LIU Shengfa, SHI Xuefa, LIU Yanguang, ZHU Aimei, YANG Gang. SEDIMENTATION RATE OF MUD AREA IN THE EAST CHINA SEA INNER CONTINENTAL SHELF[J]. Marine Geology & Quaternary Geology, 2009, 29(6): 1-7. DOI: 10.3724/SP.J.1140.2009.06001
Citation: LIU Shengfa, SHI Xuefa, LIU Yanguang, ZHU Aimei, YANG Gang. SEDIMENTATION RATE OF MUD AREA IN THE EAST CHINA SEA INNER CONTINENTAL SHELF[J]. Marine Geology & Quaternary Geology, 2009, 29(6): 1-7. DOI: 10.3724/SP.J.1140.2009.06001
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SEDIMENTATION RATE OF MUD AREA IN THE EAST CHINA SEA INNER CONTINENTAL SHELF

  • First Institute of Oceanography, SOA, Qingdao 266061, China;Key Lab of Marine Sedimentology and Environmental Geology, SOA, Qingdao 266061, China

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  • Received Date: June 08, 2009
  • Revised Date: August 09, 2009
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    • Abstract
  • Seven gravity sediment cores were collected from muddy area of inner continental shelf of the East China Sea. Measurement of 210Pb activity was performed on all cores. The results demonstrate that the sedimentation rates were between 0.79 and 3.66 cm/a, with 1.97 cm/a on average. The highest sedimentation rate was recognized in core CJ12-11, located in the high sedimentation rate area of East China Sea. Six other cores with relative low sedimentation rates were located in the sub-higher sedimentation rate area. Distribution of 210Pb activity in surface sediments is correlated closely with the types of sediments, and probably controlled by the clay mineral, but shows a positive correlation with suspended matter concentration. Furthermore, these results reveal relative stable sedimentation processes in the muddy area during the past 100 years and the northward expansion of this muddy area.
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    • References (17)
  • [1]
    Liu J P, Xu K H, Li A C, et al. Flux and fate of Yangtze River sediment delivered to the East China Sea[J]. Geomorphology, 2007, 85:208-224.
    [2]
    杨作升,郭志刚,王兆祥,等.黄东海陆架悬浮体及其向东部深海区输送的宏观格局[J].海洋学报,1992,14(2):81-90.

    [YANG Zuosheng, GUO Zhigang, WANG Zhaoxiang, et al. Suspended sediments on the Yellow and East China Sea shelf and macro-pattern of their being transported to the eastern deeper sea[J]. Acta Oceanologica Sinica, 1992, 14(2):81-90.]
    [3]
    郭志刚,杨作升,雷坤,等.东海陆架北部泥质区沉积动力过程的季节性变化[J].青岛海洋大学学报,1999,29(3):507-513.

    [GUO Zhigang, YANG Zuosheng, LEI Kun, et al. Seasonal variation of the sedimentary dynamic processes for the mud area in the northern East China Sea[J]. Journal of Ocean University of Qingdao, 1999, 29(3):507-513.]
    [4]
    郭志刚,杨作升,张东奇,等.冬、夏季东海北部悬浮体分布及海流对悬浮体输运的阻隔作用[J].海洋学报,2002,24(5):71-80.

    [GUO Zhigang, YANG Zuosheng, ZHANG Dongqi, et al. Seasonal distribution of suspended matter in the northern East China Sea and barrier effect of current circulation on its transport[J]. Acta Oceanologica Sinica, 2002, 24(5):71-80.]
    [5]
    孙效功,方明,黄伟.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.

    [SUN Xiaogong, FANG Ming, HUANG Wei. Spatial and temporal variations in suspended particulate matter transport on the Yellow and East China Sea shelf[J]. Oceanologia et Limnologia Sinica, 2000, 31(6):581-587.]
    [6]
    肖尚斌,李安春,蒋富清,等.近2ka来东海内陆架泥质沉积物地球化学特征[J].地球化学,2005,34(6):595-604.

