Size distributions of elemental carbon and its contribution to light extinction in urban and rural locations in the pearl river delta region , China

Elemental carbon (EC) in size-segregated aerosol samples were determined at five urban, one suburban, and one rural locations in the Pearl River Delta region in South China during 2006–2008 period. The size modal characteristics of EC were different at the urban and suburban/rural locations. The urban EC had a dominant condensation mode with a mass median aerodynamic diameter (MMAD) in the 0.36–0.43 μm range and a slightly less abundant mode in the droplet mode size (MMAD: 0.8–1.1 μm), while the suburban/rural EC had a prominent mode in the droplet mode size (MMAD: 0.7–1.1 μm) and a minor condensation mode (MMAD: 0.22–0.33 μm). Calculations using Mie theory and the measured size distributions of EC, organic carbon, and major inorganic ions indicate that EC-containing particles contributed 76±20% of the observed light extinction at the urban sites. Among the EC-containing particles, EC mass alone contributed 21±11% of the observed light extinction while non-EC materials on the EC particles (i.e., organic matter, ammonium sulfate, and water) contributed 55±15%. At the suburban/rural locations, EC-containing particles contributed 37–48% of the measured light extinction, with EC mass contributing 4–10% and non-EC coating materials contributing the remaining light extinction. Our results suggest that EC-containing particles were important to the overall light extinction in the urban atmospheres due to their more abundant presence from vehicular emissions. The ECcontaining particles in the suburban/rural locations had a reduced but still significant contribution to light extinction budget. Correspondence to: J. Z. Yu (chjianyu@ust.hk)

[1]  Judith C Chow,et al.  Comparison of PM2.5 carbon measurement methods in Hong Kong, China. , 2005, Environmental pollution.

[2]  K. Ho,et al.  Carbonaceous characteristics of atmospheric particulate matter in Hong Kong. , 2002, The Science of the total environment.

[3]  R. Cary,et al.  Elemental Carbon-Based Method for Monitoring Occupational Exposures to Particulate Diesel Exhaust , 1996 .

[4]  N. Takegawa,et al.  Formation of submicron sulfate and organic aerosols in the outflow from the urban region of the Pearl River Delta in China , 2009 .

[5]  W. Steen Absorption and Scattering of Light by Small Particles , 1999 .

[6]  H. V. Hulst Light Scattering by Small Particles , 1957 .

[7]  Min Hu,et al.  Size distribution characteristics of elemental carbon emitted from Chinese vehicles: results of a tunnel study and atmospheric implications. , 2006, Environmental science & technology.

[8]  W. Malm,et al.  Examining the relationship between atmospheric aerosols and light extinction at Mount Rainier and North Cascades National Parks , 1994 .

[9]  Y. Kaufman,et al.  Effects of black carbon content, particle size, and mixing on light absorption by aerosols from biomass burning in Brazil , 1998 .

[10]  I. Tang Chemical and size effects of hygroscopic aerosols on light scattering coefficients , 1996 .

[11]  P. Brimblecombe,et al.  A Thermodynamic Model of the System HCl-HNO 3H 2 S 04-H 20 , Including Solubilities of HBr , from < 200 to 328 K , 2001 .

[12]  Alexis K.H. Lau,et al.  Observational and modeling analysis of a severe air pollution episode in western Hong Kong , 2005 .

[13]  J. Yu,et al.  Size distributions of elemental carbon in the atmosphere of a coastal urban area in South China: characteristics, evolution processes, and implications for the mixing state , 2008 .

[14]  Huang Jian,et al.  Effect of Atmospheric Haze on the Deterioration of Visibility over the Pearl River Delta , 2007 .

[15]  D. Blake,et al.  Chemical characterization of water-soluble organic carbon aerosols at a rural site in the Pearl River Delta, China, in the summer of 2006 , 2009 .

[16]  Judith C. Chow,et al.  Sensitivity of estimated light extinction coefficients to model assumptions and measurement errors , 1995 .

[17]  Jing-chun Duan,et al.  Sources and characteristics of carbonaceous aerosol in two largest cities in Pearl River Delta Region, China , 2007 .

[18]  G. M. Hale,et al.  Optical Constants of Water in the 200-nm to 200-microm Wavelength Region. , 1973, Applied optics.

[19]  Alfred Wiedensohler,et al.  Mixing state of elemental carbon and non‐light‐absorbing aerosol components derived from in situ particle optical properties at Xinken in Pearl River Delta of China , 2006 .

[20]  H. Hasan,et al.  Apportioning light extinction coefficients to chemical species in atmospheric aerosol , 1983 .

[21]  J. Froines,et al.  Seasonal variation of the particle size distribution of polycyclic aromatic hydrocarbons and of major aerosol species in Claremont, California , 2004 .

