Issue 2, 2023

Exploring condensable organic vapors and their co-occurrence with PM2.5 and O3 in winter in Eastern China

Abstract

Oxygenated organic molecules (OOMs) are important oxidation products of volatile organic compounds (VOCs), and they act as key condensable vapors for new particle formation (NPF) and secondary organic aerosol (SOA) in the atmosphere. However, the large diversity and extremely low concentration make OOMs unmeasurable by conventional means, resulting in a poor understanding of OOMs, especially their formation. Herein, we observed OOMs with state-of-the-art mass spectrometry in a megacity in eastern China during the winter and characterized them by performing positive matrix factorization on binned mass spectra (binPMF). The binPMF analysis revealed 3 factors with clear precursor profiles (1 aromatic and 2 aliphatics), 2 ozone-related factors, 2 mixed-precursor-derived factors with unclear processes, and 4 factors dominated by nitrated phenols. We performed peak assignment on binPMF factors and identified over 1500 molecules with a mean total concentration of 4.7 × 107 molecules per cm3 with all nitrated phenols excluded. Most OOMs are organic nitrates produced by the oxidation of anthropogenic VOC with interactions between the derived RO2 and NOx. These molecules containing 3 to 7 effective oxygen atoms (excluding –NO2 in the nitrate moiety) introduced by autoxidation and multigenerational oxidation are less volatile, and hence, are susceptible to condensational loss. However, the observed OOM concentrations increase with the buildup of PM2.5. This can be explained by enhanced OOM photochemical production owing to accumulated VOCs and sustained oxidants that outcompete condensational loss. This suggests favored SOA production via OOM condensation during haze. Furthermore, the highest OOM concentrations occur when PM2.5 and O3 are coenhanced. Under this condition, OOMs mainly come from ozone-related factors that are generated jointly with ozone and from aliphatic-dominated factors that are closely associated with PM2.5. Overall, our results improve the understanding of OOM formation and its impact on the polluted atmosphere.

Graphical abstract: Exploring condensable organic vapors and their co-occurrence with PM2.5 and O3 in winter in Eastern China

Supplementary files

Article information

Article type
Paper
Submitted
30 out 2022
Accepted
04 jan 2023
First published
06 jan 2023
This article is Open Access
Creative Commons BY-NC license

Environ. Sci.: Atmos., 2023,3, 282-297

Exploring condensable organic vapors and their co-occurrence with PM2.5 and O3 in winter in Eastern China

Y. Liu, C. Liu, W. Nie, Y. Li, D. Ge, L. Chen, C. Zhu, L. Wang, Y. Zhang, T. Liu, X. Qi, J. Wang, D. Huang, Z. Wang, C. Yan, X. Chi and A. Ding, Environ. Sci.: Atmos., 2023, 3, 282 DOI: 10.1039/D2EA00143H

This article is licensed under a Creative Commons Attribution-NonCommercial 3.0 Unported Licence. You can use material from this article in other publications, without requesting further permission from the RSC, provided that the correct acknowledgement is given and it is not used for commercial purposes.

To request permission to reproduce material from this article in a commercial publication, please go to the Copyright Clearance Center request page.

If you are an author contributing to an RSC publication, you do not need to request permission provided correct acknowledgement is given.

If you are the author of this article, you do not need to request permission to reproduce figures and diagrams provided correct acknowledgement is given. If you want to reproduce the whole article in a third-party commercial publication (excluding your thesis/dissertation for which permission is not required) please go to the Copyright Clearance Center request page.

Read more about how to correctly acknowledge RSC content.

Social activity

Spotlight

Advertisements