Activity concentration profiles of the short-lived radon isotope Rn-220 (ha
lf-life 56 seconds) in the lowest 50 cm above the soil are used to study ne
ar-surface gas transport processes. The experimental data are compared to p
rofiles calculated by solving the one-dimensional diffusion equation for ra
dioactive atoms with a linear increase of the eddy diffusion coefficient K
with altitude according to K(z) = K-0 + K(z)z. The slope K-z in this model
and the radon nux from the surface are continuously calculated from the act
ivity measurements in time steps of one hour. Transport times for Rn atoms
from an altitude z(1) = 5 cm to an altitude z(2) = 20 cm are typically betw
een one and two minutes in stable meteorological conditions when the fricti
on velocity u* is below 0.1 m/s.