[22]  Judith C. Chow,et al.  Characteristics of carbonaceous aerosol in Pearl River Delta Region, China during 2001 winter period , 2003 .

[23]  Oleg Dubovik,et al.  Microphysical and optical properties of aerosol particles in urban zone during ESCOMPTE , 2003 .

[24]  T. Bond,et al.  Light Absorption by Carbonaceous Particles: An Investigative Review , 2006 .

[25]  J. Fung,et al.  Abundance and seasonal characteristics of elemental and organic carbon in Hong Kong PM10 , 2004 .

[26]  Naresh Kumar,et al.  Revised Algorithm for Estimating Light Extinction from IMPROVE Particle Speciation Data , 2007, Journal of the Air & Waste Management Association.

[27]  J. Kinsey,et al.  Inverting cascade impactor data for size-resolved characterization of fine particulate source emissions , 2004 .

[28]  William L. Chameides,et al.  Aerosol radiative, physical, and chemical properties in Beijing during June 1999 , 2001 .

[29]  A. Wexler,et al.  Thermodynamic Model of the System H , 2009 .

[30]  Xiao-dong Wang,et al.  The chemical composition of inorganic and carbonaceous materials in PM2.5 in Nanjing, China , 2005 .

[31]  W. Chang,et al.  A study of visibility trends in Hong Kong (1968–1982) , 1986 .

[32]  M. Jacobson,et al.  Strong radiative heating due to the mixing state of black carbon in atmospheric aerosols , 2022 .

[33]  Y. J. Kim,et al.  Summer time haze characteristics of the urban atmosphere of Gwangju and the rural atmosphere of Anmyon, Korea , 2008, Environmental monitoring and assessment.

[34]  G. Wolff,et al.  Visibility-reducing species in the denver “brown cloud”—I. Relationships between extinction and chemical composition , 1981 .

[35]  J. Seinfeld,et al.  Organics alter hygroscopic behavior of atmospheric particles , 1995 .

[36]  Annmarie Eldering,et al.  An air monitoring network using continuous particle size distribution monitors: Connecting pollutant properties to visibility via Mie scattering calculations , 1994 .

[37]  S. Friedlander,et al.  Size distributions of polycyclic aromatic hydrocarbons and elemental carbon. 2. Ambient measurements and effects of atmospheric processes. , 1994, Environmental science & technology.

[38]  J. Chow,et al.  Size-segregated fine particle measurements by chemical species and their impact on visibility impairment in Denver☆ , 1991 .

[39]  Y. H. Zhang,et al.  AEROSOL OPTICAL PROPERTIES IN A RURAL ENVIRONMENT NEAR THE MEGA-CITY GUANGZHOU, CHINA: IMPLICATIONS FOR REGIONAL AIR POLLUTION, RADIATIVE FORCING AND REMOTE SENSING , 2008 .

[40]  H. Horvath Atmospheric light absorption : a review , 1993 .

[41]  Y. Zhanga,et al.  Aerosol optical properties and related chemical apportionment at Xinken in Pearl River Delta of China , 2008 .

[42]  J. Seinfeld,et al.  Atmospheric Chemistry and Physics: From Air Pollution to Climate Change , 1997 .

[43]  J. Chow,et al.  Variability of organic and elemental carbon, water soluble organic carbon, and isotopes in Hong Kong , 2006 .

[44]  Alexis K.H. Lau,et al.  Source areas and chemical composition of fine particulate matter in the Pearl River Delta region of China , 2006 .

[45]  J. Yu,et al.  Modal Characteristics of Elemental and Organic Carbon in an Urban Location in Guangzhou, China , 2009 .

[46]  J. Chow,et al.  Spatial and seasonal variations of atmospheric organic carbon and elemental carbon in Pearl River Delta Region, China , 2004 .

[47]  B. Turpin,et al.  Mie theory evaluation of species contributions to 1990 wintertime visibility reduction in the grand canyon , 1994 .

[48]  Min Hu,et al.  Size-segregated particulate chemical composition in Xinken, Pearl River Delta, China: OC/EC and organic compounds , 2008 .

[49]  Meinrat O. Andreae,et al.  Optical properties and chemical composition of the atmospheric aerosol in urban Guangzhou, China , 2008 .

[50]  Susan M. Larson,et al.  Intercomparison of measurement methods for black carbon aerosols , 1999 .

[51]  J. Cafmeyer,et al.  Detailed mass size distributions of elements and species, and aerosol chemical mass closure during fall 1999 at Gent, Belgium , 2002 .

[52]  R. Sequeira,et al.  Visibility degradation across Hong Kong: its components and their relative contributions , 2001 .

[53]  Y. H. Zhang,et al.  Aerosol optical properties and related chemical apportionment at Xinken in Pearl River Delta of China , 2008 .

[54]  H. Horvath Size segregated light absorption coefficient of the atmospheric aerosol , 1995 .