A century-long trend of metal pollution in the Sheyang River,on the coast of Jiangsu (China), reconstructed from sedimentary record |
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Authors: | Shanshan Wu Hao Yang Qiaojia Wang Fengzhi Bi Yanhua Wang |
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Institution: | 1. School of Geographical Science, Nanjing Normal University, Nanjing, People’s Republic of China;2. Jiangsu Provincial Key Laboratory of Materials Cycling and Pollution Control, Nanjing, People’s Republic of China;3. Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application, Nanjing Normal University, Nanjing, People’s Republic of China;4. Key Laboratory of Virtual Geographic Environment, Nanjing Normal University, Ministry of Education, Nanjing, Jiangsu, People’s Republic of China;5. State Key Laboratory Cultivation Base of Geographical Environment Evolution, Nanjing, People’s Republic of China |
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Abstract: | In order to reveal the historical context of metal element accumulation under the economic boom during the last decades in eastern China, concentrations of nine metal elements, radionuclides (210Pb), Pb isotope ratios (207Pb/206Pb) and sedimentary characteristics were investigated in two sediment cores collected from the Sheyang River. The sediments have recorded the heavy metal deposition and thus allow establishing a connection between the temporal evolution of the heavy metal pollution and historical changes in industrial and urban discharges. Enrichment factors (EFs) were calculated to estimate the level of contamination in these sediments. A significant anthropogenic enrichment of Cu, Ni, Pb, Cr and Zn was highlighted, which were identified from anthropogenic discharges from cities and industrial sources, according to a cluster analysis. According to the annual variation in GDP growth rate, industrial growth rate, ratio of 207Pb/206Pb and EFs, it was obvious that sedimentary accumulation of metals has a close relationship with anthropogenic activities. In the pre-industrial period, natural inputs prevailed with lower EF and constant 207Pb/206Pb ratios around 0.82. However, during 1980–1995, the rapid industrial development caused a gradual increase in EFs and 207Pb/206Pb (>0.83). Our results disinterred the evolution of anthropogenic metal inputs in the last century into the Sheyang River. |
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Keywords: | Metal element enrichment factor 210Pb Pb isotopes sedimentary geochronology Sheyang River |
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