Reconstruction of the Long-Term Dynamics of Particulate Concentrations and Solid–Liquid Distribution of Radiocesium in Three Severely Contaminated Water Bodies of the Chernobyl Exclusion Zone Based on Current Depth Distribution in Bottom Sediments

Alexei Konoplev, Gennady Laptev, Yasunori Igarashi, Hrigoryi Derkach, Valentin Protsak, Hlib Lisovyi, Kyrylo Korychenskyi, Serhii Kirieiev, Dmitry Samoilov and Kenji Nanba
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Alexei Konoplev: Institute of Environmental Radioactivity, Fukushima University, Kanayagawa 1, Fukushima 960-1296, Japan
Gennady Laptev: Ukrainian Hydrometeorological Institute, Nauki Av., 37, 03028 Kyiv, Ukraine
Yasunori Igarashi: Institute of Environmental Radioactivity, Fukushima University, Kanayagawa 1, Fukushima 960-1296, Japan
Hrigoryi Derkach: Ukrainian Hydrometeorological Institute, Nauki Av., 37, 03028 Kyiv, Ukraine
Valentin Protsak: Ukrainian Hydrometeorological Institute, Nauki Av., 37, 03028 Kyiv, Ukraine
Hlib Lisovyi: Ukrainian Hydrometeorological Institute, Nauki Av., 37, 03028 Kyiv, Ukraine
Kyrylo Korychenskyi: Ukrainian Hydrometeorological Institute, Nauki Av., 37, 03028 Kyiv, Ukraine
Serhii Kirieiev: Chernobyl Ecocentre, State Agency of Ukraine on Exclusion Zone Management, 07270 Chernobyl, Ukraine
Dmitry Samoilov: Chernobyl Ecocentre, State Agency of Ukraine on Exclusion Zone Management, 07270 Chernobyl, Ukraine
Kenji Nanba: Institute of Environmental Radioactivity, Fukushima University, Kanayagawa 1, Fukushima 960-1296, Japan

Land, 2021, vol. 11, issue 1, 1-14

Abstract: Given the importance of understanding long-term dynamics of radionuclides in the environment in general, and major gaps in the knowledge of 137 Cs particulate forms in Chernobyl exclusion zone water bodies, three heavily contaminated water bodies (Lakes Glubokoe, Azbuchin, and Chernobyl NPP Cooling Pond) were studied to reconstruct time changes in particulate concentrations of 137 Cs and its apparent distribution coefficient K d , based on 137 Cs depth distributions in bottom sediments. Bottom sediment cores collected from deep-water sites of the above water bodies were sliced into 2 cm layers to obtain 137 Cs vertical profile. Assuming negligible sediment mixing and allowing for 137 Cs strong binding to sediment, each layer of the core was attributed to a specific year of profile formation. Using this method, temporal trends for particulate 137 Cs concentrations in the studied water bodies were derived for the first time and they were generally consistent with the semiempirical diffusional model. Based on the back-calculated particulate 137 Cs concentrations, and the available long-term monitoring data for dissolved 137 Cs, the dynamics of 137 Cs solid–liquid distribution were reconstructed. Importantly, just a single sediment core collected from a lake or pond many years after a nuclear accident seems to be sufficient to retrieve long-term dynamics of contamination.

Keywords: Chernobyl NPP; radiocesium; dissolved; particulate; lakes; cooling pond (search for similar items in EconPapers)
JEL-codes: Q15 Q2 Q24 Q28 Q5 R14 R52 (search for similar items in EconPapers)
Date: 2021
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