A physically-based bedload transport model developed for 3-D reach-scale cellular modelling

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dc.contributor.author Hodge, Rebecca A.
dc.contributor.author Richards, Keith
dc.contributor.author Brasington, James
dc.date.accessioned 2011-07-04T11:45:10Z
dc.date.available 2011-07-04T11:45:10Z
dc.date.issued 2011-07-04
dc.identifier.citation Hodge , R A , Richards , K & Brasington , J 2011 , ' A physically-based bedload transport model developed for 3-D reach-scale cellular modelling ' Geomorphology , pp. 244-262 . en
dc.identifier.other PURE: 168864
dc.identifier.other dspace: 2160/7124
dc.identifier.uri http://hdl.handle.net/2160/7124
dc.description Hodge, R., Richards, K., Brasington, J. (2007). A physically-based bedload transport model developed for 3-D reach-scale cellular modelling. Geomorphology, 90(3), 244-262. en
dc.description.abstract A bedload transport model is outlined which aims to provide a more physically-based description of bed surface and bedload grain-size distributions (GSDs) than existing empirical bedload models, but is simple enough to be incorporated in a reduced-complexity modelling framework. One motivation for this is the increasing need for 3-D models of decadal, reach-scale channel and floodplain evolution for use in river management. The computational demands of simulation at these scales mean that the appropriate models are necessarily of the reduced-complexity type. The bedload model is derived through analysis of sediment beds created using a discrete element model. These beds are “eroded” using a probabilistic entrainment algorithm which predicts the bedload GSD. There are two parts to the bedload model. The first identifies a functional relationship between the applied shear stress and the fraction of the bed undergoing active transport, while the second uses this fraction, in conjunction with the surface GSD, to produce a bedload GSD. The model produces bedload coarsening as shear stress increases from a value of one to a value of five times a reference shear stress. This model is tested in a series of numerical experiments, applied using a simple cellular model of a straight flume, which is run in both recirculation and feed modes. In both modes, the equilibrium GSDs of the bedload and surface are consistent with expected flume behaviour, suggesting that the model provides a reasonable reproduction of sediment entrainment, transport and sorting. en
dc.format.extent 19 en
dc.language.iso eng
dc.relation.ispartof Geomorphology en
dc.title A physically-based bedload transport model developed for 3-D reach-scale cellular modelling en
dc.type Text en
dc.type.publicationtype Article (Journal) en
dc.contributor.institution Institute of Geography & Earth Sciences en
dc.contributor.institution River Basin Dynamics and Hydrology en
dc.description.status Peer reviewed en


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