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Coupling bank stability and bed deformation models to predict equilibrium bed topography in river bends

Coupling bank stability and bed deformation models to predict equilibrium bed topography in river bends
Coupling bank stability and bed deformation models to predict equilibrium bed topography in river bends
Attempts to include river bank erosion predictors within morphological models are becoming increasingly common, but uncertainty surrounds the procedures used to couple bed deformation and bank erosion submodels in a way that maintains the mass continuity of eroded bank sediment. Herein we present a coupling procedure that comprises two discrete elements. First, immediately following bank failure, the slumped debris comes to rest at the bank toe as a planar surface inclined at an “angle of repose.” Second, we use a fractional transport model to simulate the subsequent erosion and deposition of the failed bank material debris. The method is demonstrated with an example in which an equilibrium bed topography model is combined with a river bank erosion model to predict the morphological response of a river bend to a large flow event.
1167-1170
Amiri-Tokaldany, Ebrahim
1a6e2108-a21e-468c-88ce-2474e854b753
Darby, Stephen E.
4c3e1c76-d404-4ff3-86f8-84e42fbb7970
Tosswell, Paul
cbb71d4e-701e-4750-8092-82e2c16843a4
Amiri-Tokaldany, Ebrahim
1a6e2108-a21e-468c-88ce-2474e854b753
Darby, Stephen E.
4c3e1c76-d404-4ff3-86f8-84e42fbb7970
Tosswell, Paul
cbb71d4e-701e-4750-8092-82e2c16843a4

Amiri-Tokaldany, Ebrahim, Darby, Stephen E. and Tosswell, Paul (2007) Coupling bank stability and bed deformation models to predict equilibrium bed topography in river bends. Journal of Hydraulic Engineering, 133 (10), 1167-1170. (doi:10.1061/(ASCE)0733-9429(2007)133:10(1167)).

Record type: Article

Abstract

Attempts to include river bank erosion predictors within morphological models are becoming increasingly common, but uncertainty surrounds the procedures used to couple bed deformation and bank erosion submodels in a way that maintains the mass continuity of eroded bank sediment. Herein we present a coupling procedure that comprises two discrete elements. First, immediately following bank failure, the slumped debris comes to rest at the bank toe as a planar surface inclined at an “angle of repose.” Second, we use a fractional transport model to simulate the subsequent erosion and deposition of the failed bank material debris. The method is demonstrated with an example in which an equilibrium bed topography model is combined with a river bank erosion model to predict the morphological response of a river bend to a large flow event.

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Published date: 1 October 2007

Identifiers

Local EPrints ID: 55523
URI: http://eprints.soton.ac.uk/id/eprint/55523
PURE UUID: 40e57537-cebb-4d79-b690-702028276a9f
ORCID for Stephen E. Darby: ORCID iD orcid.org/0000-0001-8778-4394

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Date deposited: 01 Aug 2008
Last modified: 16 Mar 2024 02:59

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Contributors

Author: Ebrahim Amiri-Tokaldany
Author: Paul Tosswell

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