Mixing state of carbonaceous aerosol in an urban environment: single particle characterization using the soot particle aerosol mass spectrometer (SP-AMS)

被引:71
作者
Lee, A. K. Y. [1 ]
Willis, M. D. [1 ]
Healy, R. M. [2 ,3 ,4 ]
Onasch, T. B. [5 ]
Abbatt, J. P. D. [1 ]
机构
[1] Univ Toronto, Dept Chem, Toronto, ON M5S 1A1, Canada
[2] Natl Univ Ireland Univ Coll Cork, Dept Chem, Cork, Ireland
[3] Natl Univ Ireland Univ Coll Cork, Environm Res Inst, Cork, Ireland
[4] Univ Toronto, Southern Ontario Ctr Atmospher Aerosol Res, Toronto, ON, Canada
[5] Aerodyne Res Inc, Billerica, MA USA
基金
加拿大自然科学与工程研究理事会; 加拿大创新基金会;
关键词
AERODYNAMIC DIAMETER MEASUREMENTS; LASER-INDUCED INCANDESCENCE; LIGHT-SCATTERING MODULE; BLACK CARBON; ORGANIC AEROSOL; SOURCE APPORTIONMENT; DENSITY CHARACTERIZATION; COLLECTION EFFICIENCIES; SPECTRAL SIGNATURES; PARTICULATE MATTER;
D O I
10.5194/acp-15-1823-2015
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Understanding the impact of atmospheric black carbon (BC)-containing particles on human health and radiative forcing requires knowledge of the mixing state of BC, including the characteristics of the materials with which it is internally mixed. In this study, we examine the mixing state of refractory BC (rBC) and other aerosol components in an urban environment (downtown Toronto) utilizing the Aerodyne soot particle aerosol mass spectrometer equipped with a light scattering module (LS-SP-AMS). k-means cluster analysis was used to classify single particle mass spectra into chemically distinct groups. One resultant particle class is dominated by rBC mass spectral signals (C-1(+) to C-5(+) while the organic signals fall into a few major particle classes identified as hydrocarbon-like organic aerosol (HOA), oxygenated organic aerosol (OOA), and cooking emission organic aerosol (COA). A gradual mixing is observed with small rBC particles only thinly coated by HOA (similar to 28% by mass on average), while over 90% of the HOA-rich particles did not contain detectable amounts of rBC. Most of the particles classified into other inorganic and organic particle classes were not significantly associated with rBC. The single particle results also suggest that HOA and COA emitted from anthropogenic sources were likely major contributors to organic-rich particles with vacuum aerodynamic diameter (d(va)) ranging from similar to 200 to 400 nm. The similar temporal profiles and mass spectral features of the organic classes identified by cluster analysis and the factors from a positive matrix factorization (PMF) analysis of the ensemble aerosol data set validate the interpretation of the PMF results.
引用
收藏
页码:1823 / 1841
页数:19
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