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

IF 2.8 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Davide Tognin, Andrea D'Alpaos, Luigi D'Alpaos, Andrea Rinaldo, Luca Carniello
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Abstract

Abstract. 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 (D'Alpaos et al., 2024). 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.
浅海潮汐环境中侵蚀和沉积物迁移力学的统计特征--第 2 部分:悬浮沉积物动力学
摘要正确理解沉积物的再悬浮和运移过程是浅海潮汐环境形态动力学的关键。然而,用于描述这些过程的悬浮沉积物浓度(SSC)几乎没有完整的时空覆盖范围,这阻碍了长期建模方法对沉积动力学的有效表述。通过在一个独特的合成理论框架中将侵蚀和沉积动力学结合起来,我们在此采用与侵蚀类似的方法研究悬浮沉积动力学(D'Alpaos 等人,2024 年)。利用完全耦合的二维模型计算的 SSC 时间序列的峰值-过阈值理论进行分析,使我们能够确定过阈值事件的到达时间、强度和持续时间,并检验将 SSC 动态模拟为泊松过程的假设。我们在威尼斯泻湖研究了形态变化对 SSC 空间和时间模式的影响。我们的研究结果表明,与侵蚀事件类似,在所有分析过的形态泻湖配置中,潮间带滩涂中的 SSC 可被模拟为一个明显的泊松过程,因为指数分布的随机变量能很好地描述超阈值事件。尽管侵蚀和再悬浮密切相关,但由于平流和扩散过程造成的非局部动态,仅靠侵蚀还不足以描述 SSC。对 SSC 事件的统计特征描述完善了侵蚀力学的框架,它们共同构成了一种很有前途的工具,可用于生成合成但真实的剪应力和 SSC 时间序列,用于潮汐环境的长期建模。
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来源期刊
Earth Surface Dynamics
Earth Surface Dynamics GEOGRAPHY, PHYSICALGEOSCIENCES, MULTIDISCI-GEOSCIENCES, MULTIDISCIPLINARY
CiteScore
5.40
自引率
5.90%
发文量
56
审稿时长
20 weeks
期刊介绍: Earth Surface Dynamics (ESurf) is an international scientific journal dedicated to the publication and discussion of high-quality research on the physical, chemical, and biological processes shaping Earth''s surface and their interactions on all scales.
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