Historical trends of trace metals in muddy deposit along the Zhejiang coast, East China Sea: response to economic development and hypoxia

© 2017, Springer-Verlag GmbH Germany. One sediment core spanning approximately 138 years was taken from the muddy deposits along the Zhejiang coast of the East China Sea, which is located in a hypoxic zone south of the Yangtze River estuary. When the sources of the trace metals in the core were anal...

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Main Authors: Xu, G., Liu, Jian, Dou, Y., Qiu, J., Chen, L.
Format: Journal Article
Published: Springer 2018
Online Access:http://hdl.handle.net/20.500.11937/71867
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author Xu, G.
Liu, Jian
Dou, Y.
Qiu, J.
Chen, L.
author_facet Xu, G.
Liu, Jian
Dou, Y.
Qiu, J.
Chen, L.
author_sort Xu, G.
building Curtin Institutional Repository
collection Online Access
description © 2017, Springer-Verlag GmbH Germany. One sediment core spanning approximately 138 years was taken from the muddy deposits along the Zhejiang coast of the East China Sea, which is located in a hypoxic zone south of the Yangtze River estuary. When the sources of the trace metals in the core were analyzed, the three geochemical sources were identified as lithogenic, anthropogenic, and reductive deposits based on both principal component analysis and the ratios of terrigenous elements. The temporal distribution of the enrichment factor of copper in the sediment core matches the timeline of economic development and national policy in China. The rapid increase in human activity and economic development in the Yangtze River catchment accounts for the enrichment of copper in the sediment core. Based on the vertical distribution of arsenic concentration, the hypoxic zone south of the Yangtze River estuary may have not only existed, but worsened since 1875.
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institution Curtin University Malaysia
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spelling curtin-20.500.11937-718672018-12-13T09:32:39Z Historical trends of trace metals in muddy deposit along the Zhejiang coast, East China Sea: response to economic development and hypoxia Xu, G. Liu, Jian Dou, Y. Qiu, J. Chen, L. © 2017, Springer-Verlag GmbH Germany. One sediment core spanning approximately 138 years was taken from the muddy deposits along the Zhejiang coast of the East China Sea, which is located in a hypoxic zone south of the Yangtze River estuary. When the sources of the trace metals in the core were analyzed, the three geochemical sources were identified as lithogenic, anthropogenic, and reductive deposits based on both principal component analysis and the ratios of terrigenous elements. The temporal distribution of the enrichment factor of copper in the sediment core matches the timeline of economic development and national policy in China. The rapid increase in human activity and economic development in the Yangtze River catchment accounts for the enrichment of copper in the sediment core. Based on the vertical distribution of arsenic concentration, the hypoxic zone south of the Yangtze River estuary may have not only existed, but worsened since 1875. 2018 Journal Article http://hdl.handle.net/20.500.11937/71867 10.1007/s11356-017-0625-7 Springer restricted
spellingShingle Xu, G.
Liu, Jian
Dou, Y.
Qiu, J.
Chen, L.
Historical trends of trace metals in muddy deposit along the Zhejiang coast, East China Sea: response to economic development and hypoxia
title Historical trends of trace metals in muddy deposit along the Zhejiang coast, East China Sea: response to economic development and hypoxia
title_full Historical trends of trace metals in muddy deposit along the Zhejiang coast, East China Sea: response to economic development and hypoxia
title_fullStr Historical trends of trace metals in muddy deposit along the Zhejiang coast, East China Sea: response to economic development and hypoxia
title_full_unstemmed Historical trends of trace metals in muddy deposit along the Zhejiang coast, East China Sea: response to economic development and hypoxia
title_short Historical trends of trace metals in muddy deposit along the Zhejiang coast, East China Sea: response to economic development and hypoxia
title_sort historical trends of trace metals in muddy deposit along the zhejiang coast, east china sea: response to economic development and hypoxia
url http://hdl.handle.net/20.500.11937/71867