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    东海东北部海域表层沉积物黏土矿物来源及输运

    黄龙 王中波 耿威 张勇 王明健

    黄龙, 王中波, 耿威, 张勇, 王明健, 2020. 东海东北部海域表层沉积物黏土矿物来源及输运. 地球科学, 45(7): 2722-2734. doi: 10.3799/dqkx.2020.046
    引用本文: 黄龙, 王中波, 耿威, 张勇, 王明健, 2020. 东海东北部海域表层沉积物黏土矿物来源及输运. 地球科学, 45(7): 2722-2734. doi: 10.3799/dqkx.2020.046
    Huang Long, Wang Zhongbo, Geng Wei, Zhang Yong, Wang Mingjian, 2020. Sources and Transport of Clay Minerals in Surface Sediments of the Northeastern East China Sea. Earth Science, 45(7): 2722-2734. doi: 10.3799/dqkx.2020.046
    Citation: Huang Long, Wang Zhongbo, Geng Wei, Zhang Yong, Wang Mingjian, 2020. Sources and Transport of Clay Minerals in Surface Sediments of the Northeastern East China Sea. Earth Science, 45(7): 2722-2734. doi: 10.3799/dqkx.2020.046

    东海东北部海域表层沉积物黏土矿物来源及输运

    doi: 10.3799/dqkx.2020.046
    基金项目: 

    国家海洋地质专项项目 DD20160137

    国家海洋地质专项项目 DD20190377

    国家海洋地质专项项目 DD20190205

    国家海洋地质专项项目 DD20190208

    国家海洋地质专项项目 GZH002-06

    国家海洋地质专项项目 GHZ201400201

    国家自然科学基金项目 41606079

    国家自然科学基金项目 41876059

    山东省博士后创新项目 201201001

    详细信息
      作者简介:

      黄龙(1983-), 男, 高级工程师, 从事海洋地质研究.ORCID:0000-0002-2540-2896.E-mail:huanglong0919@126.com

      通讯作者:

      王明健, ORCID:0000-0003-2250-7200.E-mail:wangmingjian0328@qq.com

    • 中图分类号: P736.2

    Sources and Transport of Clay Minerals in Surface Sediments of the Northeastern East China Sea

    • 摘要: 利用X射线衍射,对东海东北部海域80个表层沉积物样品进行黏土矿物的相对含量分析.结果表明:东海东北部海域表层沉积物黏土矿物中伊利石(65.1%)含量最高,其次为绿泥石(26.6%)、高岭石(8.9%)和蒙皂石(4.3%);矿物组合中伊利石-绿泥石-高岭石-蒙皂石型占绝对优势,伊利石-绿泥石-高岭石型较少.由外陆架至冲绳海槽,伊利石含量分布呈低-高-低-高;绿泥石呈低-高-低;高岭石分布趋势明显异于伊利石和绿泥石,含量值分布出现由高到低的趋势;蒙皂石在个别区域缺失,高值区呈斑块状分布在水深小于100 m的外陆架.快速聚类分析显示,黏土矿物可分为“类长江”、“类黄河”和“类台湾”3种类型,呈4个区域相间展布.“类黄河”型黏土矿物主要由黄海沿岸流将黄河、废黄河等物质再悬浮搬运而来,分布于29.5°N以北、127°E以西的外陆架区,并未越过东海外陆架进入冲绳海槽.外陆架区“类长江”型黏土矿物主要为低海平面时期古长江物质,并混有少量现代长江源悬浮物质;冲绳海槽区“类长江”型黏土矿物主要来自低海平面时期古长江物质.“类台湾”型黏土矿物主要由黑潮控制,由台湾经冲绳海槽南部搬运而来,沿陆坡附近沉积.

       

    • 图  1  研究区表层沉积物站位与周边主要河流分布(海洋环流据Huh and Su, 1999

      Fig.  1.  Locations of surface sediments and distribution of main rivers around the study area(modified from Huh and Su, 1999)

      图  2  东海东北部海域表层沉积物平均粒径趋势和粘土粒级含量分布

      Fig.  2.  Distribution of clay components and mean grain size of surface sediments in the northeast East China Sea

      图  3  东海东北部海域表层沉积物黏土矿物分布

      Fig.  3.  Distribution of clay minerals in surface sediments of the northeast East China Sea

      图  4  伊利石+高岭石、绿泥石、蒙皂石物源判别三角图

      Fig.  4.  Trigonometric map of provenance discrimination of illite+kaolinite, chlorite and montmorillonite

      图  5  东海东北部海域表层沉积物黏土矿物来源及输运

      Fig.  5.  Sources and transport of clay minerals in surface sediments in the northeastern East China Sea

      表  1  东海东北部与周边主要河流及陆架表层沉积物黏土矿物相对含量(%)

      Table  1.   Relative content of clay minerals in surface sediments of main rivers and continental shelf in northeastern East China Sea

