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Sediment mobility in response to tidal and wind-driven flows along the Belgian inner shelf, southern North Sea

Matthias Baeye UGent, Michael Fettweis, George Voulgaris and Vera Van Lancker UGent (2011) OCEAN DYNAMICS. 61(5). p.611-622
abstract
The effect of hydro-meteorological forcings (tidal and wind-induced flows) on the transport of suspended particulate matter (SPM), on the formation of high-concentrated mud suspensions and on the occurrence of sand-mud suspensions has been studied using long-term multi-parametric observations. Data have been collected in a coastal turbidity maximum area (southern North Sea) where a mixture of sandy and muddy sediments prevails. Data have been classified according to variations in subtidal alongshore currents, with the direction of subtidal flow depending on wind direction. This influences the position of the turbidity maximum; as such also the origin of SPM. Winds blowing from the NE will increase SPM concentration, whilst SW winds will induce a decrease. The latter is related to advection of less turbid English Channel water, inducing a shift of the turbidity maximum towards the NE and the Westerschelde estuary. Under these conditions, marine mud will be imported and buffered in the estuary. Under persistent NE winds, high-concentrated mud suspensions are formed and remain present during several tidal cycles. Data show that SPM consists of a mixture of flocs and locally eroded sand grains during high currents. This has implications towards used instrumentation: SPM concentration estimates from optical backscatter sensors will only be reliable when SPM consists of cohesive sediments only; with mixtures of cohesive and non-cohesive sediments, a combination of both optical and acoustic sensors are needed to get an accurate estimate of the total SPM concentration.
Please use this url to cite or link to this publication:
author
organization
year
type
journalArticle (original)
publication status
published
subject
keyword
Mixed sediments, EVENTS, High-concentrated mud suspensions, Alongshore sediment transport, Acoustic and optical backscattering, Southern North Sea, SUSPENDED PARTICULATE MATTER, TEMPORAL VARIABILITY, BACKSCATTER DEVICES, SETTLING VELOCITY, HIGH TURBIDITY, MUD, TRANSPORT, Suspended particulate matter, MIXTURES, BEHAVIOR
journal title
OCEAN DYNAMICS
Ocean Dyn.
volume
61
issue
5
pages
611 - 622
Web of Science type
Article
Web of Science id
000292274300006
JCR category
OCEANOGRAPHY
JCR impact factor
1.774 (2011)
JCR rank
23/59 (2011)
JCR quartile
2 (2011)
ISSN
1616-7341
DOI
10.1007/s10236-010-0370-7
language
English
UGent publication?
yes
classification
A1
copyright statement
I have transferred the copyright for this publication to the publisher
id
2092223
handle
http://hdl.handle.net/1854/LU-2092223
date created
2012-04-20 20:26:17
date last changed
2012-04-23 09:36:51
@article{2092223,
  abstract     = {The effect of hydro-meteorological forcings (tidal and wind-induced flows) on the transport of suspended particulate matter (SPM), on the formation of high-concentrated mud suspensions and on the occurrence of sand-mud suspensions has been studied using long-term multi-parametric observations. Data have been collected in a coastal turbidity maximum area (southern North Sea) where a mixture of sandy and muddy sediments prevails. Data have been classified according to variations in subtidal alongshore currents, with the direction of subtidal flow depending on wind direction. This influences the position of the turbidity maximum; as such also the origin of SPM. Winds blowing from the NE will increase SPM concentration, whilst SW winds will induce a decrease. The latter is related to advection of less turbid English Channel water, inducing a shift of the turbidity maximum towards the NE and the Westerschelde estuary. Under these conditions, marine mud will be imported and buffered in the estuary. Under persistent NE winds, high-concentrated mud suspensions are formed and remain present during several tidal cycles. Data show that SPM consists of a mixture of flocs and locally eroded sand grains during high currents. This has implications towards used instrumentation: SPM concentration estimates from optical backscatter sensors will only be reliable when SPM consists of cohesive sediments only; with mixtures of cohesive and non-cohesive sediments, a combination of both optical and acoustic sensors are needed to get an accurate estimate of the total SPM concentration.},
  author       = {Baeye, Matthias and Fettweis, Michael and Voulgaris, George and Van Lancker, Vera},
  issn         = {1616-7341},
  journal      = {OCEAN DYNAMICS},
  keyword      = {Mixed sediments,EVENTS,High-concentrated mud suspensions,Alongshore sediment transport,Acoustic and optical backscattering,Southern North Sea,SUSPENDED PARTICULATE MATTER,TEMPORAL VARIABILITY,BACKSCATTER DEVICES,SETTLING VELOCITY,HIGH TURBIDITY,MUD,TRANSPORT,Suspended particulate matter,MIXTURES,BEHAVIOR},
  language     = {eng},
  number       = {5},
  pages        = {611--622},
  title        = {Sediment mobility in response to tidal and wind-driven flows along the Belgian inner shelf, southern North Sea},
  url          = {http://dx.doi.org/10.1007/s10236-010-0370-7},
  volume       = {61},
  year         = {2011},
}

Chicago
Baeye, Matthias, Michael Fettweis, George Voulgaris, and Vera Van Lancker. 2011. “Sediment Mobility in Response to Tidal and Wind-driven Flows Along the Belgian Inner Shelf, Southern North Sea.” Ocean Dynamics 61 (5): 611–622.
APA
Baeye, M., Fettweis, M., Voulgaris, G., & Van Lancker, V. (2011). Sediment mobility in response to tidal and wind-driven flows along the Belgian inner shelf, southern North Sea. OCEAN DYNAMICS, 61(5), 611–622.
Vancouver
1.
Baeye M, Fettweis M, Voulgaris G, Van Lancker V. Sediment mobility in response to tidal and wind-driven flows along the Belgian inner shelf, southern North Sea. OCEAN DYNAMICS. 2011;61(5):611–22.
MLA
Baeye, Matthias, Michael Fettweis, George Voulgaris, et al. “Sediment Mobility in Response to Tidal and Wind-driven Flows Along the Belgian Inner Shelf, Southern North Sea.” OCEAN DYNAMICS 61.5 (2011): 611–622. Print.