The study on an element composition and influencing factors of total suspended matter in the Changjiang Estuary and its adjacent areas

SHAO Hebin; FAN Dejiang; ZHANG Jing; LI Qing

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SHAO Hebin, FAN Dejiang, ZHANG Jing, LI Qing. The study on an element composition and influencing factors of total suspended matter in the Changjiang Estuary and its adjacent areas[J]. Haiyang Xuebao, 2013, 35(6): 54-66.

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The study on an element composition and influencing factors of total suspended matter in the Changjiang Estuary and its adjacent areas

1.
Key Laboratory of Submarine Geosciences and Prospecting Technology of Ministry of Education, China College of Marine Geosciences, Ocean University of China, Qingdao 266100, China;Marine Oil and Gas and Environment Geology Key Laboratory of the Ministry of Land and Natural Resources, Qingdao 266071, China;Qingdao Institute of Marine Geology, Ministry of Land and Natural Resources, Qingdao 266071, China
2.
Key Laboratory of Submarine Geosciences and Prospecting Technology of Ministry of Education, China College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
3.
Marine Oil and Gas and Environment Geology Key Laboratory of the Ministry of Land and Natural Resources, Qingdao 266071, China;Qingdao Institute of Marine Geology, Ministry of Land and Natural Resources, Qingdao 266071, China

Received Date: 2012-09-02

Abstract

Abstract

Water samples and Conductance, Temperature, Depth (CTD) data have been collected through the Public Cruise of the National Research Foundation Committee, in October, 2010.After filtering of the water samples, the total suspended matter (TSM) has been obtained.The concentration of the main and trace elements of TSM has been tested using ICP-AES and ICP-MS, meanwhile an elementary composition, a spacial distribution as well as their influencing factors had also been studied.The results show that the value of main elements (aluminium, magnesium, ion, calcium) concentration between 1% and 30% and aluminium is the highest; the values of the trace elements(cadmium, chromium, cobalt, copper, manganese, nickel, lead, vanadium) concentration are between n×10^-6 and n×10^-9 and manganese is the highest.The good relationships among aluminium, ion, magnesium and most trace elements indicate that the main elements are terrigenous and the trace elements are adsorbed on the land-based suspended particles.The water masses play an important role in the elementary composition of TSM, especially aluminium, ion and chromium, cobalt, copper, manganese, nickel, vanadium.
- Changjiang Estuary,
- suspended matter,
- element composition,
- geochemistry,
- water mass

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References(39)

References

孟诩, 刘苍字.长江口区沉积地球化学特征的定量研究[J].华东师范大学学报:自然科学版, 1996, 12 (1) : 73-84

陈吉余.中国河口海岸研究回顾与展望[J].华东师范大学学报:自然科学版, 1996, 96 (1) : 1-5.

傅瑞标, 孙振斌, 何青, 等.长江口重金属元素的研究现状[J], 上海水利, 1998, 98 (2) : 35-38.

Figueres G, Martin J M, Meybeck M.Iron behavior in the Zaire esuary[J].Neth J Sea Res, 1978 (12) : 329-337

Roussiez V, Ludwig W, Radakovitch O, et al.Fate of metals in coastal sediments of a Mediterranean food-dominated system: An approach based on total and labile fractions[J].Estuarine, Coastal and Shelf Science, 2011, 92 (3) : 486-495.

Adamo P, Arienzo M, Imperato M, et al.Distribution and partition of heavy metals in surface and sub-surface sediments of Naples city port[J].Chemosphere, 2005, 61 (6) : 800-809.

Caplat C, Texier H, Barillier D, et al.Heavy metals mobility in harbour contaminated sediments: The case of Port-en-Bessin[J].Mar Pollut Bull, 2005, 50 (5) : 504-511.

Fukue M, Yanai M, Sato Y, et al.Background values for evaluation of heavy metal contamination in sediments[J].Hazard Mater, 2006, 136 (1) : 111-119.

陈宗团, 徐立, 洪华生.河口沉积物-水界面重金属生物地球化学研究进展[J].地球科学进展, 1997, 12 (5) : 434-439.

黄小平, 李向东, 岳维忠, 等.深圳湾沉积物中重金属污染累积过程[J].环境科学, 2003, 24 (4) : 144-149

Masahiro Suzumura, Haruyo Kokubun, Nao Arata.Distribution and characteristics of suspended particulate matter in a heavily eutrophic estuary, Tokyo Bay, Japan[J].Marine Pollution Bulletin, 2004, 49 (5/6) : 496-503.

Lartiges B S, Deneux-Mustin S, Villemin G, et al.Composition, structure and Size sistribution of suspended particulates from the Rhine River[J].Wat.Res., 2001, 35 (3) : 808-816.

John Zwolsman J G, Gijsbertus.Van Eck T M.Geochemistry of major elements and trace metals in suspended matter of the Scheldt estuary, southwest Netherlands[J].Marine Chemistry, 1999, 66 (1/2) :91-111.

