Abstract

Samples of vegetation (vascular plants) were collected at 14 grasslands on Kunashir, Iturup, Urup and Paramushir Islands in August–September 2012. All surveyed grasslands were virgin lands with respect to Fukushima fallout. Four plots were used as pastures for cattle in 2012. About 1 kg of green vegetation (mixed grass-forb crop) was taken from each of 13 plots. Seven samples of wormwood (Artemisia sp.) and three samples of Kuril dwarf bamboo (Sasa sp.) of the same mass were collected for comparison. A density of the above ground biomass was estimated at one of the plots. Activities of134Cs and137Cs radionuclides were determined by direct γ-ray spectrometry method using HP-germanium detectors. Inventories of134Cs and137Cs in the top 20 cm layer of soil were estimated by the authors earlier for each of these 14 plots based of the soil samples analysis. Caesium-134, a marker of Fukushima fallout, was determined in 18 of 24 vegetation samples. Caesium-137 activity was quantified in all of 24 samples. The activity concentration of the radionuclides in plants (wet weight) ranged from <0.05 Bq kg−1to 1.6 Bq kg-1for134Cs and from 0.06 Bq kg−1to 5.8 Bq kg-1for137Cs. About 2/5 (median = 41%, n = 18) of the total activity of137Cs in plants was associated with the Fukushima accident. The soil-to-plant aggregated transfer coefficient (Tag) values in mixed grass-forb crop ranged from <0.2 × 10–3m2kg-1to 11 × 10–3m2kg-1for134Cs and from 0.08 × 10–3m2kg-1to 3.3 × 10–3m2kg-1for137Cs. The Tagvalues for134Cs were statistically significantly higher compared to the Tag values for 137Cs. The median Tagfor134Cs in mixed grass-forb crop decreased in the 2011–2012 period by a factor of about two: from 12 × 10–3m2kg-1to 6.6 × 10–3m2kg-1. The ecological half-time, Teco, of134Cs in the plants was approximately one year. In 2011–2012, the median Tagfor pre-Fukushima137Cs in mixed grass-forb crop was estimated as 0.12 × 10–3m2kg-1. This value is lower by a factor of 100 and 50 compared to the median values of Tagthat were deduced for Fukushima-derived radiocaesium in 2011 and 2012, respectively. The radiocaesium Tagvalues for Sasa sp. and Artemisia sp. agreed with those for mixed grass-forb crop. At grasslands with the aboveground biomass density of 1 kg m–2and the Tagof 6 × 10–3m2kg-1 for134Cs, the contribution of the vegetation contamination to total inventory of the radionuclide did not exceed 1%. For137Cs, this contribution was less than 0.1%.

Highlights

  • Vegetation cover is the first barrier interacting with radionuclides which deposited from the atmosphere on the ground surface

  • A value of Tag declines in the course of time and its dynamics can be reasonably described by single- or doubleexponential models [7, 8]

  • Caesium-134, a marker of Fukushima fallout, was estimated in 18 of 24 vegetation samples collected on Kunashir, Iturup, Urup and Paramushir Islands in August– September 2012

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Summary

Introduction

Vegetation cover is the first barrier interacting with radionuclides which deposited from the atmosphere on the ground surface. In parallel to the cleaning and diluting processes, a secondary contamination of plants occurs due to resuspension (wind erosion and rain splash) of contaminated particles deposited on the soil surface and due to the soil-to-plant transfer of radionuclides via root uptake [2, 3]. To quantify this complex interaction between fallout radionuclides and plants, the concept of the aggregated transfer coefficient, Tag, is used widely (e.g., [5, 6]). Such models can be used for: 1) evaluation of current radiation exposure from fallout when direct measurement data are scarce or not available, and 2) prediction of possible radiation doses to humans in the case of accidental radioactive contamination of the environment in the future [5, 7]

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