2014 Vol. 34, No. 6
Article Contents

HUANG Long, ZHANG Zhixun, GENG Wei, WANG Zhongbo, LU Kai, LI Yang. GRAIN SIZE OF SURFACE SEDIMENTS IN THE EASTERN MIN-ZHE COAST: AN INDICATOR OF SEDIMENTARY ENVIRONMENTS[J]. Marine Geology & Quaternary Geology, 2014, 34(6): 161-169. doi: 10.3724/SP.J.1140.2014.06161
Citation: HUANG Long, ZHANG Zhixun, GENG Wei, WANG Zhongbo, LU Kai, LI Yang. GRAIN SIZE OF SURFACE SEDIMENTS IN THE EASTERN MIN-ZHE COAST: AN INDICATOR OF SEDIMENTARY ENVIRONMENTS[J]. Marine Geology & Quaternary Geology, 2014, 34(6): 161-169. doi: 10.3724/SP.J.1140.2014.06161

GRAIN SIZE OF SURFACE SEDIMENTS IN THE EASTERN MIN-ZHE COAST: AN INDICATOR OF SEDIMENTARY ENVIRONMENTS

  • The grain size of the 83 surface sediment samples taken from the eastern Min-Zhe coast are studied for sediment types and the distribution pattern of grain size parameters. The effect of sediment source and hydrodynamic conditions on the sediment distribution pattern is discussed. The following results have been achieved based on the detailed study of these samples:(1)There are six types of sediment in the study area and they are sand, silty sand, muddy sand, sandy silt, silt and mud. (2)The mean grain size is in a range of 2.01~7.58 φ, and the grains are coarsening seaward with the increase in sand and decrease in silt and mud. (3)The standard deviation varies between 0.48~2.86 φ. It shows a poor sorting in the whole study area and the lowest is in the middle of the study area, and from there the sorting is improved eastward and westward. (4)The inshore fine sediments are from the Yangtze River and other coastal rivers, and the offshore coarse sediments are the reworked relict deposits on shelf. Both the coastal current along the Min-Zhe coast and the Kuroshio current contribute to the distribution of sediments. Based on the data, the Min-Zhe coast is divided into three depositional zones, i.e. the inshore muddy zone, multi-sediments zone in the middle and eastern Min-Zhe coast and offshore reworked sand zone on the outer shelf.
  • 加载中
  • [1] McLaren P,Bowles D.The effects of sediment transport on grainsize distributions[J].Journal of Sedimentary Petrology,1985,55(4):457-470.

    Google Scholar

    [2] 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 Jianjun,GAO Shu,XUE Yunchuan.Grain-size parameters derived from graphic and moment methods:a comparative study[J].Oceanologia et Limnologia Sinica, 2002,33(6):577-582.]

    Google Scholar

    [3] 秦蕴珊,赵一阳,陈丽蓉,等.东海地质[M].北京,科学出版社,1987.[QIN Yunshan,ZHAO Yiyang,CHEN Lirong,et al.Geology of the East China Sea[M].Beijing:Science Press,1987.]

    Google Scholar

    [4] 肖尚斌,李安春.东海内陆架泥区沉积物的环境敏感粒度组分[J].沉积学报,2005,23(1):122-129.

    Google Scholar

    [XIAO Shangbin, LI Anchun. A study on environmentally sensitive grain-size population in inner shelf of the East China Sea[J].Acta Sedimentologica Sineca,2005,23(1):122-129.]

    Google Scholar

    [5] 肖尚斌,李安春,蒋富清,等.近2ka闽浙沿岸泥质沉积物物源分析[J].沉积学报,2005,23(2):268-274.

    Google Scholar

    [XIAO Shangbin, LI Anchun,JIANG Fuqing, et al. Provenance analysis of mud along the Min-Zhe coast since 2 kaBP[J].Acta Sedimentologica Sineca,2005,23(2):268-274.]

