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Data and code from: Size-resolved particle dry deposition velocities in a controlled spherical chamber: Effects of turbulence, surface complexity, and particle physicochemical properties

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Sep 25, 2026 version files 948.71 MB

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Abstract

Accurate quantification of size-resolved particle dry deposition velocities (vd) is essential for improving predictions of aerosol atmospheric lifetimes, surface contamination, and pollutant transport. Existing field measurement approaches such as eddy covariance and direct surface collection face fundamental limitations in resolving vd across the submicron size range. Here we report controlled laboratory experiments conducted in a spherical aluminum chamber (diameter 91.44 cm, volume ~0.4 m³) to systematically investigate how turbulence intensity, additional surface complexity, and particle physicochemical properties govern size-resolved vd. Deposition velocities were determined independently using two complementary methods: a chamber concentration decay method and a direct filter collection and re-atomization method. Experiments were conducted with three particle types chosen to span a range of morphological and hygroscopic properties: sodium chloride (NaCl), polystyrene latex (PSL) spheres, and black carbon (BC) aggregates. Conditions inside the sphere were maintained at low relative humidity (RH < 30%) and a fan was run at varying speeds from 0 to 1500 revolutions per minute (RPM). Key findings include: (1) turbulence exerts a strong, size-dependent influence on vd, with the viscous sublayer thickness governing the crossover between diffusion- and turbulence-controlled regimes; (2) flow-permeable objects (simulated vegetation) enhance normalized vd by a factor of 10-15 for particles smaller than 50 nm relative to the empty-chamber baseline, substantially exceeding predictions based on surface area addition alone; (3) particle morphology accounts for up to an order-of-magnitude spread in vd at a given mobility diameter, with BC fractal aggregates exhibiting morphology-driven deviations from spherical particle behavior. The filter and decay methods agree within a factor of 2 across the PSL size range tested, validating the filter collection approach as a quantitative tool. These results provide direct experimental constraints on dry deposition parameterizations used in regional and global aerosol models and motivate future deployment of analogous filter-based methods for in-situ determination of ambient particle deposition velocities.