Measurement report: Particle-size-dependent fluorescence properties of water-soluble organic compounds (WSOCs) and their atmospheric implications for the aging of WSOCs

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 mu m 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 mu m. The Stokes shift (SS) and the harmonic mean of the excitation and emission wavelengths (WH) reflected that pi-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 mu m) and peaked at 0.26-0.44 mu m. All evidence supported the fact that the humification degree of WSOCs increased with particle size in the submicron mode (< 0.44 mu m) 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 mu m rather than in the < 0.26 mu m range. Synthetically analyzing three-dimensional fluorescence data could efficiently reveal the secondary transformation processes of WSOCs.

Automated summary

Water-soluble organic compounds (WSOCs) play important roles in the formation, migration, and transformation of atmospheric particles. The optical properties of WSOCs were investigated using three-dimensional fluorescence spectroscopy, providing information about their atmospheric sources. WSOC concentrations and fluorescence intensity showed different distributions in winter and summer, with the dominant size range being 0.26-0.44 μm in both seasons. The fluorescence spectra of WSOCs varied with particle size due to changing sources and/or chemical transformation. The humification degree and pi-conjugated systems of WSOCs were highest in the particle size range of 0.26-0.44 μm. Humic-like substances were abundant in fine particles (< 1 μm) and peaked at 0.26-0.44 μm. Overall, the analysis of three-dimensional fluorescence data can effectively reveal the secondary transformation processes of WSOCs.