Measurement report: Particle-size-dependent fluorescence properties of water-soluble organic compounds (WSOCs) and their atmospheric implications for the aging of WSOCs
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Published:2022-01-13
Issue:1
Volume:22
Page:465-479
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ISSN:1680-7324
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Container-title:Atmospheric Chemistry and Physics
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language:en
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Short-container-title:Atmos. Chem. Phys.
Author:
Qin Juanjuan, Tan Jihua, Zhou Xueming, Yang Yanrong, Qin Yuanyuan, Wang Xiaobo, Shi Shaoxuan, Xiao Kang, Wang XinmingORCID
Abstract
Abstract. Water-soluble organic compounds (WSOCs) play important roles in atmospheric particle formation, migration, and transformation
processes. Size-segregated atmospheric particles were collected in a rural area of Beijing. Three-dimensional fluorescence spectroscopy was used to
investigate the optical properties of WSOCs as a means of inferring information about their atmospheric sources. Sophisticated analysis on
fluorescence data was performed to characteristically estimate the connections among particles of different sizes. WSOC concentrations and the average
fluorescence intensity (AFI) showed a monomodal distribution in winter and a bimodal distribution in summer, with the dominant mode in the
0.26–0.44 µm size range in both seasons. The excitation–emission matrix (EEM) spectra of WSOCs varied with particle size, likely due to
changing sources and/or the chemical transformation of organics. Size distributions of the fluorescence regional integration (regions III and V) and
humification index (HIX) indicate that the humification degree or aromaticity of WSOCs was the highest in the particle size range of
0.26–0.44 µm. The Stokes shift (SS) and the harmonic mean of the excitation and emission wavelengths (WH) reflected that
π-conjugated systems were high in the same particle size range. The parallel factor analysis (PARAFAC) results showed that humic-like substances
were abundant in fine particles (< 1 µm) and peaked at 0.26–0.44 µm. All evidence supported the fact that the humification
degree of WSOCs increased with particle size in the submicron mode (< 0.44 µm) and then decreased gradually with particle size, which
implied that the condensation of organics occurred in submicron particles, resulting in the highest degree of humification in the particle size range of
0.26–0.44 µm rather than in the < 0.26 µm range. Synthetically analyzing three-dimensional fluorescence data could efficiently reveal
the secondary transformation processes of WSOCs.
Funder
National Natural Science Foundation of China
Publisher
Copernicus GmbH
Subject
Atmospheric Science
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