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Hydro-ecological relations in the Delta Waters

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Lt has been estimated that <strong>the</strong> sedimentation process Of <strong>the</strong> channels <strong>in</strong><br />

order to establish a new equilibrium will <strong>in</strong>volve some 500 millions lU3<br />

of sediment over <strong>the</strong> next cedtnries. The total erosive effect over <strong>the</strong><br />

next 30 years h& been elculated as a lass of shoal- and mu-t area<br />

amount<strong>in</strong>g to circa l500 hectares i.e. 10 - 15% of <strong>the</strong> present total<br />

area (Rohsiek, et al. 1987).<br />

The total area of salt marshes very drastically has been reduced after<br />

caepletion of <strong>the</strong> <strong>Delta</strong> Project. S<strong>in</strong>ce 1987 only 24% of <strong>the</strong> orig<strong>in</strong>ally<br />

total area of salt marshes <strong>in</strong> <strong>the</strong> k<strong>in</strong>gvliet, Grevel<strong>in</strong>gen. Volkerak<br />

and Oaaterschelfle is rew<strong>in</strong><strong>in</strong>g <strong>in</strong> <strong>the</strong> Oosterschdde. It ia estimated<br />

that <strong>the</strong>se saltslarshes are subject to sn <strong>in</strong>creased rate of erosion.<br />

VegetatioO mid erosion resistance most probably have been weakened<br />

considerably as a result of a proloagued period of extrae tidal<br />

reductiod duritrg, <strong>the</strong> f<strong>in</strong>al constmctiDn phase of <strong>the</strong> Oostersahelde<br />

works.<br />

The Oosterechalde's ebb tidal delta has shown a cont<strong>in</strong>u<strong>in</strong>g exw<strong>in</strong>sion<br />

over <strong>the</strong> period 1960 - 1983 as a result of <strong>the</strong> tikl voluae <strong>in</strong>erease<br />

and result<strong>in</strong>g bas<strong>in</strong> erosion over this period. Van den Berg (1986) has<br />

ralculated a net sedimentation over <strong>the</strong>se years of ca. 38 millions m'.<br />

This is i n aceordance with <strong>the</strong> expeered trend as stated <strong>in</strong> Section 2.2.<br />

The decrease of tidal volume after 1987 <strong>in</strong>dicates an opposite<br />

gesmorphrtls~ical trend for <strong>the</strong> future. It is expacted that <strong>the</strong><br />

deltafront will erode. <strong>the</strong> tidal channels will silt up and longshore<br />

sandbars will develop a< <strong>the</strong> edges hheiek end Nulder, 1989). No<br />

geoolorphological data are available yet to confirm this.<br />

Tidal end gwmorphological changes af <strong>the</strong> Wastersehelde bas<strong>in</strong> ove-r <strong>the</strong><br />

last 30 years are ma<strong>in</strong>ly due to large $tale dredg<strong>in</strong>g. Because of it's<br />

importance for shippfng traffic to <strong>the</strong> harbours of Antwerp, no closure<br />

daar has been def<strong>in</strong>ed for <strong>the</strong> Westewchelde. Wifh<strong>in</strong> <strong>the</strong> fra81evork of <strong>the</strong><br />

<strong>Delta</strong> Projeet security aga<strong>in</strong>st flood<strong>in</strong>g around this estuary h- been<br />

odta<strong>in</strong>ed by streng<strong>the</strong>n<strong>in</strong>g of <strong>the</strong> dykes. The <strong>in</strong>tensified shipp<strong>in</strong>g

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