Quantitative and time-resolved nanoparticle composition measurements during new particle formation

被引:30
作者
Bzdek, Bryan R. [1 ]
Horan, Andrew J. [1 ]
Pennington, M. Ross [1 ]
DePalma, Joseph W. [1 ]
Zhao, Jun [2 ]
Jen, Coty N. [2 ]
Hanson, David R. [3 ]
Smith, James N. [4 ,5 ]
McMurry, Peter H. [2 ]
Johnston, Murray V. [1 ]
机构
[1] Univ Delaware, Dept Chem & Biochem, Newark, DE 19716 USA
[2] Univ Minnesota, Dept Mech Engn, Minneapolis, MN 55455 USA
[3] Augsburg Coll, Dept Chem, Minneapolis, MN 55454 USA
[4] Natl Ctr Atmospher Res, Atmospher Chem Div, Boulder, CO 80305 USA
[5] Univ Eastern Finland, Appl Phys Dept, Kuopio 70211, Finland
基金
美国国家科学基金会; 芬兰科学院;
关键词
AEROSOL MASS-SPECTROMETER; SULFURIC-ACID; CHEMICAL-COMPOSITION; ATMOSPHERIC NANOPARTICLES; EXPERIMENTAL SETUP; GROWTH-RATES; NUCLEATION; CLUSTERS; ORGANICS; NITRATE;
D O I
10.1039/c3fd00039g
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The chemical composition of 20 nm diameter particles was measured with the Nano Aerosol Mass Spectrometer (NAMS) in a rural/coastal environment during days when new particle formation (NPF) occurred and days when NPF did not occur. NAMS provides a quantitative measure of nanoparticle elemental composition with high time resolution. These measurements show that nanoparticle chemical composition is dynamic on both types of days and that changes in nanoparticle chemical composition do not necessarily correlate with changes in aerosol mass or number concentration. On NPF days, NAMS can distinguish between elements associated with particle formation and early mass growth from those associated with later mass growth. In the early stage of NPF, the particle phase sulphur mole fraction (S) increases simultaneously with the increase in gas phase sulphuric acid. This composition change occurs before the mode diameter has grown into the NAMS-measured size range and is quantitatively described by sulphuric acid condensation. The nitrogen mole fraction (N) also increases during this time period. The N/S mole ratio is approximately 2, indicating that particulate sulphate is fully neutralized. As the mode diameter passes into and through the NAMS-measured size range, N increases at a faster rate than S (N/S mole ratio increases above 2), indicating that a separate, nitrogen-based growth process exists, possibly involving aminium salts, inorganic nitrate and/or organonitrates. Carbonaceous matter is the most abundant component (similar to 50% by mass) of the growing nanoparticles, but it is the inorganic species that are preferentially enhanced during NPF relative to other times of day. Concurrent measurements of cloud condensation nucleation activity during NPF events suggest that these newly formed particles are hygroscopic. Nanoparticle composition on non-NPF days also shifts toward a more inorganic composition during the daytime, but the chemical species are different from NPF days and the particles are less hygroscopic. Incorporation of S into growing nanoparticles is adequately explained by existing models, but currently no models exist to satisfactorily explain incorporation of nitrogen-containing species or carbonaceous matter.
引用
收藏
页码:25 / 43
页数:19
相关论文
共 73 条
[1]  
[Anonymous], 2013, HYSPLIT HYBRID SINGL
[2]   Laboratory studies of particle nucleation:: Initial results for H2SO4, H2O, and NH3 vapors [J].
Ball, SM ;
Hanson, DR ;
Eisele, FL ;
McMurry, PH .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D19) :23709-23718
[3]   The potential contribution of organic salts to new particle growth [J].
Barsanti, K. C. ;
McMurry, P. H. ;
Smith, J. N. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2009, 9 (09) :2949-2957
[4]   Laboratory-measured H2SO4-H2O-NH3 ternary homogeneous nucleation rates: Initial observations [J].
Benson, David R. ;
Erupe, Mark E. ;
Lee, Shan-Hu .
GEOPHYSICAL RESEARCH LETTERS, 2009, 36
[5]   Laboratory study on new particle formation from the reaction OH + SO2: influence of experimental conditions, H2O vapour, NH3 and the amine tert-butylamine on the overall process [J].
Berndt, T. ;
Stratmann, F. ;
Sipilae, M. ;
Vanhanen, J. ;
Petaja, T. ;
Mikkila, J. ;
Gruener, A. ;
Spindler, G. ;
Mauldin, R. Lee, III ;
Curtius, J. ;
Kulmala, M. ;
Heintzenberg, J. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2010, 10 (15) :7101-7116
[6]   Single particle chemical analysis of ambient ultrafine aerosol: A review [J].
Bzdek, Bryan R. ;
Pennington, M. Ross ;
Johnston, Murray V. .
JOURNAL OF AEROSOL SCIENCE, 2012, 52 :109-120
[7]   Quantitative Assessment of the Sulfuric Acid Contribution to New Particle Growth [J].
Bzdek, Bryan R. ;
Zordan, Christopher A. ;
Pennington, M. Ross ;
Luther, George W., III ;
Johnston, Murray V. .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2012, 46 (08) :4365-4373
[8]   Nanoparticle Chemical Composition During New Particle Formation [J].
Bzdek, Bryan R. ;
Zordan, Christopher A. ;
Luther, George W., III ;
Johnston, Murray V. .
AEROSOL SCIENCE AND TECHNOLOGY, 2011, 45 (08) :1041-1048
[9]   New Particle Formation and Growth in the Troposphere [J].
Bzdek, Bryan R. ;
Johnston, Murray V. .
ANALYTICAL CHEMISTRY, 2010, 82 (19) :7871-7878
[10]   CLIMATE FORCING BY ANTHROPOGENIC AEROSOLS [J].
CHARLSON, RJ ;
SCHWARTZ, SE ;
HALES, JM ;
CESS, RD ;
COAKLEY, JA ;
HANSEN, JE ;
HOFMANN, DJ .
SCIENCE, 1992, 255 (5043) :423-430