CHEN Jun, CHEN Hongyou, XU Guohua, WANG Yigang, CAI Hui. GRAIN SIZE CHARACTERISTICS AND INFLUENCE FACTORS OF THE TIDAL FLAT DEPOSITS AT THE TIAOZINI SANDBANK, JIANGSU PROVINCE[J]. Marine Geology & Quaternary Geology, 2011, 31(6): 21-26. DOI: 10.3724/SP.J.1140.2011.06021
Citation: CHEN Jun, CHEN Hongyou, XU Guohua, WANG Yigang, CAI Hui. GRAIN SIZE CHARACTERISTICS AND INFLUENCE FACTORS OF THE TIDAL FLAT DEPOSITS AT THE TIAOZINI SANDBANK, JIANGSU PROVINCE[J]. Marine Geology & Quaternary Geology, 2011, 31(6): 21-26. DOI: 10.3724/SP.J.1140.2011.06021

GRAIN SIZE CHARACTERISTICS AND INFLUENCE FACTORS OF THE TIDAL FLAT DEPOSITS AT THE TIAOZINI SANDBANK, JIANGSU PROVINCE

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  • Received Date: March 19, 2011
  • Revised Date: June 27, 2011
  • The Tiaozini sandbank is located in the center of the Radiative Sandy Ridges along the coast of Jiangsu province, formed in a special hydrodynamic environment with complex geomorphology. Surface sediment samples were collected from the tidal flat of the Tiaozini sandbank on May 11, 2009. Grain size parameters (i.e. mean size, sorting coefficient, skewness and kurtosis), the composition of sediment and the elevation of tidal flat along three profiles were acquired. Our results indicate that the sediment consists of sandy silt coarsening seawards. It is about 4-6Φ in mean size, and well sorted, with positive skewness and sharp kurtosis. Components of saltation dominate. The depositional features of the tidal flat deposits are mainly influenced by tidal creeks, tidal salt marshes, the erosion and deposition of the sand banks and land reclamation activities. Irregular coastlines caused by land reclamation in different periods are the main factor influencing the characteristics of the tidal flat.
  • [1]
    Suursaar U, Jaagus J, Kont A,et al. Field observations on hydrodynamic and coastal geomorphic processes off Harilaid Peninsula (Baltic Sea) in winter and spring 2006-2007[J]. Estuarine, Coastal and Shelf Science, 2008, 80:31-41.
    [2]
    Matthew Kirwan, Stijn Temmermanb. Coastal marsh response to historical and future sea-level acceleration[J]. Quaternary Science Reviews, 2009, 28:1801-1808.
    [3]
    Paula D Pratolongo, Gerardo M E Perillo, M Cintia Piccolo. Combined effects of waves and plants on a mud deposition event at a mudflat-saltmarsh edge in the Bahía Blanca estuary[J]. Estuarine, Coastal and Shelf Science, 2010, 87:207-212.
    [4]
    Douglas A George, Paul S Hill. Wave climate,sediment supply and the depth of the sand-mud transition:A global survey[J]. Marine Geology, 2008, 254:121-128.
    [5]
    王爱军,汪亚平,杨扬,等. 江苏王港潮间带表层沉积物特征及输运趋势[J].海洋地质与第四纪地质,2004,24(1):124-129.

    [WANG Aijun, WANG Yaping, YANG Yang. Surface sediment characteristics and transport trends on the Wanggang intertidal flat, Jiangsu Province[J]. Marine Geology and Quaternany Geology, 2004, 24(1):124-129.]
    [6]
    任美锷. 江苏省海岸带和海涂资源综合调查[M]. 北京:海洋出版社, 1986:25-37.[REN Meie. Comprehensive Investigation of the Coastal Zone and Tidal Flat Resources of Jiangsu Province[M]. Beijing:China Ocean Press, 1986:25

    -37.]
    [7]
    McManus J.Grain size determination and interpretation[M]//In:Techniques in Sedimentology,Techniques in Sedimentology. Backwell, Oxford.1988:63-85.
    [8]
    Folk R L, Andrews P B, Lewis D W, Detrital sedimentary rock classification and nomenclature for use in New Zealand[J]. New Zealand Journal of Geology and Geophysica, 1970, 13:937-968.
    [9]
    Blair T C, McPherson J G. Grain-size and textural classification of coarse sedimentary particles[J]. Journal of Sedimentary Research, 1999,69(1):6-19.
    [10]
    陈才俊.江苏淤长型淤泥质潮滩的剖面发育[J].海洋与湖沼,1991,11(4):360-368.

    [CHEN Caijun. Development of depositional tidal flat in Jiangsu Province[J]. Oceanologia et Limnologia Sinica, 1991, 22(4):360-368.]
    [11]
    江苏省农业资源开发局.江苏沿海垦区[M]. 北京:海洋出版社,1999:62-85.[Agricultural Resources Development Bureau of Jiangsu Province. Coastal Reclamation of Jiangsu Province[M]. Beijing:China Ocean Press, 1999:62

    -85.]
    [12]
    毛志刚,王国祥,刘金娥,等. 苏北滨海湿地不同植被带沉积物粒度特征分析[J].海洋科学进展,2008,26(4):454-463.

    [MAO Zhigang, WANG Guoxiang, LIU Jiner, et al. Characteristics of grain-size distributions in different vegetation zones of coastal wetland in north Jiangsu[J]. Advances in Marine Science, 2008, 26(4):454-463.]
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