Evaluation of Coastal Sediment Transport Processes

A special issue of Water (ISSN 2073-4441). This special issue belongs to the section "Water Erosion and Sediment Transport".

Deadline for manuscript submissions: closed (25 January 2022) | Viewed by 2244

Special Issue Editor


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Guest Editor
Department of Physics, University of Girona, Girona, Catalonia, Spain
Interests: seagrasses; sediment transport; saltmarshes; coastal oceanography; gravity currents

Special Issue Information

Dear Colleagues,

The sediment distribution in transitional land–ocean zones, and the subsequent impact it has on many biogeochemical processes, is determined by its erosion and transport in coastal areas. In these areas, management practices or anthropogenic activities, such as dredging, recreational activities, boat anchoring, and/or fishing, among others, negatively impact coastal ecosystems. Research on management issues that involve protecting or restoring coastal ecosystems, and/or their adaptation to future climate change scenarios, might generate tools with which to maintain the ecological value of these habitats. Sediment transport is expected to vary as a result of the physical forcing associated with waves, currents, wind, gravity currents, the strength of the stratification of the water column, or turbulence. Deltas, breakwaters, and harbors, as well as seagrasses, etc., modify the fate of the sediment being transported. For instance, river plumes flowing to the sea produce high sediment concentrations along coastal areas. Coastal seagrasses and the vegetation in salt marshes are known to enhance particle sedimentation by reducing both the flow velocity and the turbulent kinetic energy, whereas anthropogenic activities are known to threaten such ecosystems by producing gaps (i.e., zones of bare soil) interspersed within the vegetation, resulting in a fragmented meadow. The capture of sediment by a fragmented meadow is expected to be reduced compared with that by a continuous meadow. Additionally, predictive modeling of the transport processes of sediment along coastlines will provide us with information on its behavior under different scenarios. In this Special Issue, we invite scientists working on the different aspects of sediment transport in coastal or watershed areas to share their most recent results. Papers submitted could deal with sediment transport, modeling, gravity current dynamics, the interaction between aquatic vegetation and sediment, sediment dynamics in fragmented meadows, or sediment resuspension.

Dr. Teresa Serra
Guest Editor

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Keywords

  • sediment transport processes
  • sediment resuspension
  • estuaries
  • coastal zones
  • coastal wetlands
  • river plume
  • nearshore processes
  • numerical modeling
  • seagrasses
  • seagrass fragmentation

Published Papers (1 paper)

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Research

25 pages, 2436 KiB  
Article
Wind-Induced Resuspension and Transport of Contaminated Sediment from the Rove Canal into the Etang De Berre, France
by Elena Alekseenko, Bernard Roux and Konstantin Kuznetsov
Water 2022, 14(1), 62; https://0-doi-org.brum.beds.ac.uk/10.3390/w14010062 - 29 Dec 2021
Cited by 1 | Viewed by 1722
Abstract
The present study concerns the erosion and transport of severely contaminated sediments in a Canal. It begins in the context of an engineering project aimed to re-introduce a forced convection at the entrance of this Canal by pumping marine water. The local wind [...] Read more.
The present study concerns the erosion and transport of severely contaminated sediments in a Canal. It begins in the context of an engineering project aimed to re-introduce a forced convection at the entrance of this Canal by pumping marine water. The local wind is often strong enough to overpass the resuspension threshold; thus, there is a serious risk of downstream contamination of a Mediterranean lagoon. So, the goal is to evaluate this risk as a function of the pumping rate; this contamination is transported by the fine suspended particles. Different scenarios are investigated to determine the downstream transport of suspensions in terms of runoff. These scenarios (of 24 h) contains a succession of 3 periods: constant wind speed, wind slowdown and calm, for two opposite wind directions. Special attention is devoted to the modeling of complex mechanisms of erosion and resuspension during wind periods, deposition during windless periods and sediment consolidation. The main results concern the total flux of the suspended particles through the exit of the Canal at the confluence with the lagoon. It is shown that even for moderate runoff (<6 m3/s) this total flux is large enough, not only during the wind period, but also after several hours of calm. Full article
(This article belongs to the Special Issue Evaluation of Coastal Sediment Transport Processes)
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