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Suspended participate matter concentration in response to tidal hydrodynamics in a long mesotidal floodway

机译:长期中流洪水中悬浮物浓度对潮汐水动力的响应

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Analyses of seasonal data obtained using acoustic Doppler current profilers provide an understanding of the behavior of suspended particulate matter concentration (SPMC) toward different forcings in tide-controlled floodways. In this work, the relative contributions of external forcings on SPMC variability were quantified in a tidal river system using singular spectrum analysis (SSA). The main environmental features affecting SPMC were identified as i) spring-neap tidal oscillation, ii) the ebb/flood velocities, and iii) tidal straining. Large SPMC fluctuations occurred under strong mixing states and were directly related to the sediment resuspension stirred up by spring-neap tidal cycles (73.6%-81.9%) and ebb/flood velocities (9.6%-19.5%). On the seasonal scale, river discharge is the key variable explaining the downstream flushing and promoting the occurrence of a convergence zone at the floodway. Upstream from the floodway (greater than 4.8 km from the river mouth), the spring-neap tidal oscillation dominated the suspended particulate matter (SPM) mobility under low river discharge. Two interesting findings were revealed in this work: (i) the SPMC/SPM transport variation responses to tidal forcing (tidal asymmetry) were dominated and modified by river discharge and (ii) the effect of river discharge on the SPMC/SPM transport did not result in a uniform state along the floodway. It is believed that these findings provide further understanding of the dynamics of suspended sediments in shallow tidal systems.
机译:使用声学多普勒电流剖面仪获得的季节性数据的分析提供了对潮汐控制洪水中悬浮颗粒物浓度(SPMC)对不同强迫作用的理解。在这项工作中,使用奇异频谱分析(SSA)在潮河系统中量化了外部强迫对SPMC变异性的相对贡献。影响SPMC的主要环境特征是:i)春季潮汐振荡,ii)潮汐/潮汐速度和iii)潮汐应变。 SPMC的大波动发生在强混合状态下,与春季潮汐周期(73.6%-81.9%)和潮汐/潮汐速度(9.6%-19.5%)引起的泥沙再悬浮直接相关。在季节性尺度上,河流流量是解释下游冲洗并促进洪水道汇聚区发生的关键变量。在洪水道上游(距河口4.8公里),春季潮汐振荡主导了河流低流量下的悬浮颗粒物(SPM)流动性。这项工作揭示了两个有趣的发现:(i)河流排放控制着SPMC / SPM对潮汐强迫的变化响应(潮汐不对称),并且(ii)河流排放对SPMC / SPM输送的影响没有导致洪水泛滥。相信这些发现提供了对浅潮汐系统中悬浮沉积物动力学的进一步理解。

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