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Volume 16, issue 11 | Copyright

Special issue: Integrated Land Ecosystem-Atmosphere Processes Study (iLEAPS)...

Atmos. Chem. Phys., 16, 7497-7506, 2016
https://doi.org/10.5194/acp-16-7497-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 16 Jun 2016

Research article | 16 Jun 2016

Fungal spores overwhelm biogenic organic aerosols in a midlatitudinal forest

Chunmao Zhu1,2,a, Kimitaka Kawamura1,b, Yasuro Fukuda1,3, Michihiro Mochida4,c, and Yoko Iwamoto4,d Chunmao Zhu et al.
  • 1Institute of Low Temperature Science, Hokkaido University, Sapporo 0600819, Japan
  • 2CMA Key Laboratory of Aerosol-Cloud-Precipitation, Nanjing University of Information Science and Technology, Nanjing 210044, China
  • 3Graduate School of Environmental Science, Hokkaido University, Sapporo 0600810, Japan
  • 4Institute of Advanced Research, Nagoya University, Nagoya 4648601, Japan
  • anow at: Department of Environmental Geochemical Cycle Research, Japan Agency for Marine–Earth Science and Technology, Yokohama 2360001, Japan
  • bnow at: Chubu Institute for Advanced Studies, Chubu University, Kasugai 4878501, Japan
  • cnow at: Graduate School of Environmental Studies, Nagoya University, Nagoya 4648601, Japan
  • dnow at: Faculty of Science Division I, Tokyo University of Science, Tokyo 1628601, Japan

Abstract. Both primary biological aerosol particles (PBAPs) and oxidation products of biogenic volatile organic compounds (BVOCs) contribute significantly to organic aerosols (OAs) in forested regions. However, little is known about their relative importance in diurnal timescales. Here, we report biomarkers of PBAP and secondary organic aerosols (SOAs) for their diurnal variability in a temperate coniferous forest in Wakayama, Japan. Tracers of fungal spores, trehalose, arabitol and mannitol, showed significantly higher levels in nighttime than daytime (p < 0.05), resulting from the nocturnal sporulation under near-saturated relative humidity. On the contrary, BVOC oxidation products showed higher levels in daytime than nighttime, indicating substantial photochemical SOA formation. Using tracer-based methods, we estimated that fungal spores account for 45% of organic carbon (OC) in nighttime and 22% in daytime, whereas BVOC oxidation products account for 15 and 19%, respectively. To our knowledge, we present for the first time highly time-resolved results that fungal spores overwhelmed BVOC oxidation products in contributing to OA especially in nighttime. This study emphasizes the importance of both PBAPs and SOAs in forming forest organic aerosols.

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We collected aerosol samples in a midlatitude forest in Wakayama, Japan and analyzed the organic tracers of various sources. We found that compounds originating from fungal spores contributed significantly to total organic aerosol mass. On the other hand, those from oxidation of biogenic volatile organic compounds, although they could not be ignored, had relatively smaller mass fractions.
We collected aerosol samples in a midlatitude forest in Wakayama, Japan and analyzed the organic...
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