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

机译:基于基座同步场调查系统的长江口北通道表层流量测量

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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/m 3 , 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.
机译:为了在台风期间测量长江口北通道底部附近的表层水流,将基于Nortek AquaPro,Nortem AquaPro HR,AWAC和OBS 3+的水下同步现场测量系统安装在基于基座的结构上。该系统用于2015年汛期的片状流场调查。基台同步场调查系统可以合理估计其自身的稳定性,同时还可以捕获海浪气候以及当前特征和附近的泥沙浓度。底端。通过分析系统收集的数据,发现潮流主导了长江口底部附近的沉积物浓度,没有波动,并且悬浮物浓度的唯一峰值出现在秋天的松弛时间。底部50cm以上的悬浮泥沙浓度通常不大于15kg / m 3,与波浪没有显着相关性。发生台风时,到底部30厘米以下的悬浮沉积物浓度会显着增加。在春季松弛期和秋季松弛期分别有两个悬浮物浓度峰值。

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