A Three-Dimensional Flow and Sediment Transport Model for Free-Surface Open Channel Flows on Unstructured Flexible Meshes

被引:18
|
作者
Lai, Yong G. [1 ]
Wu, Kuowei [2 ,3 ]
机构
[1] US Bur Reclamat, Tech Serv Ctr, Denver, CO 80225 USA
[2] Water Resources Agcy, Water Resources Planning Inst, Taichung 413, Taiwan
[3] Natl Chiao Tung Univ, Dept Civil Engn, Hsinchu 300, Taiwan
来源
FLUIDS | 2019年 / 4卷 / 01期
关键词
3D hydraulic model; 3D sediment model; turbidity current; polygonal mesh; hydrostatic assumption; BED; FORMULATION;
D O I
10.3390/fluids4010018
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Three-dimensional (3D) hydrostatic-pressure-assumption numerical models are widely used for environmental flows with free surfaces and phase interfaces. In this study, a new flow and sediment transport model is developed, aiming to be general and more flexible than existing models. A general set of governing equations are used for the flow and suspended sediment transport, an improved solution algorithm is proposed, and a new mesh type is developed based on the unstructured polygonal mesh in the horizontal plane and a terrain-following sigma mesh in the vertical direction. The new flow model is verified first with the experimental cases, to ensure the validity of flow and free surface predictions. The model is then validated with cases having the suspended sediment transport. In particular, turbidity current flows are simulated to examine how the model predicts the interface between the fluid and sediments. The predicted results agree well with the available experimental data for all test cases. The model is generally applicable to all open-channel flows, such as rivers and reservoirs, with both flow and suspended sediment transport issues.
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页数:19
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