运行水位优化对溪洛渡水库排沙影响研究OA
Study on The Impact of Optimizing Operating Water Level on Sediment Discharge in Xiluodu Reservoir
为研究运行水位优化对溪洛渡水库排沙影响,以蓄水后实测资料为基础,建立了溪洛渡水库一维非恒定流水沙数学模型,并进行了模型验证,然后计算了不同运行水位对溪洛渡水库排沙影响.计算结果表明:7-9月溪洛渡水库调度排沙条件较差,汛期7-8月仅在入库水量较大时具有一定的排沙能力,蓄水期9月水库排沙能力较小.7-8月,来水较大时,溪洛渡库水位低于590 m时变动回水区淤积量及占比均很小,库水位高于590 m后变动回水区淤积占比开始增加但淤积量仍然很小;来水较小时,变化规律类似,但对应的临界库水位降低为585 m.9月,起蓄水位低于580 m时变动回水区淤积量及占比均较小,起蓄水位高于580 m后变动回水区淤积占比开始进一步增加但变动回水区淤积量仍然很小.该研究可为溪洛渡水库建库后运行水位优化提供借鉴.
To study the impact of optimizing operating water level on sediment discharge of Xiluodu Reservoir,a one-dimensional unsteady flow and sediment mathematical model of Xiluodu Reservoir was established based on measured data after water storage,and the model was validated.Then,the impact of different operating water levels on sediment discharge in Xiluodu Reservoir was calculated.The calculation results show that the sediment discharge conditions of Xiluodu Reservoir are poor from July to September.During the flood season from July to August,the reservoir only possesses limited sediment discharge capacity when the inflow is large.During the storage period in September,the sediment discharge capacity of the reservoir is relatively small.In July and August,when there is a large influx of water,the sedimentation amount and proportion in the variable return water area of Xiluodu Reservoir are very small when the water level is below 590 m.After the water level is above 590 m,the sedimentation proportion in the variable return water area begins to increase,but the sedimentation amount is still very small.When the incoming water is small,the change pattern is similar,but the corresponding critical reservoir water level decreases to 585 m.In September,when the initial storage water level is below 580m,the sedimentation amount and proportion in the variable return water area are relatively small.When the initial storage water level exceeds 580m,the sedimentation proportion in the variable return water area begins to further increase,but the sedimentation amount in the variable return water area is still very small.This study can provide reference for optimizing the operating water level of Xiluodu Reservoir after its construction.
黄仁勇;高宇;王敏;元媛
水利部长江重点实验室,湖北 武汉 430010||长江科学院河流研究所,湖北 武汉 430010中国长江三峡集团有限公司,湖北 武汉 430010||高坝大库运行安全湖北省重点实验室,湖北 宜昌 443133水利部长江重点实验室,湖北 武汉 430010||长江科学院河流研究所,湖北 武汉 430010水利部长江重点实验室,湖北 武汉 430010||长江科学院河流研究所,湖北 武汉 430010
建筑与水利
溪洛渡水库水沙模拟水库排沙水库调度变动回水区淤积
Xiluodu Reservoirwater and sand simulationreservoir sediment dischargereservoir schedulingsedimentation in the variable return water area
《中国农村水利水电》 2026 (8)
39-43,5
国家自然科学基金长江水科学研究联合基金项目(U2240206,U2240224)中国长江三峡集团有限公司科研项目(0704209)中央级公益性科研院所基本科研业务费项目(CKSF2025153/HL,CKSF2025194L/HL).
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