Abstract. Biomass burning (BB) and coal combustion (CC) are important sources of brown
carbon (BrC) in ambient aerosols. In this study, six biomass materials and
five types of coal were combusted to generate fine smoke particles. The BrC
fractions, including water-soluble organic carbon (WSOC), humic-like
substance carbon (HULIS-C), and methanol-soluble organic carbon (MSOC), were
subsequently fractionated, and their optical properties and chemical
structures were then comprehensively investigated using UV–visible
spectroscopy, proton nuclear magnetic resonance spectroscopy (1H NMR),
and fluorescence excitation–emission matrix (EEM) spectroscopy combined with
parallel factor (PARAFAC) analysis. In addition, the oxidative potential
(OP) of BB and CC BrC was measured with the dithiothreitol (DTT) method. The
results showed that WSOC, HULIS-C, and MSOC accounted for 2.3 %–22 %,
0.5 %–10 %, and 6.4 %–73 % of the total mass of combustion-derived
smoke PM2.5, respectively, with MSOC extracting the highest
concentrations of organic compounds. The MSOC fractions had the highest
light absorption capacity (mass absorption efficiency at 365 nm
(MAE365): 1.0–2.7 m2/gC) for both BB and CC smoke, indicating
that MSOC contained more of the strong light-absorbing components.
Therefore, MSOC may represent the total BrC better than the water-soluble
fractions. Some significant differences were observed between the BrC
fractions emitted from BB and CC with more water-soluble BrC fractions with
higher MAE365 and lower absorption Ångström exponent values
detected in smoke emitted from BB than from CC. EEM-PARAFAC identified four
fluorophores: two protein-like, one humic-like, and one polyphenol-like fluorophores. The
protein-like substances were the dominant components of WSOC
(47 %–80 %), HULIS-C (44 %–87 %), and MSOC (42 %–70 %). The
1H-NMR results suggested that BB BrC contained more oxygenated
aliphatic functional groups (H-C-O), whereas CC BrC contained more
unsaturated fractions (H-C-C= and Ar−H). The DTT assays indicated that BB
BrC generally had a stronger oxidative potential (DTTm, 2.6–85 pmol/min/µg) than CC BrC (DTTm, 0.4–11 pmol/min/µg), with
MSOC having a stronger OP than WSOC and HULIS-C. In addition, HULIS-C
contributed more than half of the DTT activity of WSOC (63.1 % ± 15.5 %), highlighting that HULIS was a major contributor of reactive oxygen species (ROS) production
in WSOC. Furthermore, the principal component analysis and Pearson
correlation coefficients indicated that highly oxygenated humic-like
fluorophore C4 may be the important DTT active substances in BrC.