Monitoring of r adioactive contaminations of bottom sediments and - - PowerPoint PPT Presentation

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Monitoring of r adioactive contaminations of bottom sediments and - - PowerPoint PPT Presentation

Monitoring of r adioactive contaminations of bottom sediments and fish in the southern Baltic Sea, 2016 Maria Supliska a , Barbara Rubel a , Tamara Zalewska b a Central Laboratory for Radiological Protection, Warszawa b Institute of Meteorology


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Performed under an agreement of National Atomic Energy Agency, Warsaw

Monitoring of radioactive contaminations of bottom sediments and fish

in the southern Baltic Sea, 2016

Maria Suplińskaa, Barbara Rubela, Tamara Zalewskab

a Central Laboratory for Radiological Protection, Warszawa b Institute of Meteorology and Water Management , Maritime Branch- Gdynia

HELCOM-MORS 7, Tallinn 2017

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Methods

137Cs - gamma spectrometry;

239,240Pu, 238Pu - radiochemical method with 242Pu as a tracer, and alpha spectrometry.

90Sr - radiochemical method and the measurement of 90Y activity concentration after

establishing the radioactive equilibration of 90Sr - 90Y. 

226Ra - determined by emanation method (measurement of 222Rn in Lucas-type scintillation

chambers) preceded by separation of radium.

Research includes determination of radioactive contaminations in the southern Baltic Sea marine environment elements: bottom sediments and biota (fish). Samples were collected ones a year:

in February -fish samples (commercial catches) in June – sediment core samples (collected during the cruise onboard r/v Baltica at 6 sampling locations

HELCOM-MORS 7, Tallinn 2017

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P110 P116 P1 P140 P5

Baltic Sea

P39

Fig 1. Sampling stations of bottom sediments From each location, six core samples were taken and divided into 12 depth layers: 1cm layers ( to the depth of 5 cm), and 2 cm layers (from 5cm to 19cm depth). In addition, at each station one core sample (0-19 cm) was collected.

Bottom sediments

HELCOM-MORS 7, Tallinn 2017

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Activity concentrations of 137Cs in bottom sediments

  • Fig. 2. Vertical distribution of 137Cs in bottom sediments in 2016

* SD In 2016 concentrations of 137Cs in bottom sediments were slightly lower than in 2015. The highest concentrations of 137Cs, observed in the Gdansk Basin (P110, P116, P 1), ranged from 177 Bq kg-1

dw to 192 Bq kg-1 dw

while in Bornholm Basin (P 5, P 39) the concentrations in the upper layers were in the range 48.1 ÷ 50.8 Bq kg-1

dw.

Table 1. The average activity concentrations of 137Cs in the layers from 0 to 5 cm Sampling location

137Cs,

[Bq kg-1

dw]

P 110 172 ± 12* (156 – 187) P 116 166 ± 24 (135 – 192) P 1 155 ± 20 (123 – 177) P 140 102 ± 15 (82 – 124) P 5 41.0 ± 6.3 (30 – 48) P 39 47.4 ± 3.7 (43 – 51)

2 4 6 8 10 12 14 16 18 20 50 100 150 200 250

Depth, cm

137Cs, Bq kg-1 sdw.

P 110 P 116 P 1 P 140 P 5 P 39

HELCOM-MORS 7, Tallinn 2017

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Vertical distribution of 239,240Pu and 238Pu in bottom sediments

In 2016, plutonium was analysed in two locations:P116 (Gulf

  • f Gdansk) and P39 (Bornholm Basin)

At P116 concentrations of 239,240Pu increased from 1.41 Bq kg-1

dw (0-1cm) to 3.62 Bq kg-1 dw (3-4cm),

then were aligned in the layers from 4 cm to 13 cm with the average value of 3.28 ± 0.31 Bq kg-1

dw

the decrease to 0.50 Bq kg-1

dw was observed in the lowest layer

At P39 239,240Pu concentrations were about three times lower. After a slight increase from 1.08 Bq kg-1

dw to 1.36 Bq kg-1 dw,

concentrations of 239,240Pu were aligned in layers 2 – 9 cm with the average value equal to 1.30 ± 0.10 Bq kg-1

dw .

Below 15cm 239,240Pu concentration do not exceed 0.05 Bq kg-1

dw .

Fig.3. Vertical distribution of 239,240Pu concentrations in years 2014-2016

2 4 6 8 10 12 14 16 18 20 2 4 6 8 10 Depth, cm

239,240Pu, Bq kg-1 dw

P110/2014 P140/2015 P5/2015 P1/2015 P116/2016 P39/2016

Determination of plutonium in bottom sediments from 6 locations are carried out every three years

The activity concentrations of 238Pu in P 116 were in range 0.013 ÷ 0.099 Bq kg-1

dw

and in P 39 ranged from < 0.002 Bq kg-1

dw to 0.042 Bq kg-1 dw.

The rate of 238Pu to 239,240Pu in both locations was in range 0.02 ÷ 0.04 being similar to that determined for the fallout from nuclear weapons tests.

