Matematičeskoe modelirovanie, Tome 3 (1991) no. 4, pp. 22-30
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A. A. Givoderov; A. N. Varaksin. Calculation of the isotope effect at the interstitials diffusion in crystals by the heating method. Matematičeskoe modelirovanie, Tome 3 (1991) no. 4, pp. 22-30. http://geodesic.mathdoc.fr/item/MM_1991_3_4_a2/
@article{MM_1991_3_4_a2,
author = {A. A. Givoderov and A. N. Varaksin},
title = {Calculation of the isotope effect at the interstitials diffusion in crystals by the heating method},
journal = {Matemati\v{c}eskoe modelirovanie},
pages = {22--30},
year = {1991},
volume = {3},
number = {4},
language = {ru},
url = {http://geodesic.mathdoc.fr/item/MM_1991_3_4_a2/}
}
TY - JOUR
AU - A. A. Givoderov
AU - A. N. Varaksin
TI - Calculation of the isotope effect at the interstitials diffusion in crystals by the heating method
JO - Matematičeskoe modelirovanie
PY - 1991
SP - 22
EP - 30
VL - 3
IS - 4
UR - http://geodesic.mathdoc.fr/item/MM_1991_3_4_a2/
LA - ru
ID - MM_1991_3_4_a2
ER -
%0 Journal Article
%A A. A. Givoderov
%A A. N. Varaksin
%T Calculation of the isotope effect at the interstitials diffusion in crystals by the heating method
%J Matematičeskoe modelirovanie
%D 1991
%P 22-30
%V 3
%N 4
%U http://geodesic.mathdoc.fr/item/MM_1991_3_4_a2/
%G ru
%F MM_1991_3_4_a2
The impurity mass dependence of the diffusion coefficient $D(m)$ was investigated by the heating method (reduced version of molecular dynamics method). It is shown that $D(m)$ has a minimum near $m\sim M$ region ($M$ is the mass of a lattice atom), if the impurity interacts with the crystal by short- range potential. The dependence $D(m)$ is monotoneous (without the extremums) for long-range potential but $D(m)$ differs from prediction of the rates theory $D(m)\sim m^{-0,5}$.