Document of bibliographic reference 225316

BibliographicReference record

Type
Bibliographic resource
Type of document
Reports
Type of document
Project report
BibLvlCode
MS
Title
Interestuarine comparison: hydrogeomorphology: hydro- and geomorphodynamics of the TIDE estuaries Scheldt, Elbe, Weser and Humber
Abstract
Within the scope of the INTERREG IVb project TIDE (TIdal river DEvelopment), an interestuarine comparison of 4 partner estuaries (Scheldt, Elbe, Weser and Humber) was performed. Different aspects of the estuaries were handled within the interestuarine comparision: hydrodynamics, geomorphology, ecology, birds, historical changes and monitoring. This study reports on the hydro- and geomorphodynamics of the TIDE estuaries.

Five research topics were handled within the hydro-geomorphology study: (1) tidal damping/amplification, (2) relation between habitats and the tide, (3) suspended sediments, (4) residence times, and (5) tidal marshes. For each topic a number of specific research questions were listed (see §2). To be able to answer these questions several main parameters (i.e. Directly measured in the estuary) were collected (topo-bathymetry data, tide, salinity, SPM, freshwater discharges and tidal marsh data). Furthermore some additional parameters were derived (e.g., flow velocities, tidal energy, tidal damping scale) using some specific techniques (e.g., cubage technique, Dalrymple energy concept).

We found that tidal damping in an estuary becomes important once the estuary depth (i.e. Cross-section averaged depth at low water) becomes lower than 4.2 – 7.7 m, depending on the estuary-convergence. Similar results were found for the habitat analysis: once the area of the deep subtidal habitat (> 5 m below low water) becomes smaller than 20 %, and the area of the shallow subtidal habitat (< 5 m below low water) becomes larger than 35 %, tidal damping in an estuary prevails. Concerning SPM, turbidity maxima are associated with maxima in tidal energy. We further found that these high SPM values force tidal marshes to faster attain a high climax vegetation state with less plant diversity.

Bibliographic citation
Vandenbruwaene, W.; Plancke, Y.; Verwaest, T.; Mostaert, F. (2013). Interestuarine comparison: hydrogeomorphology: hydro- and geomorphodynamics of the TIDE estuaries Scheldt, Elbe, Weser and Humber. Version 4.0. WL Rapporten, 770_62b. Flanders Hydraulics Research: Antwerp. 70 + 14 p. appendices pp.
Access rights
open access
Is accessible for free
true

Authors

author
Name
Wouter Vandenbruwaene
Identifier
https://orcid.org/0000-0003-3779-6076
Affiliation
Vlaamse overheid; Beleidsdomein Mobiliteit en Openbare Werken; Vlaams Ministerie Mobiliteit en Openbare Werken; Departement Mobiliteit en Openbare Werken; Waterbouwkundig Laboratorium
author
Name
Yves Plancke
Identifier
https://orcid.org/0000-0002-4303-082X
author
Name
Toon Verwaest
Identifier
https://orcid.org/0000-0002-3911-6962
author
Name
Frank Mostaert
Identifier
https://orcid.org/0000-0001-8585-5056

thesaurus terms

term
Cohesive sediment (term code: 169969 - defined in term set: WL Kennisdomein)
Erosion / sedimentation (term code: 169984 - defined in term set: WL Kennisdomein)
Estuaries (term code: 2895 - defined in term set: ASFA Thesaurus List)
Geomorphology (term code: 3651 - defined in term set: ASFA Thesaurus List)
Habitats (term code: 169983 - defined in term set: WL Kennisdomein)
Hydrodynamics (term code: 4095 - defined in term set: ASFA Thesaurus List)
Intertidal zones (term code: 169985 - defined in term set: WL Kennisdomein)
Literature and desktop study (term code: 169919 - defined in term set: WL Kennisdomein types)
River flow (term code: 169963 - defined in term set: WL Kennisdomein)
Tides (term code: 169958 - defined in term set: WL Kennisdomein)

Document metadata

date created
2013-05-10
date modified
2020-06-16