Organic aerosol emitted from biomass burning absorbs
visible radiation.
However, the impact of this light absorption on the overall climate
effects of atmospheric aerosol is not well known, partly due to variability
in particle composition and absorptivity. Cinnamaldehydes, which consist
of an aromatic ring with an unsaturated aldehyde substituent, are
an important class of chromophores in light-absorbing organic aerosol,
or brown carbon. Here, light absorption by a homologous series of
three cinnamaldehydescoumaraldehyde, coniferaldehyde, and
sinapaldehydeis modeled with time-dependent density functional
theory (TD-DFT) calculations, in the gas and aqueous phases. Based
on a survey of hydration and acid dissociation equilibria, the neutral
aldehyde is expected to be the predominant form of each species in
the atmospheric aqueous phase. These species have complicated conformational
landscapes compared to many other brown carbon constituents, like
rigid polycyclic aromatic hydrocarbons. For coumaraldehyde, coniferaldehyde,
and sinapaldehyde, a total of 8, 26, and 18 conformers were located,
respectively. For each species, most of the total population is accounted
for by the four most-populated conformers. The relative contributions
of the conformers to the total light absorption of the respective
species are dictated more by differences in the relative free energies
than by differences in the molar absorption coefficients. As the functionalization
increases, the absorption is red-shifted. The peaks predicted in water
agree well with experimental spectra of coniferaldehyde and sinapaldehyde.
No conformers have vertical transitions in the visible spectral range,
so absorption above 380 nm is due to the shoulders of transitions
of major conformers at ultraviolet wavelengths. These results demonstrate
the importance of exploring potential energy landscapes, determining
conformer stability and absorptivity, to predict the light absorption
of chromophores in brown carbon.