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- W2364322436 abstract "Although the lower channel of the Yellow River is well known as accumulation formation,the river bottom and water surface are continuously increasing,the speed of automatic regulation and feedback of the river and the trend of equilibrium are very obvious under the long-term action of silt-discharge.Viewing from sediment carrying capacity and typical data of the upper and lower sections,when discharge is 1 000-4 000 m3/s,the ratio of sediment carrying capacity of the upper(Henan) and lower(Shandong) sections is 1.049-0.915,i.e.when the discharge is smaller than 2 000 m3/s,the sediment carrying capacity of the upper section is greater than that of the lower section;when discharge is greater than 2 500 m3/s,the sediment carrying capacity of the lower section is greater than that of the upper section;and when discharge is 2 300 m3/s,the capacity of the upper and lower sections are basically equilibrium.Viewing from normal process,the sediment transport of the lower section is 1.01 times of the upper section,showing the long-term sediment transport is equilibrium if not considering hyper sediment concentrated flood,no overflow and no change of discharge along the channel.Specially viewing from the data from September 1960 to October 1996,the deposition of Sanmenxia-Lijin section is 3.632 billion tons,of which,the deposition is 3.722 billion tons in 20 hyper sediment concentrated floods;the whole river scour is 90 million tons,making up 0.26% of the 34.8 billion tons coming sediment if hyper sediment concentrated flood is not calculated." @default.
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- W2364322436 date "2008-01-01" @default.
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- W2364322436 title "Huge Sediment Transporting Capacity and Trend of Equilibrium of the Lower Yellow River" @default.
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