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大坝建设和污染物增加对长江泛滥平原浅水湖泊生态水文学演变的影响。

Effects of dam construction and increasing pollutants on the ecohydrological evolution of a shallow freshwater lake in the Yangtze floodplain.

机构信息

School of Geography, University of Nottingham, Nottingham NG7 2RD, UK; State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan 430074, China.

School of Geography, University of Nottingham, Nottingham NG7 2RD, UK.

出版信息

Sci Total Environ. 2018 Apr 15;621:219-227. doi: 10.1016/j.scitotenv.2017.11.181. Epub 2017 Nov 24.

Abstract

Large river-floodplain systems which provide a variety of societal, economic and biological benefits are undergoing extensive and intensive human disturbance. However, floodplain lakes responses to multiple stressors are poorly understood. The Yangtze River and its floodplain which provide water and food resources for more than 300 million people are an important region in China. Hydrological regulation as well as socio-economic development have brought profound negative influence on this ecologically important area. To improve understanding of decadal-scale responses of floodplain lakes to multiple stressors, lake sediment proxies including particle size, geochemical elements, diatoms and chironomids were analysed in a lead-210 dated core from Futou Lake. The analyses show that dams constructed in 1935 and the early 1970s stabilized hydrological conditions in Futou Lake and impeded the interaction with the Yangtze River, resulting in a decrease in major elements (e.g., Mg, Al, Fe) transported into the lake and an increase of macrophyte-related chironomids (C. sylvestris-type, P. penicillatus-type and Paratanytarsus sp.). After the late 1990s, further decreases in major elements and increases in median grain size are attributed to the erosion of the Yangtze riverbed and declining supply of major elements-enriched sediments from the upper Yangtze caused by the impoundment of the Three Gorges Dam. Chironomid and diatom assemblages indicate that hydrological stabilization caused by dam constructions stimulated the growth of macrophytes, which may be important in buffering against an ecosystem state change towards a phytoplankton-dominated and turbid state with ongoing eutrophication. However, a recent increase in Zn, TP and the emergence of eutrophic diatom and chironomid species indicate initial signs of water quality deterioration which may be related to the combined effects of hydrological stabilization and aquaculture. Over all, the sediment record from Futou Lake emphasizes the importance of interactions between hydrological change and pollutant loads in determining floodplain lake ecosystem state.

摘要

为长江流域及长江中下游平原约 3 亿人民提供了水源和食物资源的长江及其冲积平原是中国的一个重要区域。然而,由于水文调节以及社会经济发展,该生态重要区域正受到广泛而深入的人为干扰。为了提高对长江中下游平原湖泊对多种胁迫因素的年代际响应的认识,本研究在一个有 210Pb 测年的浮头湖钻孔中,分析了粒度、地球化学元素、硅藻和摇蚊等湖泊沉积物代用指标。研究结果表明,1935 年和 20 世纪 70 年代初修建的水坝稳定了浮头湖的水文条件,阻碍了其与长江的相互作用,导致大量进入湖泊的主要元素(如 Mg、Al、Fe)减少,与大型植物相关的摇蚊(C. sylvestris 型、P. penicillatus 型和 Paratanytarsus sp.)增加。20 世纪 90 年代末以后,主要元素的进一步减少和中值粒径的增加归因于长江河床的侵蚀以及三峡大坝蓄水导致来自长江上游的富含主要元素的沉积物供应减少。摇蚊和硅藻组合表明,大坝建设引起的水文稳定刺激了大型植物的生长,这对于缓冲湖泊生态系统向富营养化导致的浮游植物占主导地位和浑浊状态的转变可能很重要。然而,Zn、TP 的增加以及富营养硅藻和摇蚊种类的出现表明水质恶化的初步迹象,这可能与水文稳定和水产养殖的综合影响有关。总的来说,浮头湖的沉积物记录强调了水文变化和污染物负荷之间的相互作用在决定冲积平原湖泊生态系统状态方面的重要性。

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