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百年来受水坝修建和人为污染影响,河漫滩湖泊中沉积磷形态和微量元素的变化。

Centurial changes in sedimentary phosphorus forms and trace elements in response to damming and anthropogenic pollution in a floodplain lake, central China.

机构信息

Hubei Key Laboratory of Critical Zone Evolution, School of Geography and Information Engineering, China University of Geosciences, Wuhan, 430078, China.

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

出版信息

Environ Sci Pollut Res Int. 2022 Apr;29(19):28446-28457. doi: 10.1007/s11356-021-18476-1. Epub 2022 Jan 6.

Abstract

A massive increase in dam construction has decreased fluvial sediment discharge at a global scale. In order to explore potential effects of the Three Gorges Dam (TGD) on floodplain lakes in the middle Yangtze reaches (central China), this study investigated phosphorus forms (i.e., Ca-bound phosphorus, Fe/Al-bound phosphorus, and organic phosphorus) and trace elements (i.e., Sc, Ba, Be, Pb, and Zn) in a Pb-dated sediment core collected from East Dongting Lake, a hydrologically open lake proximal to the TGD. Sedimentary records revealed that the fluxes of phosphorus in different forms and trace elements were high before 2005. Thereafter, the fluxes of Ca-bound phosphorus, Sc, Ba, and Be declined sharply, probably due to declining supply of riverine detritus from the upstream after the TGD operation. In contrast, the fluxes of Fe/Al-bound phosphorus and heavy metals remained high after 2005, indicating the impacts of industrial sewage inputs. Our results underscore that river damming and anthropogenic pollution have altered sedimentary geochemical composition in East Dongting Lake. This phenomenon might be widespread in similar floodplain lakes due to increasing human disturbance during recent decades.

摘要

大坝建设的大规模增加已经减少了全球范围内的河流泥沙输送。为了探讨三峡大坝(TGD)对长江中游(中国中部)漫滩湖泊的潜在影响,本研究调查了东洞庭湖一个 Pb 定年沉积物柱中的磷形态(即 Ca 结合磷、Fe/Al 结合磷和有机磷)和微量元素(即 Sc、Ba、Be、Pb 和 Zn)。沉积记录显示,2005 年以前不同形态磷和微量元素的通量都很高。此后,Ca 结合磷、Sc、Ba 和 Be 的通量急剧下降,可能是由于 TGD 运行后上游河流碎屑供应减少所致。相比之下,2005 年后 Fe/Al 结合磷和重金属的通量仍然很高,表明工业污水输入的影响。我们的结果强调了筑坝和人为污染已经改变了东洞庭湖的沉积地球化学组成。由于近几十年来人类干扰的增加,这种现象可能在类似的漫滩湖泊中广泛存在。

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