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Threshold studies of gravel size particles under the co-linear combined action of waves and currents

Threshold studies of gravel size particles under the co-linear combined action of waves and currents
Threshold studies of gravel size particles under the co-linear combined action of waves and currents
Gravel size sediment beds are tested under the combined influence of simulated wave action and co-linear currents in a laboratory flume. Critical current speed, at threshold, increases with increasing size. Superimposed wave energy causes a small reduction in the unidirectional current energy. For low values of wave-induced near bed current velocities, the resistance to erosion increases when the wave period decreases from 10 to 6 s. Finally, combined critical shear stresses are found to be lower than those predicted using the Shields curve, as modified for oscillatory flow. Grain protrusion is suggested as a mechanism to explain this divergence.
0037-0746
951-962
Panagiotopoulos, I.
bd73f82a-86a9-408e-aa60-094c936aa153
Sylaios, G.
e9d604a4-4f52-4bbf-aaab-03b32042ac6c
Collins, M.B.
3b70278b-0004-45e0-b3c9-0debdf0a9351
Panagiotopoulos, I.
bd73f82a-86a9-408e-aa60-094c936aa153
Sylaios, G.
e9d604a4-4f52-4bbf-aaab-03b32042ac6c
Collins, M.B.
3b70278b-0004-45e0-b3c9-0debdf0a9351

Panagiotopoulos, I., Sylaios, G. and Collins, M.B. (1994) Threshold studies of gravel size particles under the co-linear combined action of waves and currents. Sedimentology, 41 (5), 951-962. (doi:10.1111/j.1365-3091.1994.tb01434.x).

Record type: Article

Abstract

Gravel size sediment beds are tested under the combined influence of simulated wave action and co-linear currents in a laboratory flume. Critical current speed, at threshold, increases with increasing size. Superimposed wave energy causes a small reduction in the unidirectional current energy. For low values of wave-induced near bed current velocities, the resistance to erosion increases when the wave period decreases from 10 to 6 s. Finally, combined critical shear stresses are found to be lower than those predicted using the Shields curve, as modified for oscillatory flow. Grain protrusion is suggested as a mechanism to explain this divergence.

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Published date: October 1994

Identifiers

Local EPrints ID: 192445
URI: http://eprints.soton.ac.uk/id/eprint/192445
ISSN: 0037-0746
PURE UUID: 097a282e-123b-41a6-af2b-f3a54f782747

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Date deposited: 04 Jul 2011 14:05
Last modified: 14 Mar 2024 03:50

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Contributors

Author: I. Panagiotopoulos
Author: G. Sylaios
Author: M.B. Collins

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