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- W2355844022 abstract "Based on the field observed hydrologic and sediment data at Huanghe River estuary in flood season in 1995, the conclusion was drawn that as long as total density of turbid water is greater than 1.020 kg/m 3, the density current can flow continuously beneath the clear water. Sediment concentration and velocity vertical distribution curve may be represented by regression functions based on regression analysis of materials about sediment concentration, velocity and depth at different hydrometric stations. While sediment density current exists, vertical distribution of sediment-concentration is in unbalanced way. The deeper the water is, the larger the increment of sediment concentration will be. The velocity distribution curve is different from that which have been measured in reservoir, lake or laboratory flumes in the past, the velocity model on sediment density current at Huanghe River estuary is an unique model: the velocity doesn't change when water depth changes." @default.
- W2355844022 created "2016-06-24" @default.
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- W2355844022 date "2001-01-01" @default.
- W2355844022 modified "2023-09-25" @default.
- W2355844022 title "Distribution of Sediment and Its Impacts on Flow Structure at Huanghe(Yellow River) Estuary in Flood Season" @default.
- W2355844022 hasPublicationYear "2001" @default.
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