© R.I.
Parovik1, I.A. Iljin1, P.P. Firstov2
1Kamchatka
State University by Vitus Bering, Petropavlovsk-Kamchasky,683032, Russia
2Institute of volcanology and seismology, Far East Division, RussianAcademy
of Sciences
Petropavlovsk-Kamchatsky, 683006, Russia; e-mail: [email protected]
This
paper presents a simulated model of diffusion for mass transfer
of 222Rn - emanation in alluvium deposits and in the surface
layer of the atmosphere. Analytical solutions for this model
were found by means of operational calculation. Obtained results
meet the boundary conditions of an experiment.