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Simulation of Sediment Discharge Characteristics of Wudongde Reservoir in Main Flood Season after Impoundment
HUANG Ren-yong, GAO Yu, WANG Min, YUAN Yuan
Journal of Changjiang River Scientific Research Institute ›› 2026, Vol. 43 ›› Issue (5) : 17-22.
PDF(1152 KB)
PDF(1152 KB)
Simulation of Sediment Discharge Characteristics of Wudongde Reservoir in Main Flood Season after Impoundment
[Objective] The Wudongde Reservoir is the uppermost cascade reservoir among the Wudongde, Baihetan, Xiluodu, and Xiangjiaba cascade reservoirs in the lower reaches of the Jinsha River. To support the operation scheduling of sediment discharge in the Wudongde Reservoir, a one-dimensional unsteady flow and sediment mathematical model for the mainstream and tributaries of the Wudongde Reservoir is established. The feasibility of the model is verified using measured data after impoundment, and then the sediment discharge characteristics of typical water and sediment processes during the initial impounding period of the Wudongde Reservoir are simulated. [Methods] The water and sediment processes in July and August of 2020, 2022, and 2023 were selected as typical water and sediment processes for model calculation. Among them, 2020 was a high-flow year, while 2022 and 2023 were low-flow years. [Results] 1) During July and August, the Wudongde Reservoir had strong sediment discharge capacity when the inflow volume was large. In July 2020, due to large inflow volume, the sediment discharge ratio corresponding to a water level of 945-975 m reached 32%-14%. During the impounding period in August, the impact of initial water level on sediment discharge capacity was not significant. In August 2020, due to large inflow volume, the sediment discharge ratio corresponding to an initial water level of 952-975 m was relatively large, ranging from 24.8% to 18.8%. During July and August, the Wudongde Reservoir could utilize high water for sediment discharge. 2) Due to significant reduction in sediment inflow, the siltation volume and proportion in the fluctuating backwater area of the Wudongde Reservoir during July and August were relatively small, providing favorable conditions for optimal operation of the reservoir. During the flood season in July, when the inflow volume was large and reservoir water level was >965 m, the siltation proportion in the fluctuating backwater area gradually increased but the siltation amount was small. When the inflow volume was small, the siltation pattern in the fluctuating backwater area was similar but the corresponding reservoir water level was 960 m. 3) At the beginning of August during the impounding period, when the initial water level was raised and the inflow volume was large, the impact on the siltation volume and proportion in the fluctuating backwater area was small. When inflow volume was small, the siltation proportion in the fluctuating backwater area increased correspondingly with the rise of the initial water level, but the siltation volume remained small. When the inflow sediment volume was relatively small, the inflow water volume was the main factor affecting the siltation proportion in the fluctuating backwater area in July. When the inflow sediment volume was relatively large, the inflow sediment volume was the main factor affecting the siltation proportion in the fluctuating backwater area in August. When the inflow sediment volume was relatively small, the inflow water volume was the main factor affecting the siltation proportion in the fluctuating backwater area in August. [Conclusion] With the significant reduction in inflow sediment volume after the impounding of the Wudongde Reservoir, even though the siltation proportion in the fluctuating backwater area increases, the increase in siltation volume in the fluctuating backwater area remains small, indicating room for further optimization of reservoir operation. Therefore, when studying the optimal operation of the Wudongde Reservoir, it is not sufficient to only consider relative indicators such as the sediment discharge ratio and the siltation proportion in the fluctuating backwater area. It is also necessary to consider absolute indicators such as the outflow sediment volume, the total siltation volume in the reservoir area, and the siltation volume in the fluctuating backwater area. This requires further long-term scouring and deposition calculations based on typical series years. Further in-depth research is needed on the optimization space for reservoir operation and specific regulation indicators under the permissible siltation principles of the Wudongde Reservoir.
flow and sediment mathematical model / sediment discharge characteristics / optimal operation / model validation / Wudongde Reservoir
| [1] |
傅巧萍, 胡滢, 柳林云, 等. 金沙江乌东德水电站可行性研究报告[R]. 武汉: 长江勘测规划设计研究有限责任公司, 2015.
(
|
| [2] |
李思璇, 肖潇, 李昶, 等. 金沙江下游水沙特性、梯级水电站库区和坝下游河道冲淤分析(2023年度)[R]. 武汉: 长江水利委员会水文局,中国长江三峡集团有限公司, 2024.
|
| [3] |
李丹勋. 三峡水库上游来水来沙变化趋势研究[M]. 北京: 科学出版社, 2010.
(
|
| [4] |
卢金友, 赵瑾琼. 长江流域梯级枢纽泥沙调控关键技术[J]. 长江科学院院报, 2021, 38(1):1-7,26.
通过将水沙动力学与水库调度优化理论相结合,围绕长江流域梯级枢纽泥沙调控关键技术开展研究。在改进恢复饱和系数、非均匀沙挟沙力等关键计算模式的基础上,完善并集成长江上游梯级水库群水沙数学模型、长江中下游复杂江湖河网水沙数学模型和典型河段平面二维水沙数学模型,构建了江河湖库水沙输移模拟模块。基于泥沙对防洪、发电、航运和长期使用4个主要目标的影响,构建了长江泥沙优化调控目标函数,进而集成水沙输移模拟模块构建了长江泥沙优化调度模型,并提出了基于预构泥沙信息库、结合BP神经网络的模型求解方法和非劣解集的改进灰靶评价方法。在此基础上,以三峡水库为例,提出了汛期“蓄清排浑”动态运用方案以及长期分阶段泥沙调控策略。
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Combining flow and sediment dynamics with optimization theory, we developed a technology of sediment control for cascade reservoirs integrating simulation module, dispatching module and decision module.Firstly, we improved the coefficient of saturation recovery and the sediment carrying capacity of non-uniform sediment, and on this basis built the simulation module of water/sediment transport in rivers, lakes, and reservoirs by integrating the water/sediment models for cascade reservoirs in upstream Yangtze River, for complex river-lake network in mid-and downstream Yangtze River and the 2D model for typical reaches. Subsequently, we constructed the objective function of sediment’s optimal regulation in consideration of flood control, power generation, navigation, and long-term use, and further established the optimal sediment-dispatching model. Furthermore we employed the BP neural network in association with the pre-constructed sediment information base to fit the prediction for the sedimentation and scouring, and present an improved grey-target evaluation method based on non-inferior solution set. Taking the Three Gorges Reservoir as an example, we finally put forward the dynamic operation scheme of “storing clear water and discharging muddy water” in flood season and the long-term staged sediment control strategy.
|
| [5] |
朱玲玲, 陈翠华, 张继顺. 金沙江下游水沙变异及其宏观效应研究[J]. 泥沙研究, 2016, 41(5): 20-27.
(
|
| [6] |
朱玲玲, 董先勇, 陈泽方. 金沙江下游梯级水库淤积及其对三峡水库影响研究[J]. 长江科学院院报, 2017, 34(3): 1-7.
2012年以来,金沙江下游向家坝水电站、溪洛渡水电站相继蓄水运用,拦截了金沙江下游泥沙。为了解梯级水库泥沙淤积情况及其拦沙作用对下游三峡水库的影响,基于大量水沙、固定断面观测资料,采用输沙法和地形法,计算分析了向家坝水电站、溪洛渡水电站2库自运用以来的库区泥沙淤积量及分布特征,研究了梯级水库拦沙作用对三峡水库的影响。结果表明:向家坝、溪洛渡库区泥沙淤积量较小,金沙江下游梯级拦沙使得三峡入库沙量及库尾重点河段淤积强度均减小。研究成果对梯级水库运行、三峡水库运行及调度方式优化具有十分重要的意义。
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Xiangjiaba Reservoir and Xiluodu Reservoir have successively entered impoundment stage since 2012, and in the meantime intercepted sediment from the lower Jinsha River. According to field data of runoff, sediment and some cross-sections, the amount and distribution features of sediment deposition in the cascade reservoirs since their operation are calculated, and their influences on the Three Gorges Reservoir (TGR) are studied. Results indicate that sediment deposition in Xiluodu Reservoir and Xiangjiaba Reservoir are both less than the estimated amount. The cascade reservoirs reduced the incoming sediment of TGR, and correspondingly reduced the deposition in its tail reach. The research results are of great significance for the operation of cascade reservoirs and the regulation optimization of TGR.
|
| [7] |
杨成刚, 李圣伟, 王伟, 等. 上游水库群运行后金沙江下游梯级水库与三峡水库联合减淤调度研究[R]. 武汉: 长江水利委员会水文局, 2020.
|
| [8] |
黄仁勇, 黄悦. 三峡水库干支流河道一维非恒定水沙数学模型初步研究[J]. 长江科学院院报, 2009, 26(2): 9-13.
