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5.3 Sr-90
Traditionally, strontium-90 has been, together with
Cs-137, the other intensively monitored artificial
radionuclide in radioecological studies because
it is one of the most important fission products
and its half-life is almost as long (28.5 years) as
that of Cs-137. In the atmospheric weapons tests
during the 1950s and 1960s, the dominant fallout
nuclides were Cs-137 and Sr-90 in an activity ratio
of about 1.6. Consequently, Sr-90 was intensively
monitored in the environment after that. In recent
years, the frequency of analysis of strontium
has been significantly reduced. One reason is
the laborious and time-consuming analytical
method for Sr-90; however, in addition, there is
less interest in strontium because its share in the
Chernobyl fallout was much smaller than that of
Cs-137. The total input of Sr-90 from the Cherno
byl fallout into the Baltic Sea area was estimated
at 80 TBq (decay corrected to 1991), while it was
4 100-5 100 TBq for Cs-137 (Nies et al„ 1995).
Although the acquisition of recent data on Sr-90
in the Baltic Sea sediments was set as a target
for the Sediment Baseline Study, relatively few
results were reported to the database during the
project. Furthermore, due to the wide diversity of
the data reported (e.g., the length of the sediment
props analysed varied from 3 cm to 40 cm), it was
difficult to estimate the total current inventory of
Sr-90 in the seabed of the Baltic Sea. Typical total
amounts of Sr-90 in sediments were from about
50 Bq nr 2 to 200 Bq nr 2 . A rough estimate of the
total inventory was calculated as 26 TBq, which is
about two times higher than that (12 TBq) given by
Salo et al. (1986) for the beginning of the 1980s.
This seems to be in agreement with the deposition
values and the concentrations in sediments.
5.4 Tc-99
The concentrations of technetium-99 were low in
the sediments of the Baltic Sea. In four samples
analysed, the activity concentrations of Tc-99 in
surface layers of the sediments (0-10 cm) varied
between 0.040 Bq kg -1 and 1.3 Bq kg -1 d.w. The
highest value was in the Belt Sea and the lowest
in the Gulf of Finland.
Long-lived radionuclides in the seabed of the Baltic Sea