Forty-eight soil profiles down to a depth of 40 cm were taken in Russia and Ukraine in 1995 and 1997, re spectively, in order to investigate the feasibility of retrospective dosimetry of the 131I exposure after the Chernobyl accident via the long-lived 129I. The sampling sites covered areas almost not affected by fallout from the Chernobyl accident such as Moscow/Russia and the Zhitomir district in Ukraine as well as the highly contaminated Korosten and Narodici districts in Ukraine. 129I was analyzed by radiochemical neutron activation analysis (RNAA) and accelerator mass spectrometry (AMS). 127I was measured for some profiles by RNAA or ion chromatography. The results for 127I demonstrated large differences in the capabilities of the soils to store iodine over long time-spans. The depth profiles of I and of Cs showed large differences in the migration behavior between the two nuclides but also for each nuclide among the different sampling sites. Though it cannot be quantified how much I and Cs was lost out of the soil columns into deeper depths, the inventories in the columns were taken as proxies for the total inventories. For 129I, these invento ries were at least three orders of magnitude higher than a pre-nuclear value of 0.084 ± 0.017 mBq m-2 de rived from a soil profile taken in 1939 in Lutovinovo/Russia. From the samples from Moscow and Zhitomir a pre-Chernobyl I inventory of (44 ± 24) mBq m" was determined, limiting the feasibility of I retrospec tive dosimetry to areas where the I inventories exceed 100 mBq m . Higher average I inventories in the Korosten and Narodici districts of 130 mBq m-2 and 848 mBq m-2, respectively, allowed determination of the I fallout due to the Chernobyl accident. Based on the total I inventories and on literature data for the atomic ratio of I/ I = 13.6 ± 2.8 for the Chernobyl emissions and on aggregated dose coefficients for I, the thyroid exposure due to 131I after the Chernobyl accident was estimated for the inhabitants of 4 villages in the Korosten and of 3 villages in the Narodici districts. The limitations and uncertainties of the 129I retrospec tive dosimetry are discussed.2

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The paper gives averages of 137Cs deposition densities in soils from three areas in Northern Ukraine measured 12 to 15 y following the Chernobyl accident: in an area near Narodici (75 km west of the Chernobyl nuclear power plant in the so-called zone II) heavily contaminated by the Chernobyl fall-out and in areas around Korosten and Zhitomir showing contamination levels to be much lower. The three areas exhibited very different 137Cs deposition densities of 2.2 MBq m(-2), 400 kBq m(-2), and 5 kBq m(-2), respectively. During a 1-y observation, measurements of the 137Cs transfer in the food chain to humans and 137Cs whole body contents dependent on the 137Cs daily intake were carried out under realistic conditions of the rural inhabitants who lived in settlements within zone II. Detailed investigations of components of the daily diet showed that the high 137Cs contamination levels found in soils of zone II do not affect in any way low 137Cs concentrations of all important agricultural products harvested and consumed by villagers. With regard to consumption habits of the population of zone II, mushrooms and wild berries were found to contribute more than 95% of the 137Cs daily intake to the 137Cs whole body content of about 12 kBq (with maximum values up to 760 kBq) measured in a group of inhabitants of zone II during a period from July 1998 to July 1999. The median of the annual dose of these inhabitants from external and internal exposures was 1.2 mSv y(-1) with a geometric standard deviation of 2.6. Excluding extreme habits, the geometric mean of the total exposure was 1.0 mSv y(-1) with a geometric standard deviation of 1.3.