Publication date: December 2017
Source:Journal of Environmental Radioactivity, Volume 180
Author(s): Agata Zaborska
Although primary sources of anthropogenic
137Cs have decreased nowadays, the Arctic is exposed to a variety of secondary sources. These include riverine run-off, oceanic currents, drifting sea ice, melting glaciers and permafrost. Recent reports underline the role of glaciers, specifically cryoconite holes, in radionuclide accumulation. Therefore, this study investigates the hypothesis that melting glaciers are an important means of delivering
137Cs for Arctic fjord (Hornsund, Svalbard). As marine sediments are the final sink for most contaminants, seven 30–40 cm long sediment cores collected in 2016 were investigated for
137Cs activity concentration. Five were collected in a transect from the central to the outer part of the fjord while two were collected within one km of the different melting tidewater glaciers. Sediment layers were dated using
210Pb to reveal the history of
137Cs accumulation. The measured
137Cs activity concentrations ranged from <0.1 to 7.7 Bq kg
−1. The activity concentrations ranging from 0.3 to 3.1 Bq kg
−1 were measured in surface (0–2 cm) sediments. The total
137Cs inventories were calculated for five station and ranged from 322 to 908 Bq m
−2, of which 29–34 Bq m
−2 were deposited within the last decade. At two stations characterized by largest sediment accumulation rates only the last decade inventories were calculated and they ranged from 13 to 444 Bq·m
−2. The mean of
137Cs fluxes calculated for last decade ranged from 2.7 to 44.1 Bq m
−2yr
−1. The history of
137Cs environmental inputs was well revealed in the sediments as the
137Cs penetration depth agreed with the time of its introduction to the Arctic and the most pronounced
137Cs activity concentration peak was found in sediments dated for circa 1963. Although
137Cs fluxes and inventories were largest in the glacial bay (Brepollen), the
137Cs was diluted in a large amount of sedimenting material. Based on the results in this study, the glaciers do not appear to act as important sources of
137Cs to the marine environment in the Hornsund fjord.
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