木兰溪河口及邻近海域春季水文环境特征及悬沙输移机制分析

赵金鹏, 范代读, 涂俊彪, 张悦, 刘伟. 木兰溪河口及邻近海域春季水文环境特征及悬沙输移机制分析[J]. 海洋地质与第四纪地质, 2018, 38(1): 32-40. doi: 10.16562/j.cnki.0256-1492.2018.01.004
引用本文: 赵金鹏, 范代读, 涂俊彪, 张悦, 刘伟. 木兰溪河口及邻近海域春季水文环境特征及悬沙输移机制分析[J]. 海洋地质与第四纪地质, 2018, 38(1): 32-40. doi: 10.16562/j.cnki.0256-1492.2018.01.004
ZHAO Jinpeng, FAN Daidu, TU Junbiao, ZHANG Yue, LIU Wei. Hydrological characteristics and suspended sediment transport mechanism in spring at the Mulan Estuary and its adjacent seas[J]. Marine Geology & Quaternary Geology, 2018, 38(1): 32-40. doi: 10.16562/j.cnki.0256-1492.2018.01.004
Citation: ZHAO Jinpeng, FAN Daidu, TU Junbiao, ZHANG Yue, LIU Wei. Hydrological characteristics and suspended sediment transport mechanism in spring at the Mulan Estuary and its adjacent seas[J]. Marine Geology & Quaternary Geology, 2018, 38(1): 32-40. doi: 10.16562/j.cnki.0256-1492.2018.01.004

木兰溪河口及邻近海域春季水文环境特征及悬沙输移机制分析

  • 基金项目:
    科技基础性工作专项“典型中小入海河流河口动力沉积地貌与环境本底数据调查”(2013FY112200);中国东盟海上合作基金“长江三角洲与红河三角洲全新世沉积演化对比研究”;国家自然科学基金项目“全新世长江口低氧区形成与演化历史及控制机制”(41476031)
详细信息
    作者简介: 赵金鹏(1993—),男,硕士生,主要从事沉积动力学研究,E-mail:king_747441819@qq.com
    通讯作者: 范代读(1972—),男,教授,从事海洋地质研究,E-mail: ddfan@tongji.edu.cn
  • 中图分类号: X141

  • 周立君编辑

Hydrological characteristics and suspended sediment transport mechanism in spring at the Mulan Estuary and its adjacent seas

More Information
  • 基于2016年春季航次观测数据,分析了木兰溪河口及邻近海域温度、盐度及浊度等水文环境要素特征;并运用通量机制分解法分析该区兴化湾南日水道连续观测站位资料,以揭示该海域悬沙输移的控制机制。结果表明,春季兴化湾及邻近海域温盐变化受木兰溪径流、浙闽沿岸流和台湾暖流共同控制,湾外东南侧海域受高温高盐台湾暖流控制,西北侧近岸海域受低温低盐的浙闽沿岸流显著影响。调查海域悬沙浓度总体较低,外海泥沙通过南日水道向兴化湾内输移,但净输运量非常有限,仅为0.32×10-4kg/(m·s)。平流输沙与潮泵输沙是南日水道泥沙净输运的主要机制,底沙再悬浮作用较显著,且剪切扩散效应也不容忽视。

  • 加载中
  • 图 1  2016年春季航次木兰溪河口及邻近海域水文调查站位图

    Figure 1. 

    图 2  2016年春季兴化湾及邻近海域表层(a)、底层(b)温度分布图

    Figure 2. 

    图 3  2016年春季兴化湾邻近海域表层(a)、底层(b)盐度分布图

    Figure 3. 

    图 4  2016年春季兴化湾及邻近海域表层(a)、底层(b)浊度分布图

    Figure 4. 

    图 5  FJ3断面盐度(上)、温度(下)分布图

    Figure 5. 

    图 6  FJ4断面盐度(上)、温度(下)分布图

    Figure 6. 

    图 7  FJ4-7站两个潮周期流速、温度、盐度与浊度的变化特征

    Figure 7. 