考虑水沙运动过程中的非恒定性及众多支流的影响,建立了三峡水库干支流河道一维非恒定水沙数学模型,并对水流方程组采用三级解法求解。采用三峡水库蓄水运用后2003年6月至2004年12月的水库实测水沙资料对模型进行了验证,验证结果有良好的一致性。本模型在使用1961-1970年系列年入库水沙条件及水库正常蓄水位调度方案下进行了水库冲淤100 a预测计算,计算结果较为合理,表明本模型可用于三峡水库水沙数值模拟。
(
A numerical model for simulating 1-D unsteady flow and sediment transport in the mainstream and its tributaries of the Three Gorges Reservoir (TGR) area was presented in this paper, and a three-gradation method was applied to solve the flow governing equation. The validity of the model was checked with the observed data of the TGR from June 2003 to December 2004. The calculated result was in good agreement with observed data. The model was further applied to predict the sedimentation process in the TGR in a 100year period with the discharge and sediment data of 1961 to 1970 series and under the normal water level operation condition. And the calculation results are reasonable. The simulated results show that this model could be used to simulate the discharge and sediment transport at the TGR.
|
| [9] |
黄仁勇, 李飞, 张细兵. 三峡水库运用初期库区水沙输移数值模拟[J]. 长江科学院院报, 2012, 29(1): 7-12.
考虑水沙输移过程中的非恒定性,建立了三峡水库一维非恒定水沙数学模型。此模型为一树状河网模型,可以将更多支流纳入计算范围。采用三峡水库蓄水运用后2003-2009年实测水沙资料对模型进行了验证计算,计算结果与实测资料符合较好,表明模型能够用于三峡水库干支流河道水沙输移数值模拟。该模型可在今后三峡水库优化调度等相关研究工作中发挥其模拟和预测作用。
(
A numerical model for simulating unsteady flow and sediment transport in the mainstream and its tributaries of the Three Gorges Reservoir (TGR) area was presented in this paper. More tributaries could be included in the calculation with this tree-like rivernetwork model. The validity of the model was checked with the observed water and sediment data of the TGR from June 2003 to December 2009. Good agreement between the calculated results and the observed data indicated this model could be used to simulate the flow and sediment transport in the TGR area, and hence could be applied to the modeling and prediction for the optimal operation of the TGR in the future.
|
| [10] |
黄仁勇, 王敏, 张细兵, 等. 三峡水库区间入流过程计算[J]. 长江科学院院报, 2018, 35(6):67-69,80.
三峡水库区间支流多,入汇流量大,区间入流量及入流过程直接关系到水库调蓄计算的精度,区间入流过程的准确计算是三峡水库水动力学计算中需要考虑的重要问题。针对典型水流过程,利用一维水动力学模型,采用水流水动力逐日演进计算的方法,基于水量平衡原则,反算得到了三峡水库区间日均入流过程,区间入流过程按各支流流域面积比例分配在库区各入汇支流上以加入计算河段,并对区间加水前后的效果进行了分析。结果表明,采用此方法后,三峡水库出库流量过程计算结果与实测结果吻合良好。
(
The Three Gorges Reservoir (TGR) is endowed with many tributaries and large local inflow. The correct calculation of local inflow process is an important issue in the hydrodynamics calculation for the TGR as the amount and process of inflow directly concerns the calculation precision of reservoir regulation and storage. In this article, the daily inflow process in the TGR area is back-calculated on the premise of water balance by a 1-D mathematical unsteady flow model proposed by the author previously. The local inflow process is added to the calculated reach by being distributed to each tributary in correspondence to the proportions of catchment area. The effect of adding local inflow to each reach is analyzed. Results demonstrate that the calculation results of the discharge process of the Three Gorges Reservoir are in good agreement with the measured results after the proposed method is adopted.
|
| [11] |
谢益芹, 邓安军, 董先勇, 等. 金沙江下游流域水沙格局变化研究[J]. 水利学报, 2023, 54(11): 1309-1322.
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