HELCOM-MORS 7, Tallinn 2017

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Sampling location

90Sr

[Bq kg-1

dw] 137Cs

[Bq kg-1

dw] 239,240Pu

[Bq kg-1

dw]

P 110 2.34 ± 0.11 79.0 ± 1.4 3.11 ± 0.12 P 116 3.19 ± 0.21 73.5 ± 1.3 2.74± 0.13 P 1 3.02 ± 0.22 103 ± 2.0 1.83 ± 0.08 P 140 2.56 ± 0.16 58.9 ± 2.5 0.93 ± 0.07 P 5 2.26 ± 0.16 23.1 ± 2.1 0.47 ± 0.02 P 39 2.89 ± 0.19 21.7 ± 1.3 1.25± 0.11 Table 2. Activity concentration of 90Sr, in the layer 0-19 cm of bottom sediments and activity concentration of 137Cs and 239,240Pu recalculated for this layer

Strontium-90

Activity concentrations of 90Sr in bottom sediments were performed in integrated samples taken from the layer 0-19 cm.

90Sr concentrations were in the range

2.26 ÷ 3.19 Bq kg-1

dw , being even 30

times lower than 137Cs concentrations (recalculated for the same layer). Concentrations of 239,240Pu were in the similar range to 90Sr.

HELCOM-MORS 7, Tallinn 2017

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  • Fig. 4 Total amounts of 137Cs, 90Sr, 239,240Pu and 238Pu

in bottom sediments, layer of 0-19 cm

Spatial distribution of antropogenic isotopes in bottom sediments

HELCOM-MORS 7, Tallinn 2017

1 2 3 4 5 6 P 110 P 116 P 1 P 140 P 5 P 39

137Cs, kBqm-2

Cs-137, 2016

2 4 6 8 60 120 180 240 P110 P116 P1 P140 P5 P39

238Pu, Bq kg-1 sm 239,240Pu, Bq kg-1 sm

2014-2016

Pu-239,240 Pu-238 60 120 180 240 P110 P116 P1 P140 P5 P39

90Sr, Bq m-2

Sr-90, 2016

The total amount of 137Cs in 2016 ranged from 1.02 kBq m-2 in the Bornholm Deep (P5) to 4.77 kBq m-2 in the Gulf of Gdansk (P110). The range of total amount of 90Sr was 88 ÷ 134 Bq m-2 and total amounts of 239,240Pu and 238Pu were in ranges: 28.8 ÷ 199 Bq m-2 and 0.76 ÷ 5.98 Bq m-2, respectively

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Number of samples Species/

total number

  • f pieces

Weight of sample [g]

137Cs

[Bq kg-1

w.w] 40K

[Bq kg-1

w.w] 226Ra

[Bq kg-1

w.w]

5 Cod 30 500-670 4.52 ± 0.51a) 4.06 – 5.26b) 111 ± 17 83 – 126 0.095 ± 0.003 0.092 – 0.100 5 Herring 109 500-550 2.55 ± 0.74 1.68 – 3.33 110 ± 19 86 – 133 0.028 ± 0.003 0.023 – 0.031 5 Sprat c) 279 520-620 2.79 ± 0.19 2.53 – 2.98 105 ± 9 92 – 114 0.068 ± 0.005 0.062 – 0.076 5 Plaice 33 500-505 3.32 ± 0.52 3.15 – 4.22 97 ± 6 86 – 104 0.055 ± 0.003 0.052 – 0.059 Table 3. The average concentrations of 137Cs, 40K and 226Ra in Baltic Sea fish flesh, 2016

a) standard deviation b) range of concentrations c) whole fish without a head

The highest average activity concentration of 137Cs was found in cod – 4.52 Bq kg-1

ww

and the lowest in herring – 2.55 Bq kg-1

ww.

Activity concentrations of 226Ra ranged from 28 mBq kg-1

ww in herring to 95 mBq kg-1 ww in cod.

Activity concentrations of selected radionuclides in four fish species

HELCOM-MORS 7, Tallinn 2017

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Fig 5. Average activity concentrations of 137Cs in Baltic Sea fish flesh in the years 1985-2016 The average 137Cs concentration calculated for the four species in 2016 was equal to 3.29 ± 0.88 Bq kg-1

ww.

Activity concentration of 137Cs in the Baltic Sea fish has decreased in years, but it is still higher than before the Chernobyl accident.

2 4 6 8 10 12 14 16

137Cs, Bq kg-1 fw.

HELCOM-MORS 7, Tallinn 2017

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HELCOM-MORS 7, Tallinn 2017

Summary

  • The highest concentrations of 137Cs occurred in the upper sediment layers and decreased along the profiles.

As in previous years, differences in the concentrations of 137Cs related to the location were observed.

  • The highest concentrations of 239,240Pu and 238Pu occurred in deeper sediment layers, and the ratio of 238Pu

to 239,240Pu in the individual layers are in range 0.02- 0.04, being typical of the radioactive fallout after the nuclear weapons test.

  • In the southern Baltic Sea no significant differences in the spatial distribution of 90Sr in the bottom

sediments were observed.

  • Contamination in fish due to 137Cs was reduced about 4 times comparing with maximum observed in 1989,

but is still higher than before the Chernobyl accident. The activity concentration of 137Cs and 226Ra in fish depends on their species, mainly due to the kind

  • f nutrition.
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Thank you for your attention

HELCOM-MORS 7, Tallinn 2017