Role of eelgrass on bed-load transport and sediment resuspension under oscillatory flow

Beatriz Marin-Diaz, Tjeerd J. Bouma, Eduardo Infantes*

*Corresponding author for this work

Research output: Contribution to journalArticleScientificpeer-review

Abstract

Coastal vegetation is widely attributed to stabilize sediment. While most studies focused on how canopy causes flow reduction and thereby affects sediment dynamics, the role of roots and rhizomes on stabilizing the surface sediment has been less well studied. This study aims to quantify interactions between above- and belowground biomass of eelgrass (i.e., living Zostera marina plants and mimics) with surface sediment erosion (i.e., bed load and suspended load), under different hydrodynamic forcing that was created using a wave flume. Belowground biomass played an important role preventing bed-load erosion, by roughly halving the amount of sediment transported after being exposed to maximal orbital velocities of 27 cm s−1, with and without canopy. Surprisingly, for suspended sediment transport, we found opposite effects. In the presence of eelgrass, the critical erosion threshold started at lower velocities than on bare sediment, including sand and mud treatments. Moreover, in muddy systems, such resuspension reduced the light level below the minimum requirement of Z. marina. This surprising result for sediment resuspension was ascribed to a too small eelgrass patch for reducing waves but rather showing enhanced turbulence and scouring at meadow edges. Overall, we conclude that the conservation of the existent eelgrass meadows with developed roots and rhizomes is important for the sediment stabilization and the meadow scale should be taken into account to decrease sediment resuspension.

Original languageEnglish
Pages (from-to)426-436
Number of pages11
JournalLimnology and Oceanography
Volume65
Issue number2
DOIs
Publication statusPublished - 2020

Funding

B. Marin‐Diaz would like to thank to Erasmus+ and MOBINT grants and to the University of Gothenburg. E. Infantes will like to thank FORMAS grant Dnr. 231‐2014‐735. We thank the staff of Sven Lovén Center, Kristineberg Station for providing their great facilities. Funds for this work were also provided by the Wilhelm and Martina Lundgrens Foundation and the Royal Society of Arts and Sciences in Gothenburg.

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