长江科学院院报 ›› 2017, Vol. 34 ›› Issue (9): 36-40.DOI: 10.11988/ckyyb.20160590

• 防洪减灾 • 上一篇    下一篇

一、二维耦合数学模型在感潮河网洪水风险图编制中的应用

杨莉玲a, b, 宋利祥a, 邓军涛c, 徐爽c, 胡晓张a, 孙倩雯a   

  1. 珠江水利委员会a.珠江水利科学研究院;
    b.水利部珠江河口动力学及伴生过程调控重点实验室;
    c.防汛抗旱办公室,广州 510611
  • 收稿日期:2016-06-12 出版日期:2017-09-01 发布日期:2017-09-28
  • 作者简介:杨莉玲(1976-),女,湖北宜昌人,高级工程师,博士,主要从事水动力、水环境数值模拟相关研究,(电话)15913122415(电子信箱)yanglilingok@163.com。
  • 基金资助:
    国家自然科学基金青年基金项目(51409286)

Application of a 1-D and 2-D Coupled Mathematical Modelin the Mapping of Tidal River Flood Risk

YANG Li-ling1,2, SONG Li-xiang1,2, DENG Jun-tao3, XU Shuang3, HU Xiao-zhang1,SUN Qian-wen1   

  1. 1.Pearl River Hydraulic Research Institute,Pearl River Water Resources Commission, Guangzhou 510611,China;
    2.Key Laboratory of the Pearl River Estuarine Dynamics and Associated Process Regulation,Ministry of Water Resources,Guangzhou 510611,China;
    3.The Pearl River Basin Flood Control andDrought Relief Office, Pearl River Water Resources Commission, Guangzhou 510611, China
  • Received:2016-06-12 Online:2017-09-01 Published:2017-09-28

摘要: 为了解决感潮河网径流、潮汐交汇,动力复杂,溃决洪水难以用经验公式准确概化的问题,建立直接以溃口为耦合断面的河网一维、保护区二维侧向耦合模型,将感潮河网与保护区一体化,避免环境因素及经验参数的不确定性带来的溃口流量估算误差。典型算例和中顺大围溃决洪水情景模拟表明:洪水自溃口集中喷射出后分散流向围内,流态受围内下垫面影响显著,溃口水位、流量随外江潮位涨落而起伏变化,由溃口流量过程线计算所得溃口水量与根据淹没区各单元的面积和水深计算的围内总水量一致。模拟成果直接反映下垫面、水头差、潮位涨落,及溃口流态对溃决洪水的综合影响,反映出本耦合模型计算溃口流量及对溃决洪水模拟的合理性、可信性,具有较好的应用前景。

关键词: 溃决洪水, 一、二维耦合数学模型, 感潮河网, 洪水风险图, 侧向联解

Abstract: As the dynamics of tidal river network is complex with runoff and tide confluence, breach discharge in tidal river network is too complex to be estimated by empirical formula accurately. In view of this, a hydrodynamic model coupling 1-D model of river network and 2-D model of reserve area is developed with the breach as the lateral linkage. The model integrates the tidal river network and the reserve area, hence avoiding the deviation of breach discharge caused by the uncertainty of environmental factors and empirical parameters. Simulation results of typical example and embankment-break flood scene show that 1) the jet-flow of breach disperses into the reserve area, and the flow pattern is affected by the underlying surface significantly; 2) water level and discharge of the breach change with tide fluctuation, and the calculated total water amount according to breach discharge agrees with that from flooded areadepth. The simulation results reflect the combined influence of underlying surface, water head, tide level and flow pattern on breach flood. The proposed model is rational and reliable in calculating breach discharge and simulating embankment-break flood.

Key words: embankment-break flood, 1-D and 2-D coupling model, tidal river network, mapping of flood risk, lateral linkage

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