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洪水期水库调水调沙与黄河下游河道排沙分析

Analysis on the Adjustment of Water and Sediment from Reservoir and Sediment Delivery in the Lower Yellow River in Flood Periods

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【作者】 赵华侠; 陈建国; 李宜斌;

【Author】 Zhao Huaxia; Chen Jianguo; Li Yibin(China Institute of Water Resources and Hydropower Research)

【机构】 中国水利水电科学研究院;

【摘要】 从1973~1990年期间,选取了60个洪峰时段的实测资料,分析了黄河下游河道的泥沙淤积和排沙比,得出结论为,如果洪水期三门峡出库平均含沙量为100~200kg/m3时,出库洪峰流量在4000~5000m3/s之间,可把50%~80%左右0.025~0.05mm和0.05~0.1mm的两级中粗沙排入海里;洪水期出库平均含沙量为50~100kg/m3,出库洪峰流量为3500~4000m3/s左右时,可把50%~190%的0.025~0.05mm和0.05~0.1mm的两级中粗沙排入海里.

【Abstract】 Based on field data of 60 events of various floods in the periods of 1973~ 1990, thesediment accumulation and sediment delivery ratio in the Lower Yellow River have been analysed. It has come to the conclusion that about 50~80 percent of the sediment with grain size0. 025~0. 05 mm and 0. 05~0. 1 mrn will be delivered into the sea, if the mean sediment contentsare 100~200 kg/m3 and the flood peak discharges are 4 000~5 000 m3/s from the SanmenxiaReservoir in flood periods. About 50 ~190 percent of the sediment with grain size 0. 025 ~0. 05mm and 0. 05-0.1 mm will delivered into the sea, if the mean sediment contents are 50~ 100 kg/m3 and the flood peak dischanges are 3 500~4 000 m3/s.

  • 【文献出处】 水利水电技术 ,WATER RESOURCES AND HYDROPOWER ENGINEERING , 编辑部邮箱 ,1997年11期
  • 【分类号】TV14
  • 【被引频次】6
  • 【下载频次】69
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