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European Geosciences Union, Atmospheric Chemistry and Physics, 2(12), p. 693-707, 2012

DOI: 10.5194/acp-12-693-2012

European Geosciences Union, Atmospheric Chemistry and Physics Discussions, 7(11), p. 20973-21011

DOI: 10.5194/acpd-11-20973-2011

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Morphology, composition and mixing state of individual carbonaceous aerosol in urban Shanghai

Journal article published in 2011 by H. B. Fu, M. Zhang, W. J. Li ORCID, J. M. Chen ORCID, L. Wang, X. Quan, W. Wang
This paper is made freely available by the publisher.
This paper is made freely available by the publisher.

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Data provided by SHERPA/RoMEO

Abstract

834 individual aerosol particles were collected during Octoberober and Novemberember 2010 in urban Shanghai, China. Morphologies, compositions and mixing states of carbonaceous aerosols were investigated by transmission electron microscopy (TEM) coupled with energy-dispersive X-ray (EDX). Structures of some particles were verified using selected-area electron diffraction (SAED). Among the aerosol particles observed, carbonaceous aerosols were categorized into five types: polymeric organic compound (POC), soot, tar ball, char, and biogenic particle. Based on the detailed TEM-EDX analysis, most of particles were coated with secondary organic aerosols (SOA), which commonly formed through condensation or heterogeneous reactions of precursor gases on pre-existing particles. The internally particles of sulphates, organics and soot were encountered frequently. Such internally mixed particles may be preferentially formed during a stagnated air mass which often occurred during serious pollution events, such as a haze episode on 13 Novemberember. Although relative number counts varied with different species, sulphates (38 %-71 %) and soot (11 %-22 %) constituted the most dominant species observed in the samples. With an exception of the sample collected during a dust storm on 12 Novemberember, soil-derived particles (68 %) were relatively more frequently observed. Of particular interest was the biogenic particles encountered almost as frequently as soot on the sample collected on 13 November (18 % vs. 22 %). The result from air mass back-trajectory analysis indicated that these particles were marine-originated, most likely from the Yellow Sea.