Titlebook: Wave-Forced Sediment Erosion and Resuspension in the Yellow River Delta; Yonggang Jia,Xiaolei Liu,Jiewen Zheng Book 2020 Shanghai Jiao Ton

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Wave-Induced Pore Pressure in Relation to Sediment Erosion and Resuspension in the Modern Yellow Riuced pore pressure develop models were therefore constructed; influencing factors on the liquefaction properties were also identified. This chapter is the transitional section in this book which collected the wave-seabed interactions to sediment erosion and resuspension in the modern Yellow River Delta.

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Sediment Resuspension Process in the Modern Yellow River Delta,eabed liquefaction occurred, the process of sediment resuspension could be significantly changed. More sediments would be resuspended in addition to that eroded by wave orbital velocities, and these lately resuspended sediments seems to come from the interior of the seabed, rather than seabed surface as the conventional opinion holds.

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Physical Mechanisms of Wave-Induced Sediment Resuspension,ressure and residual pore pressure, were found to induce sediment resuspension through the way of “pumping” sediments out of the interior of the seabed. In the Yellow River Delta, waves not only erode sediments from the seabed surface, but also “pumping” internal fine-grained sediments into the overlying water column.

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Introduction,esuspension is given, finally, a literature review is given on the observational, experimental, and mathematical research advances regarding sediment erosion and resuspension. Consequently, the mainstream scientific question of this book is outlined. That is, the total book is targeted at improving

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Erodibility of Seabed Sediments in the Modern Yellow River Delta, study is undertaken to determine the spatial distribution of sediment erodibility in the modern Yellow River Delta. The critical shear stress of sediments is measured both with a mini-annular flume and a Cohesive Strength Meter (CSM) along the coastline of the Yellow River Delta (i.e., deposited in