Dynamics of shallow wakes on gravel-bed floodplains: dataset from field experiments

O. Shumilova, A. Sukhodolov, G. Constantinescu, B. MacVicar
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引用次数: 3

Abstract

Abstract. Natural dynamics of river floodplains are driven by the interaction of flow and patchy riparian vegetation, which has implications for riverbed morphology and diversity of riparian habitats. Fundamental mechanisms affecting the dynamics of flow in such systems are still not fully understood due to a lack of experimental data collected in natural environments that are free of scaling effects present in laboratory studies. Here we present a detailed dataset on hydrodynamics of shallow wake flows that develop behind solid and porous obstructions. The dataset was collected during a field experimental campaign carried out in a side branch of the gravel-bed Tagliamento River in Northeast Italy. The dataset consists of thirty experimental runs in which we varied the diameter of the surface-mounted obstruction, its solid volume fraction, and the porosity at the leading edge, the object's submergence, and the approach velocity. Each run included: (1) measurements of mean velocity and turbulence in the longitudinal transect through the centreline of the flow with up to 25–30 sampling locations, and from 8 to 10 lateral profiles measured at 14 locations; (2) detailed surveys of the free surface topography; and (3) flow visualizations and video-recordings of the wakes patterns using a drone. The field scale of the experimental setup, the precise control of the approaching velocity, configuration of models, and the natural gravel-bed context for this experiment makes this data set unique. Besides enabling the examination of scaling effects, these data also allow the verification of numerical models and provide insight into the effects of driftwood accumulations on the dynamics of wakes. Data are made available as open access via the Zenodo portal (Shumilova et al. 2020) with DOI https://doi.org/10.5281/zenodo.3968748 .
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砾石河床洪泛平原浅层尾迹动力学:野外试验数据集
摘要河流洪泛平原的自然动态是由水流和斑块状河岸植被的相互作用驱动的,这对河床形态和河岸生境的多样性具有重要影响。由于缺乏在实验室研究中没有标度效应的自然环境中收集的实验数据,影响此类系统中流动动力学的基本机制仍未完全了解。在这里,我们提出了一个关于固体和多孔障碍物后面发展的浅尾流的流体动力学的详细数据集。该数据集是在意大利东北部塔利亚门托河砾石河床侧分支进行的现场实验活动中收集的。该数据集由30个实验组成,其中我们改变了表面安装障碍物的直径,其固体体积分数,前缘孔隙率,物体的淹没度和接近速度。每次运行包括:(1)测量25-30个采样点的流动中心线纵向样带的平均速度和湍流,以及在14个地点测量8 - 10个横向剖面;(2)自由表面地形的详细调查;(3)流动可视化和视频记录尾迹模式使用无人机。实验设置的现场规模、接近速度的精确控制、模型的配置以及该实验的天然砾石床环境使该数据集独一无二。除了能够检查尺度效应,这些数据还允许验证数值模型,并深入了解浮木积累对尾流动力学的影响。数据通过Zenodo门户网站(Shumilova et al. 2020)开放获取,DOI: https://doi.org/10.5281/zenodo.3968748。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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