Characterization of water-soluble species of PM10 and PM2.5 aerosols in urban area in Nanjing, China

The characterization for water-soluble species of PM10 (particle matter with aerodynamical diameter <10 μm) and PM2.5 (particle matter with aerodynamical diameter <2.5 μm) in five sites of Nanjing, China was carried out during February–May 2001.The pH and conductivity K of water-soluble matters of PM10 and PM2.5 were determined, and the water-soluble fraction of the sample was followed to identify the total carbon (TC), total organic carbon (TOC), inorganic carbon (IC), elements, NO3−, SO42− and NH3-N.The experimental results show that water-soluble matters of PM10 and PM2.5 in Nanjing are acidic, and the pH of PM2.5 is lower than PM10. Conductivity of water-soluble species of PM10 and PM2.5 aerosols varied over a wide range from 1087 to 225 μs/cm. Conductivity between PM10 and PM2.5 has a linear correlationship, and the equation is Y=0.8459X+44.74, r2=0.9376 (Y: conductivity of PM2.5, X: conductivity of PM10). TOC make up the majority of TC and accounts for 3.17–14.13% of PM10 and/or PM2.5 loadings, while IC only accounts for 0.12–0.47% of PM10 and/or PM2.5 mass. Al, As, Ba, Ca, Cr, Cu, Fe, K, Li, Mg, Mn, Na, Ni, Pb, Ti, V and Zn, 17 elements were detected in water-soluble matters of PM10 and/or PM2.5. Ca, K and Na are the most abundant chemical components, which account for more than 95% of total water-soluble elements (TWSE). Of all the five sites, TWSE accounts for 1.80–6.13% of the particle mass and 61.28–72.73% of TWSE of PM10 is enriched in fine particles (<2.5 μm in diameter). Nitrate (NO3−), sulfate (SO42−), ammonia and ammonium (NH3-N) were determined. The highest level of nitrate was 15.49 μg/m3 for PM10 and 12.66 μg/m3 for PM2.5 at site FZ. As was the case for nitrate, the highest level of sulfate was also presented at the same site, which was 28.22 μg/m3 for PM10 and 21.48 μg/m3 for PM2.5. However, a higher level of ammonia and ammonium was presented at site ZS, which was 36.05 μg/m3 for PM10 and 22.06 μg/m3 for PM2.5.

[1]  G. Likens,et al.  Acid Precipitation in the Northeastern United States: pH and Acidity , 1976, Science.

[2]  D. Davis,et al.  Aqueous-phase source of formic acid in clouds , 1983, Nature.

[3]  John H. Seinfeld,et al.  Secondary Organic Aerosol from the Photooxidation of Aromatic Hydrocarbons: Molecular Composition , 1997 .

[4]  V. Smirnov,et al.  Variability in aerosol and air ion composition in the Arctic spring atmosphere , 1998 .

[5]  K. Prather,et al.  Real-Time Measurement of Correlated Size and Composition Profiles of Individual Atmospheric Aerosol Particles , 1996 .

[6]  M. Zheng,et al.  Characterization of the solvent extractable organic compounds in PM2.5 aerosols in Hong Kong , 2000 .

[7]  Harvi Velásquez,et al.  Inorganic water soluble ions in atmospheric particles over Maracaibo Lake Basin in the western region of Venezuela , 1998 .

[8]  A. Limbeck,et al.  Organic acids in continental background aerosols , 1999 .

[9]  J. Heintzenberg Fine particles in the global troposphere. A review , 1989 .

[10]  R. Harriss,et al.  Formic and acetic acid over the central Amazon region, Brazil: 1. Dry season , 1988 .

[11]  A. Ali-Mohamed,et al.  Estimation of atmospheric inorganic water-soluble aerosols in the western region of Bahrain by ion chromatography , 2000 .

[12]  W. R. Cofer,et al.  Atmospheric geochemistry of formic and acetic acids at a mid-latitude temperate site , 1988 .

[13]  R. Mosello,et al.  XRF determination of trace elements in aerosol insoluble matter in North Italian precipitation samples , 1996 .

[14]  Shao-Meng Li,et al.  Atmospheric measurements of pyruvic and formic acid , 1987 .

[15]  G. Likens,et al.  Acid precipitation in the northeastern United States , 1974 .

[16]  M. Scholes,et al.  Semivolatile behavior of dicarboxylic acids and other polar organic species at a rural background site (Nylsvley, RSA) , 2001 .

[17]  G. Villasenor,et al.  Scanning electron microscope and statistical analysis of suspended heavy metal particles in San Luis Potosi, Mexico , 2000 .

[18]  Risto Hillamo,et al.  LOW-MOLECULAR-WEIGHT DICARBOXYLIC ACIDS IN AN URBAN AND RURAL ATMOSPHERE , 2000 .

[19]  J. Penner,et al.  Large contribution of organic aerosols to cloud-condensation-nuclei concentrations , 1993, Nature.

[20]  J. W. Winchester,et al.  Geochemistry of organic and inorganic ions of late winter arctic aerosols , 1989 .

[21]  S. Friedlander,et al.  A Comparative Study of Chemical Databases for Fine Particle Chinese Aerosols , 2000 .

[22]  D. Murphy,et al.  Chemical composition of single aerosol particles at Idaho Hill: Positive ion measurements , 1997 .

[23]  Paulo Artaxo,et al.  Chemical composition of aerosol particles from direct emissions of vegetation fires in the Amazon Basin: water-soluble species and trace elements , 2000 .

[24]  H. Hansson,et al.  Organic atmospheric aerosols: Review and state of the science , 2000 .

[25]  S. Kadowaki Characterization of carbonaceous aerosols in the Nagoya urban area. 1. Elemental and organic carbon concentrations and the origin of organic aerosols , 1990 .

[26]  S. Koch,et al.  Formation of new particles in the gas phase ozonolysis of monoterpenes , 2000 .

[27]  K. Kawamura,et al.  Concentrations of monocar☐ylic and dicar☐ylic acids and aldehydes in southern California wet precipitations: Comparison of urban and nonurban samples and compositional changes during scavenging , 1996 .