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俞 悦, 张天舒, 方立超, 王船海, 韦 浩, 陈 钢.感潮河段港闸流量动态变化计算方法研究水资源与水工程学报[J].,2025,36(5):135-143
感潮河段港闸流量动态变化计算方法研究
Calculation methods for dynamic flow changes in harbor gates of tidal reaches
  
DOI:10.11705/j.issn.1672-643X.2025.05.16
中文关键词:  堰闸过流  非恒定流  趋势变化  BP神经网络  时间序列  流量计算  感潮河段  里下河地区
英文关键词:weir gate overflow  unsteady flow  trend change  BP neural network  time series  flow simulation  tidal reach  the Lixia River region
基金项目:国家自然科学基金联合基金项目 (U2240209)
作者单位
俞 悦1, 张天舒1, 方立超2, 王船海1, 韦 浩3, 陈 钢1 (1.河海大学 水文水资源学院 江苏 南京 210098 2.南平市自然资源局 福建 南平 350000
3.上海水文总站
上海 200232) 
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中文摘要:
      沿海感潮河段港闸排水受潮汐、上游来水及调度等因素影响显著,传统堰流公式难以准确反映非恒定流条件下的实际排水过程。为提升流量计算精度,提出一种基于趋势变化特征的三层BP神经网络模型,选取闸上水位、闸下水位及其变化率、水位差变化率以及过闸流量变化率等时间序列指标作为输入,模拟港闸出流过程。以里下河地区4座主要港闸的实测数据为例,对比分析了传统堰流公式法与趋势变化法的模拟结果。结果表明:传统方法误差较大,而所提神经网络模型在典型开关闸时段的相关系数均高于0.75,平均误差控制在3%以内,具有更高的拟合精度和适用性。该方法能有效捕捉港闸运行过程中流量与水位的动态关系,为复杂水文条件下港闸排水量模拟提供了新思路和技术支撑。
英文摘要:
      The discharge process at sluice gates in coastal tidal reaches is significantly influenced by tides, upstream inflows, and operational controls, making conventional weir formulas inadequate for accurate simulation of unsteady flow conditions. To improve calculation accuracy, this study proposes a three-layer BP neural network model based on trend variation features. Time-series indicators such as upstream and downstream water levels, their rates of change, water level difference change rate, and discharge change rate are used as model inputs to simulate sluice outflows. Using measured data from four major sluices in the Lixia River region as case studies, we compared the simulation results of the proposed method and conventional weir formulas. Results show that conventional methods yield large errors, while the BP neural network model achieves correlation coefficients above 0.75 and average errors below 3.00% during typical gate operations, indicating that the proposed model has higher accuracy and applicability. This method can effectively capture the dynamic relationship between discharge and tidal level during gate operations and offer a novel approach for accurate simulation under complex hydrological conditions.
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