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

YANG Li-ling, SONG Li-xiang, DENG Jun-tao, XU Shuang, HU Xiao-zhang,SUN Qian-wen

Journal of Changjiang River Scientific Research Institute ›› 2017, Vol. 34 ›› Issue (9) : 36-40.

PDF(3410 KB)
PDF(3410 KB)
Journal of Changjiang River Scientific Research Institute ›› 2017, Vol. 34 ›› Issue (9) : 36-40. DOI: 10.11988/ckyyb.20160590
FLOOD PREVENTION AND DISASTER REDUCTION

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
Author information +
History +

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

Cite this article

Download Citations
YANG Li-ling, SONG Li-xiang, DENG Jun-tao, XU Shuang, HU Xiao-zhang,SUN Qian-wen. Application of a 1-D and 2-D Coupled Mathematical Modelin the Mapping of Tidal River Flood Risk[J]. Journal of Changjiang River Scientific Research Institute. 2017, 34(9): 36-40 https://doi.org/10.11988/ckyyb.20160590

References

[1] 珠江水利委员会珠江水利科学研究院. 风暴潮风险分析技术开发与试点编制报告[R] . 广州:珠江水利委员会珠江水利科学研究院,2013.
[2] 夏军强,王光谦,LIN Bin-liang,等. 复杂边界及实际地形上溃坝洪水流动过程模拟[J] .水科学进展,2010 ,21(3):289-298.
[3] 董耀华,黄煜龄. 天然河道长河段一维非恒定流数模研究[J] . 长江科学院院报,1994,11(2):10-17.
[4] 李大鸣,胡永文,王 笑,等. 城市暴雨沥涝数学模型的研究与应用[J] . 长江科学院院报,2016,33(10): 46-50.
[5] 韦直林,崔占峰. 一维河网非恒定流计算程序的初步研究[J] . 人民长江,2001, 32(12):30-32.
[6] 吴寿红. 河网非恒定流四级解法[J] . 水利学报,1985,(8):42-50.
[7] 汪定扬,明道华,周建华. 三峡工程多级船闸中间引渠水力学问题的数值计算研究[J] . 长江科学院院报, 1989,6(4):6-14.
[8] 张细兵,金 琨,林木松.潮流河段温排水影响的平面二维数值模拟[J] .长江科学院院报,2006,23(3):13-16.
[9] 王智勇,陈永灿,朱德军,等. 一维-二维耦合的河湖系统整体水动力模型[J] . 水科学进展,2011,22(4):516-522.
[10] 姚志坚,陈文龙. 溃坝洪水演进数学模型研究及其在大镜山水库的应用[J] .人民珠江,2008 ,(3):7-9.
[11] 李 炜.水利计算手册[K] .2版.北京:中国水利水电出版社,2006.
PDF(3410 KB)

Accesses

Citation

Detail

Sections
Recommended

/