Abstract

Abstract. Humic-like substances (HULIS) in smoke fine particulate matter (PM2.5) emitted from the combustion of biomass materials (rice straw, corn straw, and pine branch) and fossil fuels (lignite coal and diesel fuel) were comprehensively studied in this work. The HULIS fractions were first isolated with a one-step solid-phase extraction method, and were then investigated with a series of analytical techniques: elemental analysis, total organic carbon analysis, UV–vis (ultraviolet–visible) spectroscopy, excitation–emission matrix (EEM) fluorescence spectroscopy, Fourier transform infrared spectroscopy, and 1H-nuclear magnetic resonance spectroscopy. The results show that HULIS account for 11.2–23.4 and 5.3 % of PM2.5 emitted from biomass burning (BB) and coal combustion, respectively. In addition, contributions of HULIS-C to total carbon and water-soluble carbon in smoke PM2.5 emitted from BB are 8.0–21.7 and 56.9–66.1 %, respectively. The corresponding contributions in smoke PM2.5 from coal combustion are 5.2 and 45.5 %, respectively. These results suggest that BB and coal combustion are both important sources of HULIS in atmospheric aerosols. However, HULIS in diesel soot only accounted for ∼ 0.8 % of the soot particles, suggesting that vehicular exhaust may not be a significant primary source of HULIS. Primary HULIS and atmospheric HULIS display many similar chemical characteristics, as indicated by the instrumental analytical characterization, while some distinct features were also apparent. A high spectral absorbance in the UV–vis spectra, a distinct band at λex∕λem ≈ 280∕350 nm in EEM spectra, lower H ∕ C and O ∕ C molar ratios, and a high content of [Ar–H] were observed for primary HULIS. These results suggest that primary HULIS contain more aromatic structures, and have a lower content of aliphatic and oxygen-containing groups than atmospheric HULIS. Among the four primary sources of HULIS, HULIS from BB had the highest O ∕ C molar ratios (0.43–0.54) and [H–C–O] content (10–19 %), indicating that HULIS from this source mainly consisted of carbohydrate- and phenolic-like structures. HULIS from coal combustion had a lower O ∕ C molar ratio (0.27) and a higher content of [Ar–H] (31 %), suggesting that aromatic compounds were extremely abundant in HULIS from this source. Moreover, the absorption Ångström exponents of primary HULIS from BB and coal combustion were 6.7–8.2 and 13.6, respectively. The mass absorption efficiencies of primary HULIS from BB and coal combustion at 365 nm (MAE365) were 0.97–2.09 and 0.63 m2 gC−1, respectively. Noticeably higher MAE365 values for primary HULIS from BB than coal combustion indicate that the former has a stronger contribution to the light-absorbing properties of aerosols in the atmospheric environment.

Highlights

  • In recent decades, many studies have investigated the watersoluble unresolved polyacidic compounds in atmospheric aerosols, rainwater, and fog/cloud samples (Zheng et al, 2013 and references therein)

  • It can be seen that the mass of the humic-like substances (HULIS) fractions accounted for 11.2–23.4 % of the particle matter (PM) in smoke PM2.5 emitted from biomass burning (BB), which is comparable to the results (7.6– 29.5 %) for BB reported in previous studies (Lin, 2010b, Park and Yu, 2016)

  • The primary HULIS fractions in smoke PM2.5 emitted from the combustion of biomass materials and fossil fuels were isolated and comprehensively characterized by various analytical methods, including total organic carbon (TOC) analysis, elemental analysis, UV–vis, excitation– emission matrix (EEM) fluorescence, Fourier transform infrared (FTIR), and 1H nuclear magnetic resonance (NMR) spectroscopy

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Summary

Introduction

Many studies have investigated the watersoluble unresolved polyacidic compounds in atmospheric aerosols, rainwater, and fog/cloud samples (Zheng et al, 2013 and references therein). HULIS are present ubiquitously in fine particles from urban, rural, marine, and biomass burning (BB) sources (Decesari et al, 2007; Salma et al, 2007; Lin et al, 2010b; Fan et al, 2012; Song et al, 2012; Zheng et al, 2013) They are believed to play important roles in several atmospheric processes, including light absorption, radiative forcing (Hoffer et al, 2006; Dinar et al, 2008), hygroscopicity, and cloud droplet formation (Dinar et al, 2007; Salma et al, 2008). They are reported to be harmful to human health (Lin and Yu, 2011)

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