Accumulation of Chernobyl-derived 137Cs in bottom sediments of some Finnish lakes

Title: Accumulation of Chernobyl-derived 137Cs in bottom sediments of some Finnish lakes

Author: Erkki Ilus, Ritva Saxén

Reference: Journal of Environmental Radioactivity, Volume 82, Issue 2, 2005, Pages 199-221

DOI: http://dx.doi.org/10.1016/j.jenvrad.2005.01.008

Keywords: Lake sediments; Chernobyl fallout; Caesium-137; Sedimentation rate

Abstract: The amount and vertical distribution of Chernobyl-derived ¹³⁷Cs in the bottom sediments of some Finnish lakes were studied. Sediment and surface water samples were taken in 2000 and 2003 from 12 stations in nine lakes and the results were compared with those obtained in corresponding surveys carried out in 1969, 1978, 1988 and 1990. Each of the five deposition categories of Chernobyl fallout in Finland were represented. The depth profiles of ¹³⁷Cs in the sediments showed considerable variety in the lakes studied. The peak values varied between 1.5 and 46 kBq kg⁻¹ dry wt. The size and shape of the peak did not always correlate with the amount of deposition in the area, but on the other hand, reflected differences in sedimentation processes in different lakes. In some of the lakes the peak still occurred in the uppermost (0–2 cm) sediment layer, but in an extreme case the peak occurred at a depth of 22–23 cm corresponding to a sedimentation rate of 16 mm year⁻¹ during the 14 years after the Chernobyl accident. The total amounts of ¹³⁷Cs in sediments varied from 15 to 170 kBq m⁻² at the sampling stations studied. Since 1990, the amounts have continued to increase slightly in two lakes, but started to decrease in the other lakes. In most of the lakes, the total amounts of ¹³⁷Cs in sediments were about 1.5–2 times higher than in local deposition. In two lakes, the ratio was below 1, but in one case 3.2. Compared with the total amounts of ¹³⁷Cs at the same stations in the late 1960s and 1970s, the values were now at their highest, at about 60-fold. The most important factors affecting ¹³⁷Cs values in sediments were the local amount of deposition and the type of the lake and the sediment, but in addition, there were a number of other factors to be considered.

URL: http://www.sciencedirect.com/science/article/pii/S0265931X0500041X

Sedimentation rates measurements in former channels of the upper Rhône river using Chernobyl 137Cs and 134Cs as tracers.

• Title: Sedimentation rates measurements in former channels of the upper Rhône river using Chernobyl 137Cs and 134Cs as tracers.

Author: Rostan, J C / Juget, J / Brun, A M

Reference: The Science of the total environment, 193 (3), p.251-262, Jan 1997

doi:

Keywords: Fluvial hydrosystem; Radionuclide; Sedimentation rate; Sediment organic carbon

Abstract: Former river channels are aquatic ecosystems with a different geomorphology generated by fluvial dynamics more or less linked to the main channel. They present different ecological successions to become terrestrial ecosystems and are thus supposed to have different sedimentation rates. The aim of this paper is to assess this sedimentation rate using radioactive tracer methodology commonly used in lake studies.

URL: http://www.sciencedirect.com/science/article/pii/S004896979605348X