Hostname: page-component-586b7cd67f-2plfb Total loading time: 0 Render date: 2024-11-22T04:06:22.917Z Has data issue: false hasContentIssue false

Study of sand wave migration over five years as observed in two windfarm development areas, and the implications for building on moving substrates in the North Sea

Published online by Cambridge University Press:  02 September 2015

Ken P. Games
Affiliation:
Gardline Geosurvey Ltd, Admiralty Road, Great Yarmouth, NR30 3NG. Email: [email protected]; [email protected]
David I. Gordon
Affiliation:
Gardline Geosurvey Ltd, Admiralty Road, Great Yarmouth, NR30 3NG. Email: [email protected]; [email protected]

Abstract

Sand waves are well known indicators of a mobile seabed. What do we expect of these features in terms of migration rates and seabed scour? We discuss these effects on seabed structures, both for the Oil and Gas and the Windfarm Industries, and consider how these impact on turbines and buried cables. Two case studies are presented. The first concerns a windfarm with a five-year gap between the planning survey and a subsequent cable route and environmental assessment survey. This revealed large-scale movements of sand waves, with the displacement of an isolated feature of 155 m in five years. Secondly, another windfarm development involved a re-survey, again over a five-year period, but after the turbines had been installed. This showed movements of sand waves of ∼50 m in five years. Observations of the scour effects on the turbines are discussed. Both sites revealed the presence of barchans. Whilst these have been extensively studied on land, there are few examples of how they behave in the marine environment. The two case studies presented show that mass transport is potentially much greater than expected and that this has implications for choosing turbine locations, the effect of scour, and the impact these sediment movements are likely to have on power cables.

Type
Articles
Copyright
Copyright © The Royal Society of Edinburgh 2015 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

6. References

Andreotti, B., Claudin, P. & Douady, S. 2002. Selection of dune shapes and velocities. Part 1: dynamics of sand, wind and barchans. The European Physical Journal B28, 321–39.Google Scholar
Beadnell, H. J. L. 1910. The sand dunes of the Libyan Desert. Their origin, form and rate of movement, considered in relation to the geological and meteorological conditions of the region. The Geographical Journal 35, 375–92.Google Scholar
Besio, G., Blondeaux, M. & Vittori, G. 2004. On the modelling of sand wave migration. Journal of Geophysical Research 109, C04018.Google Scholar
Bourke, M. C. 2010. Barchan Dune Asymmetry. Planetary Science Institute 205(1) 183–97.Google Scholar
EC Habitats Directive 92/43/EEC. Council Directive of 21 May 1992 on the conservation of natural habitats and of wild fauna and flora.Google Scholar
Kenyon, N. H., Belderson, R. H., Stride, A. H. & Johnson, M. A. 1981 Offshore tidal sand banks as indicators of net sand transport and as potential deposits. In Nio, S-D., Schuttenhelm, R. T. E. & Van Weering, Tj. C. E. (eds) Holocene marine sedimentation in the North Sea Basin. International Association of Sedimentologists Special Publication 5, 257–68.Google Scholar
Knaapen, M. A. F. 2005. Sand wave migration predictor based on shape information. Journal of Geophysical Research – Earth Surfaces 110, no F04S11.Google Scholar
Lorenz, R.D., Gasmi, N., Radebaugh, J., Barnes, J. W. & Ori, G. G. 2013. Dunes on planet Tatooine: Observations of barchan migration at the Star Wars film set in Tunisia. Geomorphology 201, 264–71.Google Scholar
Nemeth, A. A., Hulscher, S. J. M. H. & de Vriend, H. J. 2002. Sand wave migration in shallow shelf seas. Continental Shelf Research 22, 2795–806.Google Scholar
Reineck, H. E. & Singh, I. B. 1973. Depositional Sedimentary Environments. Berlin: Springer-Verlag. 439 pp.Google Scholar
Todd, B. J. 2005. Morphology and composition of submarine barchan dunes on the Scotian Shelf, Canadian Atlantic margin. Geomorphology 67, 487500.Google Scholar
Van Dijk, T. A. G. P. & Kleinhans, M. G. 2005. Processes controlling the dynamics of compound sand waves in the North Sea. Journal of Geophysical Research – Earth Surfaces 110, no F04S10.Google Scholar
Van Lancker, V. 1999. Sediment and morphodynamics of a siliciclastic near coastal area, in relation to hydrodynamical and meteorological conditions: Belgian continental shelf. PhD Thesis, Faculteit Wetenschappen, Universiteit Gent. 194 pp.Google Scholar