Atmospheric inertial deposition of coarse particles has been quantified by the evaluation of particle dry deposition flux data collected simultaneously on the top and bottom surfaces of a smooth plate with a sharp leading edge that was pointed into the wind by a wind vane. The deposited particles were weighed and counted. The airborne concentration of coarse particles was measured with a Rotary Impactor. Deposition velocity was determined by dividing the mass flux (plate) by the airborne concentration (Rotary Impactor). The deposition velocity was considered to be due to gravitational settling (VST) and inertial deposition (VI). Deposition to the upper plate surface (VdU) was given by: VdU = VST + VI, while deposition to the lower plate surface (VdL) was given by: VdL = − VST + VI. The inertial deposition velocity was defined as: , where is the particle effective inertial coefficient and is friction velocity. Based on these equations, was evaluated as a function of particle size as: , where da is the particle aerodynamic diameter (μm). The correlation coefficient was 0.92, varied from 0.1 to 1.0 for particles between 5 and 100 μm diameter.
The particle dry deposition fluxes obtained for the top and bottom surfaces of the plate were extended to the free atmosphere. A particle flux ratio (FR) was defined as: . The mass median aerodynamic diameter MMDa for the atmospheric coarse particle size distribution correlated closely with the geometric mean values of (FR). The flux ratio was also related to the shape of the coarse particle mass distribution. The f