论文

长江口北槽深水航道工程对周边滩涂冲淤影响研究

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  • 1. 华东师范大学河口海岸国家重点实验室, 上海, 200062;
    2. 苏州科技学院城市与环境学系, 江苏, 苏州, 215011

收稿日期: 2006-02-12

  修回日期: 2006-07-11

  网络出版日期: 2007-05-20

基金资助

上海市重大攻关项目(04DZ12049);华东师范大学河口海岸国家重点实验室开放基金(200508);国家自然科学基金项目(40576043)资助

Influence of Deep-Water Channel Project at North Passage of the Yangtze River on Erosion and Accumulation of Hengsha East Shoal and Jiuduansha Shoal

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  • 1. State Key Lab of Estuarine & Coastal Research, East China Normal University, Shanghai 200062;
    2. City and Environment Department, Suzhou University of Science and Technology, Suzhou, Jiangsu 215011

Received date: 2006-02-12

  Revised date: 2006-07-11

  Online published: 2007-05-20

摘要

采用长江口深水航道治理一、二期工程实施前后的地形资料,在G IS软件及相关的统计分析软件的支持下,分析治理工程对九段沙(包括江亚南沙)和横沙东滩冲淤演变的影响。结果表明:工程建设6年来两岸滩涂面积增长了97 km2,其中横沙东滩优先采取了促淤工程,淤积规模较大,滩地面积累计增长了46 km2,是工程前的1.68倍;九段沙的淤积主要是受整治工程南导堤的影响,其中九段上沙及江亚南沙淤积最为强烈,工程后的面积分别是工程前的1.83倍和2.34倍。

本文引用格式

杜景龙, 杨世伦 . 长江口北槽深水航道工程对周边滩涂冲淤影响研究[J]. 地理科学, 2007 , 27(3) : 390 -394 . DOI: 10.13249/j.cnki.sgs.2007.03.390

Abstract

Based on the topographic maps drawn before and after the deep-water channel project of north pdzcassage and supported by the GIS software and correlative Stat.Software,this paper has described the influence of the regulation project on Jiuduansha Shoal and Hengsha East Shoal.The results show that the area of the shoals around the dykes has increased about 97 km2 since 1998.Hengsha East Shoal has increased about 46 km2 and become 1.68 times larger than before.The area of Jiuduanshangsha Shoal and Jiangyanansha Shoal has also increased greatly.They are 1.83 times and 2.34 times larger than those in 1998 respectively.The sudden accumulation of Jiuduanshangsha Shoal and Jiangyanansha Shoal attributes to the south bank of the project;at the same time,that of Hengsha East Shoal to the north bank of the project and the siltation-promoting project.

参考文献

[1] 赵庚星,张万清,李玉环,等.GIS支持下的黄河口近期淤、蚀动态研究[J].地理科学,1999,19(5):442~445.
[2] 沈金山,朱金妹,张新琴.长江口拦门沙的成因和演变[J].海洋与湖沼,1983,14(6):582~590.
[3] 徐海根.上海市海岛资源综合调查报告——潮间带沉积地貌[M].上海:上海市科学技术出版社,1996.72~87.
[4] Shi-lun Yang,Qing-ying Zhao,Igor M Belkin.Temporal variation in the sediment load of the Yangtze river and the influencesof human activities[J].Journal of Hydrology,2002,263(3):56-71.
[5] 杨世伦,贺松林,谢文辉.长江口九段沙的形成演变及其与南北槽发育的关系[J].海洋工程,1998,16(4):55~65.
[6] 师长兴.黄河河口延伸与下游淤积关系研究中的问题分析[J].地理科学,2005,25(2):183~190.
[7] 吴华林,沈焕庭,胡辉,等.GIS支持下的长江口拦门沙泥沙冲淤定量计算[J].海洋学报,2002,24(2):126~132.
[8] 施少华,林承坤,杨桂山.长江中下游河道岸线的整治与开发利用[J].地理科学,2002,22(6):700~705.
[9] 恽才兴.长江河口潮滩冲淤和滩槽泥沙交换[J].泥沙研究,1983,94(4):43~52.
[10] 赵庆英,杨世伦,朱骏.河口河槽季节性冲淤变化及其对河流来水来沙响应的统计分析——以长江口南槽为例[J].地理科学,2003,23(1):112~118.
[11] 李茂田,丁霞,陈中原.40年来长江九江河段河道演变及其趋势预测[J].地理科学,2004,24(1):76~80.
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