反沙丘上流动振荡自由表面的三维重建:立体和速度技术

D. Douxchamps, D. Devriendt, H. Capart, Christophe Craeye, B. Macq, Y. Zech
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引用次数: 6

摘要

作者提出了成像方法发展表征振荡自由表面的快速流动,并将其应用于在泥沙反沙丘上传播的急流。目的是获得自由地表地形的高分辨率地形图,以便突出与地形相关的规则空间模式。概述并测试了两种测量原理,这两种原理都是基于分散在快速流动表面的浮动示踪剂的成像。第一种方法依赖于使用两台相机获得的直接立体测量,而第二种方法利用原始的速度测量原理,允许从使用单个相机获得的速度场中获得仰角。介绍了这两种方法的测量程序和图像分析算法,以及速度测量原理的物理假设。比较了两种方法在不同自由曲面上的结果,得到了良好的对应关系。所获得的地形图生动地描绘了浅层水流和松散沉积层之间相互作用所产生的各种图案。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Three-dimensional reconstruction of the oscillatory free-surfaces of a flow over antidunes: stereoscopic and velocimetric techniques
The authors present imaging methods developed to characterize the oscillatory free-surface of rapid flows and apply them to torrential currents propagating over sediment antidunes. The aim is to obtain high-resolution relief maps of the free-surface topography, in order to highlight the regular spatial patterns associated with the bedforms. Two measurement principles are outlined and tested, both based on the imaging of floating tracers dispersed on the rapidly flowing surface. The first relies on direct stereoscopic measurements obtained using two cameras, while the second exploits an original velocimetric principle allowing to derive elevation from the velocity field acquired using a single camera. The measurement procedures and image analysis algorithms are introduced for the two methods, along with the physical assumptions underlying the velocimetric principle. The results of the two techniques are compared for different free-surface patterns and good correspondence is obtained. The obtained relief maps vividly depict the variety of motifs that can evolve as a result of interaction between shallow flows and loose sediment beds.
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