Atmospheric Chemistry and Physics, vol. 11, issue 22 (2011) pp. 11777-11791
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, de-spite their environmental (as well as economic and political) importance, the way these properties are affected by atmo-spheric 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 wood stove were investigated on a single-particle basis. The emitted exhaust, including the particulate and the gas phase, was processed in a smog chamber with artificial solar radiation. Single particle speci-mens of both unprocessed and aged soot were characterized using near edge X-ray absorption fine structure spectroscopy (NEXAFS) and scanning electron microscopy. Comparison of NEXAFS spectra from the unprocessed particles and those resulting from exhaust photooxidation in the chamber re-vealed changes in the carbon functional group content. For the wood stove emissions, these changes were minor, related to the relatively mild oxidation conditions. For the EURO 2 transporter emissions, the most apparent change was that of carboxylic carbon from oxidized organic compounds con-densing on the primary soot particles. For the EURO 3 car emissions oxidation of primary soot particles upon pho-tochemical aging has likely contributed as well. Overall, Correspondence to: M. Ammann (email@example.com) the changes in the NEXAFS fingerprints were in qualitative agreement with data from an aerosol mass spectrometer. Fur-thermore, by taking full advantage of our in situ microreactor concept, we show that the soot particles from all three com-bustion sources changed their ability to take up water under humid conditions upon photochemical aging of the exhaust. Due to the selectivity and sensitivity of the NEXAFS tech-nique for the water mass, also small amounts of water taken up into the internal voids of agglomerated particles could be detected. Because such small amounts of water uptake do not lead to measurable changes in particle diameter, it may remain beyond the limits of volume growth measurements, especially for larger agglomerated particles.
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