      样品 纬度(°) 经度(°) 分类 伊利石 绿泥石 高岭石 蒙皂石 伊利石+高岭石 数据来源
      1 126.25 31.00 H 59.9 19.5 12.2 8.5 72.1 本文
      2 126.18 30.84 H 59.3 20.3 11.0 9.3 70.3 本文
      3 126.11 30.67 H 57.0 21.7 13.0 8.3 70.0 本文
      4 126.04 30.50 H 60.0 20.2 10.9 8.9 70.9 本文
      6 126.57 30.72 H 60.8 20.6 10.9 7.7 71.7 本文
      7 126.50 30.55 H 60.5 20.7 11.3 7.6 71.8 本文
      8 126.42 30.38 H 60.7 21.0 9.9 8.4 70.6 本文
      9 126.35 30.21 H 60.0 20.4 11.2 8.4 71.2 本文
      10 126.21 29.87 H 62.4 20.0 10.4 7.2 72.8 本文
      11 126.28 30.04 H 63.2 19.2 10.0 7.7 73.2 本文
      12 126.14 29.70 T 64.8 21.4 9.0 4.9 73.8 本文
      13 126.06 29.53 H 62.5 20.8 9.4 7.3 71.9 本文
      14 126.00 29.36 H 63.1 19.6 12.2 5.1 75.3 本文
      15 127.10 30.93 T 62.5 21.7 9.8 6.0 72.3 本文
      16 127.03 30.76 C 66.3 20.2 9.2 4.2 75.5 本文
      17 126.96 30.59 C 65.9 20.1 10 4.0 75.9 本文
      18 126.89 30.43 C 67.4 19.4 8.3 4.9 75.7 本文
      19 126.82 30.26 C 67.4 18.8 9.7 4.2 77.1 本文
      20 126.67 29.92 H 59.4 19.2 11.5 9.9 70.9 本文
      21 126.60 29.75 T 64.7 21.7 8.4 5.1 73.1 本文
      22 126.53 29.58 C 65.9 21.2 9.4 3.6 75.3 本文
      23 126.45 29.41 T 64.0 21.2 9.9 4.9 73.9 本文
      24 126.38 29.24 C 67.4 20.0 9.0 3.6 76.4 本文
      25 126.31 29.07 T 65.7 22.3 9.2 2.7 74.9 本文
      26 126.24 28.91 T 65.4 21.2 9.8 3.7 75.2 本文
      27 126.16 28.74 C 66.7 20.6 8.6 4.4 75.3 本文
      28 126.09 28.57 C 67.7 21.2 8.2 2.9 75.9 本文
      29 126.02 28.40 C 66.3 22.0 8.7 2.9 75.0 本文
      30 127.56 30.98 T 62.5 25.2 9.9 2.3 72.4 本文
      31 127.49 30.81 T 60.7 25.1 9.6 4.6 70.3 本文
      32 127.42 30.64 T 65.2 22.7 9.3 2.7 74.5 本文
      33 127.34 30.47 T 65.0 21.4 9.8 3.8 74.8 本文
      34 127.27 30.31 T 64.3 22.4 9.2 4.1 73.5 本文
      35 127.20 30.14 C 65.9 21.7 9.2 3.3 75.1 本文
      36 127.13 29.97 C 66.6 21.4 8.9 3.1 75.5 本文
      37 127.06 29.80 C 66.3 20.7 9.0 3.9 75.3 本文
      38 126.98 29.63 C 67.8 21.0 8.7 2.6 76.5 本文
      39 126.91 29.46 C 68.0 20.0 8.4 3.6 76.4 本文
      40 126.84 29.29 C 66.1 22.3 8.4 3.3 74.5 本文
      41 126.77 29.12 T 64.6 23.9 8.5 2.9 73.1 本文
      42 126.69 28.95 C 68.1 21.0 7.9 3.0 76.0 本文
      43 126.62 28.79 T 64.8 22.9 8.8 3.5 73.6 本文
      44 126.55 28.62 C 67.7 21.3 7.8 3.2 75.5 本文
      45 126.48 28.45 T 66.0 23.1 8.4 2.5 74.4 本文
      46 126.41 28.28 T 65.7 23.2 8.4 2.7 74.1 本文
      47 126.33 28.11 C 67.4 22.5 8.0 2.2 75.4 本文
      48 127.95 30.86 T 65.7 25.3 9.0 0 74.7 本文
      49 127.88 30.69 T 65.8 23.0 8.3 3.0 74.1 本文
      50 127.81 30.52 T 62.6 24.7 8.4 4.3 71.0 本文
      51 127.73 30.35 T 66.5 24.1 9.4 0 75.9 本文
      52 127.66 30.19 T 63.4 23.6 8.3 4.7 71.7 本文
      53 127.59 30.02 T 64.3 23.5 9.1 3.2 73.4 本文
      54 127.52 29.85 T 63.0 23.8 8.7 4.4 71.7 本文
      55 127.45 29.68 T 62.8 25.6 8.4 3.2 71.2 本文
      56 127.37 29.51 C 65.7 21.2 9.4 3.7 75.1 本文
      57 127.30 29.34 T 63.9 23.0 8.9 4.2 72.8 本文
