Research Article

A Coupled Model of the 1D River Network and 3D Estuary Based on Hydrodynamics and Suspended Sediment Simulation

Table 1

Parameters of the modeling.

SettingsDescription

1DTime stepsBased on the scope of model, the time step of the 1D model is 10 s
Roughness coefficientThis coefficient depends on the physical properties of the riverbed. At Beijiang, from upstream boundary to Sanshui   0.026~0.045, from Sanshui to downstream boundary   0.015~0.03; at Xijiang   0.02~0.03; at Dongjiang, from upstream boundary to Shilong   0.025~0.045, from Shilong to downstream boundary   0.015~0.036; at the mouth of the river network   0.01~0.02
Particle diameterIn channel, the median particle diameter of suspended sediment is about 0.01~0.040 mm, and the median particle diameter of bed material is about 0.17~0.44 mm.
Sediment transport capacity, where ;   0.0012~0.0016.
Recovery coefficient relating to the saturationWhen the channels are in the deposition conditions, a value of 0.25 is applied; while, in the erosion conditions, a value of 1.0 is applied.

3DTime steps, ; thus, the internal model is 10 s and the external model is 0.5 s.
Bottom roughness, , where ,  cm.
Particle diameterThe median particle diameter is 0.003~0.009 mm during the spring tide period.
Sediment settling velocity, where , , and