秦蕴珊, 李凡, 徐善民, 等.南黄海海水中悬浮体的研究[J].海洋与湖沼, 1989, 20 (2) : 101-112

杨作升.黄河、长江、珠江沉积物中粘土的矿物组合、化学特征及其物源区气候环境的关系[J].海洋与湖沼, 1988, 19 (4) : 336-346.

郭志刚, 杨作升, 范德江, 等.长江口泥质区的季节性沉积效应[J].地理学报, 2003, 58 (4) : 591-597.

孙效功, 方明, 黄伟, 等.黄、东海陆架区悬浮体输运的时空变化规律[J].海洋与湖沼, 2000, 31 (6) : 581-587.

李道季.长江河口悬浮颗粒物的研究[J].海洋与湖沼, 2000, 31 (3) : 295-301

黄海军, 李凡, 张秀荣.长江黄河水沙特征初步对比分析[J].海洋科学集刊, 2004.469 (00) : 79-90.

邵和宾, 范德江, 张晶, 等.三峡大坝启用后长江口及其邻近海域悬浮体、叶绿素的分布及其影响因素研究[J].中国海洋大学学报:自然科学版, 2012, 42 (5) : 94-104.

苏育嵩.黄、东海地理环境与环流系统分析[J].青岛海洋大学学报:自然科学版, 1989, 19 (1) : 145-158.

李铁刚, 常凤鸣.冲绳海槽古海洋学[M].北京:海洋出版社, 2009:10-13.

李云海, 杨作升.东北太平洋中国合同区悬浮颗粒物元素地球化学[J], 海洋地质与第四纪地质, 2008, 28 (5) : 45-53.

Fan D J, Neuser R D, Sun X G, et al.Authigenic iron oxide formation in the estuarine mixing zone of the Yangtze River[J].Geo-Mar Lett, 2008, 28: 7-14.

苏育嵩.黄东海地理条件概况、环流系统与中心渔场[J].山东海洋学院学报, 1986, 16 (1) :12-27.

郭志刚, 杨作升, 雷坤, 等.东海陆架北部泥质沉积动力过程的季节性变化规律[J].青岛海洋大学学报, 1999, 29 (3) : 507-513.

Su Jilan.A review of circulation dynamics of the coastal oceans near China.Acta Oceanologica Sinica[J].2001, 23 (4) : 1-16.

Saito Y, Yang Z S.Historical change of the Huanghe (Yellow River) and its impact on the sediment budget of the East China Sea[M]// ISEKI K, TSUNOGAI S, eds.Proceedings of International Symposium on Global Fluxes of Carbon and its Related Substances in the Coastal-Ocean-Atmosphere System.Sapporo: Hokkaido University, 1994: 7-12.

杨作升.黄河长江、珠江沉积物中粘土的矿物组合、化学特征及其物源区气候环境的关系[J].海洋与湖沼, 1988, 19 (4) : 336-346.

郭志刚, 杨作升, 曲艳慧, 等.东海陆架泥质区沉积地球化学比较研究[J].沉积学报, 2000, 18 (2) : 284-289.

Shen H T, Li J F, Zhu H F, et a1.Transport of the suspended sediments in the Changjiang Estuary[M]// Proceeding of International Symposium on the Sediment Action on the Continental Shelf with Special Reference to the East China Sea.Beijing: China Ocean Press, 1983: 389-399.

Xie Q C, Zhang L F, Zhou F G, et al.Features and transportation of suspended matter over the continental shelf off the Changjiang Estuary[M]// Proceeding of International Symposium on the Sedimentation on the Continental Shelf, with Special Reference to the East China Sea.Beijing: China Ocean Press, 1983: 400-412.

Milliman J D, Shen H T, Yang Z S, et al.Transport and deposition of river sediment in the Changjiang Estuary and adjacent continental shelf[J].Continental Shelf Research, 1985, (1/2) : 37-45.

Milliman J D, Qin Y S, Park Y A.Sediments and sedimentary processes in the Yellow and East China Sea[M]// I A Masuda F (ed.) Sedimentary Facies in the Active Plate Margin.Tokyo: Terra Scientific Publishing Company, 1989:233-249.

周伟华, 袁翔城, 霍文毅, 等.长江口邻域叶绿素a和初级生产力的分布[J].海洋学报, 2004, 26 (3) : 143-150.

赵保仁.长江口外的上升流现象[J].海洋学报, 1993, 15 (2) : 108-114.

Gao L, Li D, Ding P.Variation of nutrients in response to the highly dynamic suspended particulate matter in the Changjiang (Yangtze River) plume[J].Continental Shelf Research, 2008, 28 (17) : 2393-2403.

岳金萍, 李铁.黄、东海及胶州湾秋季浮游植物部分主要成分和金属元素组成的研究[D].青岛:中国海洋大学, 2012.

王宏鉴, 李铁.黄、东海悬浮颗粒物中金属元素化学组成研究[D].青岛:中国海洋大学, 2011.

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