Black
carbon (BC) from fuel combustion is an effective light absorber
that contributes significantly to direct climate forcing. The forcing
is altered when BC combines with other substances, which modify its
mixing state and morphology, making the evaluation of its atmospheric
lifetime and climate impact a challenge. To elucidate the associated
mechanisms, we exposed BC aerosol to supersaturated vapors of different
chemicals to form thin coatings and measured the coating mass required
to induce the restructuring of BC aggregates. We found that studied
chemicals fall into two distinct groups based on a single dimensionless
parameter, χ, which depends on the diameter of BC monomer spheres
and the coating material properties, including vapor supersaturation,
molar volume, and surface tension. We show that when χ is small
(low-volatility chemicals), the highly supersaturated vapor condenses
uniformly over aggregates, including convex monomers and concave junctions
in between monomers, but when χ is large (intermediate-volatility
chemicals), junctions become preferred. The aggregates undergo prompt
restructuring when condensation in the junctions dominates over condensation
on monomer spheres. For a given monomer diameter, the coating distribution
is mostly controlled by vapor supersaturation. The χ factor
can be incorporated straightforwardly into atmospheric models to improve
simulations of BC aging.