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Offshore sediment studies
The movement of sediment offshore has been studied by HR Wallingford in the
"Southern North Sea Sediment Transport Study, Phase 2". This work
looked at the implications of offshore dredging for marine aggregates on the
marine environment.
However, although not part of the remit of the study it recognised the importance
of considering in detail
"the possible physical effects of offshore
dredging with particular regard to how such operations might alter waves, tidal
currents, sediment transport and morphological changes of the seabed and along
the coast. The results from such an assessment can be used to determine the
likely effect on beaches and coastal
defences." The report can be downloaded from HR Wallingford
web site @ http://www.sns2.org/project-outputs.html.
At a regional scale studies specific studies in the southern North Sea provide
insights into the way sediment moves offshore (Brampton
& Evans 1998) as does its companion volume (PR65), the Seabed sediment
mobility study - west of the Isle of Wight. For information see the CIRIA web
site http://www.ciria.org/index.html
bookshop.
It seems clear that managing coastal shingle deposits whether for sea defence
or nature conservation, must take into account the contemporary contribution
of material to the coast. Since this will be derived from or affected by the
action of tides, winds and waves it is not only important to know how much is
coming from erosion of the land, but also from the sea. The studies mentioned
above provide some indication of the way in which the systems operate. However
the link between the land-based and marine sources has not been made.
| Guidance: The implications of offshore dredging to the stability
of the coast are implicit in the recommendations made for the revised Government
View procedure and the production of an independent 'Coastal
Impact Study' recognises this importance. Wide-ranging reviews
of the sediment budget should be undertaken of the inter-relationships between
offshore sediment movement and coastal change (erosion and accretion) in
all areas where marine aggregate extraction is, or could take place. These
should include offshore deposits and their relationship with onshore contemporary
contributions to beach volume, for example derived from eroding cliffs.
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References
Brampton, A.H. & Evans, C.D.R.
1998.
Regional Seabed Sediments Studies and Assessment of Marine Aggregate Dredging.
CIRIA.
Abstract...
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