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Massachusetts Institute of Technology

Sediment Erosion and Deposition Within Mangrove Forests

Abstract

dc:description.abstract

Mangroves are highly productive ecosystems that sequester carbon in their own biomass and by trapping carbon-rich sediment imported from outside the forest and deposited in the forest. Aboveground biomass, like mangrove pneumatophores (i.e., aerial roots), creates conditions that facilitate sediment deposition by enhancing drag and slowing currents near the bed. However, pneumatophores also generate turbulence that enhances turbulent kinetic energy (TKE), which can promote sediment resuspension. Two studies were conducted to better understand the impacts of pneumatophore-generated turbulence on sediment transport. The first study investigated whether pneumatophore-generated turbulence impacted the erosion threshold and rate of natural cohesive sediment collected from a black mangrove habitat. Sediment cores with intact belowground and aboveground biomass were placed in a recirculating channel. Pneumatophores were removed from one side of each core. Each side of the core, with and without pneumatophores, was separately exposed to the same sequence of channel velocities. Although the presence of pneumatophores significantly enhanced the turbulence in the channel, the bed stress, threshold for sediment resuspension, and rate of sediment erosion were similar for the bare and vegetated sides of each core. This result differs from non-cohesive sediments, for which pneumatophore-generated turbulence has been found to increase erosion rates. The second study considered deposition. Laboratory experiments measured TKE and net deposition of non-cohesive sediment in bare and vegetated channels. For the same velocity, as pneumatophore density increased, TKE increased and net deposition decreased. The impact of TKE on deposition was described in terms of a deposition probability model. This model was used to predict deposition over a range of typical mangrove field conditions, which indicated that pneumatophore-generated turbulence can facilitate the delivery of sediment farther into the mangrove forest. Understanding how pneumatophores impact the balance of the competing processes of deposition and erosion is critical for improving the assessment and modelling of sediment retention and carbon storage in mangrove forests.

Degree

thesis:*
Name thesis:degree_name
Master
Department dc:contributor.department
Massachusetts Institute of Technology. Department of Civil and Environmental Engineering
Grantor dc:publisher
Massachusetts Institute of Technology
Year dc:date.issued
2023

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Deitrick, Autumn Rose
Advisors dc:contributor.advisor
  • Nepf, Heidi M.
  • Ralston, David K.

Rights

dc:rights
Statement dc:rights
  • In Copyright - Educational Use Permitted
  • Copyright retained by author(s)

Identifiers

dc:identifier.*
Handle dc:identifier.uri
https://hdl.handle.net/1721.1/152741
OAI identifier oai:identifier
oai:dspace.mit.edu:1721.1/152741

Chain of custody

source
Harvested from
MIT
Base URL
dspace.mit.edu/oai/request
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
related terms
citation

Deitrick, Autumn Rose. Sediment Erosion and Deposition Within Mangrove Forests. Massachusetts Institute of Technology, 2023. https://hdl.handle.net/1721.1/152741