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首页> 外文期刊>Journal of sea research >Long-term ferry-based observations of the suspended sediment fluxes through the Marsdiep inlet using acoustic Doppler current profilers
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Long-term ferry-based observations of the suspended sediment fluxes through the Marsdiep inlet using acoustic Doppler current profilers

机译:使用声学多普勒电流剖面仪对通过Marsdiep入口的悬浮泥沙通量进行基于轮渡的长期观测

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摘要

Long-term measurements with a hull mounted acoustic Doppler current profiler (ADCP) under the ferry, crossing the Marsdiep inlet between the mainland and the island of Texel (the Netherlands), were used to determine the volume flux and the flux of suspended paniculate matter (SPM) through this inlet for the period 2003-2005. Profiles of the SPM concentration were estimated from profiles of the acoustic backscatter intensity in which the shift between the low and the high turbulent regime is taken into account Calibration constants and tuning parameters were estimated by using data collected during 7 different 13 hour anchor stations. The residual (water) volume flux through the inlet appears to vary strongly on a variety of time scales from daily to inter-annual. A regression analysis indicates that the daily residual volume transport correlates well with the daily mean wind component from the south; the latter likely drives the residual flow along the coast of Holland. The observed residual SPM transport of 7 to 11 Mton/yr is dominated by the correlation between tidal velocity and SPM concentration variations. This leads to an import as currents and SPM concentrations during flood were higher than those during ebb, a process generally known as tidal asymmetry. Our analysis has shown that regular observations with a ferry mounted ADCP is an effective method to monitor the volume and SPM transport processes in an estuary.
机译:使用渡轮下方船体安装的声学多普勒电流剖面仪(ADCP)穿越大陆和特塞尔岛(荷兰)之间的Marsdiep入口进行长期测量,以确定体积通量和悬浮颗粒物通量(SPM)通过该入口进入2003-2005年。 SPM浓度的分布图是根据声学反向散射强度的分布图估算的,其中考虑了低湍流和高湍流态之间的偏移,并使用在7个不同的13小时锚定站收集的数据估算了校准常数和调整参数。从进水口到水的残留(水)流量似乎在每天到每年的各种时间尺度上变化很大。回归分析表明,每日剩余体积输运与来自南部的每日平均风分量具有很好的相关性;后者可能会驱使沿荷兰海岸的剩余水流。潮汐速度和SPM浓度变化之间的相关性决定了观测到的7-11 Mton / yr的残留SPM迁移量。这导致输入,因为洪水期间的水流和SPM浓度高于退潮期间的水流和SPM浓度,这一过程通常称为潮汐不对称。我们的分析表明,使用轮渡安装的ADCP进行定期观测是监控河口中水量和SPM运输过程的有效方法。

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