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珠江口磨刀门泥沙絮凝特征

邓智瑞 何青 杨清书 林建良

邓智瑞, 何青, 杨清书, 林建良. 珠江口磨刀门泥沙絮凝特征[J]. 海洋学报, 2015, 37(9): 152-161.
引用本文: 邓智瑞, 何青, 杨清书, 林建良. 珠江口磨刀门泥沙絮凝特征[J]. 海洋学报, 2015, 37(9): 152-161.
Deng Zhirui, He Qing, Yang Qingshu, Lin Jianliang. Observations of in situ flocs characteristic in the Modaomen Estuary of the Pearl River[J]. Haiyang Xuebao, 2015, 37(9): 152-161.
Citation: Deng Zhirui, He Qing, Yang Qingshu, Lin Jianliang. Observations of in situ flocs characteristic in the Modaomen Estuary of the Pearl River[J]. Haiyang Xuebao, 2015, 37(9): 152-161.

珠江口磨刀门泥沙絮凝特征

基金项目: 国家自然科学基金项目(41276080,41476073,51320105005);科技部科技基础性工作专项重点项目"中国典型河口动力沉积地貌本底数据调查"(2013FY112000)。

Observations of in situ flocs characteristic in the Modaomen Estuary of the Pearl River

  • 摘要: 本文利用激光粒度仪实测得到珠江口磨刀门河口2013年夏季悬浮泥沙现场絮凝及絮凝体特征,同时对比悬沙分散粒径和含沙量,研究表明:悬沙分散粒径平均值为27.9 μm,现场实测絮团粒径平均值为91.6 μm,表明磨刀门口外的悬浮泥沙絮凝现象显著;实测絮团平均粒径变化范围为13.0~273.8 μm,小潮期间絮团粒径平均值为131.5 μm,大于大潮平均值76.9 μm;絮凝体粒径在垂向上的变化表现为由表及底先变大再变小。絮团体积浓度、沉速与粒径的关系在不同情况下有差异,体积浓度和絮团粒径在表层和中层有明显正相关关系,絮团沉速在大潮时刻随着粒径的增大而增大。综合分析影响絮凝的因素,得知在珠江口盐度对于絮团大小影响不明显;而流速大小的差异是影响大小潮之间絮团大小不同的主要因素。研究结果有助于了解珠江口细颗粒泥沙输移特性和相关生物化学过程。
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  • 收稿日期:  2015-01-22
  • 修回日期:  2015-04-09

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