Barchans与沙丘大小的障碍物相互作用:流体流动和颗粒运动的细节

IF 3.5 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
N. C. Lima, W. R. Assis, D. S. Borges, E. M. Franklin
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引用次数: 0

摘要

我们通过进行数值模拟来研究水下坝与沙丘大小障碍物相互作用的细节,其中流体在颗粒尺度上求解,并且在所有时间步长上计算单个颗粒的运动。通过输出,我们分析了流体流动的扰动,颗粒的轨迹,以及对每个颗粒的合力,后者从实验和现场测量中是不可行的。我们表明,在某些情况下,粒子越过障碍物,而在其他情况下,它们完全绕过它(没有接触它),甚至被阻挡。对于规避和阻塞情况,我们分别称之为绕过和困住,我们表明在沙丘的背风面和障碍物之间存在一个强涡。这种涡旋是再循环区域和马蹄涡相互作用的结果,在这种情况下,它有足够的强度偏离主流并携带颗粒绕过障碍物。我们的研究结果揭示了穿越、绕过和阻塞沙丘的原因,并有助于我们理解沙丘在诸如山丘、陨石坑边缘和人类建筑等大型障碍物存在时的情况。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Barchans Interacting With Dune-Size Obstacles: Details of the Fluid Flow and Motion of Grains

We investigate details of the interaction of subaqueous barchans with dune-size obstacles by carrying out numerical simulations where the fluid is solved at the grain scale and the motions of individual grains are computed at all time steps. With the outputs, we analyze the disturbances of the fluid flow, the trajectories of grains, and the resultant force on each grain, the latter being unfeasible from experiments and field measurements. We show that in some cases particles pass over the obstacle, while in others they completely circumvent it (without touching it), or are even blocked. For the circumvention and blocking cases, which we call bypass and trapped, respectively, we show the existence of a strong vortex between the lee face of the dune and the obstacle. This vortex results from the interactions of recirculation regions and horseshoe vortices, and has enough strength to deviate the main flow and carry grains around the obstacle in those cases. Our results shed light on the reasons for passing over, circumventing, and blocking, and contribute to our understanding of dunes in the presence of large obstacles such as hills, crater rims, and human constructions.

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来源期刊
Journal of Geophysical Research: Earth Surface
Journal of Geophysical Research: Earth Surface Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
6.30
自引率
10.30%
发文量
162
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