Hydro-ecological relations in the Delta Waters

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discharged through the mouths of the estuaries to the North However, local variations were apparent, with further erosion taking place in the deeper tidal gullies and corresponding increasas in sedimentatton occurring in the shallows. Moreover, sea-borne sediment was deposited in the western part of the Delta. The finer type of fluvial sediment was only deposited in more sheltered locations, with the majority of it flowing tkouah to the RarM Sea. Under the influence of the prevail* sediment was carried northwerds, where w e 10%-shore current this fine fluvial of it was deposited ia the Wadden Sea, an extensive w e s l area ~ in the north of the Netherlands. Successive closures in the Delta area produced chenges in the flaw distribution, while flow rates tended to decline as a result of the complete or partial loss of tidal motion. =is Led to tde formation of new se-ntation areas witain the Delta regfoil. By 1965 the central section of tXe Delta vaS no longer sublect fa the influence of the Rhine and Ruse. In 1965 and 1969 resptpectively the Grevelingen and Eastern Scheldt estuaries were effectively &coupled from these two rivers. The closure of the Harinmliet estuary in the northern section of the Delta had the effect of reducing tidalmotion over the whale oi? this area. Xn the sautb, the Western Scheldt estuary remained Largely unchanged, although the sand bars in the estuarp *ere dug out in the 1970's to improve the shipping route to Antwerp (Belgium). Finally, in 1987, work in rhe eastern past of the Delta led to the fomation of a separate freshwater lake (Lake Zoom3 in the Eastern Scheldt, irith the spe~ific aCm of imprwing water supplies for agricultural purposes. Lake Zom is being flusked out with frwb water from the Eollarids Diep, The overall eff&t of all these hydraulic engineering projects has been to change significantly the distribution of river water, which has had implications for the transport of fluvial sediment. Recent measurements of the transport of fine fluvial aediments are shown in tern of tons per year in Figure 3. This fi~uze also gives the yearly irccumulation of river sediment at: particular locations. Region I represents the southern lower reaches of the Rhine and the lover reaches of the Meuse. Following the closure of the Haringvliet estuary, flov rates in the
area decltned cnnside~ably, leadins eo a~rensive sedimentation. This has cause3 an Inner delta to form at this location, which is gradnag plovinp in a westerly direction. In the case ef Regien 11, the lIarinpliet, closure has led ko a thin layer of silt being deposited over this area. From 1987 onwards, a new sedimenracion area is developing in Lake Zo& (Region In). The sedimentarion in this region is essentially similar to that found in the Haringqliet area and will mainly cunsist of silt. Pbally, comparisons can be made with the sedhentntion area in the Western Scheldt (Region IVI. In this region most of the silt carried by I l t.l(.rnbsmlsl W.*l.m ..I""" Sm.ldl I I' closure dam J [ waler me.naeernm1 sluice ir~dlmsnlatlon rsgl~n X: number ot lhe raglan 200: sedlmenlallorn in 1000 tons I year Figure 3 Transport rates of fine fluvial sediments 19.87 (values in l000 tms p.a.)
