Titlebook: North Sea—Estuaries Interactions; Proceedings of the 1 Donald S. McLusky,Victor N. Jonge,John Pomfret Conference proceedings 1990 Kluwer Ac

exophthalmos

R. Barr,P. G. Watson,C. R. Ashcroft,B. E. Barnett,C. Hilton

愛花花兒憤怒

Hemoptysis

Effects of tide range alterations on salt marsh sediments in the Eastern Scheldt, S. W. Netherlandsm the change in the composition of pore waters. The rapid increase in redox potentials (up to 600 mV) and total dissolved iron (up to 5 mM 1.) and SO. (up to 65 mM 1.) and the decrease in pH (up to 4.5–2.5) all suggest a rapid oxidation of pyrite. Acidic conditions were found only in sediments with

OVER

,The phosphorus budget of the Marsdiep tidal basin (Dutch Wadden Sea) in the period 1950–1985: impornd a transformation term representing the interchange between dissolved and particulate phosphorus. Averaged over the entire period 55% of the phosphate input (SRP) to the basin is delivered by the fresh water sources, and 45% by the Vlie basin. For non-SRP components these numbers are 50% and 40% r

對待

Effects of changes in turbidity and phosphate influx on the ecosystem of the Ems estuary as obtaineeaches of the estuary a 50% reduction in the river discharge of phosphate is largely compensated for by changes in phosphate transport from the North Sea. This results in a nearly unchanged primary production in the lower reaches as compared with the standard run..In the upper reaches a 50% reductio

Meditative

Response of the Dutch Wadden Sea ecosystem to phosphorus discharges from the River Rhine,nate from the River Rhine. However, there are two possible routes for nutrients to reach that area. One is via the River IJssel and Lake IJssel (varying amounts of fresh water are sluiced out from the latter into the Wadden Sea). The other is along the coast of the North Sea, where the water transpo

激怒

有效