Fuel particles released during the accident at the Chernobyl reactor (
1986) and during the operation at the Windscale (UK) pile (1952-57) we
re investigated with respect to structure using scanning electron micr
oscopy and composition using X-ray microanalysis and gamma-, beta- and
alpha-spectrometry. Particles from Chernobyl released at a relatively
high temperature-have in general a compact crystalline-like structure
with a relatively uniform surface layer of uranium. Aggregates consis
ting of small-sized (1-2 mu m) spherical uranium granulates were also
identified. These granulates were similar to particles identified in N
orway. About 25% of the particles investigated were covered by lead, w
hich is attributed to a release during the last stage of the accident.
Particles from Windscale released under low-temperature conditions ha
ve a flake-like layered structure, varying in size (10-250 mu m) and a
ctivity levels. Thus the travelling distance for these particles may b
e substantially longer than previously anticipated for spheres. The su
rfaces of these particles were also composed of uranium. The mobility
of radionuclides associated with fuel particles of different structure
is believed at least initially to be low when compared with those ass
ociated with condensed particles or with ionic tracers. However, mobil
ization of especially Sr-90 due to weathering of hot particles should
be expected in the years to come.