Journal of Geophysical Research Atmospheres · 2009 · 204 citations · 62 references
Natural SciencesChemistryEarth SciencesAtmospheric ChemistryAtmospheric ScienceElemental AnalysisAerosol ChemistryAerosol PhysicsAerosol ScienceIndustrial EmissionsParticulate MatterSecondary Organic AerosolsAerosol CharacterizationAerosol Chemical CompositionAerosol EmissionsAerosol Particle Size DistributionAerosol PropertiesAirborne ParticlesIndustrial Air EmissionsSoot Particle Size Distribution
Airborne aerosol collections were performed in urban areas of Beijing that were affected by regional brown haze episodes over northern China from 31 May to 12 June 2007. Morphologies, elemental compositions, and mixing states of 810 individual aerosol particles of different sizes were obtained by transmission electron microscopy coupled with energy‐dispersive X‐ray spectrometry. The phases of some particles were verified using selected‐area electron diffraction. Aerosol particle types less than 10 μ m in diameter include mineral, complex secondary (Ca‐S, K‐, and S‐rich), organic, soot, fly ash, and metal (Fe‐rich and Zn‐bearing). Most soot, fly ash, and organic particles are less than 2 μ m in diameter. Approximately 84% of the analyzed mineral particles have diameters between 2 and 10 μ m, while 81% of the analyzed complex secondary and metal particles are much smaller, from 0.1 to 2 μ m. Trajectory analysis with fire maps show that southerly air masses arriving at Beijing have been transported through many agricultural biomass burning sites and heavy industrial areas. Spherical fly ash and Fe‐rich particles were from industrial emissions, and abundant K‐rich and organic particles likely originated from field burning of crop residues. Abundant Zn‐bearing particles are associated with industrial activities and local waste incinerators. On the basis of the detailed analysis of 443 analyzed aerosol particles, about 70% of these particles are internally mixed with two or more aerosol components from different sources. Most mineral particles are covered with visible coatings that contain N, O, Ca (or Mg), minor S, and Cl. K‐ and S‐rich particles tend to be coagulated with fly ash, soot, metal, and fine‐grained mineral particles. Organic materials internally mixed with K‐ and S‐rich particles can be their inclusions and coatings.
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Air pollution in mega cities in China
Chak K. Chan, Xiaohong Yao · Atmospheric Environment · 2007 · 2.6K citations
Size Matters More Than Chemistry for Cloud-Nucleating Ability of Aerosol Particles
Ulrike Dusek, G. P. Frank, L. Hildebrandt et al. · Science · 2006 · 1.3K citations