    表 1  观测方法及仪器参数设置

    Table 1.  Method of observation and instrumental parameters

    仪器/布放方式 观测参数 采样方式
    Campbell OBS 3A/绞车 浊度 1Hz,表中底或六点法观测,每层位观测2min左右
    CTD/绞车 温、盐、深 同OBS
    Flowquest ADCP 600k/船舷固定,探头朝下 流速 2Hz,连续观测,bin:0.5m,ping:120
    双频测深仪/船舷固定,探头距水面约30cm 水位变化 连续测量
    下载: 导出CSV

    表 2  各项悬沙输沙量及其所占百分比

    Table 2.  Distribution of suspended sediment transport influenced by different factors in Xinghua Bay

    T1 T2 T3 T4 T5 T6 T7 T8 T
    输沙量(10-4kg/(m·s)) 1 -0.065 0.016 -1.1 0.11 -0.0025 -0.64 0.35×10-4 -0.32
    占总输沙量之比(%) 40.5 2.22 1.37 37.64 3.84 0.08 15.62 0.0014
    下载: 导出CSV
  • [1]

    Tian T, Merico A, Su J, et al. Importance of resuspended sediment dynamics for the phytoplankton spring bloom in a coastal marine ecosystem[J]. Journal of Sea Research, 2009, 62(4):214-228. doi: 10.1016/j.seares.2009.04.001

    [2]

    Liu J T, Hsu R T, Hung J J, et al. From the highest to the deepest: The Gaoping River-Gaoping Submarine Canyon dispersal system[J]. Earth-Science Reviews, 2016, 153:274-300. doi: 10.1016/j.earscirev.2015.10.012

    [3]

    Milliman J D, Farnsworth K L. River Discharge to the Coastal Ocean——A Global Synthesis[M]// River discharge to the coastal ocean: a global synthesis. 2011.

    [4]

    Liu J P, Liu C S, Xu K H, et al. Flux and fate of small mountainous rivers derived sediments into the Taiwan Strait[J]. Marine Geology, 2008, 256(1): 65-76. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dc54df5d21a0280d8807d0991ae92ed1

    [5]

    高建华, 高抒, 董礼先, 等.鸭绿江河口地区沉积物特征及悬沙输送[J].海洋通报, 2003, 22(5):26-33. doi: 10.3969/j.issn.1001-6392.2003.05.005

    GAO Jianhua, GAO Shu, DONG Lixian, et al. Sediment distribution and suspended sediment transport in Yalu River Estuary[J]. Marine Science Bulletin, 2003, 22(5):26-33. doi: 10.3969/j.issn.1001-6392.2003.05.005

    [6]

    陈斌, 印萍, 高飞, 等.滦河口水文环境要素季节性变化特征及动力响应关系[J].海洋环境科学, 2015, 34(5):729-735. http://www.cnki.com.cn/Article/CJFDTotal-HYHJ201505015.htm

    CHEN Bin, YIN Ping, GAO Fei, LIU Jinqing, et al. Seasonal variation characteristics of hydrological environment factors and dynamic response relationship in Luanhe Estuary[J].Marine Environment Science, 2015, 34(5):729-735.

    [7]

    赵建春, 戴志军, 李九发, 等.强潮海湾近岸表层沉积物时空分布特征及水动力响应——以杭州湾北岸为例[J].沉积学报, 2008, 26(6): 1043-1051. http://www.cnki.com.cn/Article/CJFDTotal-CJXB200806020.htm

    ZHAO Jianchun. Study on the characteristics of temporal and spatial changes in properties of surface sediment on near-shore seabed of strong-tide Bay: a case from the north bank of Hangzhou Bay in Shanghai[J]. Acta Sedimentologica Sinica, 2008, 26(6): 1043-1051.

    [8]

    陈小英, 刘金庆, 郭磊, 等.胶州湾大沽河河口近岸海域短时间尺度沉积动力过程[J].海洋地质与第四纪地质, 2016, 36(6):45-50. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201606006

    CHEN Xiaoying, LIU Jinqing, GUO Lei, et al. Short term depositional dynamic processes at Duge River Mouth of Jiaozhou Bay[J]. Marine Geology & Quaternary Geology, 2016, 36(6):45-50. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201606006

    [9]

    郭琳, 陈植华.椒江口-台州湾悬浮泥沙分布特征遥感研究[J].武汉理工大学学报, 2007, 29(5):49-52. doi: 10.3321/j.issn:1671-4431.2007.05.015

    GUOLin, CHEN Zhihua.Remote sensing research on the distributed characteristics of suspended matter in Jiaojiang Estuary and Taizhou Gulf[J].Journal of Wuhan University of Technology, 2007, 29(5):49-52. doi: 10.3321/j.issn:1671-4431.2007.05.015

    [10]

    Rao V P, Shynu R, Kessarkar P M, et al. Suspended sediment dynamics on a seasonal scale in the Mandovi and Zuari estuaries, central west coast of India[J]. Estuarine Coastal & Shelf Science, 2011, 91(1):78-86. https://www.sciencedirect.com/science/article/pii/S0272771410003495

