Fungal spores overwhelm biogenic organic aerosols in a midlatitudinal forest

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 biomarker...

Full description

Bibliographic Details
Main Authors: C. Zhu, K. Kawamura, Y. Fukuda, M. Mochida, Y. Iwamoto
Format: Article
Language:English
Published: Copernicus Publications 2016-06-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/7497/2016/acp-16-7497-2016.pdf
_version_ 1818110347267014656
author C. Zhu
C. Zhu
C. Zhu
K. Kawamura
K. Kawamura
Y. Fukuda
Y. Fukuda
M. Mochida
M. Mochida
Y. Iwamoto
Y. Iwamoto
author_facet C. Zhu
C. Zhu
C. Zhu
K. Kawamura
K. Kawamura
Y. Fukuda
Y. Fukuda
M. Mochida
M. Mochida
Y. Iwamoto
Y. Iwamoto
author_sort C. Zhu
collection DOAJ
description 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 (<i>p</i> &lt; 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.
first_indexed 2024-12-11T02:45:42Z
format Article
id doaj.art-019ded19fcbd45f48ead731afcae315e
institution Directory Open Access Journal
issn 1680-7316
1680-7324
language English
last_indexed 2024-12-11T02:45:42Z
publishDate 2016-06-01
publisher Copernicus Publications
record_format Article
series Atmospheric Chemistry and Physics
spelling doaj.art-019ded19fcbd45f48ead731afcae315e2022-12-22T01:23:25ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-06-01167497750610.5194/acp-16-7497-2016Fungal spores overwhelm biogenic organic aerosols in a midlatitudinal forestC. Zhu0C. Zhu1C. Zhu2K. Kawamura3K. Kawamura4Y. Fukuda5Y. Fukuda6M. Mochida7M. Mochida8Y. Iwamoto9Y. Iwamoto10Institute of Low Temperature Science, Hokkaido University, Sapporo 0600819, JapanCMA Key Laboratory of Aerosol-Cloud-Precipitation, Nanjing University of Information Science and Technology, Nanjing 210044, Chinanow at: Department of Environmental Geochemical Cycle Research, Japan Agency for Marine–Earth Science and Technology, Yokohama 2360001, JapanInstitute of Low Temperature Science, Hokkaido University, Sapporo 0600819, Japannow at: Chubu Institute for Advanced Studies, Chubu University, Kasugai 4878501, JapanInstitute of Low Temperature Science, Hokkaido University, Sapporo 0600819, JapanGraduate School of Environmental Science, Hokkaido University, Sapporo 0600810, JapanInstitute of Advanced Research, Nagoya University, Nagoya 4648601, Japannow at: Graduate School of Environmental Studies, Nagoya University, Nagoya 4648601, Japan Institute of Advanced Research, Nagoya University, Nagoya 4648601, Japannow at: Faculty of Science Division I, Tokyo University of Science, Tokyo 1628601, JapanBoth 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 (<i>p</i> &lt; 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.https://www.atmos-chem-phys.net/16/7497/2016/acp-16-7497-2016.pdf
spellingShingle C. Zhu
C. Zhu
C. Zhu
K. Kawamura
K. Kawamura
Y. Fukuda
Y. Fukuda
M. Mochida
M. Mochida
Y. Iwamoto
Y. Iwamoto
Fungal spores overwhelm biogenic organic aerosols in a midlatitudinal forest
Atmospheric Chemistry and Physics
title Fungal spores overwhelm biogenic organic aerosols in a midlatitudinal forest
title_full Fungal spores overwhelm biogenic organic aerosols in a midlatitudinal forest
title_fullStr Fungal spores overwhelm biogenic organic aerosols in a midlatitudinal forest
title_full_unstemmed Fungal spores overwhelm biogenic organic aerosols in a midlatitudinal forest
title_short Fungal spores overwhelm biogenic organic aerosols in a midlatitudinal forest
title_sort fungal spores overwhelm biogenic organic aerosols in a midlatitudinal forest
url https://www.atmos-chem-phys.net/16/7497/2016/acp-16-7497-2016.pdf
work_keys_str_mv AT czhu fungalsporesoverwhelmbiogenicorganicaerosolsinamidlatitudinalforest
AT czhu fungalsporesoverwhelmbiogenicorganicaerosolsinamidlatitudinalforest
AT czhu fungalsporesoverwhelmbiogenicorganicaerosolsinamidlatitudinalforest
AT kkawamura fungalsporesoverwhelmbiogenicorganicaerosolsinamidlatitudinalforest
AT kkawamura fungalsporesoverwhelmbiogenicorganicaerosolsinamidlatitudinalforest
AT yfukuda fungalsporesoverwhelmbiogenicorganicaerosolsinamidlatitudinalforest
AT yfukuda fungalsporesoverwhelmbiogenicorganicaerosolsinamidlatitudinalforest
AT mmochida fungalsporesoverwhelmbiogenicorganicaerosolsinamidlatitudinalforest
AT mmochida fungalsporesoverwhelmbiogenicorganicaerosolsinamidlatitudinalforest
AT yiwamoto fungalsporesoverwhelmbiogenicorganicaerosolsinamidlatitudinalforest
AT yiwamoto fungalsporesoverwhelmbiogenicorganicaerosolsinamidlatitudinalforest