The distribution and enrichment of trace elements in surface and core sediments from the Changjiang River Estuary, China: Evidence for anthropogenic inputs and enhanced availability of rare earth elements (REE)

被引:3
|
作者
Zhang, Xiaoyu [1 ,2 ]
Du, Wen [3 ]
Xu, Zhijie [1 ]
Cundy, Andrew B. [4 ]
Croudace, Ian W. [4 ]
Zhang, Weiyan [5 ,6 ]
Jin, Haiyan [5 ,6 ]
Chen, Jianfang [5 ,6 ]
机构
[1] Zhejiang Univ, Sch Earth Sci, Hangzhou 310027, Peoples R China
[2] Zhejiang Univ, Hainan Inst, Sanya 572000, Peoples R China
[3] South China Univ Technol, Guangzhou 511442, Peoples R China
[4] Univ Southampton, Sch Ocean & Earth Sci, Natl Oceanog Ctr Southampton, GAU Radioanalyt, Southampton SO14 3ZH, England
[5] Minist Nat Resources, State Ocean Adm, Key Lab Marine Ecosyst & Biogeochem, Hangzhou 310012, Peoples R China
[6] Minist Nat Resources, Inst Oceanog 2, Hangzhou 310012, Peoples R China
基金
中国国家自然科学基金;
关键词
Changjiang River Estuary; Trace elements; Elevated content; Anthropogenic input; Availability of REE; PLATINUM-GROUP METALS; YANGTZE-RIVER; HEAVY-METALS; SPATIAL-DISTRIBUTION; MARINE-SEDIMENTS; SEA; WATER; SPECIATION; BARIUM; GEOCHEMISTRY;
D O I
10.1016/j.marpolbul.2023.115082
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Huge amount of trace metals emitted through manmade activities are carried by the Changjiang River into the East China Sea. Most of them deposit in the Changjiang River Estuary and threaten the regional aquatic envi-ronment. In this study, major and trace elements of 34 archive surface sediments and two cores are examined. Sequential extraction procedures were also performed on surface sediments from 12 sites. We found that Tl, Tm, Er show distinct accumulation in surface sediments in the order of Tm > Tl > Er. Particularly, abnormally elevated HREE are observed mainly in those sites near the mouth of the estuary. Most elements exhibit an obvious reduction in the upper 30 cm of core B8, reflecting a decrease of sediment discharge from Changjiang River runoff. The increase of some trace elements recorded in the upper 20 cm of core C3 demonstrates a distinct local anthropogenic input in recent years.
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页数:17
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