Effects of volatile organic compounds and new particle formation on real-time hygroscopicity of PM 2.5 particles in Seosan, Republic of Korea

The hygroscopicity of PM particles plays an important role in PM haze in Northeast Asian countries by influencing particle growth and chemical composition. New particle formation (NPF) and atmospheric volatile organic compounds (VOCs) are factors that influence particle hygroscopicity. However, the...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:The Science of the total environment 2024-03, p.171516
Hauptverfasser: Kim, Jeongbeen, Ha, Yoonkyeong, Cho, Kyungil, Lee, Soodong, Jung, Jinsang, Lee, Seung-Bok, Lee, Ji Yi, Song, Mijung, Jang, Kyoung-Soon, Lee, Kwangyul, Ahn, Junyoung, Kim, Changhyuk
Format: Artikel
Sprache:eng
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:The hygroscopicity of PM particles plays an important role in PM haze in Northeast Asian countries by influencing particle growth and chemical composition. New particle formation (NPF) and atmospheric volatile organic compounds (VOCs) are factors that influence particle hygroscopicity. However, the lack of real-time hygroscopicity measurements has deterred the understanding of their effects on particle hygroscopicity. In this study, two intensive monitoring campaigns were conducted during the summer of 2021 and spring of 2022 using real-time aerosol instruments, including a humidified tandem differential mobility analyzer (HTDMA), in Seosan, Republic of Korea. The hygroscopicity parameter κ was calculated from the real-time HTDMA measurement data (κ ). The diurnal variations in κ exhibited strong inverse linear correlations with the total concentration of VOCs (C ) during the two campaigns. The higher atmospheric C in summer increased the growth rate of the particle diameter from 10 to 40 nm (6 nm/h) compared with that in spring (2.7 nm/h), resulting in a faster change in κ for 40-nm particles in summer than in spring because of the increase in organic matter in the chemical compositions of particles. In addition, NPF events introduced additional tiny fresh particles into the atmosphere, which reduced the κ of 40-nm particles and increased the intensity of the less hygroscopic peaks (κ   0.2) measured in Beijing and Guangzhou, but those for 100-nm particles were close to those measured in the two cities.
ISSN:1879-1026