Open AccessCurrent state and trends in the content of 137Cs and 90Sr in abiotic and biotic components of Arctic ecosystems (Barents and Kara Seas case study)
Author(s) -
Г. Г. Матишов,
I. S. Usyagina,
N. E. Kasatkina
Publication year - 2019
Publication title -
iop conference series. earth and environmental science
Language(s) - English
Resource type - Journals
eISSN - 1755-1307
pISSN - 1755-1315
DOI - 10.1088/1755-1315/302/1/012026
Subject(s) - radionuclide , abiotic component , seawater , biota , oceanography , environmental science , arctic , marine ecosystem , water column , contamination , environmental chemistry , current (fluid) , ecosystem , geology , ecology , chemistry , biology , physics , quantum mechanics
This publication summarizes long-term data on radioactive contaminants in seawater, bottom sediments, and marine fish and describes current patterns in radionuclide distribution using data collected by the Murmansk Marine Biological Institute during cruises to the Barents and Kara Seas in 2015–2017. During the study period, no short-lived artificial radionuclides were found in the Barents and Kara Seas. 137 Cs and 90 Sr isotopes with a longer half-life are still registered in Atlantic waters that are the main source of radioactive contamination in these Arctic seas. Volumetric activity of 137 Cs and 90 Sr was compared at different depths. A uniform distribution of 137 Cs in the vertical column of water and a tendency to increase the volume activity of 90 Sr from surface to bottom were observed in the Barents Sea. Bottom sediments in the Kara Sea contain on average 2 times more 137 Cs than the Barents Sea. Atlantic cod is characterized by an extremely low concentration of 137 Cs in muscular tissue, about an order of magnitude lower than in the period of maximum contamination of Barents Sea waters observed in 1982. Currently there is a decreasing trend in concentrations of anthropogenic radioisotopes in the environment and biota. Processes of 137 Cs and 90 Sr removing from biotic and abiotic components are described with exponential functions. Due to natural marine purification processes, the decrease of 137 Cs and 90 Sr concentrations in the Barents and Kara Seas occur 2–4 times faster than the physical radioactive decay of these radionuclides.