2007 Vol. 27, No. 6
Article Contents

WANG Hua-qiang, GAO Shu. TIDAL FLAT SEDIMENT CHARACTERISTICS AND TRANSPORT TRENDS ALONG THE NORTHERN BANK OF HANGZHOU BAY[J]. Marine Geology & Quaternary Geology, 2007, 27(6): 25-30.
Citation: WANG Hua-qiang, GAO Shu. TIDAL FLAT SEDIMENT CHARACTERISTICS AND TRANSPORT TRENDS ALONG THE NORTHERN BANK OF HANGZHOU BAY[J]. Marine Geology & Quaternary Geology, 2007, 27(6): 25-30.

TIDAL FLAT SEDIMENT CHARACTERISTICS AND TRANSPORT TRENDS ALONG THE NORTHERN BANK OF HANGZHOU BAY

  • During November 2004, surficial sediment samples were collected from the upper part of the tidal flat on the northern bank of Hangzhou Bay. Grain size analysis of the samples, using a Mastersize2000 layer particle sizer, shows that the major constituent of the sediment is silt, with the mean grain size mainly between 5 and 6.5 Φ. The other grain size parameters, i.e. sorting coefficient, skewness and kurtosis, are indicative of the deposit formed in a high energy tidal environment. The sediment is poorly sorted and positively skewed, with a broad kurtosis.Results from the Gao-Collins model for grain size trend analysis show that the sediment transport is directed to west near Haiyan and Luchao Port, but to east between Zhapu and Tuolin. Compared with the residual current patterns in the adjacent waters, the transport trend along the northern bank has the same direction as the residual current. This agreement is related to the inherent relationship between suspended sediment transport and residual currents in this estuarine system, which provides suspended sedimentary materials to the tidal flat.
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  • [1] 杨宗严. 河口及浅海环境中细颗粒悬浮泥沙长期输运过程研究[J]. 海洋技术, 1993, 12(1):13-19.

    Google Scholar

    [YANG Zong-yan. Study of long-term transport process of suspended fine sand-mud at estuary and shallow-water environment[J]. Ocean Technology, 1993, 12(1):13-19.]

    Google Scholar

    [2] Postma H. Transport and accumulation of suspended matter in the Dutch Wadden Sea[J]. Netherlands Journal of Sea Research, 1961, 1:148-190.

    Google Scholar

    [3] Van Straaten K N J U, Kuenen Ph H. Tidal action as a cause for clay accumulation[J]. Journal of Sedimentary Petrology, 1958, 28:406-413.

    Google Scholar

    [4] 刘永学,张忍顺,陈君.粒径趋势分析法在细颗粒潮坪上的应用[J]. 南京师范大学学报自然科学版, 2001, 24(1):105-109.

    Google Scholar

    [LIU Yong-xue, ZHANG Ren-shun, CEHN Jun. Application of trend analysis on Jiangsu coast[J]. Journal of Nanjing Normal University (Natural Science), 2001, 24(1):105-109.]

    Google Scholar

    [5] 王晓辉,邹欣庆,徐庆珂. 江苏梁垛闸潮间带表层沉积物特征及输运趋势[J].海洋学研究, 2006, 24(2):20-27.

    Google Scholar

    [WANG Xiao-hui, ZOU Xin-qing, XU Qing-ke. Surface sediment characteristics and transport trends in intertidal flat of Liangduo sluice, Jiangsu Province[J]. Journal of Marine Science, 2006, 24(2):20-27.]

    Google Scholar

    [6] 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[J]. 长江流域资源与环境, 2005, 14(6):735-739.

    Google Scholar

    [DAI Zhi-jun, CHENG Ji-yu, CHENG He-qin,et al. Sediment characteristics and transport patterns in Nanhui joint area[J]. Resources and Environment in the Yangtze Basin, 2005, 14(6):735-739.]

    Google Scholar

    [7] 中国海湾志编纂委员会.中国海湾志第五分册(上海市和浙江北部海湾)[M]. 北京:海洋出版社,1990:1-87.[Anonymous. Coastal Embayments in China (V.5:Shanghai and Northern Zhejiang)[M]. Beijing:China Ocean Press, 1990

    Google Scholar

    :1-87.]

    Google Scholar

    [8] 林承坤. 长江口泥沙的来源分析与数量计算[J]. 泥沙研究, 1984(2):22-31.[LIN Cheng-kun. A study on the source and quantity of sediment at the Yangtze River estuary[J]. Journal of Sediment Research, 1984

    Google Scholar

    (2):22-31.]

    Google Scholar

    [9] 曹沛奎,董永发,严肃庄,等. 杭州湾北岸高能潮滩的基本特征[J]. 海洋与湖沼, 1989, 20(5):412-422.

    Google Scholar

    [CAO Pei-kui, DONG Yong-fa, YAN Su-zhuang,et al. Basic characteristics of the tidal flat on the north coast of Hangzhou Bay[J]. Oceanologia et Limnologia Sinica, 1989, 20(5):412-422.]

