Delayed inputs of hot 137Cs and 241Am particles from Chernobyl to sediments from three Finnish lakes: implications for sediment dating

Abstract

Anomalous peaks in the 137Cs and 241Am records from three lake sediment cores from southern Finland appear to be due to the presence of micron-size hot radioactive particles, almost certainly originating in fallout from the 1986 Chernobyl accident. Since the imbedding sediments all post-date 1986 by several decades, it appears that they were initially deposited on the catchments of these lakes and transported to the lakes some years later. The activities of the particles were determined using a sequential splitting process. Two of the particles were found to contain 137Cs with activities of 64 ± 4 mBq and 266 ± 15 mBq respectively. The third contained 241Am with an activity of 17 ± 2 mBq, but no evidence of significant amounts of 137Cs. The delayed input of such particles into the sedimentary records highlights the need for care in using 137Cs or 241Am as chronostratigraphic markers in areas subject to significant levels of contamination from Chernobyl fallout.

Borrowing from the palaeolimnologists toolkit; the use of lake sediment cores in diagnosing the causes of freshwater species decline

“…Radiometric dating (Appleby, 1997) of the cores was undertaken at the Bloomsbury Environmental Isotope Facility (BEIF) at University College London (UCL). The timescale covered by each slice of the cores was established by measuring naturally occurring lead-210 ( 210 Pb) radionuclides in addition to artificially produced Caesium-137 ( 137 Cs) and Americium-241 ( 241 Am) released by nuclear weapons testing and nuclear reactor accidents (Appleby et al, 2023). The accuracy of the dates from the Constant Rate of Supply (CRS) models was further assessed by cross correlation of the LOI's of short cores and lead profiles generated from the XRF analyses (see Supplementary Materials and (Robson, 2017).…”