    [11]

    Priya K L, Jegathambal P, James E J. On the factors affecting the settling velocity of fine suspended sediments in a shallow estuary[J]. Journal of Oceanography, 2015, 71(2):1-13. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=a69f85b24b9a6f2fb81ba4c48bc14907

    [12]

    李孟国.兴化湾水文泥沙特征分析[J].水道港口, 2001, 22(4):156-159. doi: 10.3969/j.issn.1005-8443.2001.04.002

    LI Mengguo. Hydrographic and sediment analyses of Xinghua Bay[J]. Journal of Waterway & Harbor, 2001, 22(4):156-159. doi: 10.3969/j.issn.1005-8443.2001.04.002

    [13]

    高劲松, 周良明.兴化湾的潮流研究[J].海岸工程, 2009, 28(4):1-10. doi: 10.3969/j.issn.1002-3682.2009.04.001

    GAO Jinsong, ZHOU Liangming. Study on tide current of the Xinghua Bay[J]. Coastal Engineering, 2009, 28(4):1-10. doi: 10.3969/j.issn.1002-3682.2009.04.001

    [14]

    童朝锋, 王俊杰, 张青.兴化湾潮汐潮流特性及工程影响分析[J].水利水运工程学报, 2015(1):53-60. http://d.old.wanfangdata.com.cn/Periodical/slsykxyj201501008

    TONG Chaofeng, WANG Junjie, ZHANG Qing. Tidal regime and impacts of works in Xinghua bay on hydrodynamics[J].Hydro-Science and Engineering, 2015(1): 53-60. http://d.old.wanfangdata.com.cn/Periodical/slsykxyj201501008

    [15]

    童朝锋, 郑联枭, 孟艳秋, 等.兴化湾悬沙输移机理分析[J].水利水运工程学报, 2016(2):1-10. http://d.old.wanfangdata.com.cn/Periodical/slsykxyj201602001

    TONG Chaofeng, ZHENG Lianxiao, MENG Yanqiu, et al.Mechanism of suspended sediment transport in Xinghua bay[J].Hydro-Science and Engineering, 2016(2):1-10. http://d.old.wanfangdata.com.cn/Periodical/slsykxyj201602001

    [16]

    万新宁, 李九发, 何青, 等.国内外河口悬沙通量研究进展[J].地球科学进展, 2002, 17(6):864-870. doi: 10.3321/j.issn:1001-8166.2002.06.010

    WAN Xinning, LI Jiufa, HE Qing, et al. Review of suspended sediment flux in the world[J]. Advance in Earth Sciences, 2002, 17(6):864-870. doi: 10.3321/j.issn:1001-8166.2002.06.010

    [17]

    Hansen D V. Currents and Mixing in the Columbia River Estuary[J]. Ocean Science and Ocean Engineering, 1965, 2:943-955.

    [18]

    Fisher H B.Mixing and dispersion in estuaries[J].Annual Review of Fluid Mechanics, 1976, 8:107-133. doi: 10.1146/annurev.fl.08.010176.000543

    [19]

    Jay D A, Uncles R J, Largeir J, et al. A review of recent developments in estuarine scalar flux estimation[J]. Estuaries, 1997, 20(2):262-280. doi: 10.2307/1352342

    [20]

    Uncles R J, Easton A E, Griffiths M L, et al. Seasonality of the Turbidity Maximum in the Humber-Ouse Estuary, UK[J]. Marine Pollution Bulletin, 1999, 37(3-7):206-215. doi: 10.1016/S0025-326X(98)90157-6

    [21]

    王康墡, 苏纪兰.长江口南港环流及悬移物质输运的计算分析[J].海洋学报, 1987, 9(5):627-637. http://www.cnki.com.cn/Article/CJFDTotal-SEAC198705013.htm

    WANG Kangshan, SU Jilan. Analysis and calculation of circulation and suspended sediment transportation in the Yangtze Estuary[J]. Acta Oceanologica Sinica, 1987, 9(5):627-637. http://www.cnki.com.cn/Article/CJFDTotal-SEAC198705013.htm

    [22]

    万新宁, 李九发, 沈焕庭.长江口外海滨典型断面悬沙通量计算[J].泥沙研究, 2004(6):64-70. doi: 10.3321/j.issn:0468-155X.2004.06.012

    WAN Xinning, LI Jiufa, SHEN Huanting. Suspended sediment flux at the typical cross sections in the offshore area of Changjiang Estuary[J]. Journal of Sediment Research, 2004(6):64-70. doi: 10.3321/j.issn:0468-155X.2004.06.012

