Vertical distribution of natural radionuclides in soils
P. Blanco Rodríguez1, F. Vera Tomé1* and J. C. Lozano2
1 Natural Radioactivity Group, Universidad de Extremadura Avd. Elvas s/n, 06071 Badajoz, Spain
2 Laboratorio de Radiaciones Ionizantes, Facultad de Ciencias Universidad de Salamanca - 37008, Salamanca Spain
* E-mail: firstname.lastname@example.org
Published online: 04 April 2012
Low-level alpha spectrometry techniques using semiconductor detectors (PIPS) and liquid scintillation counters (LKB Quantulus 1220™) were used in order to determine the activity concentration of 238U, 232Th, 234U, 230Th, 226Ra, and 210Pb in soil samples. The soils were collected from an old disused uranium mine located in southwest Spain. The soils were selected with different levels of influence from the installation, in such a way that they had different levels of radioactive contamination. The vertical profiles in the soils (down to 40 cm depth) were studied in order to evaluate the vertical distribution of the natural radionuclides. The possible contamination of subsurface waters depends strongly on vertical migration, and the transfer to plants (herbs, shrubs, and trees) also will depend on the distribution of the radionuclides in the root zone. The study of the activity ratios between radionuclides belonging to the same series allowed us to assess the differing behaviour of the radionuclides involved. The vertical profiles for these radionuclides were different at each sampling point, showing the local impact of the installation. However, the profiles per point were similar for the long-lived radionuclides of the 238TJ series (238U, 234U, 230Th, and 226Ra). Also, a major disequilibrium was observed between 210Pb and 226Ra in the surface layer, due to 222Rn emanation and subsequent surface deposition of 210Pb.
© Owned by the authors, published by EDP Sciences - SIF 2012