Radioactive contamination of tropical rainforest soils in Southern Costa Rica.

Abstract Radionuclide content in soils from four locations in a tropical rainforest near Golfito in Southern Costa Rica was investigated. For comparison, two nearby locations in open grassland were also studied. From each site 5 soil cores down to a depth of 15 cm were taken. The median contamination with 137 Cs was 584 Bq m −2 (reference date 1 January 1996) and the coefficient of variation (CV) was 50%. This contamination can be attributed to global fallout from atmospheric nuclear weapon tests between 1945 and 1980. The mean contamination is slightly lower than the value expected for the latitude (8°42′: 700 Bq m −2 ), which may be explained by migration of radiocaesium to subsoil below 15 cm or by uptake into the living biomass. Out of the total variability of 50%, around 20% can be attributed to the sampling and measuring process uncertainties, thus leaving a 45% contribution of spatial variability. A significant difference between forest and meadow sites could be detected: the meadow sites showed lower radiocaesium soil inventories (median: 291 Bq m −2 ) than the forest sites (643 Bq m −2 ). This may be explained by the agricultural activities carried out on meadow sites which lead to an increased redistribution of caesium in the soil profile and therefore a larger fraction of the total 137 Cs lying below 15 cm. Another reason for higher contamination levels under forest can be attributed to the high interception potential of dense tree canopies for dry deposition. Extrapolating the 137 Cs concentration below the sampling horizon, i.e. accounting for the cut-off of the profiles by the sampling technique, results in an estimated mean of 710 Bq m −2 for the forest sites, which is very close to the expected figure. The mainly mineral part of the forest soil profiles was analysed for the 137 Cs transport parameters, apparent convection velocity ( v =0.14±0.09 cm a −1 ) and apparent diffusion constant ( D =0.79±0.49 cm 2  a −1 ). The maximum concentration can be found at 5.3±2.9 cm depth, the half-value depth being 7.4±1.3 cm. The mean 40 K activity concentration was 175 Bq kg −1 dry matter (CV=69%) and 226 Ra and 228 Ra concentrations of 9.90 Bq kg −1 (CV=23%) and 7.93 Bq kg −1 (CV=20%) have been found, respectively.