O/C and OM/OC ratios of primary, secondary, and ambient organic aerosols with high-resolution time-of-flight aerosol mass spectrometry

被引:1195
作者
Aiken, Allison C. [1 ,2 ]
Decarlo, Peter F. [2 ,3 ]
Kroll, Jesse H. [4 ]
Worsnop, Douglas R. [4 ]
Huffman, J. Alex [1 ,2 ]
Docherty, Kenneth S. [2 ]
Ulbrich, Ingrid M. [1 ,2 ]
Mohr, Claudia [2 ]
Kimmel, Joel R. [2 ]
Sueper, Donna [2 ]
Sun, Yele [5 ]
Zhang, Qi [5 ]
Trimborn, Achim [4 ]
Northway, Megan [4 ]
Ziemann, Paul J. [6 ]
Canagaratna, Manjula R. [4 ]
Onasch, Timothy B. [4 ]
Alfarra, M. Rami [7 ]
Prevot, Andre S. H. [7 ]
Dommen, Josef [7 ]
Duplissy, Jonathan [7 ]
Metzger, Axel [7 ]
Baltensperger, Urs [7 ]
Jimenez, Jose L. [1 ,2 ]
机构
[1] Univ Colorado, Dept Chem & Biochem, Boulder, CO 80309 USA
[2] Univ Colorado, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
[3] Univ Colorado, Dept Atmospher & Ocean Sci ATOC, Boulder, CO 80309 USA
[4] Aerodyne Res Inc, Billerica, MA 01821 USA
[5] SUNY Albany, Atmospher Sci Res Ctr, Albany, NY 12222 USA
[6] Univ Calif Riverside, Dept Environm Sci, Riverside, CA 92521 USA
[7] Paul Scherrer Inst, Lab Atmospher Chem, CH-5232 Villigen, Switzerland
基金
英国自然环境研究理事会;
关键词
D O I
10.1021/es703009q
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A recently developed method to rapidly quantify the elemental composition of bulk organic aerosols (OA) using a high-resolution time-of-flight aerosol mass spectrometer (HR-ToF-AMS) is improved and applied to ambient measurements. Atomic oxygen-to-carbon (O/C) ratios characterize the oxidation state of OA, and O/C from ambient urban OA ranges from 0.2 to 0.8 with a diurnal cycle that decreases with primary emissions and increases because of photochemical processing and secondary OA (SOA) production. Regional O/C approaches similar to 0.9. The hydrogen-to-carbon (H/C, 1.4-1.9) urban diurnal profile increases with primary CIA (POA) as does the nitrogen-to-carbon WC, similar to 0.02). Ambient organic-mass-to-organic-carbon ratios (OM/OC) are directly quantified and correlate well with O/C (R-2 = 0.997) for ambient OA because of low N/C. Ambient O/C and OWN have values consistent with those recently reported from other techniques. Positive matrix factorization applied to ambient OA identifies factors with distinct O/C and OM/OC trends. The highest O/C and OM/OC (1.0 and 2.5, respectively) are observed for aged ambient oxygenated OA, significantly exceeding values for traditional chamber SOA, while laboratory-produced primary biomass burning OA (BBOA) is similar to ambient BBOA, O/C of 0.3-0.4. Hydrocarbon-like OA (HOA), a surrogate for urban combustion POA, has the lowest O/C (0.06-0.10), similar to vehicle exhaust. An approximation for predicting O/C from unit mass resolution data is also presented.
引用
收藏
页码:4478 / 4485
页数:8
相关论文
共 30 条
[1]   Elemental analysis of organic species with electron ionization high-resolution mass spectrometry [J].
Aiken, Allison. C. ;
DeCarlo, Peter F. ;
Jimenez, Jose L. .
ANALYTICAL CHEMISTRY, 2007, 79 (21) :8350-8358
[2]   A generalised method for the extraction of chemically resolved mass spectra from aerodyne aerosol mass spectrometer data [J].
