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

被引:8
|
作者
Xiao, Cong [1 ]
Kawanisi, Kiyosi [1 ]
Al Sawaf, Mohamad Basel [1 ]
机构
[1] Hiroshima Univ, Grad Sch Engn, Dept Civil & Environm Engn, 1-4-1 Kagamiyama, Higashihiroshima 7398527, Japan
基金
日本学术振兴会;
关键词
Acoustic Doppler current profiling; Tidal hydrodynamics; Suspended particulate matter; Estuary; Single spectrum analysis; Spring-neap tidal oscillation; SINGULAR-SPECTRUM ANALYSIS; SAN-FRANCISCO BAY; SEDIMENT CONCENTRATION; RIVER ESTUARY; TURBIDITY; WATER; VARIABILITY; SUSPENSION; TURBULENCE; TRANSPORT;
D O I
10.1016/j.ecss.2019.106525
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
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.
引用
收藏
页数:15
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