Sheet flow measurement in the north passage of Yangtze estuary with pedestal based synchronous field survey system

Xiao Jia , Hua-Cong Huang , Yuan-Ye Wang , Hua Liu
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Abstract

In order to measure sheet flow near the bottom in the north passage of Yangtze Estuary during the typhoon, a submerged synchronous field survey system composited of Nortek AquaPro, Nortem AquaPro HR, AWAC and OBS 3+ was equipped on a pedestal based structure. The system was used to survey sheet flow field during the flooding season in 2015. The pedestal base synchronous field survey system can give reasonable estimation about stability of itself, and also capture simultaneously the wave climate as well as the current feature and the sediment concentration near the bottom. Analyzing the data collected by the system, it is found that the tidal current dominates the sedimentation concentration near the bottom in the Yangtze Estuary without waves, and the only peak value of suspended sediment concentration occurs at the fall slack time. The suspended sediment concentration above 50cm to the bottom is usually not larger than 15kg/m3, and it is not significantly correlated with the wave. When typhoon happens, the suspended sediment concentration increases significantly below 30cm to the bottom. There are two peaks of the suspended sediment concentration at the spring slack and the fall slack time respectively.

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基于台座式同步野外测量系统的长江口北槽片流测量
为了在台风期间测量长江口北通道近底部的片流,在台座式结构上安装了由Nortek AquaPro、Nortem AquaPro HR、AWAC和OBS 3+组成的水下同步野外测量系统。该系统用于2015年汛期的片材流场测量。台基同步野外调查系统可以对其自身的稳定性进行合理的估计,并能同时捕获波浪气候、水流特征和近底沉积物浓度。对系统采集的数据进行分析发现,长江口近底沉积浓度主要由潮流主导,无波浪,悬沙浓度的唯一峰值出现在秋季松弛期。离底50cm以上的悬沙浓度通常不大于15kg/m3,与波浪的相关性不显著。台风发生时,底部30cm以下的悬沙浓度显著增加。悬沙浓度在春季松弛期和秋季松弛期分别出现两个峰值。
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