Long-term retention of Cs-137 in three forest soil types with different soil properties

摘要

Current Cs-137 activity concentrations were studied at three localities in individual soil horizons of Stagnosol, Arenic Podzol and Haplic Cambisol soil units in soil blocks with dimensions of 20 x 20 x 40 cm situated below pine canopies (n = 3) and spruce canopies (n = 3), and below small canopy gaps, at least 15 x 15 m in area (n = 3 + 3), which have probably endured since 1986. The main zone of Cs-137 accumulation in all the localities was found to be in the organic horizons (H and F). No significant transport and accumulation of Cs-137 into illuvial soil horizons (Bm, Bs or Bhs, Bv and Bv/IIC) was found. The estimated current total Cs-137 activity concentrations in the soil blocks 40 cm in depth were only slightly higher below the coniferous canopy than they were below nearby canopy gaps. The inventory of Cs-137 in the soils was found to be in accordance with the estimated Cs-137 inputs from the Chernobyl fallout and from global fallout. The low amounts of Cs-137 found accumulated in the above-ground biomass (mosses, grasses, needles) did not substantially bias the studied radiocaesium balance in the soils. The vertical migration rate of Cs-137 in soils (cm/year) had a tendency to be higher below canopies than below canopy gaps and below pine canopies than below spruce canopies. We expected the current Cs-137 activity concentrations in the individual soil horizons to be related to the studied soil parameters: pH (H2O), pH (CaCl2), content of organic matter and mineral portion and portion of humic and fulvic acid contents (Q(4/6)). However, this was not confirmed. Similarly, we observed a weak tendency toward higher Cs-137 activity in soils below the canopy than in soils below canopy gaps. The available gaps used in our study may have been too small, and they may have been affected by an accumulation of litter and humus containing Cs-137 from the surrounding plots situated below neighbouring canopies. 2016 Elsevier Ltd. All rights reserved.