Gysel, M - Risultato della ricerca - CERN Document Server

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Modelling the gas–particle partitioning and water uptake of isoprene-derived secondary organic aerosol at high and low relative humidity / Amaladhasan, Dalrin Ampritta (McGill U.) ; Heyn, Claudia (PSI, Villigen) ; Hoyle, Christopher R (PSI, Villigen ; Zurich, ETH) ; Haddad, Imad El (PSI, Villigen) ; Elser, Miriam (PSI, Villigen) ; Pieber, Simone M (PSI, Villigen ; EMPA, Dubendorf) ; Slowik, Jay G (PSI, Villigen) ; Amorim, Antonio (Lisbon U.) ; Duplissy, Jonathan (Helsinki U. ; Helsinki Inst. of Phys.) ; Ehrhart, Sebastian (CERN ; Helsinki U.) et al.
Abstract. This study presents a characterization of the hygroscopic growth behaviour and effects of different inorganic seed particles on the formation of secondary organic aerosols (SOAs) from the dark ozone-initiated oxidation of isoprene at low NOx conditions [...]
2022 - 30 p. - Published in : Atmos. Chem. Phys. 22 (2022) 215-244 Fulltext: PDF;

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Aqueous phase oxidation of sulphur dioxide by ozone in cloud droplets / Hoyle, C R (PSI, Villigen ; Davos Observ.) ; Fuchs, C (PSI, Villigen) ; Järvinen, E (KIT, Karlsruhe) ; Saathoff, H (KIT, Karlsruhe) ; Dias, A (CERN) ; El Haddad, I (PSI, Villigen) ; Gysel, M (PSI, Villigen) ; Coburn, S C (Colorado U., CIRES) ; Tröstl, J (PSI, Villigen) ; Bernhammer, A -K (Innsbruck U. ; Ionicon Analytik GmbH, Innsbruck) et al.
The growth of aerosol due to the aqueous phase oxidation of sulfur dioxide by ozone was measured in laboratory-generated clouds created in the Cosmics Leaving OUtdoor Droplets (CLOUD) chamber at the European Organization for Nuclear Research (CERN). Experiments were performed at 10 and −10 °C, on acidic (sulfuric acid) and on partially to fully neutralised (ammonium sulfate) seed aerosol. [...]
2016 - 20 p. - Published in : Atmosph. Chem. Phys. 16 (2016) 1693-1712 Fulltext: PDF;

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The role of low-volatility organic compounds in initial particle growth in the atmosphere / Tröstl, Jasmin (PSI, Villigen) ; Chuang, Wayne K (Carnegie Mellon U. (main)) ; Gordon, Hamish (CERN) ; Heinritzi, Martin (Goethe U., Frankfurt (main)) ; Yan, Chao (Helsinki U.) ; Molteni, Ugo (PSI, Villigen) ; Ahlm, Lars (Stockholm U. (main)) ; Frege, Carla (PSI, Villigen) ; Bianchi, Federico (PSI, Villigen ; Helsinki U. ; ETH, Zurich (main)) ; Wagner, Robert (Helsinki U.) et al.
About half of present-day cloud condensation nuclei originate from atmospheric nucleation, frequently appearing as a burst of new particles near midday. Atmospheric observations show that the growth rate of new particles often accelerates when the diameter of the particles is between one and ten nanometres. [...]
2016 - Published in : Nature 533 (2016) 527-531 NPG Open Access article: PDF;

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Evolution of particle composition in CLOUD nucleation experiments / Keskinen, H (UEF, Kuopio) ; Virtanen, A (UEF, Kuopio) ; Joutsensaari, J (UEF, Kuopio) ; Tsagkogeorgas, G (TROPOS, Leibniz) ; Duplissy, J (Helsinki U.) ; Schobesberger, S (Helsinki U.) ; Gysel, M (PSI, Villigen) ; Riccobono, F (PSI, Villigen) ; Bianchi, F (PSI, Villigen) ; Yli-Juuti, T (Helsinki U.) et al.
Sulphuric acid, ammonia, amines, and oxidised organics play a crucial role in nanoparticle formation in the atmosphere. In this study, we investigate the composition of nucleated nanoparticles formed from these compounds in the CLOUD (Cosmics Leaving Outdoor Droplets) chamber experiments at CERN (Centre europ ́ een pour la recherche nucl ́ eaire). [...]
2013 - Published in : Atmos. