Identification of the mass spectral signature of organic aerosols from wood burning emissions

被引:368
作者
Alfarra, M. Rami [1 ]
Prevot, Andre S. H.
Szidat, Sonke
Sandradewi, Jisca
Weimer, Silke
Lanz, Valentin A.
Schreiber, Daniel
Mohr, Martin
Baltensperger, Urs
机构
[1] Paul Scherrer Inst, Lab Atmospher Chem, CH-5232 Villigen, Switzerland
[2] Univ Bern, Dept Chem & Biochem, CH-3012 Bern, Switzerland
[3] Swiss Fed Labs Mat Testing & Res, CH-8600 Dubendorf, Switzerland
关键词
D O I
10.1021/es062289b
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Throughout the winter months, the village of Roveredo, Switzerland, frequently experiences strong temperature inversions that contribute to elevated levels of particulate matter. Wood is used as fuel for 75% of the domestic heating installations in Roveredo, which makes it a suitable location to study wood burning emissions in the atmosphere in winter. An Aerodyne quadrupole aerosol mass spectrometer (Q-AMS) was used to characterize the composition of the submicrometer, non-refractory aerosol particles at this location during two field campaigns in March and December 2005. Wood burning was found to be a major source of aerosols at this location in winter. Organics dominated the composition of the aerosols from this source, contributing up to 85% of the total AMS measured mass during the afternoon and evening hours. Carbonaceous particle analysis showed that organic carbon composed up to 86% of the total carbon mass collected at evening times. Results from C-14 isotope determination revealed that up to 94% of the organic mass came from nonfossil sources, which can be attributed mostly to wood burning. The unique combination of off-line C-14 isotope analysis and on-line aerosol mass spectrometry was used to identify periods during which organic mass was mainly from wood burning emissions and allowed for the identification of the AMS spectral signature of this source in the atmosphere. The identified ambient signature of wood burning was found to be very similar to the mass spectral signature obtained during the burning of chestnut wood samples in a small stove and also to the spectrum of levoglucosan. Particles from wood burning appeared to be composed of highly oxygenated organic compounds, and mass fragments 60, 73, and 137 have been suggested as marker fragments for wood burning aerosols. Mass fragment 44, which is used as a marker for oxygenated organic aerosols (OOA), contributed about 5% to the total organic signal from primary wood burning sources, The ratio of the organic mass emitted from wood burning to m/z 60 in Roveredo is 36. This ratio may be used to provide an estimate of the organic aerosol mass emitted from wood burning in other locations.
引用
收藏
页码:5770 / 5777
页数:8
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