Distribution of Surficial Tidal Flat Sediments in the Yangtze Estuary

  • State Key Lab. of Estuarine and Coastal Research,East China Normal University,Shanghai 200062,China

Received date: 2008-12-05

  Revised date: 2009-03-03

  Online published: 2009-05-25

Supported by

Natural Science Foundation of Shanghai,No.07DJ14003;Foundation of Ministry of Science and Technology of China,No.SKLEC-2008KYQN03;Shanghai Youth Science and Technology Venus Program,No.06QA14016


Large-scale and dense sediment samples and associated hydrological data were collected in July 2005 and May 2007 from submarine sectors of Chongming Eastern Shoal, Hengsha Eastern Shoal, Jiuduan Shoal and Nanhui Shoal, which are four important tidal flats located at the mouth-bar river segment of the Yangtze Estuary. Based on the above data, the grain size and related parameters, compositions, classifications in sediments and their distributed characteristics are analyzed, and then mainly impacted dynamic factors on the distributions of sediments are discussed. The results are shown as follows: sediments located at these tidal flats of the Yangtze Estuary are mainly composed of sand, silty sand and silt. The median grain size in sediments is relatively complex with a range from 2.5φ to 8φ. The distributions of sorting coefficients in sediments ranging from 1 to 2 are agreed with that of the median grain size. Moreover, it is suggested that sediments of the tidal flats is coarser, better sorted or finer, and worse sorted. The skewness and kurtosis in sediments are ranged from 0.1 to 0.8 and from 1 to 4, respectively. In addition, the distributions of the grain size parameters, including sorting coefficient, skewness and kurtosis in sediments of Chongming Eastern Shoal, Hengsha Eastern Shoal and Jiuduan Shoal are of similar characteristics because there are closely positive correlated relationships among these parameters. However, due to the location difference between Nanhui Southern Shoal and Eastern Shoal, three parameters of grain size in sediments such as sorting coefficient, skewness and kurtosis have relatively large distinctions. Moreover, the tracks of sediment transport can be described based on the distribution of sediments which may reveal sediment transport controlled by the two dominant hydrodynamic factors of current and wave. It is appreciable that coarse sediments with better sorted is subjected to dominant ebb current action and intense wave action resulted from rapidly dissipated wave energy. In addition, due to the effects of obstructed branches, guided current and broken wave actions of the Deep Water Channel Project, grain size in sediments located on two sides of the groyne is of uneven distribution characteristics.

Cite this article

YAN Hong,DAI Zhijun,LI Jiufa,ZHAO Jianchun,ZHANG Xiaoling . Distribution of Surficial Tidal Flat Sediments in the Yangtze Estuary[J]. Acta Geographica Sinica, 2009 , 64(5) : 629 -637 . DOI: 10.11821/xb200905012


[1] Li Jiufa, Dai Zhijun, Ying Ming et al. Analysis on the development and evolution of tidal flats and reclamation of land resource along shore of Shanghai city. Journal of Natural Resources, 2007, 22(3): 361-371.
[李九发, 戴志军, 应铭等. 上海市沿海滩涂土地资源圈围与潮滩发育演变分析. 自然资源学报, 2007, 22(3): 361-371.]

[2] Wan Xinning, Li Jiufa, He Qing et al. Water and sediments fluxes in the middle and lower Yangtze River. Journal of Sediments Research, 2003, (4): 29-35.
[万新宁, 李九发, 何青等. 长江中下游水沙通量变化规律. 泥沙研究, 2003, (4): 29-35.]

[3] Fu Renshou, Yu Zhiying, Jin Liu et al. Variation trend of runoff and sediments load in Yangtze River. Journal of Hydraulic Engineering, 2003, (11): 21-29.
[府仁寿, 虞志英, 金镠等. 长江水沙变化发展趋势. 水利学报, 2003, (11): 21-29.]

[4] Shen Huanting, Zhang Chao, Mao Zhichang. Patterns of variations in the water and sediments fluxes from the Changjiang River to the estuary. Oceanlogia et Limnologia Sinica, 2000, (3): 288-294.
[沈焕庭, 张超, 茅志昌. 长江入 河口区水沙通量变化规律. 海洋与湖沼, 2000, (3): 288-294.]

[5] Liu Hong, He Qing, Meng Yi et al. Characteristics of surface sediments distribution and its hydrodynamic responses in the Yangtze River estuary. Acta Geographica Sinica, 2007, 62(1): 81-92.
[刘红, 何青, 孟翊等. 长江口表层沉积物分 布特征及动力响应. 地理学报, 2007, 62(1): 81-92.]

[6] Yang Ou, Liu Cangyu. Analysis on sediments transport patterns sediments sources of north branch of Changjiang Estuary. Journal of Hydraulic Engineering, 2002, (2): 79-84.
[杨欧, 刘苍宇. 长江口北支沉积物粒径趋势及泥沙来源 研究. 水利学报, 2002, (2): 79-84.]

[7] Dai Zhijun, Chen Jiyu, Cheng Heqin et al. Sediments characteristics and transport patterns in Nanhui adjacent area. Resources and Environment in the Yangtze Basin, 2005, 14(6): 735-739.
[戴志军, 陈吉余, 程和琴等. 南汇边滩的沉 积特征和沉积物输运趋势. 长江流域资源与环境, 2005, 14(6): 735-739.]

