On the diurnal variability of particle properties related to light absorbing carbon in Mexico City

被引:50
作者
Baumgardner, D. [1 ]
Kok, G. L.
Raga, G. B.
机构
[1] Univ Nacl Autonoma Mexico, Ctr Ciencias Atmosfera, Mexico City 04510, DF, Mexico
[2] Droplet Measurement Technol, Boulder, CO USA
关键词
D O I
10.5194/acp-7-2517-2007
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The mass of light absorbing carbon ( LAC) in individual, internally mixed aerosol particles was measured with the Single Particle Soot Photometer (SP2) in April of 2003 and 2005 and evaluated with respect to concentrations of carbon monoxide ( CO), particle bound polycyclic aromatic hydrocarbons (PPAH) and condensation nuclei (CN). The LAC and CO have matching diurnal trends that are linked to traffic patterns and boundary layer growth. The PPAH reaches a maximum at the same time as CO and LAC but returns rapidly back to nighttime values within three hours of the peak. The number of particles containing LAC ranges between 10% to 40% of all particles between 150 nm and 650 nm and the mass is between 5% and 25% of the total mass in this size range. The average LAC equivalent mass diameter varies between 160 and 230 nm and the thinnest coating of non-light absorbing material is observed during periods of maximum LAC mass. The coating varies between 10 nm and 30 nm during the day, but is a strong function of particle size. The mass absorption cross sections, sigma(abs), derived from the SP2, are 5.0 +/- 0.2 m(2)g(-1) and 4.8 +/- 0.2m(2) g(-1), dependent on the optical model used to describe LAC mixtures. The LAC contributes up to 50% of the total light extinction in the size range from 100 nm to 400 nm. The estimated emission rate of LAC is 1200 metric tons per year in Mexico City, based upon the SP2 measurements and correlations between LAC and CO.
引用
收藏
页码:2517 / 2526
页数:10
相关论文
共 43 条
[21]   Temporal variations of elemental carbon in Tokyo [J].
Kondo, Y. ;
Komazaki, Y. ;
Miyazaki, Y. ;
Moteki, N. ;
Takegawa, N. ;
Kodama, D. ;
Deguchi, S. ;
Nogami, M. ;
Fukuda, M. ;
Miyakawa, T. ;
Morino, Y. ;
Koike, M. ;
Sakurai, H. ;
Ehara, K. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2006, 111 (D12)
[22]   OPTICAL AND THERMAL MEASUREMENTS OF BLACK CARBON AEROSOL CONTENT IN DIFFERENT ENVIRONMENTS - VARIATION OF THE SPECIFIC ATTENUATION CROSS-SECTION, SIGMA (SIGMA) [J].
LIOUSSE, C ;
CACHIER, H ;
JENNINGS, SG .
ATMOSPHERIC ENVIRONMENT PART A-GENERAL TOPICS, 1993, 27 (08) :1203-1211
[23]   Sources and transformations of particle-bound polycyclic aromatic hydrocarbons in Mexico City [J].
Marr, L. C. ;
Dzepina, K. ;
Jimenez, J. L. ;
Reisen, F. ;
Bethel, H. L. ;
Arey, J. ;
Gaffney, J. S. ;
Marley, N. A. ;
Molina, L. T. ;
Molina, M. J. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2006, 6 :1733-1745
[24]   Dynamic field measurements of submicron particles from diesel engines [J].
Matter, U ;
Siegmann, HC ;
Burtscher, H .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1999, 33 (11) :1946-1952
[25]   Optical properties of soot-water drop agglomerates: An experimental study [J].
Mikhailov, EF ;
Vlasenko, SS ;
Podgorny, IA ;
Ramanathan, V ;
Corrigan, CE .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2006, 111 (D7)
[26]   Effects of mixing state on black carbon measurements by laser-induced incandescence [J].
Moteki, Nobuhiro ;
Kondo, Yutaka .
AEROSOL SCIENCE AND TECHNOLOGY, 2007, 41 (04) :398-417
[27]  
NOVAKOV T, 1982, PARTICULATE CARBON A, P19
[28]   Spectrothermography of carbonaceous particles [J].
Peralta, Oscar ;
Baumgardner, Darrel ;
Raga, Graciela B. .
JOURNAL OF ATMOSPHERIC CHEMISTRY, 2007, 57 (02) :153-169
[29]   The dependence of the specific attenuation cross-section on black carbon mass fraction and particle size [J].
Petzold, A ;
Kopp, C ;
Niessner, R .
ATMOSPHERIC ENVIRONMENT, 1997, 31 (05) :661-672
[30]  
*PROAIRE, 1999, PROGR MEJ CAL AIR VA, P244