The coordinate dependence of the ratio (6,122)J = (6) Y/(122) Y of the
radiation components of Co-57 localized in diffusion zones of polycry
stalline Au and W was examined theoretically and experimentally. Here
Y is the radiation intensity of the residual polycrystal. It is shown
that among all the known characteristics of the intercrystallite diffu
sion (ICD) the ratio (6,122)J represents a parameter, which is most se
nsitive to the type of the atomic probes profile in the diffusion zone
. The increase in the ratio (6,122)J with the depth in the diffusion z
one is a unique criterion of the Gaussian profile (for the volume diff
usion or the ICD in a single crystallite conjugation region in the 'C-
regime'). The decrease in the ratio (6,122)J with increasing depth in
the ICD zone in a polycrystal is due to the manifestation of the cryst
allite conjugation regions distribution function G(D-CCR(-1)) on the r
eciprocal values of the diffusion coefficients D-CCR(-1) in the crysta
llite conjugation region core. A complicated behavior of the ratio (6,
122)J in the diffusion zone of Co-57 in polycrystallite Au after a hig
h-temperature annealing is due to the dominance of different types of
profiles in various parts of the diffusion zone. (C) 1998 Elsevier Sci
ence B.V. All rights reserved.