首页> 外文期刊>Continental Shelf Research: A Companion Journal to Deep-Sea Research and Progress in Oceanography >Observations of cohesive sediment behaviors in the muddy area of the northern Taiwan Strait, China
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Observations of cohesive sediment behaviors in the muddy area of the northern Taiwan Strait, China

机译:台湾海峡北部泥泞地区黏性泥沙行为的观测

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摘要

To study cohesive sediment behaviors and their time-variability in the near-bottom layer in the muddy area of the northern Taiwan Strait (TS), a short-term bottom-mounted tripod, which was equipped with an acoustic Doppler velocimeter (ADV), an upward acoustic Doppler current profiler (ADCP) and a CTD with a Seapoint turbidity sensor, was deployed at the northern TS over seven days between July 22 and 29, 2012. The near-bed current velocity, wave orbital velocity, bottom shear stress induced by wave and current, near-bed suspended sediment concentration (SSC) and variations in the bed elevation were resolved. The observation results indicate that the most important semidiurnal constituent at the northwest TS is M-2 and that the near-bed (0.7 mab) current speed showed spring-neap cyclic characteristics, with a maximum value of 0.453 m/s. Additionally, the water flowed in acounter-clockwise rotary current pattern. The weather was fair during the observation, and the significant wave height ranged from 0.60 m to 1.81 m, which generated an extremely low wave orbital velocity (the maximum value was 0.128 m/s). The near-bed SSC estimated from the signal-noise ratio recorded by the ADV ranged from 1.48 mg/L to 74.95 mg/L. The relation between the bottom shear stress and the SSC suggested that the local sediment resuspension is primarily controlled by a tidal current and that the wave action was practically negligible during the observation. The resulting net near-bed horizontal transport flux was 1387.59 kg/m(2) during the observations, dominated by the along-shelf flux (approximately 3.74 times than cross-shelf flux) and directed toward the NNE. The bed elevation revealed that the mean value of the erosion and deposition depth during a tidal cycle could reach 14.8 mm in an intermediate tide, with a maximum value of 17.9 mm; the net effect during the observation was erosion, with a depth of 0.4 mm. (C) 2014 Elsevier Ltd. All rights reserved.
机译:为了研究台湾海峡北部(TS)泥泞地区近底部的粘性沉积物行为及其随时间的变化,这是一个短期的底部安装的三脚架,配有声学多普勒测速仪(ADV),在2012年7月22日至29日的7天内,在北部TS部署了向上声学多普勒电流剖面仪(ADCP)和带有Seapoint浊度传感器的CTD。感应到的近床层流速,波轨道速度,底部切应力通过波和电流,解决了近床悬浮沉积物浓度(SSC)和床高的变化。观测结果表明,西北部TS最重要的半日成分是M-2,近床层(0.7 mab)的当前速度呈现出春季-春季的周期性特征,最大值为0.453 m / s。另外,水以逆时针旋转电流模式流动。观测期间天气晴朗,有效波高在0.60 m至1.81 m范围内,产生极低的波轨道速度(最大值为0.128 m / s)。根据ADV记录的信噪比估算的近床SSC范围为1.48 mg / L至74.95 mg / L。底部切应力与SSC之间的关系表明,局部泥沙的重新悬浮主要是由潮流控制的,在观测过程中波浪作用实际上可以忽略不计。在观测期间,所得净近床水平输送通量为1387.59 kg / m(2),主要由沿架通量(比跨架通量约大3.74倍)主导,并指向NNE。床高表明,在一个潮汐周期中,一个潮汐周期的侵蚀和沉积深度的平均值可以达到14.8mm,最大值为17.9mm。观察期间的净效应是侵蚀,深度为0.4毫米。 (C)2014 Elsevier Ltd.保留所有权利。

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