Concurrent photochemical whitening and darkening of ambient brown carbon
Chemistry
13. Climate action
Physics
QC1-999
QD1-999
01 natural sciences
0105 earth and related environmental sciences
DOI:
10.5194/acp-23-9439-2023
Publication Date:
2023-08-25T13:32:56Z
AUTHORS (14)
ABSTRACT
Abstract. The light-absorbing organic aerosol (OA), known as brown
carbon (BrC), has important radiative impacts; however, its sources and
evolution after emission remain to be elucidated. In this study, the light
absorption at multiple wavelengths, mass spectra of OA and microphysical
properties of black carbon (BC) were characterized at a typical suburban
environment in Beijing. The absorption of BC is constrained by its size
distribution and mixing state, and the BrC absorption is obtained by
subtracting the BC absorption from the total aerosol absorption. Aerosol
absorption was further apportioned to BC, primary BrC and secondary BrC by
applying the least correlation between secondary BrC and BC. The
multilinear regression analysis on the factorized OA mass spectra indicated that the OA from traffic and biomass burning emission contributed to primary BrC. Importantly, the moderately oxygenated OA (O / C = 0.62) was revealed to
highly correlate with secondary BrC. These OA had higher nitrogen content,
in line with the nitrogen-containing functional groups detected by the
Fourier transform infrared spectrometer. The photochemical processes were
found to reduce the mass absorption cross section (MAC) of primary OA,
reducing its contribution to total absorption by 20 %, at the same time
increasing MAC for secondary OA, which showed a 30 % enhancement in
contribution to total absorbance, implying the concurrent whitening and
darkening of BrC. This provides field evidence that the photochemically
produced secondary nitrogen-containing OA can considerably compensate for some
bleaching effect on the primary BrC, hereby causing radiative impacts.
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