Abstract
Brown carbon (BrC) has recently received much attention because of its light absorption features. The chemical compositions, optical properties, and sources of fine aerosol at a high-elevation mountain observatory (4730 m a.s.l.) in the central Tibetan Plateau were measured between 31 May and 1 July 2015. A low flow-rate sampler was used to collect 24-h average fine particulate matter (PM2.5) filter samples. Water-soluble ions, organic carbon (OC), elemental carbon, water-soluble organic carbon (WSOC), and light absorption by water-soluble BrC were determined for 26 filter samples. The mean (± 1σ) OC and WSOC concentrations were 0.76 ± 0.43 and 0.39 ± 0.15 μgC/m3, respectively, and the mean WSOC/OC mass ratio was 0.59 ± 0.22. The OC and WSOC concentrations were relatively higher (0.59–1.80 and 0.33–0.83 μgC/m3, respectively) during the pre-monsoon period (2–13 June) and were relatively lower (0.27–0.77 and 0.12–0.50 μgC/m3, respectively) during the monsoon period (14 June to 1 July), probably because of wet scavenging of aerosols during long-range transport and the presence of cleaner marine air masses during the monsoon period. The absorption spectra of PM2.5 water extracts smoothly increase from visible range to ultraviolet range. The absorption Ångström exponent, which describes the wavelength dependence of water-soluble BrC, was 2.74–10.61 (mean 6.19 ± 1.70), and its value was similar in the pre-monsoon period (6.57 ± 0.56) to that in the monsoon period (5.91 ± 2.14). The water-soluble BrC mass absorption efficiency, 0.38 ± 0.16 m2/(g C), was much lower than those observed in most urban areas but similar to those in other remote sites. Absorption coefficient at 365 nm, typically used as a proxy for water-soluble BrC, correlated well with the WSOC concentration (R 2 = 0.57), K+ concentration (R 2 = 0.75), and organic aerosol biomass burning markers characterized by an Aerodyne aerosol mass spectrometer (C2H4O2 + + C3H5O2 +, R 2 = 0.60). It can be inferred that biomass burning was an important source of water-soluble BrC in the study area combined with air mass back trajectory analysis using the NOAA HYSPLIT as well as MODIS data of fire dots and aerosol optical depths. The water-soluble BrC to BC light absorption (at 365 nm) coefficient ratios were 9–27%.
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Acknowledgements
Thanks to the logistics support of NCOS. This research was supported by grants from the Key Laboratory of Cryospheric Sciences Scientific Research Foundation (SKLCS-ZZ-2016-01), the National Natural Science Foundation of China Science Fund for Creative Research Groups (41121001), open fund by Jiangsu Key Laboratory of Atmospheric Environment Monitoring and Pollution Control (KHK1406), a Project Funded by the Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD), and the Chinese Academy of Sciences Hundred Talents Program.
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Zhang, Y., Xu, J., Shi, J. et al. Light absorption by water-soluble organic carbon in atmospheric fine particles in the central Tibetan Plateau. Environ Sci Pollut Res 24, 21386–21397 (2017). https://doi.org/10.1007/s11356-017-9688-8
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DOI: https://doi.org/10.1007/s11356-017-9688-8