洪泽湖出入流格局变化下汛期起调水位抬升影响研究
作者:
作者单位:

(1.河海大学水灾害防御全国重点实验室,江苏 南京210098;2.河海大学水利水电学院,江苏 南京210098;3.河海大学水利部水循环与水动力系统重点实验室,江苏 南京210098;4.江苏省水利勘测设计研究院有限公司,江苏 扬州225009 )

作者简介:

陈震宇(1999—),男,硕士研究生,主要从事水力学数值模拟研究。E-mail:chenzhenyu@hhu.edu.cn

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中图分类号:

X522

基金项目:

国家重点研发计划项目(2022YFC3202600);国家自然科学基金青年科学基金项目(52309086);江苏省水利科技项目(2023013,2022061)


Influence of elevated water control level during flood season under varying inflow and outflow patterns in Hongze Lake
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Affiliation:

(1.The National Key Laboratory of Water Disaster Prevention, Hohai University, Nanjing 210098, China;2.College of Water Conservancy & Hydropower Engineering, Hohai University, Nanjing 210098, China;3.Key Laboratory of Hydrologic-Cycle and Hydrodynamic-System of Ministry of Water Resources, Hohai University, Nanjing 210098, China;4.Jiangsu Surveying and Design Institute of Water Resources Co., Ltd., Yangzhou 225009, China )

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    摘要:

    为研究洪泽湖在新的出入流格局下,汛期起调水位抬升对洪泽湖湖区水位及运行调度的影响,构建二维水动力模型分析了起调水位抬升和环湖工程组合条件下湖区蒋坝水位的变化特征,并根据洪泽湖滞洪区调度规则给出了不同来水与环湖工程组合条件下汛期起调水位的建议值。结果表明:现状起调水位(12.5 m)下,入海水道二期工程可显著降低蒋坝峰值水位;冯铁营引河工程在入海水道工程协同作用下对蒋坝水位几乎没有影响;对于2007年量级洪水,起调水位小于或等于14.0 m不会增大湖周滞洪区洪水风险,洪泽湖汛期起调水位可上调1.0~1.5 m;百年一遇洪水下起调水位小于或等于14.0 m将不改变蒋坝峰值水位,但起调水位抬升会使滞洪区提前破圩,在不增大滞洪区洪水风险前提下起调水位可上调0.5~1.0 m。

    Abstract:

    Under the new inflow and outflow patterns of Hongze Lake, a two-dimensional hydrodynamic model was established to investigate the impact of elevated water control levels during flood season on water levels and operational scheduling of the lake. The variation characteristics of the water level at Jiangba in the lake area under the conditions of elevated water control levels and the lakeside projects were analyzed. According to the dispatching rules for flood detention areas in Hongze Lake, suggested values for the water control levels during flood season for different combinations of water inflows and lakeside projects were given. The results show that the second stage of the project on the sea-entering channel can significantly reduce the peak water level at Jiangba when the current water control level of Hongze Lake is 12.5 m. The Fengtieying River Diversion Project has almost no impact on the water level at Jiangba under the synergistic effect of the project on the sea-entering channel. For a flood event with the same magnitude in 2007, the water control level within 14.0 m does not increase the flood risk in the detention area around the lake. Therefore, the water control levels of Hongze Lake during flood season can be raised by 1.0-1.5 m. Under the condition of the once-in-a-century flood event, the peak water level at Jiangba will not change when the water control level remains within 14.0 m. However, the elevated water control level can cause the detention area to open ahead of time, and the water control level can be raised by 0.5-1.0 m without increasing the flood risk in the detention area.

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陈震宇,王玲玲,徐津,等.洪泽湖出入流格局变化下汛期起调水位抬升影响研究[J].河海大学学报(自然科学版),2025,53(3):15-21, 29.(CHEN Zhenyu, WANG Lingling, XU Jin, et al. Influence of elevated water control level during flood season under varying inflow and outflow patterns in Hongze Lake[J]. Journal of Hohai University (Natural Sciences),2025,53(3):15-21, 29.(in Chinese))

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  • 收稿日期:2024-07-09
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  • 在线发布日期: 2025-05-26
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