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- W2384203419 abstract "The water discharge of the Changjiang Estuary is plentiful and the sediment movement is active. The annual total runoff is 924,000 million cubic meters; the annual averaged sediment discharge reaches 486 million tons. The runoff and the sediment discharge during the flood seasons amount to 71.7% and 87.2 % of the annual total value based on the statistics of the metrical data. When the flood peak water discharge exceeds 6,000 m 3/s at the Datong Station, the water level of the middle and lower reaches of the river arrives at the flood preparation cautionary state and the riverbed changes obviously due to erosion and accumulation; when the flood discharge exceeds 7,000 m 3/s, the new branch of a river and cluster ditches cutting the beach occur frequently, which affects the estuary and the navigation channel development. The studies on the characteristics of the evolution of the river trough and the bedload transport of the South Channel and North Passage show that the floods rebuild the riverbed of the Changjiang Estuary." @default.
- W2384203419 created "2016-06-24" @default.
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- W2384203419 date "2002-01-01" @default.
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- W2384203419 title "Floods rebuilding the riverbed of the Changjiang estuary" @default.
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