Chemical evolution of primary and secondary biomass burning aerosols during daytime and nighttime

被引:6
|
作者
Yazdani, Amir [1 ]
Takahama, Satoshi [1 ]
Kodros, John K. [2 ]
Paglione, Marco [2 ,3 ]
Masiol, Mauro [2 ]
Squizzato, Stefania [2 ]
Florou, Kalliopi [2 ]
Kaltsonoudis, Christos [2 ]
Jorga, Spiro D. [2 ]
Pandis, Spyros N. [2 ,4 ]
Nenes, Athanasios [1 ,2 ]
机构
[1] Ecole Polytech Fed Lausanne EPFL, Lab Atmospher Proc & their Impacts LAPI, ENAC IIE, Lausanne, Switzerland
[2] Fdn Res & Technol Hellas ICE HT FORTH, Inst Chem Engn Sci, Patras, Greece
[3] Italian Natl Res Council, Inst Atmospher Sci & Climate CNR ISAC, Bologna, Italy
[4] Univ Patras, Dept Chem Engn, Patras, Greece
基金
欧洲研究理事会; 瑞士国家科学基金会;
关键词
VAPOR WALL-LOSS; FINE-PARTICLE EMISSIONS; ORGANIC AEROSOL; MASS-SPECTROMETRY; INFRARED-SPECTROSCOPY; FUNCTIONAL-GROUPS; ELEMENTAL COMPOSITION; SIZE EVOLUTION; OH OXIDATION; OLEIC-ACID;
D O I
10.5194/acp-23-7461-2023
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Primary emissions from wood and pellet stoves were aged in an atmospheric simulation chamber under daytime and nighttime conditions. The aerosol was analyzed with online aerosol mass spectrometry and offline Fourier transform infrared spectroscopy (FTIR). Measurements using the two techniques agreed reasonably well in terms of the organic aerosol (OA) mass concentration, OA V OC trends, and concentrations of biomass burning markers - lignin-like compounds and anhydrosugars. Based on aerosol mass spectrometry, around 15% of the primary organic aerosol (POA) mass underwent some form of transformation during daytime oxidation conditions after 6-10 h of atmospheric exposure. A lesser extent of transformation was observed during the nighttime oxidation. The decay of certain semi-volatile (e.g., levoglucosan) and less volatile (e.g., lignin-like) POA components was substantial during aging, highlighting the role of heterogeneous reactions and gas-particle partitioning. Lignin-like compounds were observed to degrade under both daytime and nighttime conditions, whereas anhydrosugars degraded only under daytime conditions. Among the marker mass fragments of primary biomass burning OA (bbPOA), heavy ones (higher m=z) were relatively more stable during aging. The biomass burning secondary OA (bbSOA) became more oxidized with continued aging and resembled that of aged atmospheric organic aerosols. The bbSOA formed during daytime oxidation was dominated by acids. Organonitrates were an important product of nighttime reactions in both humid and dry conditions. Our results underline the importance of changes to both the primary and secondary biomass burning aerosols during their atmospheric aging. Heavier fragments from aerosol mass spectrometry seldom used in atmospheric chemistry can be used as more stable tracers of bbPOA and, in combination with the established levoglucosan marker, can provide an indication of the extent of bbPOA aging.
引用
收藏
页码:7461 / 7477
页数:17
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