Statistical characterization of erosion and sediment transport mechanics in shallow tidal environments - Part 2: Suspended sediment dynamics

被引:3
作者
Tognin, Davide [1 ]
D'Alpaos, Andrea [2 ]
D'Alpaos, Luigi [1 ]
Rinaldo, Andrea [1 ,3 ]
Carniello, Luca [1 ]
机构
[1] Univ Padua, Dept Civil Environm & Architectural Engn, Padua, Italy
[2] Univ Padua, Dept Geosci, Padua, Italy
[3] Ecole Polytech Fed Lausanne, Lab Ecohydrol ECHO IEE ENAC, Lausanne, Switzerland
关键词
IN-SITU MEASUREMENTS; SAN-FRANCISCO BAY; SATELLITE DATA; VENICE LAGOON; WIND-WAVES; WATER; TURBIDITY; GROWTH; MODEL; FLOW;
D O I
10.5194/esurf-12-201-2024
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
A proper understanding of sediment resuspension and transport processes is key to the morphodynamics of shallow tidal environments. However, a complete spatial and temporal coverage of suspended sediment concentration (SSC) to describe these processes is hardly available, preventing the effective representation of depositional dynamics in long-term modelling approaches. Through aiming to couple erosion and deposition dynamics in a unique synthetic theoretical framework, we here investigate SSC dynamics, following a similar approach to that adopted for erosion . The analysis with the peak-over-threshold theory of SSC time series computed using a fully coupled, bi-dimensional model allows us to identify interarrival times, intensities, and durations of over-threshold events and test the hypothesis of modelling SSC dynamics as a Poisson process. The effects of morphological modifications on spatial and temporal SSC patterns are investigated in the Venice Lagoon, for which several historical configurations in the last 4 centuries are available. Our results show that, similar to erosion events, SSC can be modelled as a marked Poisson process in the intertidal flats for all the analysed morphological lagoon configurations because exponentially distributed random variables describe over-threshold events well. Although erosion and resuspension are intimately intertwined, erosion alone does not suffice to describe also SSC because of the non-local dynamics due to advection and dispersion processes. The statistical characterization of SSC events completes the framework introduced for erosion mechanics, and together, they represent a promising tool to generate synthetic, yet realistic, time series of shear stress and SSC for the long-term modelling of tidal environments.
引用
收藏
页码:201 / 218
页数:18
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