    Google Scholar

    [6] 张晓东,许淑梅,翟世奎,等.东海内陆架沉积气候信息的端元分析模型反演[J].海洋地质与第四纪地质,2006,26(2):25-32.

    Google Scholar

    [ZHANG Xiaodong,XU Shumei,ZHAI Shikui,et al.The inversion of climate information from the sediment of inner shelf of East China Sea using end-member model[J].Marine Geology and Quaternary Geology,2006,26(2):25-32.]

    Google Scholar

    [7] 王可,郑洪波,Maarten Prins,等.东海内陆架泥质沉积反映的古环境演化[J].海洋地质与第四纪地质,2008,28(4):1-10.

    Google Scholar

    [WANG Ke,ZHENG Hongbo,Maarten Prins,et al. High-resolution paleoenvironmental record of the mud sediments of the East China Sea inner shelf[J].Marine Geology and Quaternary Geology,2008,28(4):1-10.]

    Google Scholar

    [8] 刘升发,刘焱光,朱爱美,等.东海内陆架表层沉积物粒度及其净输运模式[J].海洋地质与第四纪地质,2009,29(1):1-6.

    Google Scholar

    [LIU Shengfa,LIU Yanguang,ZHU Aimei,et al. Grain size trends and net transport patterns of surface sediments in the East China Sea inner continental shelf[J].Marine Geology and Quaternary Geology,2009,29(1):1-6.]

    Google Scholar

    [9] 李云海,陈坚,黄财宾,等.浙闽沿岸南部泥质沉积中心表层沉积物粒度特征及其季节性差异[J].沉积学报,2010,28(1):150-157.

    Google Scholar

    [LI Yunhai,CHEN Jian,HUANG Caibin,et al. Grain-size characteristics of the surface sediments and their seasonal variability in the mud depocenter off the southern Zhejiang-Fujian coast[J].Acta Sedimentologica Sinica,2010,28(1):150-157.]

    Google Scholar

    [10] 刘莹,翟世奎,李军.长江口与闽浙沿岸泥质区现代沉积记录及其影响因素[J].海洋地质与第四纪地质,2010,30(5):1-10.

    Google Scholar

    [LIU Ying,ZHAI Shikui,LI Jun.Depositional records in the mud areas of Changjiang estuary and off Min-Zhe coast and their influence factors[J].Marine Geology and Quaternary Geology,2010,30(5):1-10.]

    Google Scholar

    [11] Folk R L,Ward W C.Barazos River bar:A study in the significance for grain parameters[J].Journal of Sedimentary Petrology,1957,31:514-519.]

    Google Scholar

    [12] 张怀静,翟世奎,范德江,等.三峡工程一期蓄水后长江口及其临近海域悬浮物浓度分布特征[J].环境科学,2007,28(8):1655-1661.

    Google Scholar

    [ZHANG Huaijing,ZHAI Shikui,FAN Dejiang,et al. Distribution of suspended matter concentration in the Changjiang estuary and adjacent area after the first-stage storage of the three gorges project[J].Environmental Science, 2007,28(8):1655-1661.]

    Google Scholar

    [13] Folk R L,Andrews P B,Lewis D.Detrital sedimentary rock classification and nomenclature for use in New Zealand[J].New Zealand Journal of Geology and Geophysics,1970,13(4):937-968.]

    Google Scholar

    [14] 杨旭辉,冯秀丽,褚忠信,等.中国东部陆架表层沉积物粒度特征及其沉积环境浅析[J].中国海洋大学学报,2012,42(7-8):126

    Google Scholar

    -134.[YANG Xuhui,FENG Xiuli,CHU Zhongxin,et al. Surface sediment distribution and sedimentary environment on the East China continental shelf[J].Periodical of Ocean University of China,2012,42(7-8):126-134.]

    Google Scholar

    [15] 何起祥.海洋沉积作用的物源控制[J].海洋地质前沿,2011,27(1):8-13.

    Google Scholar

    [HE Qixiang. Sediment sources and their bearing on marine sedimentation[J].Marine Geology Frontiers,2011,27(1):8-13.]

