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平面二维溃坝水沙输移动床数学模型研究
引用本文:史英标,潘存鸿,程文龙,李志永.平面二维溃坝水沙输移动床数学模型研究[J].水利学报,2012,43(7):834-841,851.
作者姓名:史英标  潘存鸿  程文龙  李志永
作者单位:浙江省水利河口研究院,浙江杭州310020 浙江省河口海岸重点实验室,浙江杭州310016
基金项目:基金项目:国家自然科学基金资助项目,国家水体污染控制与治理科技重大专项,水利部公益性行业专项,浙江省重点科技创新团队建设项目
摘    要:为数值模拟溃坝洪水作用下泥沙输移及河床变形,建立了无结构三角形网格的平面二维水沙耦合数学模型。水动力学模型采用浑水流动方程,考虑了泥沙输移及床面冲淤变化对水流动量的影响;泥沙输移采用不平衡泥沙输移模式。模型数值计算格式采用守恒性较好的有限体积法,单元界面的对流通量采用基于近似黎曼解的Roe格式计算,扩散通量采用中心格式,不平衡泥沙输移方程采用坡度限制的二阶空间精度格式离散。模型经经典算例和小尺度瞬间全溃的动床实验资料检验,水面、床面及流速等计算结果与实验资料或解析解等比较吻合,分析了动床与定床水面及洪水传播速度的差异。在上述检验的基础上,采用动床模型对某河道型水库溃坝诱发的水沙运动进行了数值模拟,结果表明溃坝洪水下水流、泥沙及河床变形发生强烈的相互作用,采用水沙及河床变形耦合的数学模型是必要的。

关 键 词:溃坝洪水  泥沙输移  河床冲淤  有限体积法  Roe数值格式

2D movable-bed mathematical model for dam-break flow and sediment transport
SHI Ying-biao,PAN Cun-hong,CHENG Wen-long and LI Zhi-yong.2D movable-bed mathematical model for dam-break flow and sediment transport[J].Journal of Hydraulic Engineering,2012,43(7):834-841,851.
Authors:SHI Ying-biao  PAN Cun-hong  CHENG Wen-long and LI Zhi-yong
Affiliation:1,2 (1. Zhejiang Institute of Hydraulics and Estuary,Hangzhou 310020,China; 2. Key Laboratory of Estuarine and Coast of Zhejiang Province,Hangzhou 310020,China)
Abstract:A two-dimensional movable-bed mathematical model with unstructured grid has been established to simulate sediment transport and riverbed deformation under dam-break flow over movable beds. The hydrodynamic model adopts water-sediment mixture flow equations, which consider the effects of sediment transport and bed deformation on the flow. The sediment model adopts the nonequilibrium transport of suspended load. The governing equations are solved by an explicit finite-volume method with the second-order Roe’ scheme based approximate Riemann for intercell advection fluxes, and centre difference scheme with unstructured grid is adopted to compute diffusive fluxes. The model was tested by two examples with exact solution or experimental data on dam-break flow, with fairly good agreement between simulations and measurements or exact solution. Based on the verifications, the flow and sediment transport due to a dam failure were simulated respectively by means of this model. The result shows that dam-break flows over mobile beds can provoke very active sediment exchange between the water column and the bed, and it is quite necessary to simulate the flow and sediment transport process by means of coupled mathematical model.
Keywords:Flood routing due to dam failure  sediment transport  bed deformation  finite volume method  Roe's numerical scheme
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