长江流域资源与环境 >> 2010, Vol. 19 >> Issue (12): 1433-.

• 生态环境 • 上一篇    下一篇

长江口南港近期的演变及其与重大工程之间的关系

张志林|胡国栋|朱培华|廖建英   

  1. (长江水利委员会长江口水文水资源勘测局|上海 200136)
  • 出版日期:2010-12-20

CURRENT EVOLUTION OF THE SOUTH CHANNEL OF THE YANGTZEESTUARY AND ITS IMPACTS ON MAJOR PROJECTS

ZHANG Zhilin| HU Guodong| ZHU Peihua| LIAO Jianying   

  1. (The Survey Bureau of the Hydrology and Water Resources of Changjiang Estuary,Changjiang Water Resources Commission,Shanghai 200136,China)
  • Online:2010-12-20

摘要:

长江口为典型的多级分汊中等潮汐河口,口门宽阔、径潮流强劲、泥沙运动复杂、河槽交替多变,给河口综合治理带来困难。长江口各分流汊道演变过程中,此消彼长是永恒的主旋律,其产生、发展、扭曲、萎缩、消亡具有周期性演变规律。为发挥长江黄金水道的优势,促进国民经济发展,长江口先后实施了深水航道治理工程、南北港分流口处的新浏河沙护滩和南沙头通道限流工程,以及中央沙促淤圈围工程和青草沙水源地工程等,南北港和南北槽分流口河段得到有效控制,对长江口未来的演变产生深远影响。基于南北港分流口以下丰富的地形、水文现场资料,对近年来南港地形演变进行了深入分析,在肯定工程稳定河势的同时,认为目前南北港分流口以下,尚存在南港主流偏离南岸致使发生近岸淤积,以及瑞丰沙中下段沙体刷深导致水流分散,不利于河势稳定等问题。并探讨了长江口“先下后上”治理模式的优缺点,建议在长江口河势尚未发生较大变化时,站在整体的高度,综合考虑河势、航道、水土资源、防洪潮及排灌、生态环境保护等诸多因素,尽快实施长江口综合整治工程。

Abstract:

The Yangtze Estuary is a typical medium tidal estuary with multiorder bifurcations.Its significant width,strong tidal flows,complicated sediment movement,and the diversity of alternated channel and floodplain contribute the difficulties of comprehensive regulation of the estuary.During the evolution of multiple branches,the balance of one branch developing and the other decaying among these branches is always the constant rule;meanwhile,the cycle of creation,development,distortion,decay and disappearance for an individual branch presents a periodic evolution law.In order to strengthen the benefits of the“golden”waterway of the Yangtze River,and contribute to the domestic economic development,a series of projects have been carried out recently,including the Yangtze Estuary deepwater channel regulation,sand protection project of the Xinliuhe sand at the diversion between the South and North Channel,Nanshatou project of constraining flow,the enclosure at Zhongyangsha and protecting the water source site at Qingcaosha etc.As a result,the diversion of the South and North Channel has been stabilized effectively,and the future evolution of the Yangtze Estuary will be influenced significantly.This paper presented that based on abundant topographical and hydrological data of downstream the diversion of the South and North Channel,thorough analysis of the recent evolution of the South Channel,South and North Passages were conducted.Affirming that the projects contribute to the stabilization of river regime,the paper also pointed out that the following problems still exist at the downstream diversion of the South and North Channel.Sedimentation occurs close to the South incurred by the main flow of the South Channel deviating from the south bank.Scour and deepening at the middle and end sections of Ruifeng Sandbar causes flow dispersion,and has negative impacts on the stabilization of river regime and etc.Besides,the paper also discussed the advantages and disadvantages of the“downstream prior to upstream”pattern of regulation,and suggested that with strategic considerations of riverregime,navigable channel,soil and water resources conservation,flood and tide protection,drainage and irrigation,ecological environment protection and other factors,before the current Yangtze Estuary regime occurs significant alternation,and the comprehensive treatment projects of the Yangtze Estuary should be implemented as soon as possible.

No related articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 吴开亚, 王玲杰. 巢湖流域大气污染的经济损失分析[J]. 长江流域资源与环境, 2007, 16(6): 781 .
[2] 陈德敏,池尔敏,李世龙. 重庆市工业化进程与新型工业化道路探析[J]. 长江流域资源与环境, 2006, 15(2): 147 -151 .
[3] 刘良国|杨品红|杨春英|邹万生|王文彬|韩 庆. 湖南境内澧水鱼类资源现状与多样性研究[J]. 长江流域资源与环境, 2013, 22(8): 1165 .
[4] 谢 涛| 纪道斌| 刘德富| 朱冠霖| 张 宇| 向经文. 三峡水库库首水温监测及初步分析[J]. 长江流域资源与环境, 2013, 22(8): 1201 .
[5] 梁流涛|曲福田|冯淑怡. 经济发展与农业面源污染:分解模型与实证研究[J]. 长江流域资源与环境, 2013, 22(11): 1369 .
[6] 王亚力,吴云超,赵 迪,熊建新. 基于流动人口特征的环洞庭湖区县域城镇化的水平和性质分析[J]. 长江流域资源与环境, 2014, 23(11): 1519 .
[7] 李飞, 董锁成, 武红, 李泽红, 于会录. 中国东部地区农业环境-经济系统耦合度研究[J]. 长江流域资源与环境, 2016, 25(02): 219 -225 .
[8] 赵丽, 姜霞, 王雯雯, 王书航, 常乐, 陈俊伊. 丹江口水库表层沉积物不同形态氮的赋存特征及其生物有效性[J]. 长江流域资源与环境, 2016, 25(04): 630 -637 .