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

YU Wen-chou, LUAN Hua-long

Journal of Changjiang River Scientific Research Institute ›› 2020, Vol. 37 ›› Issue (12) : 1-7.

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Journal of Changjiang River Scientific Research Institute ›› 2020, Vol. 37 ›› Issue (12) : 1-7. DOI: 10.11988/ckyyb.20200579
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Recent Evolution Features of Tongzhou Shoal Channel in Chengtong Reach of Lower Yangtze River

  • YU Wen-chou1,2, LUAN Hua-long1,2
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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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YU Wen-chou, LUAN Hua-long. Recent Evolution Features of Tongzhou Shoal Channel in Chengtong Reach of Lower Yangtze River[J]. Journal of Changjiang River Scientific Research Institute. 2020, 37(12): 1-7 https://doi.org/10.11988/ckyyb.20200579

References

[1] 余文畴. 长江中下游河道水力和输沙特性的初步分析:初论分汊河道形成条件[J]. 长江科学院院报,1994,11(4): 16-22.
[2] 李 明,胡春宏. 三峡工程运用后坝下游分汊型河道演变与调整机理研究[J]. 泥沙研究,2017,42(6): 1-7.
[3] 韩剑桥,张 为,袁 晶,等. 三峡水库下游分汊河道滩槽调整及其对水文过程的响应[J]. 水科学进展,2018, 29(2): 186-195.
[4] 姚仕明,余文畴,董耀华. 分汊河道水沙运动特性及其对河道演变的影响[J]. 长江科学院院报,2003,20(1): 7-9.
[5] 刘晓芳,黄河清,邓彩云. 江心洲平衡形态水动力条件的理论分析[J]. 水科学进展,2014,25(4): 477-483.
[6] 栾华龙,刘同宦,黄卫东. 水沙条件变化下长江下游典型江心洲汊道形态演变及趋势[J]. 长江科学院院报, 2018, 35(11): 7-12.
[7] 陈 立,周银军,闫 霞,等. 三峡下游不同类型分汊河段冲刷调整特点分析[J]. 水力发电学报. 2011,30(3): 109-116.
[8] 林木松,卢金友,张岱峰,等. 长江镇扬河段和畅洲汊道演变和治理工程[J]. 长江科学院院报,2006,23(5): 10-13.
[9] 吴门伍,严 黎,杨留柱,等. 珠江河口磨刀门口外拦门沙近期演变分析[J]. 长江科学院院报,2018, 35(6): 141-145.
[10]XIE D, PAN C, GAO S, et al. Morphodynamics of the Qiantang Estuary, China: Controls of river flood events and tidal bores[J]. Marine Geology,2018,406:27-33.
[11]朱博渊,李义天,杨培炎,等. 长江澄通河段河床冲淤对流域减沙的响应[J]. 水科学进展,2018, 29(5): 706-716.
[12]LEONARDI N,CANESTRELLI A,SUN T,et al. Effect of Tides on Mouth Bar Morphology and Hydrodynamics[J]. Journal of Geophysical Research: Oceans,2013,118(9):4169-4183.
[13]陈前海,徐照明,侯卫国. 长江澄通河段综合整治规划要点及实施效果分析[J]. 人民长江, 2013, 44(21): 12-15.
[14]朱巧云,刘传杰,刘桂平,等. 长江下游通州沙西水道整治工程效果分析[J]. 水运工程,2020(6): 1-7.
[15]袁文昊,徐 元,刘 红. 新开沙—裤子港沙河段近期河床演变及对深水航道工程的影响[J]. 水运工程,2019(5): 1-6.
[16]徐 华,闻云呈,杜德军,等. 新水沙条件下长江澄通河段河床演变特征研究[C]//第十九届中国海洋(岸)工程学术讨论会.重庆,2019:824-829.
[17]栾华龙,余文畴. 长江下游澄通河段九龙港节点控制作用变化趋向研究[J]. 水利水电快报,2020,41(2): 22-26.
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