20
northern Baltic Proper, the Gulf of Bothnia, and
the Gulf of Finland, the total amounts were slightly
higher (1.6-6.7 Bq nr 2 ) than generally in the
southern Baltic Proper, as the activity concentra
tions ranged from 10 mBq kg -1 to 480 mBq kg -1
dry weight.
5.9 Pu-239,240
Plutonium is created from uranium in nuclear
reactors. During the 1950s and 1960s, plutonium
was dispersed worldwide from atmospheric test
ing of nuclear weapons. The fallout from these
tests left low concentrations of plutonium in soils
and sediments around the world. The fallout from
Figure 8. the Chernobyl accident brought a small addition of
Vertical distribution of plutonium to the aquatic environment of the Baltic
Pu-239,240 (Bq kg’ 1
d.w.) at the station Teili 1
(northern Baltic Proper)
in 2002.
Teili 1
Bq/kg d.w.
Concentration peaks of
Chernobyl-derived Cs-137
and weapons-tests-origin
Pu-239,240 at the station
K15 in the Gulf of Finland
(Mattila et al., 2006).
W)
M
cr 1
PQ
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<N
On
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<N
S
Qh
Sea, but its contribution was minor compared to
that of the weapons test fallout.
Data on Pu-239,240 were reported from 51 sedi
ment cores taken from all sub-regions of the Baltic
Sea, although most were from the southern Baltic
Proper. The plutonium peak caused by the weap
ons test fallout provides an excellent time marker
(1963), in addition to that of Cs-137 resulting from
the Chernobyl accident, for the estimation of
recent sediment accumulation rates in the Baltic
Sea (Figures 8 and 9).
The total amounts of Pu-239,240 at different
sampling stations in the Baltic Sea are shown
in Figure 10. The inventories of Pu-239,240 in
the sediments of different sub-regions are given
in Table 3, as well as the maximum values and
the median values (Bq nr 2 ) used in the inven
tory calculations. The ratio 1:10 was used in the
estimation of Pu-239,240 values for hard bottoms
versus soft bottoms, analogously with the earlier
calculations published by Salo et al. (1986) from
the beginning of the 1980s.
The total inventory of Pu-239,240 in the seabed
of the Baltic Sea was estimated at 15.3 TBq. The
portion for the Bothnian Sea was 45% of the total
inventory and that for the Baltic Proper was 32%.
If the ratios 1:20 or 1:5 were to be used for the
total amounts of Pu-239,240 on hard bottoms
compared to those on soft bottoms, the result
would be 14.6 TBq or 16.8 TBq, respectively.
The estimate is equal to that of Salo et al. (1986)
from the beginning of the 1980s. This may be
realistic taking into account the fact that the input
of plutonium from Chernobyl into the Baltic Sea
was relatively small, and on the other hand, the
present estimation was based on a clearly more
extensive study material.
5.10 Am-241
Americium is a man-made radionuclide produced
in nuclear reactors and nuclear weapons detona
tions. Most americium-241 in the environment
originates from the atmospheric testing of nuclear
weapons during the 1950s and 1960s. Results
on Am-241 were reported from three stations in
the southern Baltic Proper and the Belt Sea and
three stations in the Bothnian Bay and the Gulf
of Finland. The activity concentrations in the
samples ranged from 0.08 Bq kg -1 to 3.5 Bq kg -1
dry weight.