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. 2018 Nov 2;318(3):2389–2399. doi: 10.1007/s10967-018-6300-8

Table 3.

Results on 239+240Pu and 238Pu activity concentrations for second set of samples (calculated for summer 2001)

Layer depth (contracted) (cm) Recovery (%) 239+240Pu (mBq/kg) 238Pu (mBq/kg) 239+240Pu (Bq/m2)
Białe Wigierskie 0–2 78 ± 4 662 ± 75 29 ± 12 7.0 ± 0.8
Białe Wigierskie 2–4 89 ± 4 1118 ± 103 30 ± 10 12.0 ± 1.1
Gaładuś 0–2 74 ± 4 150 ± 25 23 ± 11 3.6 ± 0.6
Gaładuś 2–4 > 93 157 ± 18 < 12 3.6 ± 0.4
Gaładuś 4–6 > 99 172 ± 19 17 ± 6 3.8 ± 0.4
Garbaś 0–2 15 ± 1 480 ± 98 < 26 4.0 ± 0.8
Garbaś 2–4 94 ± 4 98 ± 13 6 ± 5 < 0.9
Garbaś 4–6 56 ± 3 13 ± 6 < 13 0.1 ± 0.1
Guzki 0–2 97 ± 5 1129 ± 99 181 ± 23 12.9 ± 1.1
Guzki 2–4 111 ± 6 1079 ± 94 39 ± 12 13.2 ± 1.1
Guzki 4–6 97 ± 6 722 ± 76 < 106 9.0 ± 0.9
Płaskie 0–2 > 98 812 ± 82 27 ± 12 7.1 ± 0.7
Płaskie 2–4 111 ± 9 226 ± 46 10 ± 10 1.7 ± 0.4
Płaskie 4–6 79 ± 4 29 ± 11 8 ± 8 0.2 ± 0.1
Rogale Duże 0–2 64 ± 5 3668 ± 348 166 ± 43 43.4 ± 4.1
Rogale Duże 2–4 72 ± 5 177 ± 37 16 ± 10 2.5 ± 0.5
Rogale Duże 4–6 80 ± 5 1381 ± 128 12 ± 7 19.5 ± 1.8
Rogale Duże 6–8 89 ± 5 9 ± 7 < 2 0.1 ± 0.1
Sawinda Wielka 0–2 86 ± 6 1276 ± 130 48 ± 15 9.4 ± 1.0
Sawinda Wielka 2–4 > 96 613 ± 61 54 ± 13 5.0 ± 0.5
Sumowo 0–2 116 ± 7 893 ± 95 33 ± 10 7.1 ± 0.8
Sumowo 2–4 > 98 1369 ± 110 35 ± 10 11.7 ± 0.9
Sumowo 4–6 93 ± 4 1691 ± 120 48 ± 13 14.0 ± 1.0
Toczyłowo 0–2 99 ± 5 95 ± 18 9 ± 6 1.8 ± 0.3
Toczyłowo 2–4 88 ± 5 142 ± 31 12 ± 19 2.7 ± 0.6
Toczyłowo 4–6 92 ± 5 141 ± 22 < 14 2.7 ± 0.4
Zawadzkie 0–2 90 ± 4 21 ± 7 11 ± 9 0.4 ± 0.1
Zawadzkie 2–4 93 ± 7 32 ± 9 12 ± 7 0.6 ± 0.2
Zawadzkie 4–6 60 ± 3 102 ± 18 < 3 1.9 ± 0.3
IAEA 300* 99 ± 7 3400 ± 320 141 ± 53

The last row contains results for the Reference Material IAEA 300 obtained with 242Pu tracer. Uncertainties are 1σ counting statistic only

*Baltic Sea sediment, certified value [7] for 239+240Pu is 3550 mBq/kg (range 3440–3650 mBq/kg)