Preprints
https://doi.org/10.5194/acpd-10-9391-2010
https://doi.org/10.5194/acpd-10-9391-2010
14 Apr 2010
 | 14 Apr 2010
Status: this preprint was under review for the journal ACP. A revision for further review has not been submitted.

Composition and sources of particulate matter in an industrialised Alpine valley

N. Perron, J. Sandradewi, M. R. Alfarra, P. Lienemann, R. Gehrig, A. Kasper-Giebl, V. A. Lanz, S. Szidat, M. Ruff, S. Fahrni, L. Wacker, U. Baltensperger, and A. S. H. Prévôt

Abstract. A three-week long field campaign was carried out under autumnal meteorological conditions at four valley floor sites in the industrialised Swiss Rhone Valley. For one week of stable meteorological conditions, particulate matter with an aerodynamic diameter below 10 μm (PM10) was analysed from daily filters using ion chromatography, X-ray fluorescence, anhydrosugars and radiocarbon analysis of the organic and elemental matter (OM and EM, respectively). Furthermore, PM1 composition along the whole campaign was monitored in Massongex (a site near industries) by a seven-wavelength aethalometer and a quadrupole aerosol mass spectrometer (Q-AMS). At all sites, PM10 secondary inorganics and non-fossil EM and OM exhibited relatively stable concentrations over the selected days. On the contrary, PM10 fossil carbonaceous fractions, mineral dust components and several trace elements showed a significant decrease on Sunday, compared to the analysed working days. Their concentrations were also highly correlated. This evidenced the role of exhaust and resuspension emissions by heavy-duty vehicle traffic to the PM10 concentrations along the valley.

In Massongex, organic matter and black carbon (BC) were the main contributors to PM1 over the campaign (accounting for 45% and 18% of PM1, respectively). An optical discrimination of BC highlighted the prevalence of fossil over wood-burning sources. Three types of PM1 organics could be identified by factor analysis: primary wood-burning organic aerosol (P-WBOA) dominated the PM1 carbonaceous fraction, followed by oxygenated organics (OOA) mostly representing secondary organics, and by traffic or possibly industry-related hydrocarbon-like organics (HOA) as the smallest carbonaceous contribution.

Furthermore, unusually high contributions of fine chloride were detected at all sites. They were attributed to ammonium chloride (NH4Cl) in Massongex and represented the only significant component exclusively attributable to industrial emissions.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
N. Perron, J. Sandradewi, M. R. Alfarra, P. Lienemann, R. Gehrig, A. Kasper-Giebl, V. A. Lanz, S. Szidat, M. Ruff, S. Fahrni, L. Wacker, U. Baltensperger, and A. S. H. Prévôt
 
Status: closed (peer review stopped)
Status: closed (peer review stopped)
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
 
Status: closed (peer review stopped)
Status: closed (peer review stopped)
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
N. Perron, J. Sandradewi, M. R. Alfarra, P. Lienemann, R. Gehrig, A. Kasper-Giebl, V. A. Lanz, S. Szidat, M. Ruff, S. Fahrni, L. Wacker, U. Baltensperger, and A. S. H. Prévôt
N. Perron, J. Sandradewi, M. R. Alfarra, P. Lienemann, R. Gehrig, A. Kasper-Giebl, V. A. Lanz, S. Szidat, M. Ruff, S. Fahrni, L. Wacker, U. Baltensperger, and A. S. H. Prévôt

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