Welkom op het expertplatform!
Dit platform verschaft informatie en kennis omtrent de WL expertisedomeinen 'hydraulica en sediment', 'havens en waterwegen', 'waterbouwkundige constructies', 'waterbeheer' en 'kustbescherming' - gaande van WL medewerkers met hun expertise, het curriculum van deze instelling, tot publicaties, projecten, data (op termijn) en evenementen waarin het WL betrokken is.
Het WL onderschrijft het belang van "open access" voor de ontsluiting van haar onderzoeksresultaten. Lees er meer over in ons openaccessbeleid.
| one publication added to basket [203864] |
Long-term influence of maritime access works on the distribution of cohesive sediments: analysis of historical and recent data from the Belgian nearshore area (Southern North Sea)
Fettweis, M.; Houziaux, J.-S.; Du Four, I.; Van Lancker, V.; Baeteman, C.; Mathys, M.; Van den Eynde, D.; Francken, F.; Wartel, S. (2009). Long-term influence of maritime access works on the distribution of cohesive sediments: analysis of historical and recent data from the Belgian nearshore area (Southern North Sea). Geo-Mar. Lett. 29(5): 321-330. dx.doi.org/10.1007/s00367-009-0161-7
In: Geo-Marine Letters. Springer: Heidelberg; Berlin. ISSN 0276-0460; e-ISSN 1432-1157
|   |
| Auteurs | | Top |
- Fettweis, M.
- Houziaux, J.-S.
- Du Four, I.
|
- Van Lancker, V.
- Baeteman, C.
- Mathys, M.
|
- Van den Eynde, D.
- Francken, F.
- Wartel, S.
|
| Abstract |
Long-term changes in the cohesive sediment distribution of the Belgian—Dutch nearshore zone (southern North Sea) are related to human activities (port construction, deepening of navigation channels, disposal of dredged sediments) and to natural variability, due to tides and meteorological effects. Results are based on the combined analyses of recent and historic (100 years ago) sediment sample information and bathymetric maps. Data processing was based mainly on field descriptions of the samples (consolidation, thickness) and on bathymetric maps of 1866–1911. Results indicate that the distribution of fresh mud and suspended sediment has changed during the last100 years, due mainly to maritime access works. Most of the present deposition of thick layers of fresh mud (>30 cm) has anthropogenic causes. The results further indicate that erosion of older Holocene mud has increased in recent times and, as a consequence, higher amounts of fine-grained sediments are being released into the southern North Sea today. |
IMIS is ontwikkeld en wordt gehost door het VLIZ.
