长江科学院院报 ›› 2020, Vol. 37 ›› Issue (12): 1-7.DOI: 10.11988/ckyyb.20200579

• 专家特约稿 • 上一篇    下一篇

长江下游澄通河段通州沙汊道演变新特征

余文畴1,2, 栾华龙1,2   

  1. 1.长江科学院 河流研究所,武汉 430010;
    2.长江科学院 水利部江湖治理与防洪重点实验室,武汉 430010
  • 收稿日期:2020-06-17 修回日期:2020-10-08 接受日期:2016-12-05 出版日期:2020-12-01 发布日期:2020-12-28
  • 通讯作者: 栾华龙(1988-),男,湖北云梦人,高级工程师,博士,主要从事河湖演变与治理方面的研究工作。E-mail:luanhualong@126.com
  • 作者简介:余文畴(1940-),男,江西景德镇人,教授级高级工程师,主要从事河道水流泥沙运动与河床演变研究。E-mail:heliusuo@sina.com
  • 基金资助:
    国家重点研发计划项目(2016YFC0402305);国家自然科学基金项目(42006156,51679011);中央级公益性科研院所基本科研业务费项目(CKSF2019167/HL);流域水治理重大科技问题研究项目(CKSC2020791/HL)

Recent Evolution Features of Tongzhou Shoal Channel in Chengtong Reach of Lower Yangtze River

YU Wen-chou1,2, LUAN Hua-long1,2   

  1. 1. River Research Department, Yangtze River Scientific Research Institute, Wuhan 430010, China;
    2. Key Laboratory of River-Lake Regulation and Flood Control of Ministry of Water Resources,Yangtze River Scientific Research Institute, Wuhan 430010, China
  • Received:2020-06-17 Revised:2020-10-08 Accepted:2016-12-05 Online:2020-12-01 Published:2020-12-28

摘要: 长江下游澄通河段通州沙汊道为典型的多滩分汊河道,在径潮流共同作用下,河势与航道条件复杂多变。近期该河段实施了一系列河道(航道)整治工程后,通州沙西水道涨落潮流归顺主槽,该水道淤积萎缩态势得到缓解,但疏挖拓展后的水深条件难以维持,西水道将经历整治后的调整平衡过程。东水道局部河势发展趋向不利,其中:龙爪岩上段呈现主流右摆、滩槽交错的特征,右侧洲滩冲刷,滩面串沟依然存在,并有进一步冲刷发展的趋势;龙爪岩下段营船港外边滩冲刷左移,新开沙尾-10 m(高程)潜心滩冲刷,对航道不利。建议及时采取守护东水道右侧洲滩的措施,整治新开沙外滩,并考虑实施通州沙圈围工程,有利于维持洲滩与汊道分流格局长远稳定。

关键词: 滩槽演变, 整治工程, 河势稳定, 通州沙汊道, 澄通河段

Abstract: Tongzhou shoal channel in Chengtong Reach of the lower Yangtze River is a typical bifurcation channel with multiple shoals as well as complex and variable river regime and waterway condition under combined riverine and tidal forcing. After river and waterway regulation projects in recent years, the flooding and ebb currents converged along the main west channel of the Tongzhou Shoal, alleviating the channel’s silting and shrinking. However, the west channel was unable to maintain its water depth after dredging and will adjust and approach to equilibrium, whereas the local river regime of the east channel tended to be unfavorable. The mainstream of upstream segment of the Longzhuayan node moved rightward and the shoals and channels intertwined. The right side of the Tongzhou shoal was scoured, with a trend of further scour along the connecting channels on the Tongzhou shoal. The marginal shoal near the Yingchuan port in the segment downstream the Longzhuayan node was scoured to the left, and the submerged shoals -10 m under the tail of Xinkai shoal was scoured, which is unfavorable to navigation. Measures should be taken to protect the right side of the east channel in time, to renovate the Xinkai shoal, and to consider reclamation of the Tongzhou shoal. Such measures are conducive to maintain the long-term stability of the shoals and the flow diversion pattern of the bifurcation channel.

Key words: channel-shoal evolution, regulation project, stable river regime, Tongzhou shoal channel, Chengtong Reach

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