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The rapid flow model (equivalent to the distributed delayed Muskingum model)
is an attractive linear flood routing model meeting the conflicting demands
of physical significance and simplicity. Afte...
Hydrodynamic dispersion characteristics of lateral inflow into a river tested by a laboratory model
Hydrodynamic dispersion Groundwater river-water lateral inflow
2009/4/27
Groundwater and river-water have a different composition and interact in and below the riverbed. The riverbed-aquifer flux interactions have received growing interest because of their role in the exch...