The dry deposition velocity of fine particles is usually on the order of se
veral tenths of cm s(-1), and accordingly, the concentration gradient of pa
rticles above the surface is very small. This makes the application of the
gradient method to the determination of the particle deposition velocity ve
ry difficult. This study is a trial to find a way around this difficulty. T
he idea is to evaluate the thickness of the molecular diffusion layer, zb b
y simultaneously measuring the concentration gradient of gaseous species su
ch as SO2; zb is obtained by combining the turbulent and molecular transpor
t equations for the gas. Then the particle deposition velocity is estimated
oil the basis of zb and the Brownian diffusion coefficient with an assumpt
ion that zb is equal to the thickness of the Brownian diffusion layer. By a
pplying this method to the data collected in a field observation, the veloc
ity of deposition onto a cropland was estimated for submicron particles.