三门峡水库汛期敞泄排沙冲刷—平衡发展过程研究
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1.华北水利水电大学;2.中国水利水电科学研究院

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国家自然科学基金联合基金资助项目(U22A20237);水利部泥沙科学与北方河流治理重点实验室开放研究基金资助(IWHR-SEDI-2025-09);水利部黄河流域水治理与水安全重点实验室(筹)研究基金资助(2023-SYSJJ-08).


Simulation on the scouring- equilibrium process of full open discharge for Sanmenxia reservoi
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1.North China University of Water Resources and Electric Power;2.China Institute of Water Resources and Hydropower Research

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    摘要:

    三门峡水库汛期敞泄排沙对库区冲刷与库容恢复具有重要作用,并往往表现为冲刷—平衡的发展过程,现有研究多有不足。综合采用资料统计、理论分析、试验研究、概化模拟等方法,深入研究三门峡水库汛期敞泄排沙规律与冲刷-平衡发展过程。通过资料分析认为,三门峡水库汛期敞泄排沙可采用考虑上站来水含沙量的输沙幂律函数公式,且输沙系数随累计冲刷时间及总量增大而不断衰减,这是形成冲刷-平衡发展过程的根本原因,也是造成以往率定流量幂律指数出现小于1.0不合理现象的重要原因。进一步考虑敞泄排沙初期床面新淤泥沙与后期床面淤积固结泥沙冲刷起动临界条件差别,对考虑上站来水含沙量的输沙幂律函数公式进行改进,并对后期输沙系数进行修正,结果显示修正后输沙系数总体变化趋势更为光滑、合理;经三门峡水库泥沙淤积固结及冲刷起动试验验证,水库泥沙淤积固结干密度的小幅增大确会导致起动临界条件(流速、剪切应力、流量等)的大幅增长。最后,再进一步结合河流自动调整原理及滞后响应模型,建立输沙系数及累计冲刷量的滞后响应模型,并对三门峡水库汛期敞泄排沙冲刷—平衡发展过程进行概化模拟。结果表明计算输沙系数随累计冲刷时间变化曲线与实测值变化趋势基本符合,计算累计冲刷量随累计入库水量变化曲线与实测值变化趋势符合良好,确定性系数与Nash-Sutcliffe效率系数均在0.98以上,初步说明了所建模型方法的合理性。

    Abstract:

    The full open discharge scouring during flood season is important for the scouring of Sanmenxia reservoir, and often presents a scouring-equilibrium process. But the current related research is still insufficient. Using the combination methods of field data analysis, theory research, experiment study and model simulation, the sediment transport law and scouring-equilibrium process of full open discharge are studied. Data analysis show that the sediment transport rate of full open discharge during flood season can be calculated by the power law relationship model by addition of the upstream sediment supply function, in which the sediment transport coefficient decrease with the increase of accumulated scouring time and volume. The decrease of sediment transport coefficient is a fundamental reason for the formation of the scouring-equilibrium process, and is an important reason for the unreasonable phenomenon of the power law index of discharge being less than 1.0 in previous calibrations. Furthermore, considering the difference of incipient motion condition for upper layer new deposited sediment and lower layer consolidated sediment, the power law relationship model is improved and the sediment transport coefficient is revised. It shows that the variation of revised sediment transport coefficient becomes more smooth and reasonable. Scouring experiment for the consolidated sediment proves that if the dry density of consolidated sediment increases slightly, the incipient motion condition (velocity, shear stress and discharge) will increase significantly. Finally, according to the principle of self-adjustment of alluvial river and using the delayed response model theory, the delayed response model for sediment transport coefficient and accumulated scouring volume are established and applied to simulate the scouring-equilibrium process of full open discharge for Sanmenxia reservoir. The simulation results show that the calculated curve of sediment transport coefficient varied with the accumulated scouring time are in agreement with the measured values, the calculated curve of accumulated scouring volume varied with the accumulated incoming water are in good agreement with the measured values. The values of determination coefficient and Nash-Sutcliffe efficiency are 0.98 and 0.98, which preliminarily illustrate the rationality of the proposed model.

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  • 收稿日期:2025-08-30
  • 最后修改日期:2025-12-17
  • 录用日期:2025-12-17
  • 在线发布日期: 2026-05-07
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