A MODEL FOR MASS TRANSFER OF RADON (222Rn) IN THE ATMOSPHERE NEAR THE SURFACE

R.I. Parovik1, I.A. Iljin2, P.P.Firstov3

1Institute of Cosmophysical Researches and Radio Wave Propagation, Far East Division, Russian Academy of Sсiences,
Paratunka, 684034, Russia; e-mail: romano_kgu@rambler.ru
2Kamchatka State University by Vitus Bering, Petropavlovsk-Kamchatsky, 683032, Russia
3Institute of volcanology and seismology, Far East Division, Russian Academy of Sciences, Petropavlovsk-Kamchatsky, 683006, Russia

The paper presents a generalized one-dimensional model for mass transfer of radon 222Rn- emanation in alluvium deposits and the surface layer of the atmosphere. Analytical solutions for this model were found which meet the boundary conditions of an experiment and the numerical analysis is lead. Curve distributions of concentration of radon-emanation in the top part in alluvium deposits and the surface layer of the atmosphere were constructed depending on coefficients of effective diffusion and convection speeds transfer.

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