及河流在分散进出湖泊的微量元素中的作用。在这项研究中,我们旨在评估河流对冰川后河床系统所包含的天然湖泊底部沉积物中重金属积累的影响。结果表明,流经湖泊的河流是导致大部分可用重金属(锌,锰,镉和镍)输入水体并沿河水积累的重要因素。在湖里。其他累积元素的起源是流域的线性和点源。反过来,铅的含量与直接集水区中道路的位置有关,而沉积物的结构(尤其是分数的大小和密度)可能会影响Cr和Zn的积累,这表明这些金属与精细分数之间存在相关性。我们的结果表明,湖泊可以充当过滤器,并有助于流经湖泊的水的自净。结果,湖泊沉积物中大多数金属的含量下降了约。上游(流入)部分和下游(流出)部分之间为75%。仅两种金属(例如铬和镉)的含量增加(穿过湖泊后分别增加了2.0倍和2.5倍),这是由于这些金属与细砂的相关性所致。湖泊沉积物中重金属的含量和分布方式都表明了水生生态系统对环境压力的自然反应,例如随着河水或气候变化的污染物进口。形成每个湖泊水生态系统的复杂元素可以通过暂时清除循环中的有毒金属等污染物并将其主要沉积在三角洲周围而抵消压力。

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