Abstract

A new method, namely, force–distance curve mapping, was developed to directly measure the adhesion force of individual aerosol particles by atomic force microscopy. The proposed method collects adhesion force from multiple points on a single particle. It also takes into account the spatial distribution of the adhesion force affected by topography (e.g., the variation in the tip angle relative to the surface, as well as the force imposed upon contact), thereby enabling the direct and quantitative measurement of the adhesion force representing each particle. The topographic effect was first evaluated by measuring Polystyrene latex (PSL) standard particles, and the optimized method was then applied on atmospherically relevant model dust particles (quartz, ATD, and CJ-1) and inorganic particles (ammonium sulfate and artificial sea salt) to inter-compare the adhesion forces among different aerosol types. The method was further applied on the actual ambient aerosol particles collected on the western coast of Japan, when the region was under the influence of Asian dust plume. The ambient particles were classified into sea salt (SS), silicate dust, and Ca-rich dust particles based on individual particle analysis (micro-Raman or Scanning Electron Microscope/Energy Dispersive X-ray Spectroscopy (SEM-EDX)). Comparable adhesion forces were obtained from the model and ambient particles for both SS and silicate dust. Although dust particles tended to show smaller adhesion forces, the adhesion force of Ca-rich dust particles was larger than the majority of silicate dust particles and was comparable with the inorganic salt particles. These results highlight that the original chemical composition, as well as the aging process in the atmosphere, can create significant variation in the adhesion force among individual particles. This study demonstrates that force–distance curve mapping can be used as a new tool to quantitatively characterize the physical properties of aerosol particles on an individual basis.

Highlights

  • Aerosol particles interact with the deposition surface through their “adhesion force”, which consists of van der Waals, electrostatic, and capillary forces [1]

  • While sticky particles with larger adhesion force remain on the impaction plate, less sticky particles with smaller adhesion force tend to bounce off, which leads to a reduced collection efficiency and a source of size classification bias [2]

  • The tip loading force and surface slopes particles were found to affect the adhesion force based on the initial tests on Polystyrene latex (PSL)

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Summary

Introduction

Aerosol particles interact with the deposition surface through their “adhesion force”, which consists of van der Waals, electrostatic, and capillary forces [1]. It is a force by which particles continue to Atmosphere 2020, 11, 489; doi:10.3390/atmos11050489 www.mdpi.com/journal/atmosphere. It is closely related to the collection efficiency of particles on an impaction substrate, which is commonly used as the sampling method for offline chemical analysis. This collection method depends largely on the particle adhesion force [1]. Whether a once deposited particle detaches and re-disperses into the atmosphere (i.e., the resuspension process) depends largely on the adhesion force

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