XU Shu-mei, ZHAI Shi-kui, ZHANG Ai-bin, ZHANG Huai-jing, LU Hai-jian. REDOX ENVIRONMENT EFFECT ON THE REDOX SENSITIVE ELEMENTS IN SURFACE SEDIMENTS FROM THE YANGTZE ESTUARY HYPOXIA ZONE[J]. Marine Geology & Quaternary Geology, 2007, 27(3): 1-8.
Citation: XU Shu-mei, ZHAI Shi-kui, ZHANG Ai-bin, ZHANG Huai-jing, LU Hai-jian. REDOX ENVIRONMENT EFFECT ON THE REDOX SENSITIVE ELEMENTS IN SURFACE SEDIMENTS FROM THE YANGTZE ESTUARY HYPOXIA ZONE[J]. Marine Geology & Quaternary Geology, 2007, 27(3): 1-8.
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REDOX ENVIRONMENT EFFECT ON THE REDOX SENSITIVE ELEMENTS IN SURFACE SEDIMENTS FROM THE YANGTZE ESTUARY HYPOXIA ZONE

  • Ocean University of China, Qingdao 266100, China

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  • Received Date: November 08, 2006
  • Revised Date: April 15, 2007
    Graphical Abstract
    • Abstract
  • The grain sizes and element concentration, including redox-sensitive elements(RSE) and terrigenous elements of the sediments from the Yangtze Estuary hypoxia zone and its contiguous sea area were measured. Based on these data,the hypoxic environment's influence on the distribution of elements in surface sediments was studied and it is believed that the "redox environment effect" has important influence on the distribution of the RSE from the Yangtze Estuary hypoxia zone. Redox-sensitive elements Cd,Mo,U,and V and detrophile elements K,Sc and Al belong to different element associations and have distinct distribution and regularity characteristics.These two kinds of elements are controlled by different factors in the study area.Detrophile elements are mainly affected by provenance and "granularity effect",and the high value area goes nearshore in banded way.RSEs(such as Cd,Mo,U,and V)are less controlled by the "granularity effect" but evidently affected by hypoxic environment,and the high value area is distributed in patches and away from the shoreline.
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  • [1]
    王贤觉. 东海大陆架海底沉积物稀土元素地球化学[J]. 地球化学,1982, 1:56-65.[WANG Xian-jue. Geochemistry of sedimentary REE of the East Sea Shelf[J]. Geochemistry,1982

    , 1:56-65.]
    [2]
    李柚霞. 东海陆架沉积物的中子活化分析和地球化学研究[J]. 海洋学报,1986, 8(2):566-572.

    [LI You-xia. The neutron activation analysis and geochemistry research on sediment in East China Sea Shelf[J]. Acta Oecanologica Sinica,1986, 8(2):566-572.]
    [3]
    杨作升. 黄河、长江、珠江沉积物中黏土矿物的组合、化学特征及其与物源区气候的关系[J]. 海洋与湖沼,1988, 19(4):336-346.

    [YANG Zuo-sheng. Clay mineral combination in sediment of the Huanghe, Changjiang and Zhujiang River. chemical characteristic and their relations with climate of resource area[J]. Oceanologia et Limnologia Sinica,1988, 19(4):336-346.]
    [4]
    赵一阳, 鄢明才. 黄河、长江、中国浅海沉积物化学元素丰度比较[J]. 科学通报,1992, 13:1202-1204.[ZHAO Yi-yang, YAN Ming-cai. The comparison of elements concentration in sediment in Huanghe, Changjiang and shallow Sea in China[J]. Chinese Sci. Bull.,1992

    , 13:1202-1204.]
    [5]
    赵一阳, 鄢明才. 中国浅海沉积物地球化学[M]. 北京:科学出版社, 1994.[ZHAO Yi-yang, YAN Ming-cai. The Geochemistry of Sediment in Shallow Sea of China[M]. Beijing:Science Press,1994.]
    [6]
    Gao A G, Cai D L,Gao S L. Geochemical characteristics of the elements in the sediment of the Yangtze Estuary[C]//Proceeding of the Japan-China workship on the cooperative study of the marine environment.Research report from the National Institute of Environmental Studies, Japan.2000, 151:151-158.
    [7]
    王正方. 长江口海域铜的地球化学初步探讨[J]. 地球化学,1990, 1:90-96.[WANG Zheng-fang. Primary research on the geochemistry of Cu in Changjiang Estuary[J]. Geochemistry,1990

    , 1:90-96.]
    [8]
    陈松, 许爱玉, 骆柄坤,等. 长江口表层沉积物中Fe、Mn、Zn、Co、Ni的地球化学特征[J]. 台湾海峡,1987, 6(1):13-18.

    [CHEN Song, XU Ai-yu, LUO Bing-kun. The Geochemistry of Fe,Mn,Zn,Co and Ni in surface sediments in Changjiang Estuary[J]. Journal of Oceanography in Taiwan Strait,1987, 6(1):13-18.]
    [9]
    张经,应时理. 长江口中的颗粒态重金属[M]//中国主要河口的生物地球化学研究.北京:海洋出版社,1996:146-159.[ZHANG Jing, YING Shi-li. Granular Heave Metal in Changjiang Estuary[M]//Bio-geochemistry Research of Primary Estuary in China. Beijing:China Ocean Press,1996:146

    -159.]
    [10]
    赵一阳. 中国海大陆架沉积物地球化学的若干模式[J].地质科学,1983, 4:307-314.[ZHAO Yi-yang. Several geochemistry modes in Chinese sea shelf[J]. Geology Science,1983

