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首页> 外文期刊>Environmental fluid mechanics >Influence of seafloor topography on the depositional behavior of bi-disperse turbidity currents: a three-dimensional, depth-resolved numerical investigation
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Influence of seafloor topography on the depositional behavior of bi-disperse turbidity currents: a three-dimensional, depth-resolved numerical investigation

机译:海底地形对双分散浊流沉积行为的影响:三维深度解析数值研究

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We discuss the results of direct numerical simulations of bi-disperse turbidity currents interacting with a flat bottom wall and a Gaussian bump, respectively, with a focus on the final deposit profiles of the coarse and fine particles. We identify regions of reduced and enhanced deposition, as a result of the presence of the bump. Coarse particles are predominantly deposited towards the sides of the bump, as a result of the bi-section and lateral deflection of the current by the bump. In contrast, for fine particles the influence of the bump is felt more in its far wake.We furthermore employ Lagrangian markers in order to track the coarse and fine particles in the current, and to investigate their deposit locations as function of their location of origin. By comparing the final deposit maps, we observe that the bump has the strongest influence on those particles originating in the central lock sections.
机译:我们讨论了分别与平坦底壁和高斯凸点相互作用的双分散浊度电流的直接数值模拟结果,重点是粗颗粒和细颗粒的最终沉积轮廓。由于存在凸点,我们确定了沉积减少和增加的区域。由于电流的两部分和横向偏转,粗颗粒主要沉积在凸块的侧面。相比之下,对于细颗粒,凹凸的影响在远处更为明显。我们还采用拉格朗日标记,以跟踪电流中的粗颗粒和细颗粒,并研究其沉积位置与原点的关系。通过比较最终的沉积图,我们观察到凸点对源自中央锁定部分的那些粒子的影响最大。

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