Chemical features and seasonal variation of fine aerosol water-soluble organic compounds in the Po Valley, Italy

Citation
S. Decesari et al., Chemical features and seasonal variation of fine aerosol water-soluble organic compounds in the Po Valley, Italy, ATMOS ENVIR, 35(21), 2001, pp. 3691-3699
Citations number
16
Categorie Soggetti
Environment/Ecology,"Earth Sciences
Journal title
ATMOSPHERIC ENVIRONMENT
ISSN journal
13522310 → ACNP
Volume
35
Issue
21
Year of publication
2001
Pages
3691 - 3699
Database
ISI
SICI code
1352-2310(200107)35:21<3691:CFASVO>2.0.ZU;2-L
Abstract
We present here an investigation on the annual cycle of the carbonaceous fr action of the Po Valley (Italy) fine (d < 1.5 mum) aerosol. Water-soluble o rganic compounds (WSOC) characterisation was accomplished using a simplifie d procedure, described in the paper, of a previously proposed methodology. The new simplified procedure allows the analysis of large sets of samples, which was difficult to achieve with the previous complex and labour-intensi ve method. The results of this study show that the aerosol total carbon (TC ) concentration follows the same annual trend as the aerosol inorganic ion constituents, characterised by lower concentration values during the summer and higher concentrations in winter. The total aerosol organic carbon (OC) represents from 90 to 97% of TC, the rest being accounted for by elemental carbon. Within this study, we studied in particular the aerosol WSOC, a cl ass of chemical compounds for which present knowledge is rather limited. In our samples, WSOC account for between 38% (in winter) and 50% (in summer) of OC, in terms of carbon. WSOC were fractionated into three main classes: (a) neutral/basic compounds; (b) mono- and di-carboxylic acids; (c) polyaci dic compounds. The three fractions together accounted for an average 87% of total aerosol WSOC. The acidic compounds (mono- and di-carboxylic acids polyacidic compounds) were found to be far more abundant than the neutral o nes in all seasons, with polycarboxylic acids being the most abundant class of WSOC in spring, fall, and winter, while the mono/di-acids are dominant in summer. The main structural features of aerosol WSOC, revealed by proton nuclear magnetic resonance, suggest that WSOC are composed of highly oxidi sed species with residual aromatic nuclei and aliphatic chains. In particul ar, neutral compounds are mainly polyols or polyethers, mono/di-acids are m ainly hydroxylated aliphatic acidic compounds, and polyacids are highly uns aturated compounds of predominantly aliphatic character, with a minor conte nt of hydroxy groups. (C) 2001 Elsevier Science Ltd. All rights reserved.