Page 1 and 2: Netherlands organkation fw applied
Page 4 and 5: TNO Commlitee on Hydrological Resea
Page 6 and 7: 2 RIVER WATER AM) THE QPALITH OF TB
Page 8: B.J.M. Baptist BIJkswaterstaat. Tid
Page 11 and 12: This approach will put to use what
Page 13 and 14: Estuaries that have not been influe
Page 15: 2 CHIWGES XN TEE DELTA The Delta ar
Page 19 and 20: Plan, then it is apparent tbt the s
Page 21 and 22: Tiddl flats df the Eastem Seheldt v
Page 23 and 24: tracefore possible to convert the a
Page 25 and 26: Figsrlre 7 Changes in the cadrnrum
Page 27 and 28: prevention measures are desirable h
Page 29 and 30: elationships between different spec
Page 31 and 32: Bio-essay Weriments with polluted s
Page 33 and 34: considerable thought to drawing up
Page 35 and 36: ShLOUONS, W. and BYSINK, W.D., 1981
Page 37 and 38: are taken. The first year after the
Page 39 and 40: The Hollands DiepJnaringpllet is pa
Page 41 and 42: In 1976 the determination of chlozo
Page 43 and 44: , 0.66 m 0,s - 0.02 1989 I 0.86 - 0
Page 45 and 46: Table 3 Eutrophication of the Volke
Page 47 and 48: Laks Volkarek ---- Lake Zoom 0.40 0
Page 49 and 50: 4 WAGBEET MEdSIIRaS TO PEEVBT OR LT
Page 51 and 52: Table 5 gives estimtes of the phosp
Page 53 and 54: In principle, two states of equilib
Page 55 and 56: Zooplankton (Alma affinis) Pike (Es
Page 58 and 59: EUTROPHICATION OF ESTUAAIES AND BRA
Page 60 and 61: The average discharge of Xhine and
Page 62 and 63: and only l-2% cows frm the aive Sch
Page 64 and 65: highest trophic potential: nutrient
Page 66 and 67:
period 1980-19$3 in an increase of
Page 68 and 69:
model calculations reveal that a ni
Page 70 and 71:
Table 3 PreUmInary carbon budget of
Page 72 and 73:
Water life of Lake Grevelingen
Page 74 and 75:
macrophytes livkg on or rooting in
Page 76 and 77:
less predictable for water managers
Page 78 and 79:
ILWNEWIJK, A.. KEIP, C., 1988. De v
Page 80 and 81:
XBE CHANGING TmAL LAMXiCAPE I N TEE
Page 82 and 83:
The storm surke of L&Z1 A.D., knorm
Page 84 and 85:
osi* rn@8IOIP m .SL 4 Has F~~ULB 3
Page 86 and 87:
During the 19th century man starts
Page 88 and 89:
mudflats have retreated some 100-20
Page 90 and 91:
aq811~33a.e~ pue 3pTatlJS uxaJsafi
Page 92 and 93:
Erosion by waves of sandy shoals (c
Page 94 and 95:
Lt has been estimated that the sedi
Page 96 and 97:
Implementafion of the Delta Project
Page 98 and 99:
ECOLOGICAL DEVELOWdENT OF SALT MAKS
Page 100 and 101:
fn tidal water systems sedimentatio
Page 102 and 103:
hierarchical position. Tn the egtua
Page 104 and 105:
Of course. tke environmental change
Page 106 and 107:
wind erasson, desaliuation, aeratio
Page 108 and 109:
Fonner tirtal flats with saltmarsh
Page 110 and 111:
Grevelingen. Lake Veere and Krammer
Page 112 and 113:
As mentioned above aa important que
Page 114 and 115:
A seaond important perspective for
Page 116:
BEEEXNX, W.D. and 80ZBf&. J. L9M. T
Page 119 and 120:
are determining the dfstrlbution af
Page 121 and 122:
this volume or in Duutsaa, et aL, 1
Page 123 and 124:
artificial waterflow was created af
Page 125 and 126:
of waterbirds occur regulsrly. The
Page 127 and 128:
. DISTRIBUXIOBI OF WATEJBIRoS OVER
Page 129 and 130:
small bird$ extludiag them vill net
Page 131 and 132:
In order to lsok for relatiouehips
Page 133 and 134:
Table 3 Biomass of macroroobenthos
Page 135 and 136:
freshwater basins. Clearly the pres
Page 137 and 138:
scmthem bottueary o-f the winter di
Page 139 and 140:
OCLURRENCE AND DIET QF B ~T .tUQ 80
Page 141 and 142:
5.2 H- factors Next to all fartors
Page 143 and 144:
Bewick's Swans (Cygnus columbariusl
Page 145 and 146:
m's activiries do not always have t
Page 147 and 148:
measure affecting food supply or av
Page 149 and 150:
DOQiWT$QS, G. 4 TWISK, F., 1987. De
Page 151 and 152:
MEININGEB, P.L. and HAPEREX, A.M.M.
Page 153 and 154:
PISCIVORES Litfle Grebe Great Crest
Page 156 and 157:
IPYBRO-EGOLOOIOAL BELATIONB ZN THE
Page 158 and 159:
apart from upstream purification; -
Page 160 and 161:
Storm surge barrier Eastern Scheldt
Page 162 and 163:
- In addition to existing managemen
Page 164 and 165:
Nature is pliable. Belattvely young
Page 166 and 167:
Ro. 1. No. 2. SQ. 3. Investigations
Page 168 and 169:
25. The relation between water quan
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Hydro-ecological relations in the Delta Waters

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