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Size, composition, and mixing state of individual aerosol particles in a South China coastal city. | LitMetric

Size, composition, and mixing state of individual aerosol particles in a South China coastal city.

J Environ Sci (China)

State Key Laboratory of Coal Resources and Safe Mining & College of Geoscience and Surveying Engineering, China University of Mining and Technology (Beijing), Beijing 100083, China.

Published: July 2010

AI Article Synopsis

  • Aerosol samples were collected in summer from Macao, revealing a diverse mixture of particles primarily made up of soot (32%), minerals (17%), secondary particles (22%), and unknown fine particles (29%).
  • The study utilized advanced microscopy techniques (SEM/EDX and TEM) to analyze 5711 aerosol particles, which were mostly sized between 0.1 and 0.4 micrometers, with distinct mineral types identified as Si-rich, Ca-rich, and Na-rich.
  • Mineral particles collected near busy streets showed traces of heavy metals, while many Na-rich particles were identified as aged sea salt influenced by reactions with acidic gases, indicating the role of local conditions like humidity and temperature in particle aging.

Article Abstract

Aerosol samples were collected in summer in Macao, a coastal city of the Pearl River Delta Region in China. Morphology, size, elemental composition, and mixing state of individual aerosol particles were determined by scanning electron microscopy coupled energy dispersive X-ray (SEM/EDX) and transmission electron microscopy (TEM). Based on the morphologies of 5711 aerosol particles, they consist of soot (32%), mineral (17%), secondary (22%), and unknown fine particles (29%). The sizes of these particles were mostly distributed between 0.1 and 0.4 microm. Compositions of 202 mineral particles were obtained by SEM/EDX. Mineral particles were mainly classified into three types: Si-rich, Ca-rich, and Na-rich. The compositions of typical mineral particles can indicate their sources in sampling location. For example, mineral particles, collected along the main street, were associated with trace amounts of heavy metals, such as Zn, Ti, Mn, Ba, Pb, and As. TEM observations indicate that most Na-rich particles were aged sea salt particles (e.g., Na2SO4 and NaNO3) which formed through heterogeneous chemical reactions between sea salt and acidic gases. Additionally, aging time of soot was short in Macao due to high humidity, high temperature, and high levels of sunlight in Macao. Most of soot and fine mineral dust particles were internally mixed with secondary particles.

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Source
http://dx.doi.org/10.1016/s1001-0742(09)60146-7DOI Listing

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