Allan, JD ;
Delia, AE ;
Coe, H ;
Bower, KN ;
Alfarra, MR ;
Jimenez, JL ;
Middlebrook, AM ;
Drewnick, F ;
Onasch, TB ;
Canagaratna, MR ;
Jayne, JT ;
Worsnop, DR .
JOURNAL OF AEROSOL SCIENCE, 2004, 35 (07) :909-922
[3]   Secondary formation and the Smoky Mountain organic aerosol: An examination of aerosol polarity and functional group composition during SEAVS [J].
Blando, JD ;
Porcja, RJ ;
Li, TH ;
Bowman, D ;
Lioy, PJ ;
Turpin, BJ .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1998, 32 (05) :604-613
[4]   Chemical and microphysical characterization of ambient aerosols with the aerodyne aerosol mass spectrometer [J].
Canagaratna, M. R. ;
Jayne, J. T. ;
Jimenez, J. L. ;
Allan, J. D. ;
Alfarra, M. R. ;
Zhang, Q. ;
Onasch, T. B. ;
Drewnick, F. ;
Coe, H. ;
Middlebrook, A. ;
Delia, A. ;
Williams, L. R. ;
Trimborn, A. M. ;
Northway, M. J. ;
DeCarlo, P. F. ;
Kolb, C. E. ;
Davidovits, P. ;
Worsnop, D. R. .
MASS SPECTROMETRY REVIEWS, 2007, 26 (02) :185-222
[5]   Fast airborne aerosol size and chemistry measurements above Mexico City and Central Mexico during the MILAGRO campaign [J].
DeCarlo, P. F. ;
Dunlea, E. J. ;
Kimmel, J. R. ;
Aiken, A. C. ;
Sueper, D. ;
Crounse, J. ;
Wennberg, P. O. ;
Emmons, L. ;
Shinozuka, Y. ;
Clarke, A. ;
Zhou, J. ;
Tomlinson, J. ;
Collins, D. R. ;
Knapp, D. ;
Weinheimer, A. J. ;
Montzka, D. D. ;
Campos, T. ;
Jimenez, J. L. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2008, 8 (14) :4027-4048
[6]   Field-deployable, high-resolution, time-of-flight aerosol mass spectrometer [J].
DeCarlo, Peter F. ;
Kimmel, Joel R. ;
Trimborn, Achim ;
Northway, Megan J. ;
Jayne, John T. ;
Aiken, Allison C. ;
Gonin, Marc ;
Fuhrer, Katrin ;
Horvath, Thomas ;
Docherty, Kenneth S. ;
Worsnop, Doug R. ;
Jimenez, Jose L. .
ANALYTICAL CHEMISTRY, 2006, 78 (24) :8281-8289
[7]   Water soluble organic compounds formed by oxidation of soot [J].
Decesari, S ;
Facchini, MC ;
Matta, E ;
Mircea, M ;
Fuzzi, S ;
Chughtai, AR ;
Smith, DM .
ATMOSPHERIC ENVIRONMENT, 2002, 36 (11) :1827-1832
[8]   Cloud forming potential of secondary organic aerosol under near atmospheric conditions [J].
Duplissy, J. ;
Gysel, Martin ;
Alfarra, M.R. ;
Dommen, J. ;
Metzger, A. ;
Prevot, A.S.H. ;
Weingartner, E. ;
Laaksonen, A. ;
Raatikainen, T. ;
Good, N. ;
Turner, S.F. ;
McFiggans, G. ;
Baltensperger, U. .
Geophysical Research Letters, 2008, 35 (02)
[9]   Oligomers in the early stage of biogenic secondary organic aerosol formation and growth [J].
Heaton, Katherine J. ;
Dreyfus, Matthew A. ;
Wang, Shenyi ;
Johnston, Murray V. .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2007, 41 (17) :6129-6136
[10]  
HUFFMAN JA, 2008, VOLATILITY PRI UNPUB