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Thermal pollution of the Scheldt estuary

Some new data on the sedimentary history of the mouth of the river Scheldt in International Colloquy on the Quaternary and Tertiary geology of the Southern Bight, North Sea. Collected abstracts. Oral presentations.
Belgique ; Cours d'eau ; Estuaire ; Fluviatile ; Géographie de l'Europe ; Scheldt ; Sédimentation

The Late Holocene evolution of the perimarine part of the river Scheldt in The Quaternary and Tertiary geology of the Southern Bight, North Sea.
Following a brief overview of the Holocene evolution of the river Scheldt, the late Holocene evolution of the tidal part of the river is presented in detail. A number of different phases could be distinguished.

Morphological changes of the ebb-tidal delta of the Eastern Scheldt during recent decades
Study based on the results of detailed soundings of the area carried out in connection with the Delta-project. A main conclusion is that a rather small increase in tidal discharge at the entrance of the Eastern Scheldt basin resulted in a remarkable

The Lateglacial and Holocene evolution of the middle and lower River Scheldt, Belgium
Belgique ; Cours d'eau ; Fluviatile ; Holocène ; Quaternaire ; Scheldt
, but mostly they have remained limited in scope. This chapter attempts to synthesize the results of those studies, many of which are unpublished, and to combine them with newly collected data into an overall view of the evolution of the River Scheldt during

De holocene evolutie van de alluviale vlakte van de Beneden-Schelde. (The holocene evolution of the alluvial plain of the Lower Scheldt)

A case of drowning. The end of Subatlantic peat growth and related palaeoenvironmental changes in the lower Scheldt basin (Belgium) based on diatom and pollen analysis
The sequence of events in the lower Scheldt basin (Belgium) during the last 3 000 year is very complex. Remaining problems regarding its paleogeographical history include changes occurring at the rivermouth and the peat digging in the 13-14th

Numerical simulations of salinity, turbidity and sediment accumulation in the Scheldt Estuary in Ecohydrodynamics.

lithostratigraphic framework is proposed. The provenance of the sediments was established by heavy mineral and gravel analysis. Rhine, Meuse and rivers from the Scheldt basin contributed their sediments to the southern North Sea basin during different stages
of the Early-Pleistocene. The major importance of the rivers from the Scheldt basin in the upbuilding of the sedimentary sequence is emphasized.

-investigation methods for soil mechanics and foundation engineering in deltaic regions. Engineering geology and the Thames Barrier project. The storm surge barrier in the Oosterschelde. Foundation aspects of the Eastern Scheldt storm surge barrier. Engineering
-geological investigations in the mouth of the'easter Scheldt (SW Netterlands).

De holocene evolutie van de alluviale vlakte van de Beneden-Schelde. (The holocene evolution of the alluvial plain of the Lower Scheldt)

Etude des relations entre la géométrie des dunes subaquatiques et les caractéristiques des sédiments dans la partie maritime de l'estuaire de la Scheldt
In 2 study areas in the maritime part of the Scheldt estuary, grab samples were taken and side-scan sonar recordings were carried out. Within the study areas, the strong variation in both the geometry of the subaqueous dunes and the sedimentological

Paleomorphology in the Eastern Scheldt basin (central Belgium). The Dijle-Demer-Grote Nete confluence area

A reconstruction of middle Holocene alluvial hardwood forests (Lower Scheldt River, Northern Belgium) and their exploitation during the Mesolithic-Neolithic transition period (Swifterbant culture, ca. 4,500-4,000 BC)
Agro-pastoralisme ; Analyse pollinique ; Antwerpen ; Belgique ; Belgique du Nord ; Charbon de bois ; Forêt alluviale ; Holocène ; Palynologie ; Paléo-environnement ; Quaternaire ; Scheldt ; Site archéologique ; Swifterbant
Les taxons identifiés indiquent la présence d'une forêt alluviale de bois dur, développée sur la dune sableuse sur laquelle le campement se situait, sur la rive gauche de la Scheldt inférieure. Les résultats anthracologiques sont comparés avec ceux

European rivers: first results

at high discharge. Preliminary results are presented here. The rivers Meuse and Scheldt have been sampled respectively at Heusden and Temse. (LW).

confirm the general tendancy of isolines to be parallel to the coast. The plankton distribution shows the influence of Scheldt water farer to the south-west than proposed by previous models and observations.

Results obtained during a 36-hours dial cycle, anchored in the Scheldt Estuary, are discussed in terms of CO2 dynamics. The complete set of measured parameters (salinity, temperature, alkalinity, pH, dissolved oxygen and total inorganic carbon

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