Abstract

In this study, the source-based optical properties of polydisperse carbonaceous aerosols were determined from PM2.5 concentrations measured at a Global Atmospheric Watch station in South Korea. The extinction and absorption coefficients of carbonaceous aerosols were calculated using the Mie theory and assuming a lognormal size distribution. Based on the mass concentration from the EPA’s Positive Matrix Factorization (PMF) receptor model, which considers five source identification and apportionment factors (biogenic source, local biomass burning, secondary organic aerosol, transported biomass burning, and mixed sources), the source-based size-resolved mass extinction and absorption efficiencies were estimated for each source using a multilinear regression model. The results show that the source-based optical properties depend on the aerosol size and physicochemical characteristics of the chemical compounds. The long-range transport of biomass burning (LBB) aerosol, which has a mass concentration of 20%, holds a 12.1–23.1% total extinction efficiency—depending on the size and refractive index—in the range of 0.1–0.5 μm in geometric mean diameter and humic-like substances (HULIS) imaginary refractive index of 0.006–0.3. Biogenic sources of aerosols with small diameters have higher mass absorption efficiencies (MAE) than other sources, depending on the size and refractive index.

Highlights

  • An organic aerosol is either directly emitted in particulate form or generated in the air [4]

  • Organic aerosols can be divided into water-soluble organic carbon and water-insoluble organic carbon

  • Humic-like substances account for a substantial fraction of the water-soluble organic carbon

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Summary

Introduction

Carbonaceous aerosols are composed of organic aerosols and refractory light-absorbing components, generally referred to as elemental carbon or black carbon [1]. The organic aerosols originate from both anthropogenic sources, such as fossil fuel combustion, and biogenic sources. Organic aerosols can be divided into water-soluble organic carbon and water-insoluble organic carbon. Humic-like substances account for a substantial fraction of the water-soluble organic carbon. The results of several studies have showed that the imaginary refractive index of absorbing aerosols, such as humic-like substances and brown carbon, is much higher and its contribution to absorption may be important [5,6,7,8,9,10]. One of the goals of the GAW station is to monitor the variations in components that might affect climate change

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