| Abstract: | A comprehensive analysis is conducted based on observations on topography, tidal current, salinity, suspended sediment and bed load during the years ot" 1982. 1983. 1988. 1989. 1996 and 1997 in the Yangtze Hstuary. Results show that the deformation of tidal waves is distinct and the sand carrying capacity
is large within the mouth bar due to strong tidal currents and large volume of incoming water and sediments. Owing to both temporal and spatial variation of lidal current, deposition and erosion are extremely active. In general a change of up to 0.1 m of bottom sediments takes place during a tidal period. The maximum siltalion and erosion are around 0.2 m in a spring to neap tides cycle. The riverbed is silted during Hood when there is heavy sediment load, eroded during dry season when sediment load is low. The annual average depth of erosion and siltation on the riverbed is around 0.6 m. In particular cases, it may increase to 1.4 m to 2.4 m at some locations. |
