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Massachusetts Institute of Technology

The effect of fluid acceleration on sediment transport in the surf zone

Abstract

dc:description.abstract

The surf zone is defined by highly non-linear, breaking waves that have very different acceleration signatures beneath their respective crests and troughs. The consequences of this dissimilarity on sediment transport is not fully understood. This thesis develops methodologies to predict sediment transport under these asymmetric, skewed waves. Two different transport mechanisms are considered: bedload transport and "subsurface" transport. The potential for subsurface transport was first realized by Madsen (1974) who found that the large pressure gradient beneath a breaking wave was sufficient to drive a substantial porous-media flow, adequate to create a soil-mechanics type failure extending several centimeters into a sandy sediment bed. The theoretical model of Madsen (1974) is extended to obtain estimates of subsurface transport by subdividing the sediment in failure into distinct, kinematically admissible slip circles. An equation governing the rotation of each slip circle is developed, yielding the subsurface sediment's horizontal movement as a function of depth. By integration, subsurface transport can predicted. In addition, a method is developed for estimating bedload transport under breaking waves, accounting for the enhanced shear stress beneath the wave's crest. An existing bedload formula is used as the foundation for this predictive model.

Degree

thesis:*
Department dc:contributor.department
Massachusetts Institute of Technology. Dept. of Civil and Environmental Engineering.
Grantor dc:publisher
Massachusetts Institute of Technology
Year dc:date.issued
2007

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Durham, William McKinney
Advisor dc:contributor.advisor
  • Ole Secher Madsen.

Subjects

dc:subject × 1

Rights

dc:rights
Statement dc:rights
  • M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission.
Language dc:language.iso
eng

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/1721.1/38512
OAI identifier oai:identifier
oai:dspace.mit.edu:1721.1/38512

Chain of custody

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

Durham, William McKinney. The effect of fluid acceleration on sediment transport in the surf zone. Massachusetts Institute of Technology, 2007. http://hdl.handle.net/1721.1/38512