13
(average 3%) of those on soft bottoms. Thus, the
lower value given in our inventory estimates may
be more realistic, but since the inventory is still
based on a limited number of observations, and
taking into account the considerable variability of
the data, it is more relevant to give a range rather
than a single value as a result.
The spatial distribution of the total amounts of Cs-
137 at different sampling stations in the Baltic Sea
is shown in Figure 2. The highest total amounts
of Cs-137 per m 2 were observed in the Bothnian
Sea. The maximum value, 125 000 Bq nr 2 , was
recorded in 1998 from the northernmost part of
the Bothnian Sea (llus et al., 2003), and values
exceeding 110 000 Bq nr 2 were also recorded in
the sea area off Gavle. The median total amount
of Cs-137 was 36 400 Bq nr 2 on the soft bottoms
of the Bothnian Sea. The corresponding value for
the soft sediments in the Bothnian Bay was 9 700
Bq nr 2 .
In the Gulf of Finland, the maximum amount
of Cs-137 was 42 700 Bq nr 2 in the middle of
the eastern part in 2003, and values exceeding
38 000 Bq nr 2 were also recorded in the eastern
most parts of the Gulf. The median total amount
in the soft sediments of the Gulf of Finland was
10 400 Bq nr 2 . In the Gulf of Riga, the maximum
total amount of Cs-137 was 21 800 Bq nr 2 at a
h
£
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pin
OlA
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w
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t
Q
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• Jbi5
• •
i m
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/A ' '
4 • •• •
•
•
rf* i
r
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Total amounts of Cs-137 (Bq/m2)
»
100
000
to
150
000
50
000
to
100
000
20
000
to
50
000
10
000
to
20
000
0
to
10
000
Figure 2.
Total amounts of
Cs-137 (Bq nr 2 ) at
different sampling sta
tions in the Baltic Sea
at the beginning of the
2000s.
Long-lived radionuclides in the seabed of the Baltic Sea