    Google Scholar

    [10] 毛汉礼,沈鸿书,甘子钧,等. 杭州湾的基本水文特征[J]. 海洋科学集刊, 1965, 1:126-168.[MAO Han-li, SHEN Hong-shu, GAN Zi-jun,et al. Basic hydrologic characteristics of Hangzhou Bay[J]. Studia Marina Sinica, 1965

    Google Scholar

    , 1:126-168.]

    Google Scholar

    [11] 张华国,郭艳霞,黄韦艮,等. 1986年以来杭州湾围垦淤涨状况卫星遥感调查[J]. 国土资源遥感,2005,2:50-54.[ZHANG Hua-guo, GUO Yan-xia, HUANG Wei-gen,et al. A remote sensing investigation of inning and silting in Hangzhou Bay since 1986

    Google Scholar

    [J]. Remote Sensing for Land & Resources, 2005, 2:50-54.]

    Google Scholar

    [12] McManus J. Grain size determination and interpretation[C]//Techniques in Sedimentology.Oxford:Blackwell,1988:63-85.

    Google Scholar

    [13] 贾建军, 高抒, 薛允传. 图解法与矩法沉积物粒度参数的对比[J]. 海洋与湖沼, 2002, 33(6):577-582.

    Google Scholar

    [JIA Jian-jun, GAO Shu, XUE Yun-chuan. Grain-size parameters derived from graphic and moment methods:a comparative study[J]. Oceanologia et Limnologia Sinica, 2002, 33:577-582.]

    Google Scholar

    [14] Shepard F P. Nomenclature based on sand-silt-clay ratios[J]. Journal of Sedimentary Petrology, 1954, 24:151-158.

    Google Scholar

    [15] Gao S, Collins M. Net sediment transport patterns inferred from grain-size trends,based upon definition of "transport vectors"[J]. Sedimentary Geology, 1992, 81:47-60.

    Google Scholar

    [16] Gao S, Collins M B. Analysis of grain size trends, for defining sediment transport pathways in marine environments[J]. Journal of Coastal Research, 1994, 10(1):70-78.

    Google Scholar

    [17] 李身铎,胡辉. 杭州湾流场的研究[J].海洋与湖沼, 1987, 18(1):28-38.

    Google Scholar

    [LI Shen-duo, HU Hui. A study of the current field of the Hangzhou Bay[J]. Oceanologia et Limnologia Sinica, 1987, 18:28-38.]

    Google Scholar

    [18] 陈倩,黄大吉, 章本照,等. 浙江近海潮流和余流的特征[J].东海海洋,2003, 21(4):1-14.

    Google Scholar

    [CHEN Qian, HUANG Da-ji, ZHANG Ben-zhao,et al. Characteristics of the tidal current and residual current in the seas adjacent to Zhejiang[J]. Donghai Marine Science, 2003, 21(4):1-14.]

    Google Scholar

    [19] 倪勇强,耿兆全,朱军政. 杭州湾水动力特性研讨[J].水动力学研究与进展A辑, 2003, 18(4):439-445.

    Google Scholar

    [NI Yong-qiang, GENG Zhao-quan, ZHU Jun-zheng. Study on characteristic of hydrodynamics in Hangzhou Bay[J]. Journal of Hydrodynamics (A), 2003, 18(4):439-445.]

    Google Scholar

    [20] 刘新成,卢永金,潘丽红,等. 长江口和杭州湾潮流数值模拟及水体交换的定量研究[J]. 水动力学研究与进展A辑, 2006, 21(2):171-180.

    Google Scholar

    [LIU Xin-cheng, LU Yong-jin, PAN Li-hong,et al. Tidal current numerical simulating and water exchange research in Yangtze estuary and Hangzhou Bay[J]. Journal of Hydrodynamics (A), 2006, 21(2):171-180.]

    Google Scholar

    [21] 许卫忆, 苏纪兰. 杭州湾二维潮波计算与底质分布的动力成因[J]. 海洋与湖沼, 1986, 17(6):493-503.

    Google Scholar

    [XU Wei-yi, SU Ji-lan. The computation of two-dimensional tidal waves and the analysis of sedimentational distribution in Hangzhou Bay[J]. Oceanologia et Limnologia Sinica, 1986, 17:493-503.]

    Google Scholar

    [22] Passega R. Grain size representation by CM pattern as a geologic tool[J]. Journal of Sedimentary Petrology, 1964, 34:830-847.

    Google Scholar

    [23] 曹沛奎,谷国传,董永发,等. 杭州湾泥沙运移的基本特征[J]. 华东师范大学学报自然科学版, 1985, 3:75-84.[CAO Pei-kui, GU Guo-chuan, DONG Yong-fa,et al. Basic characteristics of sediment transport in Hangzhou Bay[J]. Journal of East China Normal University (Natural Science Edition), 1985

    Google Scholar

    , 3:75-84.]

    Google Scholar

    [24] 李伯根, 杨昭庆, 谢钦春. 杭州湾悬沙输移及其有关水动力因素分析[J]. 中国海洋学文集, 1992, 2:29-36.[LI Bo-gen, YANG Zhao-qing, XIE Qin-chun. Suspended sediment transport and its concerned dynamic analysis in the Hangzhou Bay[J]. Oceanography in China, 1992

    Google Scholar

    , 2:29-36.]

    Google Scholar

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