Large amounts of fine sediment infiltration into void spaces of coarse bed material have
the ability to alter the morphodynamics of rivers and their aquatic ecosystems. Modelling the
mechanisms of fine sediment infiltration in gravel-bed is therefore of high significance. We
proposed a framework for calculating the sediment exchange in two layers. On the basis of the
conventional approaches, we derived a two-layer fine sediment sorting, which considers the
transportation of fine sediment in the form of infiltration into the void spaces of the gravel-bed. The
relationship between the fine sediment exchange and the affected factors was obtained by using the
discrete element method (DEM) in combination with feedforward neural networks (FNN). The
DEM model was validated and applied for gravel-bed flumes with different sizes of fine sediments.
Further, we developed algorithms for extracting information in terms of gravel-bed packing, grain
size distribution, and porosity variation. On the basis of the DEM results with this extracted
information, we developed an FNN model for fine sediment sorting. Analyzing the calculated
results and comparing them with the available measurements showed that our framework can
successfully simulate the exchange of fine sediment in gravel-bed rivers.
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Large amounts of fine sediment infiltration into void spaces of coarse bed material have
the ability to alter the morphodynamics of rivers and their aquatic ecosystems. Modelling the
mechanisms of fine sediment infiltration in gravel-bed is therefore of high significance. We
proposed a framework for calculating the sediment exchange in two layers. On the basis of the
conventional approaches, we derived a two-layer fine sediment sorting, which considers the
transportation of fine sediment in...
»