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The paper observe suspended sediment concentration and hydrodynamic in the Yellow River Delta front.Discussing the suspended sediment concentration changes and influencing factors.Calculating the suspended sediment fluxes in tidal cycles,and the contribution of waves and currents to sediment resuspension.Analyzing the source of the suspend sediment.The results is as fallow: the distribution of suspended sediment in the vertical is well-distributed; the main resource of suspended sediment is advection transport sediment;under moderate and rough,the suspended sediment induced by wave more than the suspended sediment induced by current.