Abstract

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.

Highlights

  • Soil sampling was carried out in the “Los Ratones” mine, located in the Region of Extremadura in the south-west of Spain

  • The activity concentrations of the uranium, thorium, and radium isotopes in the different soil fractions were determined by alpha-spectrometry with PIPS semiconductor detectors of 450 mm2 active area

  • The activity concentration of 210Pb was determined by liquid scintillation counting (LSC) [7]

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Summary

Study area

Soil sampling was carried out in the “Los Ratones” mine, located in the Region of Extremadura in the south-west of Spain. This installation, with an area of 2.3 km, was in production from 1960 to 1974. Afterwards, it was inactive for several years, and restoration work was performed (1998-1999). More details about the characteristics of this mine, as well as other studies of interest performed in this area are given elsewhere ([1,2,3])

Sampling and sample preparation
Radiochemical methods and measurement techniques
Results and discussion
Full Text
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