47
5 Radioactivity in the Baltic Sea
compared to other sea regions
lolanda Osvath
International Atomic Energy Agency (IAEA)
Marine Environment Laboratories
A recently published study on worldwide
marine radioactivity (IAEA, 2005) enables a
comparison of levels of anthropogenic radionu
clides in Baltic seawater against those in other
areas of the world ocean. The Baltic Sea ranked
highest for average Cs-137 levels in surface
water in the year 2000 (Figure 1), closely fol
lowed by the Irish Sea. In terms of Sr-90 levels,
the Baltic Sea ranks third, after the Irish Sea
and the Black Sea. Average Pu-239,240 levels
in surface water in the Baltic Sea are similar to
those measured in other areas of the northern
ocean at large, but two orders of magnitude
below those estimated for the Irish Sea.
These levels clearly reflect the dominant
regional sources for the respective radionu
clides, as described in detail for the Baltic Sea
in Chapter 2, as well as the processes affecting
the fates of these radionuclides, quite different
in terms of physico-chemical properties, after
their release to the environment. A compari
son with other semi-enclosed European Seas,
such as the Black Sea and the Mediterranean
Sea, helps set this in perspective. The follow
ing comparison will focus on Cs-137, which
has been considered as the most significant
man-made radionuclide in the marine environ
ment in terms of inventory, transfer and global-
scale dosimetry (IAEA, 1995). Input from the
Chernobyl accident is significantly higher for
the Baltic Sea than the contribution of global
fallout from nuclear weapons testing, while for
the Black Sea these two sources contributed
more equally to the inventory of Cs-137 (Table
1). Although it drains a smaller land area than
the Black Sea, the Baltic Sea also received
larger long-term post-Chernobyl inputs of Cs-
137 through rivers than the Black Sea. This
reflects the pattern of contamination by fall
out from Chernobyl of the respective drainage
basins (OECD, 1996; EC, 1998) and the latitu
dinal distribution of global fallout (UNSCEAR,
2000). The contribution of global fallout is con
siderably higher for the Mediterranean Sea,
given the large surface area of this sea and of
its drainage basin. Basin-specific freshwater
inflow patterns, seawater circulation and mixing
as well as geochemical processes further con
trol the transport and transfer of radionuclides
through the marine environment and explain
the observed distributions and differences from
region to region.
During the period 2000-2005, Cs-137 levels
of up to 125 kBq-nr 2 were found in Baltic Sea
bottom sediments, with median levels of 36
kBq nr 2 in the Bothnian Sea and 10 kBq nr 2
in the Gulf of Finland (HELCOM, 2007). For
comparison, Cs-137 inventories in Black Sea
bottom sediments reported by Egorov et al.
(2006) for the years 1990-1994 range between
0.2 kBq m' 2 in the abyssal basin and continen
tal slope areas, and 30 kBq m' 2 at the mouths
of the River Danube. Sediment inventories up
to 18 kBq m' 2 Cs-137 were reported for the lat
ter area for 2003 (Laptev and Voitsekhovitch,
2006). Western Mediterranean inventories
of Cs-137 in deep-sea sediment of 0.2 - 0.3
kBq m' 2 were reported for the early 1990s
(Delfanti et al., 1995).
A comprehensive study of radioactivity in the
marine environment and doses from marine
exposure pathways published in 1995 (IAEA,
1995) shows that average levels of Cs-137 in
fish in the Baltic Sea in 1990 were similar to
Source
Baltic Sea
Black Sea
Mediterranean Sea
Chernobyl atmospheric deposition on the sea surface, PBq
4.1-5.1
1.7-2.4
3-5
Chernobyl river inflow (1), inflow from the Black Sea through the
0.3 (1)
0.03 (1)
0.3 (2)
Bosphorus Strait (2), PBq
Global fallout/atmospheric nuclear weapons tests, PBq
0.8
1.4
12
Nuclear waste reprocessing plants, PBq
0.25
-
0.03
Sea surface area, 10 3 km 2
415
436.4
2500
(average depth, m)
(55)
(1253)
(1500)
Drainage basin surface area, 10 3 km 2
1700
2400
3300
Table 1:
Contributions to
cumulative Cs-137
inventory: comparative
table for semi-enclosed
European seas (This
report; Egorov et al,
2007; IAEA 2005)
Baltic Sea Environment Proceedings No. 117