    [23]

    Yu Q, Wang Y P, Flemming B, et al. Tide-induced suspended sediment transport: Depth-averaged concentrations and horizontal residual fluxes[J]. Continental Shelf Research, 2012, 34(1):53-63. https://www.sciencedirect.com/science/article/pii/S0278434311003694

    [24]

    Becherer J, Flöser G, Umlauf L, et al. Estuarine circulation vs tidal pumping: Sediment transport in a well-mixed tidal inlet[J]. Journal of Geophysical Research Oceans, 2016, DOI: 10.1002/2016JCO∥640.

    [25]

    中国海湾志编纂委员会.中国海湾志(第七分册)[M].海洋出版社, 1994.

    Compilation Committee of China Bays. China Bay in Seventh Volumes (north of Fujian Bay)[M]. Beijing: China Ocean Press, 1994.

    [26]

    闫新兴, 刘国亭.福建兴化湾近岸地貌特征与泥沙来源分析[J].水道港口, 2012, 33(6):469-474. doi: 10.3969/j.issn.1005-8443.2012.06.002

    YAN Xinxing, LIU Guoting. Analysis of geomorphic characteristics and sediment source of near-shore area in Xinghua Bay[J]. Journal of Waterway & Harbor, 2012, 33(6):469-474. doi: 10.3969/j.issn.1005-8443.2012.06.002

    [27]

    Dyer K R. The salt balance in stratified estuaries[J]. Estuarine & Coastal Marine Science, 1974, 2(3):273-281. https://www.sciencedirect.com/science/article/abs/pii/0302352474900176

    [28]

    沈健, 沈焕庭, 潘定安, 等.长江河口最大浑浊带水沙输运机制分析[J].地理学报, 1995(5):411-420. doi: 10.3321/j.issn:0375-5444.1995.05.004

    SHEN Jian, SHEN Huanting, PAN Dingan, et al. Analysis of transport mechenism of water and suspended sediment in the turbidity maximum of the Changjiang Estuary [J]. Acta Geographica Sinica, 1995(5):411-420. doi: 10.3321/j.issn:0375-5444.1995.05.004

    [29]

    Dyer K R. Fine Sediment Particle Transport in Estuaries[M]// Physical Processes in Estuaries. Springer Berlin Heidelberg, 1988: 295-310. https://link.springer.com/chapter/10.1007%2F978-3-642-73691-9_16

    [30]

    Uncles R J, Elliott R C A, Weston S A, et al. Synoptic Observations of Salinity, Suspended Sediment and Vertical Current Structure in a Partly Mixed Estuary[M]// Physics of Shallow Estuaries and Bays. Springer-Verlag, 1986: 58-70. https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/LN016p0058

    [31]

    万小芳, 潘爱军, 郭小钢, 等.台湾海峡西侧水动力环境的季节变化特征[J].应用海洋学学报, 2013, 32(2):156-163. doi: 10.3969/J.ISSN.2095-4972.2013.02.002

    WAN Xiaofang, PAN Aijun, GUO Xiaogang, et al. Seasonal variation features of the hydrodynamic environment in the western Taiwan Strait[J]. Journal of Applied Oceanography, 2013, 32(2):156-163. doi: 10.3969/J.ISSN.2095-4972.2013.02.002

    [32]

    Gao S, Wang D, Yang Y, et al. Holocene sedimentary systems on a broad continental shelf with abundant river input: Process-product relationships[J]. Geological Society London Special Publications, 2015:1-37. https://www.researchgate.net/publication/281629535_Holocene_sedimentary_systems_on_a_broad_continental_shelf_with_abundant_river_input_Process-product_relationships

    [33]

    Su Y S, Weng X C. Water Masses in China Seas[M]// Oceanology of China Seas. Springer Netherlands, 1994: 3-16.

    [34]

    唐晓晖, 王凡.长江口邻近海域夏、冬季水文特征分析[J].海洋科学集刊, 2004:46-70.

    TANG Xiaohun, WANG Fan. Analyses on hydrographic structure in the Changjiang River Estuary adjacent waters in summer and winter[J]. Studia Marina Sinica, 2004:46-70.

  • 加载中

(7)

(2)

计量
  • 文章访问数:  1270
  • PDF下载数:  17
  • 施引文献:  0
出版历程
收稿日期:  2017-06-28
修回日期:  2018-01-10
刊出日期:  2018-02-28

目录