Evaluation of 137Cs soil-to-plant transfer: Natural and model experiments

Estimation of rooting depth of 137Cs uptake by plants

Understanding the soil-to-plant transfer process of ¹³⁷Cs is essential for predicting the contamination levels of plants in contaminated areas. The rooting depth is considered one of the key factors explaining the difference in the activity concentration of ¹³⁷Cs in different plant species. In this study, the distributions of ¹³⁷Cs and ¹³³Cs in soils and plants were investigated, and the plants' rooting depth of ¹³⁷Cs uptake was estimated using the ¹³⁷Cs/¹³³Cs ratios in exchangeable fractions of soils and biological samples. The results showed that different plant species accumulate different levels of ¹³⁷Cs and ¹³³Cs. The ¹³⁷Cs/¹³³Cs ratios were fairly constant in plants of the same species. The average ¹³⁷Cs/¹³³Cs ratios in bamboo grasses and ferns were 0.015 ± 0.009 (n = 5) and 0.13 ± 0.04 Bq ng^-1 (n = 10) in Yamakiya, respectively. The percentage of ¹³⁷Cs in the exchangeable fraction of the uppermost soil layer was lower than that in the deeper soil layers. The activity concentrations of ¹³⁷Cs in the soil profiles decreased sharply with depth, whereas the depth distributions of ¹³³Cs were uniform. Therefore, the ¹³⁷Cs/¹³³Cs ratios were driven mainly by the ¹³⁷Cs activity concentrations in soil. The plants' rooting depths of ¹³⁷Cs uptake were estimated on the basis of the relationships between the averaged ¹³⁷Cs/¹³³Cs ratio in the soil layer and the ¹³⁷Cs/¹³³Cs ratio in the plant. The results indicate that the deeper-rooted species such as bamboo grasses have a lower accumulation of ¹³⁷Cs than the superficial-rooting species such as ferns. The soil-to-plant transfer factors would be determined using rooting depth by calculating the averaged activity concentration of ¹³⁷Cs within the estimated rooting depth.

Accumulation and transfer of 137Cs and 90Sr in the plants of the forest ecosystem near the Ignalina Nuclear Power Plant

The radioecological state of the forest ecosystem in the vicinity of the Ignalina Power Plant prior to decommissioning was analysed with specific emphasis on (137)Cs and (90)Sr activity concentrations in plant species growing in two reference sampling sites (Tilze and Grikiniskes). In the period of 1996-2008 the mean contamination of plants with (137)Cs was from 45 to 119 Bq/kg and with (90)Sr - from 3 to 42 Bq/kg. Measured (137)Cs TF values for soil-root transfer mainly ranged between 1.0-1.4, except for Calamagrostis arundinacea which had a TF value of 0.1. On average, the (137)Cs TF value from root to shoot was 1.7 fold higher than for soil to root transfer. (90)Sr TF values (soil-root) were in the range of 1.2-1.8 but for Calluna vulgaris it was 0.2. The mean root to shoot TF value for (90)Sr was 7.7 fold higher. These results indicate the higher (90)Sr bioavailability than that of (137)Cs in the forested area. The Grikiniskes reference site is located nearby the Ignalina NPP, specifically the heated water outlet channel, which results in altered microclimatic conditions. These specific microclimatic conditions result in relationships between (137)Cs TF (soil-root) values and pH, moisture and organic matter content in the soil at Grikiniskes which appear to be different to those at the Tilze reference sampling site.