Abstract

Two theoretical models are presented which allow computing the efficiency with which electrically charged aerosol particles of radius 0.001 ≤ r ≤ 10 μm are collected by electrically charged plate-like ice crystals of radius 50 ≤ a c ≤ 640 μm in air of various relative humidities and of 700 mb and −10°C. Particle capture due to thermophoresis, diffusiophoresis, Brownian diffusion, inertial impaction, and electrostatic forces is considered. It is shown that Brownian diffusion dominates the capture process by ice crystals if r ≤ 0.01 μm, while inertial impaction controls the capture process if r > 0.1 μm. For aerosol particles of 0.01 ≤ r ≤ 0.1 μm, the collection efficiency is controlled by phoretic forces. Electrical forces significantly affect the collection of aerosol particles in the size range of 0.01 ≤ r ≤ 5 μm. Trajectory analysis demonstrates that electrically charged and uncharged aerosol particles are preferentially captured at the rim of plate-like ice crystals. Electrically neutral ice crystals of N Re < 50 capture particles only on the underside of the ice crystal. Ice crystals which are electrically charged collect aerosol particles by rear capture if N Re ≤ 0.5.

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