Hybrid Lattice Boltzmann Method–Finite Difference Method Model for Sediment Transport and Riverbed Deformation
In this study, a two‐dimensional hybrid numerical model for sediment transport based on lattice Boltzmann method and finite difference method is presented. The governing equations for water flow and suspended sediment transport are the shallow water equations and the advection–diffusion equations, r...
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Published in | River research and applications Vol. 31; no. 4; pp. 447 - 456 |
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Main Authors | , , , , , |
Format | Journal Article |
Language | English |
Published |
Bognor Regis
John Wiley & Sons
01.05.2015
Blackwell Publishing Ltd Wiley Subscription Services, Inc |
Subjects | |
Online Access | Get full text |
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Summary: | In this study, a two‐dimensional hybrid numerical model for sediment transport based on lattice Boltzmann method and finite difference method is presented. The governing equations for water flow and suspended sediment transport are the shallow water equations and the advection–diffusion equations, respectively. Sediment load is also involved, so that riverbed deformation is numerically simulated. The model is verified by testing transportation of bank‐slump sediment in a sharp bended channel with the comparison to the results of well‐accepted finite volume method, illustrating the effectiveness of the proposed hybrid model. Copyright © 2014 John Wiley & Sons, Ltd. |
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Bibliography: | http://dx.doi.org/10.1002/rra.2735 ark:/67375/WNG-QKXZ9S9T-L istex:21C89545915156B2B6CBA4B8E8849A9FF7CA333A ArticleID:RRA2735 ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 1535-1459 1535-1467 |
DOI: | 10.1002/rra.2735 |