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This study presents the results of determinations of Cs-137 in full-fat cow milk powder originating from four regions of Poland. The assays performed demonstrated differences in the content of Cs-137 in milk powder depending on the region. The higher content of Cs-137 was found in powdered milk samples collected from Opole (3.50 Bq/dm³). The lowest content of Cs-137 was in milk samples from Września (0.98 Bq/dm³). In powdered milk samples from Łapy and Krotoszyn the amount of Cs-137 was 2.02 and 1.11 Bq/dm³, respectively. The average content of Cs-137 in full-fat cow milk powder from all examined regions was 1.90 Bq/dm³ after reconstituting to liquid milk, and did not exceed the admissible level of Cs-137 in food.
Recent sediment accumulation rates in Adventfjorden (Svalbard), a small subpolar fjord, were determined by 210Pb and 137Cs dating. Modern rates in the central basin decrease downfjord from 1.87 to 0.87 cm y−1 (2.6 to 1.19 g cm−2 y−1). Comparison of the modern values (1986–2001) with older ones (1963–86) reveals a marked increase in sediment accumulation rates in the last ten years. This correlates well with recent climate changes (warming and increase in precipitation). Comparison with particulate matter flux data indicates that a portion of the sediment is passed on to Isfjorden.
In 2005, in the administrative district (powiat) of Garwolin (the Province of Mazowsze), the samples of forest, cropland and fallow land soils were collected from three depths: 0-3 cm, 3-7 cm, 7-12 cm. The litter from the sampling sites located in forests was also collected for studies. In the samples, the contents of isotopes 137Cs and 40K were measured. The highest amount of 137Cs was measured in litter and the upper layer of forest soils; the content of the isotope decreased in deeper layers of the soil. Forest soils were the richest in 137Cs; fallow and cropland soils contained less of this isotope. The content of 40K in forest and fallow land soils did not depend on the depth from which the samples were collected. The highest amount of 40K isotope was found in arable soil, the lowest - in forest soils. The content of 137C in the soils decreased as the soil reaction increased but rose at higher organic carbon content. The content of 40K isotope correlated negatively with the soil reaction and with the content of sand fraction but it correlated positively with the content of clay fraction.
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