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This page provides a simple browsing interface for finding entities described by a property and a named value. Other available search interfaces include the page property search, and the ask query builder.
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- Model:Equilibrium Calculator + (We present an equilibrium solution that ma … We present an equilibrium solution that may or may not be reached. The fundamental assumption is that in the absence of subsidence, uplift and change of downstream water surface base level, an alluvial river will evolve toward an equilibrium state in which overbank and bar deposition (floodplain construction) are perfectly balanced by the removal of floodplain sediment due to channel migration (floodplain shaving) (Lauer & Parker, 2006). This equilibrium state can be reached if hydrologic regime, sediment supply and caliber do not vary in time. </br></br>Reference</br>Lauer, J. W. & Parker, G. (2006). Net local removal of floodplain sediment by river meander migration, Geomorphology 96, 123-149.iver meander migration, Geomorphology 96, 123-149.)
