Hydro-ecological relations in the Delta Waters
Hydro-ecological relations in the Delta Waters Hydro-ecological relations in the Delta Waters
occwrence of floating mats of blue-green algae often causes a nuisance in tMs lake. The mean transparency does not exceed 1 m. Figure 6 shows the changes in fhe chlorophyl level in bofh parts of the lgke system in 1988. ' Laks VoLsrak ---- Lake zom - 0 6 TO 9 6 20 26 30 85 week no. Figure 6 Chlorophyl level id take Volkerak and lake Zoom in 1988 From this Figure it can be seen that peaks of up tn 100 mg/m9 o a r tn the s~ring. There fs an abrupt downturn at Che end of &lax/he~inning of June, and fn the reat of the summer the chlorophyl levels remain very low - especially in Lake Volkerak. The next two Sigures (Fig. 7 and 8) show the changes in the total P-level and the transparency. There was a clear decrease is the level of total pho~gharrrs in the spring. In the perirvd of the sharp deeIine in the ehlorophyl level towaras the end of May there is a clear increase in traneparency, first in Lake Polkerak and later Ln Me Zoom too. In hrvth lakes a transparency of alnurst 4 m was measured in August - a unique situation fos fresh water in the Netfierlds.
Laks Volkarek ---- Lake Zoom 0.40 0 5 10 16 20 25 30 35 week no. Figure 7 Total P-level in 1988 Lake Volkerak ---- Laka Zoom O L ~ " ' ~ ~ ' ~ ' ~ " ~ " " " ' " ~ " " ~ " ' ~ ~ 0 5 10 16 20 26 30 S6 40 weak no. Figure 8 TrBmpareucy in 1988
- 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 and 16: 2 CHIWGES XN TEE DELTA The Delta ar
- Page 17 and 18: area decltned cnnside~ably, leadins
- 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: Table 3 Eutrophication of the Volke
- 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
occwrence of float<strong>in</strong>g mats of blue-green algae often causes a nuisance<br />
<strong>in</strong> tMs lake. The mean transparency does not exceed 1 m.<br />
Figure 6 shows <strong>the</strong> changes <strong>in</strong> fhe chlorophyl level <strong>in</strong> bofh parts of<br />
<strong>the</strong> lgke system <strong>in</strong> 1988.<br />
' Laks<br />
VoLsrak<br />
---- Lake zom<br />
-<br />
0 6 TO 9 6 20 26 30 85<br />
week no.<br />
Figure 6 Chlorophyl level id take Volkerak and lake Zoom <strong>in</strong> 1988<br />
From this Figure it can be seen that peaks of up tn 100 mg/m9 o a r tn<br />
<strong>the</strong> s~r<strong>in</strong>g. There fs an abrupt downturn at Che end of &lax/he~<strong>in</strong>n<strong>in</strong>g of<br />
June, and fn <strong>the</strong> reat of <strong>the</strong> summer <strong>the</strong> chlorophyl levels rema<strong>in</strong> very<br />
low - especially <strong>in</strong> Lake Volkerak.<br />
The next two Sigures (Fig. 7 and 8) show <strong>the</strong> changes <strong>in</strong> <strong>the</strong> total<br />
P-level and <strong>the</strong> transparency.<br />
There was a clear decrease is <strong>the</strong> level of total pho~gharrrs <strong>in</strong> <strong>the</strong><br />
spr<strong>in</strong>g. In <strong>the</strong> perirvd of <strong>the</strong> sharp deeI<strong>in</strong>e <strong>in</strong> <strong>the</strong> ehlorophyl level<br />
towaras <strong>the</strong> end of May <strong>the</strong>re is a clear <strong>in</strong>crease <strong>in</strong> traneparency, first<br />
<strong>in</strong> Lake Polkerak and later Ln Me Zoom too. In hrvth lakes a<br />
transparency of alnurst 4 m was measured <strong>in</strong> August - a unique situation<br />
fos fresh water <strong>in</strong> <strong>the</strong> Netfierlds.