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首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Lattice Boltzmann simulation of the flocculation process of cohesive sediment due to differential settling
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Lattice Boltzmann simulation of the flocculation process of cohesive sediment due to differential settling

机译:差异沉降引起的粘性沉积物絮凝过程的格子Boltzmann模拟

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The flocculation processes for differential settling of cohesive sediment were simulated via the Lattice Boltzmann method (LBM) in which the hydrodynamics and attractive van der Waals forces were considered. The simulations were performed with different initial sediment concentrations, and hydrodynamic properties of flocs formed by differential settling, such as size spectra, settling velocities, flow fields around flocs and particle motion trajectories, are discussed in detail. Results indicate that flocs containing the same primary particles formed by different sediment concentrations have similar settling velocities, which means that sediment concentrations exert few effects on flocs settling velocities themselves. Otherwise, sediment concentrations influence the bulk mean settling velocity of suspended sediment. The higher the sediment concentration, the larger the bulk mean settling velocity, which is attributed to the higher-concentration particles colliding easily and quickly forming larger flocs. Statistical analysis shows that numerical results clearly reproduce collision properties because of the differential settling at the mesoscale. These results suggest that LBM may be a promising approach to study the flocculation mechanisms of cohesive sediments.
机译:通过莱迪思·玻尔兹曼方法(LBM)模拟了凝聚性沉积物差异沉降的絮凝过程,其中考虑了流体动力学和范德华力。在不同的初始沉积物浓度下进行了模拟,并详细讨论了由微分沉降形成的絮凝物的流体力学特性,例如尺寸谱,沉降速度,絮凝物周围的流场和颗粒运动轨迹。结果表明,由不同沉积物浓度形成的包含相同初级颗粒的絮凝物具有相似的沉降速度,这意味着沉积物浓度对絮凝物沉降速度本身几乎没有影响。否则,泥沙浓度会影响悬浮泥沙的体积平均沉降速度。沉积物浓度越高,堆积平均沉降速度越大,这归因于浓度较高的颗粒容易碰撞并迅速形成较大的絮凝物。统计分析表明,由于中尺度的差异沉降,数值结果清楚地再现了碰撞属性。这些结果表明,LBM可能是研究粘性沉积物絮凝机理的一种有前途的方法。

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