Abstract
The mathematical model describing the physical phenomenon of one-dimensional bed-load sediment transport in channels and rivers consists of three equations. Two of them represent conservation laws for one-dimensional shallow water equations, and third is the conservation law governing bed-load sediment transport. Here we considerone possibletype of the sediment flux proposed by Hudson and Sweby [7]. We compare numerical results for test problems using different numerical schemes: Q-scheme, Hubbard’s scheme, ENO Roe and ENO locally Lax-Friedrichs scheme. The obtained results illustrate good properties of ENO schemes with the source term decomposition, developed by authors. We also prove that these schemes have the exact C-property when applied to the sediment transport equations.
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© 2002 Springer Science+Business Media New York
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Sopta, L., Črnjarić-Žic, N., Vuković, S. (2002). Numerical Approximations of the Sediment Transport Equations. In: Drmač, Z., Hari, V., Sopta, L., Tutek, Z., Veselić, K. (eds) Applied Mathematics and Scientific Computing. Springer, Boston, MA. https://doi.org/10.1007/978-1-4757-4532-0_16
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DOI: https://doi.org/10.1007/978-1-4757-4532-0_16
Publisher Name: Springer, Boston, MA
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