      58 127.23 29.17 T 64.0 23.0 8.2 4.7 72.2 本文
      59 127.16 29.00 T 63.5 23.2 9.3 4.0 72.8 本文
      60 127.08 28.83 T 62.6 22.3 9.0 6.1 71.6 本文
      61 127.01 28.66 C 66.1 20.3 8.0 5.7 74.1 本文
      62 126.94 28.50 C 67.2 21.5 7.3 4.1 74.5 本文
      63 126.87 28.30 C 69.2 20.4 7.8 2.6 77.0 本文
      64 126.80 28.16 C 68.2 21.2 8.2 2.5 76.4 本文
      65 127.40 28.55 C 66.2 22.6 6.5 4.7 72.7 本文
      66 127.33 28.38 C 65.7 20.7 8.4 5.3 74.1 本文
      67 127.26 28.29 C 69.8 21.4 6.1 2.7 75.9 本文
      68 127.19 28.04 C 69.5 23.1 5.8 2.6 75.3 本文
      69 128.87 30.96 C 69.2 20.7 7.6 2.5 76.8 本文
      70 128.80 30.79 C 68.8 21.0 7.5 2.7 76.3 本文
      71 128.73 30.62 C 69.5 20.5 8.1 1.8 77.6 本文
      72 128.65 30.45 C 66.4 22.0 7.9 3.7 74.3 本文
      73 128.58 30.28 C 69.4 21.3 5.9 3.4 75.3 本文
      74 128.51 30.11 C 68.6 21.3 7.0 3.1 75.6 本文
      75 128.44 29.94 T 64.2 22.8 8.8 4.3 73.0 本文
      76 128.37 29.78 C 69.3 20.1 7.3 3.2 76.6 本文
      77 128.29 29.61 C 66.1 22.1 7.1 4.8 73.2 本文
      78 128.22 29.44 C 68.9 19.1 8.3 3.8 77.2 本文
      79 128.15 29.27 T 63.9 22.3 8.1 5.8 72.0 本文
      80 128.07 29.10 C 67.7 20.6 7.1 4.6 74.8 本文
      81 128.00 28.93 C 69.3 19.5 6.9 4.3 76.2 本文
      标准偏差 2.9 1.6 1.4 2.0 1.9 本文
      黄河 62.0±0.5 16.0±2.4 10.0±0.8 12.0±1.2 72.0 Yang et al.(2003)
      黄河 62.0 12.0 10.0 16.0 72.0 杨作升(1988)
      废黄河 63.7 8.3 7.7 20.3 71.4 梁小龙等(2015)
      黄海西南泥质区 70.0 7.0 7.0 16.0 77.0 Wang et al.(1999)
      黄海中部泥质区 66.0±1.3 12.0±0.7 10.0±0.5 13±1.0 76.8 Park and Khim(1992)
      南黄海 62.2 9.9 12.8 15.0 75.0 蓝先洪等(2011a)
      汉江 63.0 18.4 18.3 0.4 81.3 梁小龙等(2015)
      锦江 59.3 17.4 18.9 4.4 78.2 Yang et al.(2003)
      荣山江 63.9 16.8 19.2 0.1 83.1 Park and Khim(1992)
      长江 67.9±0.5 12.7±0.3 13.9±1.0 5.5±0.1 81.8 梁小龙等(2015)
      长江 67.7±0.7 12.1±0.9 14.3±1.4 5.9±0.4 82.0 Ren and Shi(1986)
      长江 65.5±2.9 15.6±2.6 14.5±1.6 4.3±1.3 80.0 何良彪(1989)
      长江口 67.5±3.3 18.1±2.4 8.7±0.1 5.7±1.1 76.2 Xu et al.(2009)
      钱塘江 64.4 18.8 13.8 3.4 78.2 Xu et al.(2012)
      瓯江河口 64.5 17.7 14.7 2.9 79.2 梁小龙等(2015)
      东海内陆架 68.7 16.3 10.0 5.3 78.7 Liu et al.(2014)
      台湾西部河流 69.0±1.8 30.0±2.3 1.0±1.3 0±0.1 70.0 徐勇航等(2013)
      台湾西部河流 70.0±0.8 29.0±1.3 1.0±1.3 0±0.1 71.0 李传顺等(2012)
      台湾东部河流 77.0±7.6 23.0±4.4 0±3.4 0±0.1 77.0 Li et al.(2012)
      台湾海峡 65.3±2.1 23.3±2.2 6.5±2.7 4.0±2.0 71.8 Xu et al.(2009)
      注:表中n±1,n为均值,1为标准偏差.
      下载: 导出CSV

      表  2  东海东北部海域表层沉积物黏土矿物分类统计

      Table  2.   Classification and statistics of clay minerals in surface sediments of the northeastern East China Sea

      类别 样品数(个) 伊利石(%) 绿泥石(%) 高岭石(%) 蒙皂石(%)
      T 29 64.2±1.3 23.2±1.3 9.0±0.6 3.7±1.5
      C 38 67.5±1.3 20.9±1.0 8.9±1.0 3.5±0.9
      H 13 60.7±1.8 20.2±0.7 11.1±1.0 8.0±1.2
      注:表中n±1,n为均值,1为相对偏差.
      下载: 导出CSV
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