    Google Scholar

    [16] Emery K.O.Relict sediment on continental shelves of the world[J].Bulletin of the American Association of Petroleum Geologists,1968,52:445-464.]

    Google Scholar

    [17] 汪亚平,潘少明,H V Wang,等.长江口水沙入海通量的观测与分析[J].地理学报,2006,61(1):35-46.

    Google Scholar

    [WANG Yaping,PAN Shaoming, H V Wang,et al. Measurements and analysis of water discharges and suspended sediment fluxes in Changjiang estuary[J].Geographica Sinica,2006,61(1):35-46.]

    Google Scholar

    [18] 郭志刚,杨作升,曲艳慧,等.东海陆架泥质区沉积地球化学比较研究[J].沉积学报,2000,18(2):284-289.

    Google Scholar

    [GUO Zhigang,YANG Zuosheng,QU Yanhui,et al. Study on comparison sedimentary geochemistry of mud area on east china sea continental shelf[J].Acta Sedimentologica Sinica,2000,18(1):284-289.]

    Google Scholar

    [19] 石学法,刘升发,乔淑卿,等.东海闽浙沿岸泥质区沉积特征与古环境记录[J].海洋地质与第四纪地质,2010,30(4):19-30.

    Google Scholar

    [SHI Xuefa,LIU Shengfa,QIAO Shuqing,et al. Depositional features and palaeoenvironmental records of the mud deposits in Min-Zhe coastal mud area,east china sea[J].Marine Geology and Quaternary Geology,2010,30(4):19-30.]

    Google Scholar

    [20] 贺松林.东海近岸带沉积物陆源矿物组份的比较研究[J].华东师范大学学报:自然科学版,1991(1):78-86.[HE Songlin.Comparative study on terrigenous miniral component of sediment along nearshore area of the east china sea[J].Journal of East China Normal University(Natural science),1991

    Google Scholar

    (1):78-86.]

    Google Scholar

    [21] LIU J P,LIU C S,XU K H,et al.Flux and fate of small mountainous rivers derived dediments into the Taiwan strait[J].Marine Geology,2008,256(1/4):65-76.

    Google Scholar

    [22] 刘锡清.中国陆架的残留沉积[J].海洋地质与第四纪地质,1987,7(1):1-14.

    Google Scholar

    [LIU Xiqing.Relict sediments in China continental shelf[J].Marine Geology and Quaternary Geology, 1987,7(1):1-14.]

    Google Scholar

    [23] 王中波,杨守业,张志珣,等.东海陆架中北部沉积物粒度特征及其沉积环境[J].海洋与湖沼,2012,43(6):1039-1049.

    Google Scholar

    [WANG Zhongbo,YANG Shouye,ZHANG Zhixun,et al. The grain size compositions of the surface sediments in the East China Sea:indication for sedimentary environments[J].Oceanologia et Limnologia Sinica,2012,43(6):1039-1049.]

    Google Scholar

    [24] 沈华悌,梁居廷,王秀昌.东海陆架残留沉积物的改造[J].海洋地质与第四纪地质,1984,4(2):67-76.

    Google Scholar

    [SHEN Huati,LIANG Juting,WANG Xiuchang.Reworking of relict sediments on the continental shelf of the East China Sea[J].Marine Geology and Quaternary Geology, 1984,4(2):67-76.]

    Google Scholar

    [25] 鲍献文,林霄沛,吴德星,等.东海陆架环流季节变化的模拟与分析[J].中国海洋大学学报,2005,35(3):349-356.

    Google Scholar

    [BAO Xianwen,LIN Xiaopei,WU Dexing,et al.Simulation and analysis of shelf circulation and its seasonal variability in the East China Sea[J].Periodical of Ocean University of China,2005,35(3):349-356.]

    Google Scholar

    [26] 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.

    Google Scholar

    [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.]

    Google Scholar

  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(1029) PDF downloads(3) Cited by(0)

Access History

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint