A large amount of radioiodine isotopes (mainly
131I, t
1/2 = 8 days) was released from the accident at Chernobyl Nuclear Power Plant (CNPP) in April-May 1986. An increase in childhood-thyroid cancer in the contaminated areas in Belarus, Russia and the Ukraine was demonstrated to be caused by radioiodine released at the time of the accident. However, there is a lack of quantitative data on the
131I levels in the local environment (e.g. air, plant, soil). At this point, a long-lived iodine isotope,
129I (t
1/2 = 15.7 million years), also released with a certain ratio to
131I from CNPP, could be used for estimating the
131I levels in the environment. In this paper we present analytical results of the
129I concentrations and
129I/
127I atom ratios in soil samples collected from the CNPP exclusion zone (30-km zone), with the aim of assessing current contamination levels and distribution patterns. For the analysis of the iodine fraction in the investigated soil samples, the pyrohydrolysis method was utilized for separation of
127I and
129I nuclides, and subsequently their concentration was determined using inductively coupled plasma mass spectrometry (ICP-MS) and accelerator mass spectrometry (AMS), respectively. The concentration of
129I and the
129I/
127I atom ratio in the surface soil samples in the 30 km-zone of CNPP ranged from 4.6 to 170 mBq/kg, and from 1.4 × 10
-6 to 13 × 10
-6, respectively. These values are significantly higher than those from global
129I fallout, indicating that most of the measured
129I was due to the deposition of the accident. Stable iodine concentrations in this area were found to be very low (below 1 ppm) for most of the samples, suggesting the environmental iodine levels in this area to be potentially low. The
129I/
137Cs activity ratio in surface and sub-surface soils was not so constant, i.e., in the range (7.3-20.2) × 10
-7. This might be due to the different behavior of deposition and/or migration of these nuclides in soil. These results suggest the obtained data of
129I to be useful for the reconstruction of the
131I deposition in the contaminated areas.
View full abstract