In situ flume measurements of resuspension in the North Sea

Autor: Carl L. Amos, E.R. Parker, Fay Couceiro, Peter J. Statham, K. Black, B.A. Kelly-Gerreyn, Charlotte Thompson, Gary R. Fones, R. Helsby, Naomi Greenwood
Rok vydání: 2011
Předmět:
Zdroj: Thompson, C, Couceiro, F, Fones, G, Helsby, R, Amos, C, Black, K, Parker, E, Greenwood, N, Statham, P & Kelly-Gerreyn, B 2011, ' In situ flume measurements of resuspension in the North Sea ', Estuarine, Coastal and Shelf Science, vol. 94, no. 1, pp. 77-88 . https://doi.org/10.1016/j.ecss.2011.05.026
ISSN: 0272-7714
DOI: 10.1016/j.ecss.2011.05.026
Popis: The in situ annular flume, Voyager II, was deployed at three sites in the North Sea in order to investigate resuspension events, to determine the physical characteristics of the seabed, to determine the threshold of resuspension of the bed and to quantify erosion rates and erosion depths. These are the first controlled, in situ flume experiments to study resuspension in the North Sea, and were combined with long-term measurements of waves and currents. Resuspension experiments were undertaken at two muddy, and one sandy site: north of the Dogger Bank (DG: water depths ∼80 m, very fine, poorly sorted, very fine-skewed sediment experiencing seasonal thermal stratification of the water column along with oxygen depletion); the Oyster Grounds (OG: ∼40 m, similar bed properties, year round water column thermal stratification, Atlantic forcing); and in the Sean Gas Field (SGF: ∼20 m, moderately sorted, very coarse-skewed sand, and well mixed water column). The erosion thresholds of the bed were found to be 0.66–1.04 Pa (DG) and 0.91–1.27 Pa (OG), with corresponding erosion depths of 0.1–0.15 mm and 0.02–0.06 mm throughout the experiments. Evaluation of a year of current velocities from 2007 indicated that at OG, resuspension of the consolidated bed was limited to on average ∼8% of the time as a result of tidal forcing alone for short ( Resuspension of bed material and erosion rates were closely related to applied bed shear stresses, and eroded depths were significantly correlated with the physical properties of the bed. Therefore, while complex variations in biogeophysical factors affected the critical threshold of erosion, once exceeded, erosion rates were related to the nature of the sediment.
Databáze: OpenAIRE
Externí odkaz: