Pb. Dubois et al., A QUANTITATIVE ESTIMATE OF ENGLISH-CHANNEL WATER FLUXES INTO THE NORTH-SEA FROM 1987 TO 1992 BASED ON RADIOTRACER DISTRIBUTION, Journal of marine systems, 6(5-6), 1995, pp. 457-481
Seven oceanographic campaigns carried out in the North Sea between Jul
y 1987 and January 1992 by the Marine Radioecology Laboratory (LRM) of
La Hague have led to the drawing of general maps showing the distribu
tion of the radionuclides Sb-125, Cs-137, Cs-134 and Tc-99 in seawater
. In this way, the total amounts of radioactivity (inventories) presen
t in the southern North Sea were evaluated from each separate campaign
, thus leading to an assessment of the mean distribution of water mass
es, originating from the English Channel, which is siutated between th
e Straits of Dover and Skagerrak. On this basis, it is possible to lin
k the flux of radionuclides released from the nuclear fuel reprocessin
g plant at La Hague (Sb-125 and Tc-99) with the inventories of radiotr
acers observed in the southern North Sea. Hence, the most probable mea
n transit time of Channel waters entering the North Sea were calculate
d for each campaign; Channel waters take 110-152 days to flow from Cap
de la Hague to the Straits of Dover and 170-250 days to travel from t
here to the entrance of the Baltic. The water flux through the Straits
of Dover is estimated to lie in the range 97,000-195,000 m(3)/s for t
he period between January and July 1988. Very good agreement is found
between the activities measured at different times and the results of
a model simulating the hydrodynamic behaviour of the North Sea.