Sediment resuspension events induced by the wake wash of deep-draft vessels
Sediment resuspension events induced by the wake wash of deep-draft vessels
Hydrodynamics and sediment resuspension events, induced at the shoreline by a deep-draft vessel passing nearby, are described. Measurements (pressure, currents and turbidity) were obtained at 4 Hz, on a lower beach ~50 m from a channel where large car ferries operate in Wootton Creek, Isle of Wight. The study focuses on a representative 8-min 32-s-long record, during which two large vessels passed the channel section. At the shore, the passage of each vessel induced a long-period water-level drawdown, followed by a water-level oscillation (seiche) of similar period, and the short-period waves of the wake. Both drawdowns were the main constituents of the prevailing wave pattern. The second drawdown was the largest in amplitude, in response to a higher speed of the ferry, and the influence of the seiche which had been activated during the preceding event. Two successive peaks of turbidity were observed shortly after this drawdown. Analyses of current velocity and direction indicate that the sediments resuspended originated from the shallower upper beach. Anthropogenically induced erosion of the foreshore is predicted at Wootton Creek.
205-211
Garel, Erwan
1abe47b5-da25-47c3-aa74-c80ab4295c82
López Fernández, Laura
2f3527b7-2e05-42a9-9fe0-62b25f2025ed
Collins, Mike
3b70278b-0004-45e0-b3c9-0debdf0a9351
August 2008
Garel, Erwan
1abe47b5-da25-47c3-aa74-c80ab4295c82
López Fernández, Laura
2f3527b7-2e05-42a9-9fe0-62b25f2025ed
Collins, Mike
3b70278b-0004-45e0-b3c9-0debdf0a9351
Garel, Erwan, López Fernández, Laura and Collins, Mike
(2008)
Sediment resuspension events induced by the wake wash of deep-draft vessels.
Geo-Marine Letters, 28 (4), .
(doi:10.1007/s00367-008-0101-y).
Abstract
Hydrodynamics and sediment resuspension events, induced at the shoreline by a deep-draft vessel passing nearby, are described. Measurements (pressure, currents and turbidity) were obtained at 4 Hz, on a lower beach ~50 m from a channel where large car ferries operate in Wootton Creek, Isle of Wight. The study focuses on a representative 8-min 32-s-long record, during which two large vessels passed the channel section. At the shore, the passage of each vessel induced a long-period water-level drawdown, followed by a water-level oscillation (seiche) of similar period, and the short-period waves of the wake. Both drawdowns were the main constituents of the prevailing wave pattern. The second drawdown was the largest in amplitude, in response to a higher speed of the ferry, and the influence of the seiche which had been activated during the preceding event. Two successive peaks of turbidity were observed shortly after this drawdown. Analyses of current velocity and direction indicate that the sediments resuspended originated from the shallower upper beach. Anthropogenically induced erosion of the foreshore is predicted at Wootton Creek.
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Published date: August 2008
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Local EPrints ID: 57929
URI: http://eprints.soton.ac.uk/id/eprint/57929
ISSN: 0276-0460
PURE UUID: 8cf83db7-d41a-4816-9f16-b45b8837d08d
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Date deposited: 11 Aug 2008
Last modified: 15 Mar 2024 11:09
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Author:
Erwan Garel
Author:
Laura López Fernández
Author:
Mike Collins
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