南京大学学报(自然科学版) ›› 2014, Vol. 50 ›› Issue (5): 679–686.

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不同围填海方案对南黄海辐射沙脊群海域的冲淤影响研究

赵 强1,2,*,曹 维1,蔡燕红1   

  • 出版日期:2014-09-12 发布日期:2014-09-12
  • 作者简介:(1.国家海洋局宁波海洋环境监测中心,宁波315040;2.中国海洋大学物理海洋实验室,青岛,266003)

Study on reclamation impact on sedimentary erosion and deposition in radial tidal sand ridge system in the South Yellow Sea

Zhao Qiang1, 2, Cao Wei1, Cai Yanhong1   

  • Online:2014-09-12 Published:2014-09-12
  • About author:(1. Ningbo Marine Environment Monitoring Center, SOA, Ningbo, 305040, China;
    2. Laboratory of Physical Oceanography, Ocean University of China, Qingdao, 266003, China)

摘要: 本文采用MIKE21二维水动力模型模拟了南黄海辐射沙脊群海域的潮流形态,模拟结果与实测潮流基本一致。在此基础上,比较了三套不同围填海方案对工程附近区域的冲淤影响。从整体上看,三套方案都会对工程周边海域的海底冲淤产生明显影响。条子泥围填海工程后在其北部产生淤积,在东南部产生冲刷。东沙和高泥两座人工岛的建立使原本以弶港为中心扇形辐聚、辐散的潮流格局有所改变,潮流进出主要集中在西洋水道南端和黄沙洋水道西端这两条潮流通道,通道内流速增大,产生冲刷;而两人工岛东部和弶港东部海域产生淤积。基于目前的模拟结果,只建设高泥和东沙两座人工岛更有利于维持西洋水道和黄沙洋水道的畅通,对近岸港口资源具有保护作用。

Abstract: In order to study the reclamation impact on sedimentary erosion and deposition by reclamation projects in the radial tidal sand ridge system in the South Yellow Sea, the two-dimensional hydrodynamic model, MIKE21, was applied to simulate the tidal currents, and erosion and deposition were calculated using empirical formula. Then the sediment erosions and depositions caused by three different kinds of reclamation projects are calculated. Three cases of reclamation project were numerical tested. They were Tiaozini reclamation project (Case 1), Dongsha and Gaoni reclamation project (Case 2), and Case 3 was a combination of Case 1 and Case 2. All the three cases showed obvious impacts on the sedimentary erosion and deposition. In Case 1, sedimentary deposition occurred on the north of Tiaozini and erosion occurred on the south of it. In Case 2, the fan-shaped, Jianggang centered tidal current system was changed, and the tidal currents were constrained to the two water channels of Xiyang and Huangshayang, which induced velocity increasing and sedimentary erosion in the channels. While depositions occurred at the east of Dongsha and Gaoni. In Case 3, the erosion and deposition areas were similar to the combined impacts of the former cases. Based on the model results, Case 2 was the appropriate case for keeping the tidal channel unimpeded and protecting the harbor resources

[1] 任美锷. 江苏省海岸带和海涂资源综合调查报告.北京: 海洋出版社, 1986.
[2] 吴德安. 江苏辐射沙洲水道潮流及悬沙动力研究. 博士学位论文. 南京: 南京师范大学, 2004.
[3] Liu Z X, Huang Y C, Zhang Q N. Tidal current ridges in the southwestern Yellow Sea. Journal of Sedimentary Petrology, 1989, 59: 432~437.
[4] Jung K T, Park C W, Oh I S, et al. An analytical model with three sub-regions for M2 tide in the Yellow Sea and the East China Sea. Ocean Science Journal, 2005, 40: 191~200.
[5] 郭 磊, 杨树森. 江苏如东人工岛工程对周边海域水动力的影响. 水道港口, 2009, 30(5): 342~346.
[6] Xing F, Wang Y P, Wang H V. Tidal hydrodynamics and fine-grained sediment transport on the radial sand ridge system in the southern Yellow Sea. Marine Geology, 2012, 291-294: 192~210
[7] 陆丽云, 张忍顺, 陈 君. 江苏沿海辐射沙洲开发利用的前景. 南京师范大学学报(自然科学版), 2002, 25(3): 18~24.
[8] 张振东. 江苏近海辐射沙脊群人工岛建设工程问题初探. 淮海工学院学报, 2010, 19(3): 89~92.
[9] 窦国仁, 董凤舞, 窦希萍, 等. 河口海岸泥沙数学模型研究. 中国科学(A辑), 1999, 25(9): 995~1001.
[10] 曹文洪, 舒安平. 潮流和波浪作用下悬移质挟沙能力研究述评. 泥沙研究, 1999, (5): 74~80.
[11] 曹文洪, 张启舜. 潮流和波浪作用下悬移质挟沙能力的研究. 泥沙, 1999 (5): 16~21.
[12] 王义勇. 江苏岸外沙洲围填规模适宜性研究—以条子泥、高泥、东沙为例. 硕士学位论文. 南京: 南京师范大学, 2011.
[13] 卫晓庆, 陈 君, 周 永. 江苏条子泥匡围工程对临近水道流场影响分析. 人民长江, 2013, 44(9): 79~83.
[14] 吴德安, 张忍顺, 严以新等. 江苏辐射沙洲潮流水道挟沙力的分析与构建. 水动力学研究与进展(A辑), 2007, 22(3): 371-379.
[15] 吴德安, 张忍顺, 童朝锋. 东大港水道水体含沙量的变化及垂线分布. 海洋科学, 2007, 31(11): 55~60
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