Aqueous‐Phase Secondary Processes and Meteorological Change Promote the Brown Carbon Formation and Transformation During Haze Events

Author:

Jiang Hongxing1ORCID,Cai Junjie1,Feng Xinxin1,Chen Yingjun12ORCID,Wang Lina1ORCID,Li Jun3ORCID,Tang Jiao3,Mo Yangzhi3,Zhang Xiangyun3ORCID,Zhang Gan3ORCID,Mu Yunjing4ORCID,Chen Jianmin1

Affiliation:

1. Shanghai Key Laboratory of Atmospheric Particle Pollution and Prevention (LAP3) Department of Environmental Science and Engineering Fudan University Shanghai China

2. Shanghai Institute of Pollution Control and Ecological Security Shanghai China

3. State Key Laboratory of Organic Geochemistry and Guangdong Province Key Laboratory of Environmental Protection and Resources Utilization Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou China

4. Research Centre for Eco‐Environmental Sciences Chinese Academy of Sciences Beijing China

Abstract

AbstractThe evolution and the impacts of meteorological conditions on brown carbon (BrC) absorption are not understood, which hinders the assessment of BrC radiative forcing. To address this issue, 1‐hr time‐resolved PM2.5 samples collected during three haze events in the North China Plain prior to the COVID‐19 pandemic were used to measure the optical properties of BrC. By coupling excitation‐emission matrix spectroscopy, chemical tracer analysis with multiple model analysis including positive matrix factorization (PMF) and a deweather‐random forest model, we found that a higher proportion of highly oxidized chromophoric components was present in water‐soluble BrC than in methanol‐soluble BrC, indicating the conversion of low‐oxidized water‐insoluble BrC into highly oxidized water‐soluble BrC during the day. The results of the PMF and the deweather‐random forest model showed that aqueous secondary processes were the major contributor to the BrC absorption (68% ± 38%), and the changes in meteorological conditions such as relative humidity (RH) could significantly lead to the changes in the light‐absorbing capacity of BrC, especially the enhancement for water‐soluble BrC and bleaching for methanol‐soluble BrC during the noon and afternoon. We further found that the BrC absorption capacity increased as RH increases to a maximum of ∼65%, and then decreased when RH >65%, highlighting the important role of RH in the generation of water‐soluble BrC.

Funder

National Natural Science Foundation of China

Postdoctoral Research Foundation of China

State Key Laboratory of Organic Geochemistry

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

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