Onderzoeksoutput

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.

log in

• 
  People
• 
  Curriculum
• 
  Projects
• 
  Data sets
• 
  Publications
• 
  Events

[ meld een fout in dit record ]

mandje (0): toevoegen | toon

---

Modeling of historical evolution of salt water distribution in the phreatic aquifer in and around the silted up Zwin estuary mouth (Flanders, Belgium) Lebbe, L.; Jonckheere, S.; Vandenbohede, A. (2008). Modeling of historical evolution of salt water distribution in the phreatic aquifer in and around the silted up Zwin estuary mouth (Flanders, Belgium), in: Proceedings of the SWIM 20: 20th Salt Water Intrusion Meeting. June 23-27, 2008. Naples, Florida, USA. pp. 141-144 In: (2008). Proceedings of the SWIM 20: 20th Salt Water Intrusion Meeting. June 23-27, 2008. Naples, Florida, USA. U.S. Geological Survey: [s.l.]. 360 pp.

---

Beschikbaar in	Auteurs
VLIZ: Open access 239941 [ download pdf ]

---

Trefwoorden

Phreatic water Water bodies > Coastal waters > Coastal landforms > Coastal inlets > Estuaries ANE, België, Zwin [Marine Regions]; Belgium, Het Zwin natuurreservaat Marien/Kust

---

Auteurs		Top
Lebbe, L. Jonckheere, S. Vandenbohede, A.

---

Abstract

The evolution of the salt-water distribution around the Zwin estuary mouth is modeled for a period of about five centuries. The modeled area is situated in the Flemisch coastal plain near the border of The Netherlands and Belgium. The Zwin estuary is the former waterway to the medieval seaports of Bruges and Damme. During the considered period this alluvial estuary silted up and the modeled area changes from an area around a tidal channel, over a mud flat to a rather complex polder dune area. The evolution is simulated by the 3D density depended groundwater flow model MOCDENS3D (Lebbe & Oude Essink, 1999). The row direction of the applied finite-difference grid is parallel to the present coast line. The simulation is based on old paintings and a large number of maps which allow a relatively detailed reconstruction of the evolution of the landscape. The results show the historical evolution of a large number of different inverse density problems in this area.

---

Alle informatie in het Integrated Marine Information System (IMIS) valt onder het VLIZ Privacy beleid

Top | Auteurs

IMIS is ontwikkeld en wordt gehost door het VLIZ.