Vegetation‐Generated Turbulence Does Not Impact the Erosion of Natural Cohesive Sediment

Author:

Deitrick Autumn R.12ORCID,Ralston David K.3ORCID,Esposito Christopher R.4ORCID,Baustian Melissa M.5ORCID,Burgos Maricel Beltrán4ORCID,Courtois Andrew J.4,Nepf Heidi1ORCID

Affiliation:

1. Civil and Environmental Engineering M.I.T Cambridge MA USA

2. MIT‐WHOI Joint Program in Oceanography/Applied Ocean Science and Engineering Cambridge and Woods Hole MA USA

3. Department of Applied Ocean Physics and Engineering Woods Hole Oceanographic Institution Woods Hole MA USA

4. The Water Institute Baton Rouge LA USA

5. U.S. Geological Survey Wetland and Aquatic Research Center, Baton Rouge LA United States Previously at the Water Institute Baton Rouge LA USA

Abstract

AbstractPrevious studies have demonstrated that vegetation‐generated turbulence can enhance erosion rate and reduce the velocity threshold for erosion of non‐cohesive sediment. This study considered whether vegetation‐generated turbulence had a similar influence on natural cohesive sediment. Cores were collected from a black mangrove forest with aboveground biomass and exposed to stepwise increases in velocity. Erosion was recorded through suspended sediment concentration. For the same velocity, cores with pneumatophores had elevated turbulent kinetic energy compared to bare cores without pneumatophores. However, the vegetation‐generated turbulence did not increase bed stress or the rate of resuspension, relative to bare cores. It was hypothesized that the short time‐scale fluctuations associated with vegetation‐generated turbulence were not of sufficient duration to break cohesion between grains, explaining why elevated levels of turbulence associated with the pneumatophores had no impact on the erosion threshold or rate.

Funder

National Science Foundation Graduate Research Fellowship Program

Publisher

American Geophysical Union (AGU)

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