2011
DOI: 10.5194/acp-11-11777-2011
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Aging induced changes on NEXAFS fingerprints in individual combustion particles

Abstract: Abstract. Soot particles can significantly influence the Earth's climate by absorbing and scattering solar radiation as well as by acting as cloud condensation nuclei. However, despite their environmental (as well as economic and political) importance, the way these properties are affected by atmospheric processing of the combustion exhaust gases is still a subject of discussion. In this work, individual soot particles emitted from two different vehicles, a EURO 2 transporter, a EURO 3 passenger car, and a woo… Show more

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Cited by 19 publications
(11 citation statements)
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“…In addition, the oxygen XANES spectra recorded using near edge X‐ray absorption fine structure (NEXAFS) O K‐edge (Figure c) reveal the fine spectroscopic signature of different oxygen corresponding to the specific functional groups of the PEG (C=O(CH=CH 2 ) at 531.1 eV and COC at 535.2 eV) before and after GraftFast . First, the spectra recorded using extreme surface probe clearly show the disappearance of the band at 531.1 eV, assigned to the carbonyl group after GraftFast.…”
Section: Resultsmentioning
confidence: 97%
“…In addition, the oxygen XANES spectra recorded using near edge X‐ray absorption fine structure (NEXAFS) O K‐edge (Figure c) reveal the fine spectroscopic signature of different oxygen corresponding to the specific functional groups of the PEG (C=O(CH=CH 2 ) at 531.1 eV and COC at 535.2 eV) before and after GraftFast . First, the spectra recorded using extreme surface probe clearly show the disappearance of the band at 531.1 eV, assigned to the carbonyl group after GraftFast.…”
Section: Resultsmentioning
confidence: 97%
“…The mass absorption coefficients ( μ ) for both inorganic and organic components were calculated using the same method as O'Brien et al [] using an average O/C value of 0.4 [ Setyan et al , ] and assuming that the dominant inorganic component was ammonium sulfate: μ in,320 = 11,460 cm 2 /g, μ in,278 = 15,230 cm 2 /g, μ org,320 = 22,500 cm 2 /g, μ org,278 = 1,100 cm 2 /g [ Henke et al , ]. For soot, an average O/C of 0.3 was assumed [ Hopkins et al , ; Zelenay et al , ] and μ org,320 = 29,556 cm 2 /g, μ org,278 = 3,095 cm 2 /g were used. The known density for ammonium sulfate (1.77 g/cm 3 ) was used for the inorganic.…”
Section: Methodsmentioning
confidence: 99%
“…There are several methods and instruments for studying different properties of the surface of airborne particulate matter (PM), ranging from morphology to elemental composition (Braun et al, 2007;Coury and Dillner, 2008;Faude and Goschnick, 1997;Kirchner et al, 2003;Ortner et al, 1998;Osan et al, 2006;Zelenay et al, 2011;Zhu et al, 2001). The use of X-ray Photoelectron Spectroscopy (XPS) for chemical surface analysis of airborne particles is not a routine method in environmental applications.…”
Section: Introductionmentioning
confidence: 99%