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The sediment suspension and transport process under complex breaking wave situation is investigated using large eddy simulation (abbreviated as LES hereafter) method. The coupled level set (LS) and volume of fluid (VOF) method is used to accurately capture the evolution of air?water interface. The wall effect at the bottom is modeled based on the wave friction term while the complicate bottom boundary condition for sediment is tackled using Chou and Fringer’s sediment erosion and deposition flux method. A simulation is carried out to study the sediment suspension and transport process under periodic plunging breaking waves. The comparison between the results by CLSVOF method and those obtained by the LS method is given. It shows that the latter performs as well as the CLSVOF method in the pre-breaking weak-surface deformation situation. However, a serious mass conservation problem in the later stages of wave breaking makes it inappropriate for this study by use of the LS method and thus the CLSVOF method is suggested. The flow field and the distribution of suspended sediment concentration are then analyzed in detail. At the early stage of breaking, the sediment is mainly concentrated near the bottom area. During the wave breaking process, when the entrapped large-scale air bubble travels downward to approach the bottom, strong shear is induced and the sediment is highly entrained.  相似文献   
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各向异性密度流模型及其验证   总被引:1,自引:0,他引:1       下载免费PDF全文
针对密度流流动各向异性的特性,采用非线性k-ε模式求取雷诺应力,结合RNG模型及浮力修正建立了三维密度流模型.应用该三维模型计算了水库温差异重流,分析了温差异重流演进过程,并就流速分布与水温下泄过程与实测资料进行了比较.结果表明,所建模型由于引入非线性RNG模式,能有效反映密度流的各向异性特性,较好地模拟了流场和温度场强烈耦合的水库温差异重流,能准确预测温度分层过程与异重流潜行时间,具有较高精度.  相似文献   
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