[8] Chen Jiyu (eds.). The Research and Practice on Chinese Estuary and Coast. Beijing: Higher Education Press, 2007.
[陈 吉余主编. 中国河口海岸研究与实践. 北京: 高等教育出版社, 2007.]

[9] Wang Baocan, Huang Yangsong (eds.). Coastal Dynamic Geomorphology. Shanghai: East China Normal University Press, 1989: 77-87.
[王宝灿, 黄仰松主编. 海岸动力地貌. 上海: 华东师范大学出版社, 1989. 77-87.]

[10] Francis P Shepard, Wang Zhongbo. The method for classifying sediments based on the proportion of sand-silt-clay. Marine Geology Letters, 2006, (10): 33-35.
[Francis P Shepard, 王中波. 基于砂—粉砂—黏土含量的沉积物命名方 法. 海洋地质动态, 2006, (10): 33-35.]

[11] Zuo Shuhua, Li Jiufa, Ying Ming et al. Characteristics of hydrology and sediments transportation and influence by Reservoir Project in the Meimaosha of Yangtze Estuary. Journal of East China Normal University (Natural Science), 2006, (2): 41-48.
[左书华, 李九发, 应铭等. 没冒沙水域水沙运动特性及筑库工程对其影响. 华东师范大学学报(自 然科学版), 2006, (2): 41-48.]

[12] Roberts W, Hir P L, Whitehouse R J S. Investigation using simple mathematical models of the elect of tidal currents and waves on the profile shape of intertidal mudflats, Continental Shelf Research. 2000, 20(10/11): 1079-1097.

[13] Green M O, Black K P, Amos C L. Control of estuarine sediments dynamics by interactions between currents and waves at several scales. Marine Geology, 1997, 144: 97-116.

[14] Yang Shilun, Zhao Qingying, Ding Pingxing et al. Seasonal changes in bed level of the passage in the mouth bar area of the Yangtze (Changjiang) River. Resources and Environment in the Yangtze Basin, 2001, 10(3): 258-265.
[杨世伦, 赵庆英, 丁平兴等. 长江口拦门沙河槽季节性冲淤的主控因子探讨. 长江流域资源与环境, 2001, 10(3): 258-265.]

[15] Li Jiufa, Mao Zhichang, Sun Jiemin. Analysis of hydrological and sediments conditions in Nanhui Nearshore of the Yangtze Estuary and its adjacent sea areas during flood season. In: Chen Jiyu, Shen Huanting, Yun Caixing (eds.). Process of Dynamics and Geomorphology of the Changjiang Estuary. Shanghai: Shanghai Scientific and Technical Publishers, 1988. 253-267.
[李九发, 茅志昌, 孙介民. 长江口南汇边滩及邻近水域洪季水文泥沙条件分析. 见: 陈吉 余, 沈焕庭, 恽才兴主编. 长江河口动力过程和地貌演变. 上海: 上海科学技术出版社, 1988. 253-267.]

[16] Zhu Huifang, Yun Caixing, Mao Zhichang et al. The characteristics and empirical relationships of wind-wave of theChangjiang Estuary, 1988. 166-177. In: Chen Jiyu, Shen Huanting, Yun Caixing (eds.). Process of Dynamics and Geomorphology of the Changjiang Estuary. Shanghai: Shanghai Scientific and Technical Publishers, 1988. 166-177.
[朱慧芳, 恽才兴, 茅志昌等. 长江河口的风浪特性和风浪经验关系. 见: 陈吉余, 沈焕庭, 恽才兴主编. 长江河口动 力过程和地貌演变. 上海: 上海科学技术出版社, 1988. 166-177.]

[17] Zhang Hongsheng. Mathematical Models of Wave Propagation in Coastal Region. Shanghai: East China Normal University, 2002.
[张洪生. 近岸水域波浪传播的数学模型. 上海: 华东师范大学, 2002.]

[18] Du Jinglong, Yang Shilun. Influence of deep-water channel project at north passage of the Yangtze River on erosion and accumulation of Hengsha East Shoal and Jiuduansha Shoal. Scientia Geographica Sinica, 2007, 27(3): 390-394.
[杜景龙, 杨世伦. 长江口北槽深水航道工程对周边滩涂冲淤影响研究. 地理科学, 2007, 27(3): 390-394.]

[19] Yan Yixin, Gao Jin, Zhu Yuliang et al. Preliminary study on relationship between deepwater channel regulation and riverbed evolution. Journal of Hohai University, 2001, (5): 7-12.
[严以新, 高进, 诸裕良等. 长江口深水航道治理与 河床演变关系初探. 河海大学学报, 2001, (5): 7-12.]

[20] Li Jiufa, Wan Xinning et al. Study on formation and evolvement of Jiuduan Shoal in the Changjiang Estuary. Journal of Sediments Research, 2006, (6): 44-49.
[李九发, 万新宁等. 长江河口九段沙沙洲形成和演变过程研究. 泥沙研究, 2006, (6): 44-49.]