Coupled model of surface water flow, sediment transport and morphological evolution
Computers & Geosciences
A bi-fluid lattice boltzmann model for water flow in an irrigation channel
ACRI'06 Proceedings of the 7th international conference on Cellular Automata for Research and Industry
Hi-index | 31.45 |
The D1Q3 lattice Boltzmann (LB) shallow water equation is analyzed in detail and compared with other numerical schemes. Analytical results are derived and used to discuss the accuracy and stability of the model. We show how such D1Q3 LB models for canal reaches may be easily coupled with various hydraulic interconnection structures to build models of complex irrigation networks.