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Experimental observation of turbulent structure at region surrounding the mid-channel braid bar

机译:中通道编织杆周围区域湍流结构的实验观察

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摘要

Abstract River morphological processes are among the most complex and least understood phenomenon in nature. Recent research indicates that the braiding of marine waterways of the estuary zone occurs at an aspect ratio similar to the alluvial braided river. The instability of complex sporadic fluvial processes at river-sea interface is responsible for bar formation in alluvial as well as in marine waterbodies Due to the lack of knowledge of flow characteristics around bar, the flow structure around the sand bar is analyzed. The bursting events play the crucial role in understanding the fluvial characteristics in the vicinity of submerged structure. The study of bursting events around the mid-channel bar is only done by the present author. The effect of submergence ratio on the turbulence behavior in the proximity of bar is analyzed in this study. The flow turbulence generated by the mid-channel bar is also analyzed in detail. The extreme turbulent burst is segregated from low intensity turbulent events by using the hole size concept. The effect of hole size on the parameter Dominance Function is analysed which is not yet studied by any researcher for mid-channel bar. The Momentum Dominance Function parameter increases with increase in the Hole Size. This indicates that the magnitude of upward flux increases with increase in the hole size. The effect of bar height on the turbulent burst which is not yet studied by any researchers is analyzed in the present research. The joint probability distribution of bursting events is modeled using the Gram-Charlier bivariate joint probability function. The joint probability distribution gives the details of probabilistic structure of flow in the vicinity of bar. The effect of bar is predominant only in the lower flow layer. The joint probability distribution graph becomes more eccentric toward the dominant quadrants with increase in the submergence ratio. This indicates that the probability of dominant events further increases with increase in the submergence ratio.
机译:摘要 河流形态过程是自然界中最复杂、最不为人所知的现象之一。最近的研究表明,河口带海水道的辫状发生在与冲积辫状河流相似的长宽比上。由于缺乏对沙洲周围流动特性的了解,分析了沙洲周围沙洲周围流态结构,河海界面复杂零星河流过程的不稳定性是冲积水和海洋水体形成沙洲的原因。爆裂事件对理解水下结构附近的河流特征起着至关重要的作用。对中通道柱周围的爆破事件的研究仅由本文作者完成。分析了淹没率对钢筋附近湍流行为的影响。还详细分析了中通道杆产生的流动湍流。极端湍流爆发通过使用孔尺寸概念将极端湍流爆发与低强度湍流事件分开。分析了孔径对参数优势函数的影响,但目前还没有任何研究人员对中通道棒进行研究。动量优势函数参数随着孔尺寸的增加而增加。这表明向上磁通量的大小随着孔尺寸的增加而增加。本文分析了棒高对湍流爆发的影响,这是目前尚未有研究的。使用 Gram-Charlier 双变量联合概率函数对突发事件的联合概率分布进行建模。联合概率分布给出了棒附近流动概率结构的细节。棒材的影响仅在下部流动层中占主导地位。随着淹没率的增加,联合概率分布图向优势象限变得更加偏心。这表明,随着淹没率的增加,主导事件的概率进一步增加。

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