Initiation of Sediment Resuspension by Combined Wave‐Current Conditions in an Artificial Seagrass Meadow
Name
JGR Earth Surface - 2025 - Zhao - Initiation of Sediment Resuspension by Combined Wave‐Current Conditions in an Artificial.pdf
Description
Published version
Size
2.01 MB
Format
Adobe PDF
Checksum (MD5)
3cdfb288263f0e7003ba504de860937d
Author(s)
Zhao, Chuyan
Nepf, Heidi
Date Issued
June 8, 2025
Journal
Journal of Geophysical Research: Earth Surface
Publisher
Wiley
Citation
Zhao, C., & Nepf, H. (2025). Initiation of sediment resuspension by combined wave-current conditions in an artificial seagrass meadow. Journal of Geophysical Research: Earth Surface, 130, e2024JF008050.
Version
Final published version
Abstract
Laboratory experiments examined the impact of current on ripple formation and the onset ofwave‐driven resuspension within an artificial seagrass meadow modeled after Zostera marina. Within themeadow, the current was less than or equal to the wave velocity. Meadows were constructed with three shootdensities: 247, 455 and 962 stems/m2, and each shoot had six flexible blades. The sediment bed, consisting of65 μm spherical grains, was initially 1.4 cm thick, allowing ripple and scour hole formation. The formation ofwave‐orbital ripples was dependent on meadow density and current magnitude. Over bare beds and sparsemeadows, ripples were present and not impacted by the addition of current, such that the wave velocityresuspension threshold with current was the same as that in pure wave conditions. In medium‐density meadows,the addition of current reduced ripple height due to plant‐generated turbulence. As current increased, ripple sizeand ripple‐generated turbulence decreased, requiring a higher wave velocity to resuspend sediment. That is, formedium density meadows, the critical wave velocity increased as the current velocity increased. Finally, indense meadows, no ripples formed and resuspension was driven by a critical value of plant‐induced turbulence,which was proportional to the total velocity (current plus wave velocity), such that as the current velocityincreased, the critical wave velocity decreased. A model predicting the critical wave velocity for the densemeadow was derived based on the assumption that resuspension was driven by a critical level of stem‐generatedturbulence.
MIT Department
Massachusetts Institute of Technology. Department of Civil and Environmental Engineering
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Creative Commons Attribution
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DOI of Published Version
https://doi.org/10.1029/2024JF008050
