Distributional characteristics of grain sizes of surface sediments in the Zhujiang River Estuary

JIANG Siyi XU Fangjian LI Yan LIU Xiling ZHAO Yongfang XU Wei

JIANGSiyi, XUFangjian, LIYan, LIUXiling, ZHAOYongfang, XUWei. Distributional characteristics of grain sizes of surface sediments in the Zhujiang River Estuary[J]. 海洋学报英文版, 2014, 33(4): 30-36. doi: 10.1007/s13131-014-0462-1
引用本文: JIANGSiyi, XUFangjian, LIYan, LIUXiling, ZHAOYongfang, XUWei. Distributional characteristics of grain sizes of surface sediments in the Zhujiang River Estuary[J]. 海洋学报英文版, 2014, 33(4): 30-36. doi: 10.1007/s13131-014-0462-1
JIANG Siyi, XU Fangjian, LI Yan, LIU Xiling, ZHAO Yongfang, XU Wei. Distributional characteristics of grain sizes of surface sediments in the Zhujiang River Estuary[J]. Acta Oceanologica Sinica, 2014, 33(4): 30-36. doi: 10.1007/s13131-014-0462-1
Citation: JIANG Siyi, XU Fangjian, LI Yan, LIU Xiling, ZHAO Yongfang, XU Wei. Distributional characteristics of grain sizes of surface sediments in the Zhujiang River Estuary[J]. Acta Oceanologica Sinica, 2014, 33(4): 30-36. doi: 10.1007/s13131-014-0462-1

Distributional characteristics of grain sizes of surface sediments in the Zhujiang River Estuary

doi: 10.1007/s13131-014-0462-1
基金项目: The Special Fund of State Oceanic Administration under contract No. 908-ZC-II-01; the National Natural Science Foundation of China under contract No. 41106040; the Fundamental Research Funds for the Central Universities under contract Nos 14CX02038A and R1201062A; the Qingdao Science and Technology Development Plan Projects under contract No. 13-1-4-197-jch.

Distributional characteristics of grain sizes of surface sediments in the Zhujiang River Estuary

  • 摘要: Distributions of the parameters of sedimentary grain sizes and their correlations were studied to trace the sources of silts and their movement trends in the Zhujiang River Estuary based on the analyses of grain sizes from more than 1 080 sedimentary samples. The distributions of the median diameter, public value, quartile deviation, and skewness of sediments were complex in the Zhujiang River Estuary mainly because of the impact of the matter source regions, distances from the source regions, and hydrodynamic conditions, such as waves, tidal currents, and coastal currents. Analyses of the parameters of the grain sizes for the various types of sediments showed that the distributions of the surface sediments in the Zhujiang River Estuary were controlled by many factors. Their matter sources were mainly the sediments discharged from the runoffs and ebb tidal currents, and from the open sea. The sediments mainly moved by suspension movement. The silts formed a large area of sediments with suspended fine silts in the Zhujiang River Estuary by internal adjustment transportation in the area, and moved toward the western coast of the Zhujiang River Estuary under the effect of Coriolis forces and coastal currents.
  • Chen Minghao. 1978. Preliminary Analysis of Surface Sediment Distributionof Lingdingyang and the Pearl River Delta. Guangzhou:Guangdong Science and Technology Publishing House
    Chen Shaoyong, Shizuko Ambe, Fumitoshi Ambe. 1997. 57Fe Mossbauerspectroscopic studies of sediments in Northeastern SouthChina Sea and Zhujiang River mouth. Tropic Oceanology (in Chinese),16(4): 83-87
    He Zhigang, Wu Chaoyu, Mo Wenyuan, et al. 2006. A preliminary studyon sediment flux in the Zhujiang River Delta during the postglacialperiod. Acta Oceanologica Sinica (in Chinese), 28(6): 72-77
    Jia Jianjun, Gao Shu, Gao Jianhua, et al. 2005. Linkage of grain size informationwith river sediment discharge and estuarine depositionat the Pearl River Estuary. Advances in Marine Science (inChinese), 23(3): 297-304
    Lu Mengyu, Chen Shuzhen, Jiang Siyi, et al. 1993. Composition anddistribution of suspended load in sea water off Zhujiang Rivermouth and its vicinal shelf. Acta Sedimentologica Sinica (in Chinese),11(2): 99-104
    Pan Jianming, Zhou Huaiyang, Hu Chuanyu, et al. 2002. Nutrient profilesin interstitial water and flux in water-sediment in terface ofZhujiang Estuary of China in summer. Acta Oceanologica Sinica(in Chinese), 24(3): 52-59
    Sun Baiyun. 1990. Detrital mineral assemblages in the Huanghe,Changjiang and Zhujiang River delta sediments. Marine Geologyand Quaternary Geology (in Chinese), 10(3): 23-34
    Xu Fangjian, Li Anchun, Xiao Shangbin, et al. 2009. Paleoenvironmentalevolution in the inner shelf of the East China Sea since the lastdeglaciation. Acta Sedimentologica Sinica (in Chinese), 27(1):118-127
    Yang S, Tang M, Yim W W S, et al. 2011. Burial of organic carbon in Holocenesediments of the Zhujiang (Pearl River) and Changjiang(Yangtze River) estuaries. Marine Chemistry, 123(1-4): 1-10
    Yang S, Yim W W S, Huang G. 2008. Geochemical composition of innershelf Quaternary sediments in the northern South China
    Sea with implications for provenance discrimination and paleoenvironmentalreconstruction. Global and Planetary Change,60(3-4): 207-221
    Zong Y, Lloyd J M, Leng M J, et al. 2006. Reconstruction of Holocenemonsoon history from the Pearl River Estuary, southern China,using diatoms and carbon isotope ratios. The Holocene, 16(2):251-263
    Zou Dapeng, Wu Baihai, Lu Bo. 2007. Analysis and study on the soundvelocity empirical equations of seafloor sediments. Acta OceanologicaSinica (in Chinese), 29(4): 43-50
  • 加载中
计量
  • 文章访问数:  1128
  • HTML全文浏览量:  29
  • PDF下载量:  1520
  • 被引次数: 0
出版历程
  • 收稿日期:  2012-01-12
  • 修回日期:  2012-10-20

目录

    /

    返回文章
    返回