Abstract
The accurate measurement of aerosol particles and clusters smaller than 3 nm in diameter is crucial for the understanding of new particle formation processes. The particle counters used for measuring these particles are typically calibrated with metal or salt particles under dry conditions, which does not always represent the field conditions where these instruments are later used. In this study, we calibrated the A11 nano Condensation Nucleus Counter (nCNC), consisting of the PSM (Particle Size Magnifier) and a laminar flow butanol based CPC (Condensational Particle Counter), with well-defined biogenic oxidation products from β-caryophyllene oxidation and compared it to a calibration with tungsten oxide under the same conditions. The organic particles were detected less efficiently than the inorganic ones. This resulted in a higher cut-off size for β-caryophyllene oxidation products than for tungsten oxide. At the same PSM settings, the cut-off size for tungsten oxide was 1.2 nm and for β-caryophyllene oxidation products 1.9 nm. However, repeating the calibration of the biogenic particles at 13% relative humidity at 31°C, increased their detection efficiency in the PSM, increasing the cut-off diameter to 1.6 nm.Additionally, we present a comparison of the ion concentrations measured with the PSM and the NAIS (Neutral Cluster and Air Ion Spectrometer) during new particle formation experiments in the CLOUD (Cosmics Leaving Outdoors Droplets) chamber. In these experiments, we produced particles from different organic precursors, such as α-pinene, β-caryophyllene and isoprene, as well as iodine. This way, we could determine the shift in cut-off diameter of the PSM for several different atmospherically relevant chemical compounds and compare it to the laboratory calibrations. We saw a diameter shift for the organic precursors of +0.3 nm in the PSM compared to the NAIS. These two approaches agreed well with each other and show that it is important to know the chemical composition of the measured particles to determine the exact size distribution using a supersaturation scanning method.
Highlights
Atmospheric aerosol particles can cause human health deterioration
Tungsten oxide particles are detected with a higher detection efficiency than BCY oxidation products at the same settings, especially in sizes smaller than 1.7 nm, where the activation probability of organic particles drops quickly
We characterised the particle size magnifiers (PSM) with atmospherically relevant organic particles and determined the shift of the cut-off size relative to the standard calibration done with tungsten oxide
Summary
Atmospheric aerosol particles can cause human health deterioration (K.-H. Kim et al, 2015) and significantly impact the global climate directly by scattering the sunlight and indirectly by affecting cloud formation (Albrecht, 1989; Bauer et al, 2012). While some aerosol particles are directly emitted from sources such as biomass burning, volcanoes or sea spray, most aerosol particles are created in the atmosphere due to clustering of vapour molecules (Merikanto et al, 2009). These clusters will grow by condensation and form aerosol particles. This process is called new particle formation (Kulmala et al, 2013). Accurate measurements of ultrafine particles in the size range between 1 and 10 nm are essential for a detailed understanding of this process and quantifying the new particle formation rate and growth rates (Kulmala et al, 2012). Quantitative measurements in this size range remain a challenge (Kangasluoma et al, 2020)
Sign-in/Register to view highlights & summary Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