    , 4:307-314.]
    [11]
    Adelson J M, Helz G R,Miller C V.Reconstructing the rise of recent coastal anoxia; molybdenum in Chesapeake Bay sediments[J]. Geochim. Cosmochim. Acta,2001, 65:237-252.
    [12]
    Chaillou G, Anschutz P,Lavaux G, et al. The distribution of Mo, U and Cd in relation to major redox species in muddy sediments of the Bay of Biscay[J]. Mar. Chem.,2002, 80:41-59.
    [13]
    Crusius J.Thomson J.Comparative behavior of authigenic Re, U, and Mo during reoxidation and subsequent long-term burial in marine sediments[J]. Geochimica et Cosmochimica Acta,2000,64(13):2233-2242.
    [14]
    Crusius J, Calvert S, Pedersen T, et al.Rhenium and molybdenum enrichments in sediments as indicators of oxic, suboxic and sulfidic conditions of deposition[J]. Earth and Planetary Science Letters,1996, 145:65-78.
    [15]
    Rosenthal Y, Lam P,Boyle E A,et al.Authigenic cadmium enrichments in suboxic sediments:precipitation and post depositional mobility[J]. Earth and Planetary Science Letters,1995, 132:99-111.
    [16]
    Koschinsky A.Heavy metal distributions in Peru Basin surface sediments in relation to historic, present and disturbed redox environments[J]. Deep-Sea Research Ⅱ,2001, 48:3757-3777.
    [17]
    Morford J L,Emeson S.The geochemistry of redox sensitive trace metals in sediments[J]. Geochimica Cosmochimica Acta,1999, 63:1735-1750.
    [18]
    许淑梅, 翟世奎, 张爱滨,等. 长江口外缺氧区及邻近海域氧化还原敏感性微量元素的分布规律及环境指示意义[J]. 沉积学报,2007(待刊).[XU Shu-mei, ZHAI Shi-kui, ZHANG Ai-bin,et al.Distribution and environment significance of redox sensitive elements off the Changjiang Estuary hypoxia zone and its contiguous sea area[J]. Sedimentology, 2007.]
    [19]
    顾宏堪. 黄海溶解氧垂直分布中的最大值[J]. 海洋学报,1980, 2:70-79.[GU Hong-kan. The maximum value of the vertical distribution for dissolved oxygen in Huanghai[J]. Acta Oecanologica Sinica, 1980

    , 2:70-79.]
    [20]
    Limeburner R,Beardsley R C,Zhao J. Water Masses and Circulation in the East China Sea[C]//Proceedings of International Symposium on Sedimentation on the Continental Shelf,with Special Reference to the East China Sea.Beiiing:China Ocean Press,1983:285-294.
    [21]
    陈吉余, 陈祥禄, 杨启伦. 上海海岸带和滩涂资源综合调查报告[C]. 上海:上海科技出版社,1988:114-116.[CHEN Ji-yu, CHEN Xiang-lu, YANG Qi-lun. Investigation Research on the Resources of Sea Shore and Beach of Shanghai[M]. Shanghai:Shanghai Science and Technology Press.1988.]
    [22]
    Tian R C, HU F X,Martin J M.Summer nutrient fronts in the Changjiang (Yangtze River) Estuary[J]. Estuarine, Coastal and Shelf Science,1993, 37:27-41.
    [23]
    李道季, 张经, 黄大吉,等. 长江口外氧亏损[J]. 中国科学D辑,2002, 32:686-694.[LI Dao-ji, ZHANG Jing, HUANG Da-ji,et al.Oxygen depletion off the Changjiang(Yangtze River) estuary[J]. Science in China(Series D),2002

    , 32:686-694.]
    [24]
    许淑梅. 长江口外缺氧区及其邻近海域氧化还原敏感元素的分布规律及环境指示意义[D]. 中国海洋大学博士论文.2005.[XU Shu-mei. The Distribution and Environmental Significance of Redox Sensitive Elements in the Hypoxia Zone of the Changjiang Estuary and its Contiguous Area[D].Doctor Dissertation of Ocean University of China, 2005.]
    [25]
    Emerson S,Huested S S.Ocean anoxia and the concentration of molybdenum in sea water[J]. Mar. Chem.,1991, 34:177-196.
    [26]
    Colodner D, Sachs J,Ravizza G, et al.The geochemical cycle of rhenium:a reconnaissance[J]. Earth and Planetary Science Letters,1993, 117:205-221.
    [27]
    王金土. 黄海表层沉积物稀土元素地球化学[J]. 地球化学,1990, 1:44-53.[WANG Jin-tu. REE geochemistry of surface sediments in Huanghai[J]. Geochemistry,1990

    , 1:44-53.]
    [28]
    业渝光. 现代黄河三角洲ZK226孔岩心210Pb、Al、Fe、Mn和Cu的地球化学[J]. 海洋地质与第四纪地质,1991, 11(4):25-33.

    [YE Yu-guang. The geochemistry of 210Pb,Al,Fe,Mn and Cu of the core ZK226 in modern Huanghe delta[J]. Marine Geology and Quaternary Geology,1991, 11(4):25-33.]
    [29]
    张晓东, 翟世奎, 许淑梅,等. 长江口外缺氧区及其邻近海域沉积物中氧化还原敏感性元素的"粒度效应"[J].中国海洋大学学报,2005, 35(5):868-874.

    [ZHANG Xiao-dong, ZHAI Shi-kui, XU Shu-mei,et al.Study on the "granulatity effect"on the redox sensitive elements of sediments off the Changjiang Estuary hypoxia zone and its contiguous sea area[J].Journal of Ocean University of China,2005, 35(5):868-874.]
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