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Full text: 62: Die Auswirkungen des Kernkraftwerkunfalles von Tschernobyl auf Nord- und Ostsee

Summary 
The Deutsches Hydrographisches Institut, since the accident has in- 
vestigated with even more intensity the radioactive contamination of 
the North Sea and the Baltic Sea. Thereby, the input of the radioac- 
tive Fallout from Chernobyl could be detected not only from the rise 
of the measurement values in the radiological measurement network, 
but also by the analysis of the water samples which were taken at 
the corresponding moments in time. The temporal and spatial investi- 
gations indicated that the input took place differently in intensity 
and local distribution. 
Mixing processes effected a rapid decrease in activity concentration 
already during the first hours after the input. The direct Gamma- 
spectroscopical determination of individual nuclides without che- 
mical enrichment was no longer possible after a few days. For that 
reason, the concentration in the following period was essentially 
determined from the tracer isotopes Cs 134 and Cs 137. A series of 
Samples for Gamma-spectroscopy was concentrated by evaporation. 
The Fallout from Chernobyl, according to its characteristic nuclide 
composition, can be clearly differentiated from the contaminations 
of the North Sea and the Baltic Sea which derive from the nuclear 
fuel reprocessing plants Sellafield Works and La Hague. The concen- 
tration decrease observed as the result of mixing processes also ap- 
ply exemplarily for other toxic substances entering the sea from the 
atmosphere« 
In spite of the time-consuming methods of analysis, a series of 
Sr 90, Pu 239, Pu 238, Am 241, and Cm 242 determinations were 
carried out. For the time being, Tritium was not determined further, 
after the analysis of an intensively radioactive rainwater sample 
indicated no significant increase of the Tritium concentration. 
The data gained, permit the recognition of no immediate hazard by 
external radiation burden from the biosphere for the marine environ- 
ment as a whole. To what extent enrichments of nuclides in the sedi- 
ments and suspended matter, and enrichment in biological systems can 
lead in the long term to relevant effects, must be clarified in the 
future by extended {investigations. The further investigation pro- 
jects are aimed in that direction.
	        
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