4.6 Article

Beyond size classification: The dynamic-aerosol-size electrical mobility spectrometer

Journal

JOURNAL OF AEROSOL SCIENCE
Volume 170, Issue -, Pages -

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.jaerosci.2023.106141

Keywords

Aerosol instrumentation; Dynamic -aerosol -size EMS; Particle growth; shrinkage process; Particle evaporation

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This paper presents a new operation mode of the Electrical Mobility Spectrometer (EMS), called the Dynamic-aerosol-size Electrical Mobility Spectrometer (DEMS), which allows the aerosol particles to change their size during mobility classification in response to chemical/physical processes in the classification region. Unlike traditional EMS, DEMS focuses on probing the kinetics of aerosol-related processes rather than classifying the particle size. A theoretical framework is developed to analyze the transmission of size-changing particles in the classification region, and the validity of the framework is demonstrated through simulations and experiments.
This paper overviews an alternative operation mode of the Electrical Mobility Spectrometer (EMS), herein termed as the Dynamic-aerosol-size Electrical Mobility Spectrometer (DEMS) where the size of aerosol particles evolves during mobility classification in response to any chemical/physical processes taking place within the device's classification region. Unlike the conventional EMS designed to classify the aerosol particle size, the function of the DEMS is to probe the kinetics (in terms of corresponding growth/shrinkage rates) of aerosol related chemi-cal/physical processes. This is achievable because the particle trajectory in the device's classifi-cation region contains full information about the particle size change history. A theoretical framework is developed for analyzing the transmission of size-changing particles in the device's classification region. Expressions for the particle mobility at the device outlet and size change rate are derived based on known initial mobility and DEMS response, using the evaporation of monodisperse and single-component aerosols as an example. The theoretical framework is applicable to the entire Knudsen number range and is compared against simulations and exper-iments, demonstrating excellent validity in the test conditions.

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