“…It was found that with respect to atmospheric transport and deposition, these aerosols can be divided into two groups: a volatile group, which includes 137 Cs, 134 Cs, 103 Ru, 131 I, 106 Ru, 132 Te and 99 Mo and a refractory group including 90 Sr, 89 Sr, 141 Ce, 144 Ce, 95 Zr, 140 Ba, 95 Nb, 240 La and 124 Sb. Measurements made in various European countries after the Chernobyl accident rather consistently showed that outside the immediate vicinity of the Chernobyl nuclear power plant, the AMAD (Activity Median Aerodynamic Diameter) of the volatile radioactive aerosols was of the order of 0.7 mm, whereas a higher AMAD value of the order of 5 mm was found for those belonging to the refractory group (Reineking et al, 1987;Tschiersch and Georgi, 1987;Rulik et al, 1989;Dorrian, 1997). The Chernobyl accident also led to high air concentrations of both iodine in aerosol form, elemental (or other inorganic) iodine and organic iodine (notably CH 3 I) (Roed, 1987).…”