    [XIAO Shangbin, LI Anchun, JIANG Fuqing, et al. Geochemical characteristics of recent 2ka mud on the inner shelf of the East China Sea[J]. Geochimica, 2005, 34(6):595-604.]
    [7]
    Milliman J D,Qin Y S,Park Y A.Sediments and sedimentary processes in the Yellow Sea[C]//Sedimentary Facies in the Active Plate Margin. Tokyo:Terra Scientific Publishing Company,1989:233-249.
    [8]
    Demaster D J,Mckee B A,Nitrouer C A, et al. Rates of sediment accumulation and particles reworking based on radiochemical measurements from shelf deposits in the East China Sea[J]. Continental Shelf Research,1985,4:143-158.
    [9]
    范德江,杨作升,郭志刚.中国陆架210Pb测年应用现状与思考[J].地球科学进展,2000,15(3):297-232.

    [FAN Dejiang, YANG Zuosheng, GUO Zhigang. Review of 210Pb dating in the continental shelf of China[J]. Advance in Earth Sciences, 2000, 15(3):297-232.]
    [10]
    Hong Ci-Hon,Park Sun-Kyu,Baskaran M,et a1.Lead-210 and polonium-210 in the winter well-mixed turbid waters in the mouth of the Yellow Sea[J].Continental Shelf Research,1999,l9:l049-l064.
    [11]
    齐君,李凤业,宋金明,等.北黄海沉积速率及其沉积通量[J].海洋地质与第四纪地质,2004,24(2):9-14.

    [QI Jun, LI Fengye, SONG Jinming, et al. Sedimentation rate and flux of the north Yellow Sea[J]. Marine Geology and Quaternary Geology, 2004, 24(2):9-14.]
    [12]
    齐君,李凤业,宋金明.黄海和渤海沉积物210Pb活度的分布特征[J].地球化学,2005,34(4):351-356.

    [QI Jun, LI Fengye, SONG Jinming. Distribution of 210Pb activity of sediments in the Yellow and Bohai Seas[J]. Geochimica, 2005, 34(4):351-356.]
    [13]
    李凤业,高抒,贾建军,等.黄、渤海泥质沉积区现代沉积速率[J].海洋与湖沼,2002,33(4):364-369.

    [LI Fengye, GAO Shu, JIA Jianjun, et al. Contemporary deposition rates of fine-grained sediment in the Bohai and Yellow Seas[J]. Oceanologia et Limnologia Sinica, 2002, 33(4):364-369.]
    [14]
    张志忠,李双林,董岩翔,等.浙江近岸海域沉积物沉积速率及地球化学[J].海洋地质与第四纪地质,2005,25(3):15-24.

    [ZHANG Zhizhong, LI Shuanglin, DONG Yanxiang, et al. Deposition rate and geochemical characters of sediments in Zhejiang offshore[J]. Marine Geology and Quaternary Geology, 2005, 25(3):15-24.]
    [15]
    庄振业,叶银灿,刘杜鹃,等.东海全新世沉积强度分区[J].青岛海洋大学学报,2002,32(6):941-948.

    [ZHUANG Zhenye, YE Yincan, LIU Dujuan, et al. Holocene depositional strength zoning in the East China Sea[J]. Journal of Ocean University of Qingdao, 2002, 32(6):941-948.]
    [16]
    李凤业,宋金明,李学刚,等.胶州湾现代沉积速率和沉积通量研究[J].海洋地质与第四纪地质,2003,23(4):29-33.

    [LI Fengye, SONG Jinming, LI Xuegang, et al. Modern sedimentation rate and flux in the Jiaozhou Bay[J]. Marine Geology and Quaternary Geology, 2003, 23(4):29-33.]
    [17]
    Yang Z S, Wang H J, Satio Y, et al. Dam impacts on the Changjiang(Yangtze River) sediment discharge to the sea:The past 55 years and afer the Three Gorges dam[J]. Water Resources Research, 2006, 42:1-10.
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