Abstract

Abstract. Black carbon aerosols play an important role in climate change because they directly absorb solar radiation. In this study, the mixing state of refractory black carbon (rBC) at an urban site in Beijing in the early summer of 2018 was studied with a single-particle soot photometer (SP2) as well as a tandem observation system with a centrifugal particle mass analyzer (CPMA) and a differential mobility analyzer (DMA). The results demonstrated that the mass-equivalent size distribution of rBC exhibited an approximately lognormal distribution with a mass median diameter (MMD) of 171 nm. When the site experienced prevailing southerly winds, the MMD of rBC increased notably, by 19 %. During the observational period, the ratio of the diameter of rBC-containing particles (Dp) to the rBC core (Dc) was 1.20 on average for Dc=180 nm, indicating that the majority of rBC particles were thinly coated. The Dp∕Dc value exhibited a clear diurnal pattern, with a maximum at 14:00 LST and a Dp growth rate of 2.3 nm h−1; higher Ox conditions increased the coating growth rate. The microphysical properties of rBC were also studied. Bare rBC particles were mostly found in fractal structures with a mass fractal dimensions (Dfm) of 2.35, with limited variation during both clean and polluted periods. The morphology of rBC changed with coating thickness increasing. When the mass ratio of nonrefractory matter to rBC (MR) was <1.5, rBC-containing particles were primarily found in external fractal structures, and they changed to a core–shell structure when MR>6, at which point the measured scattering cross section of rBC-containing particles was consistent with that based on the Mie-scattering simulation. We found that only 28 % of the rBC-containing particles were in core–shell structures with a particle mass of 10 fg in the clean period but that proportion increased considerably, to 45 %, in the polluted period. Due to the morphology change, the absorption enhancement (Eabs) was 12 % lower than that predicted for core–shell structures.

Highlights

  • Black carbon (BC) aerosol is one of the principal lightabsorbing aerosols in the atmosphere

  • By extrapolating a lognormal function fit to the observed mass distribution, we found that refractory black carbon (rBC) particles outside the detection range caused an ∼ 15 % underestimation of the rBC mass concentration

  • The mixing characteristics of rBC-containing particles were investigated in Beijing during the early summer of 2018 using a single-particle soot photometer (SP2)

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Summary

Introduction

Black carbon (BC) aerosol is one of the principal lightabsorbing aerosols in the atmosphere. BC is regarded as one of the most important components contributing to global warming (Bond et al, 2013). BC has a much shorter lifetime than CO2. BC’s radiative perturbation on a regional scale may be different from globally averaged estimates. It has been reported that BC’s direct radiative forcing can reach an order of ≥ 10 W m−2 over eastern and southern Asia (Bond et al, 2013). BC aerosols can influence the climate by altering cloud properties, such as the evaporation of cloud droplets, cloud lifetime and albedo (Ramanathan et al, 2001; Ramanathan and Carmichael, 2008)

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