Light-absorbing organic aerosol,
or brown carbon (BrC), has significant
but poorly constrained effects on climate. A large fraction of the
absorptivity of ambient BrC is unassigned, and organic charge-transfer
(CT) complexes have the potential to contribute to this fraction.
Here, the contributions of CT complexes to the absorptivity of laboratory-generated
BrC and ambient aerosol material influenced by biomass burning have
been investigated, using a wide range of chemical, spectroscopic,
and physical analyses. Chemical functionalization experiments are
inconclusive about the role of CT complexes, whereas fluorescence
spectra exhibit distinct spectral features indicative of individual
chromophores. Determinations of the concentration and temperature
dependences of absorbance are more conclusive. In particular, for
laboratory-generated BrC extracted in either water or methanol, absorbance
scaled linearly with orders-of-magnitude changes in concentration,
indicating that intermolecular complexes do not contribute to the
absorptivity. Furthermore, whereas the absorbance of BrC extracts
in dimethyl sulfoxide exhibited a slight temperature dependence, consistent
with a 15% contribution from intramolecular CT complexes at 15 °C,
the complete temperature independence of absorbance of water-soluble
extracts from surrogate and ambient BrC indicates a negligible role
for CT complexes. Overall, our results find little evidence for CT
complexes in the primary BrC studied, suggesting that they do not
contribute significantly to the missing absorptivity of ambient BrC.