327-344
The Influence of Soil Physical and Chemical Characteristics on Bioavailability of 60Co
Authors: Vyacheslav S. Anisimov, Dmitry V. Dikarev, Lidia N. Anisimova, Yury N. Korneev, Ilja V. Kochetkov
Number of views: 562
Based on the study of the relationships between the physico-chemical characteristics of different mineral soils that have previously spiked with the same amounts of 60Co, and the uptake of this radionuclide in the above-ground parts of test plants, there were estimated the abilities of the soils to limit the mobility of the radionuclide in the soil – plant system (soils inactivating abilities – SIA). To evaluate the latter in relation to 60Co, the model vegetation pot experiment was carried out in controlled conditions, using as test plant barley (Hordeum vulgare L.). With the aim of providing a wide range of variation of the studied physico-chemical parameters, there were selected soil samples from arable and humus-accumulative horizons of the 16 types, species and varieties of soils belonging to different climatic zones of the European part of the Russian Federation in the quantities sufficient for the determination of physical and chemical characteristics of the soils and for the vegetation experiment conducting. Based on the obtained experimental results the effect of each of the selected indicators of soil condition on the radionuclide uptake by test plants was determined. To do this, the methods of principal components and multiple regression analysis were used. At first, the independent variables (physical and chemical indicators of soil condition), which, as supposed, rendered the influence on the uptake of 60Co by plants were selected with use the principal components method. Further, on the basis of private correlation coefficients, calculated using the linear regression model, the contribution of soil characteristics in SIA was estimated and their ranking was produced. Directly the values of the SIA in relation to the investigated radionuclide, expressed in scores, for each soil were calculated as the sum of products of contributions corresponding soil characteristics in the variation of resultant (concentration ratio – CR 60Co) on a dimensionless quantity, equal to the difference between the specific and minimum values of the soil characteristics (variables) in the sampling to the scale of variation of the relevant variables in the sampling.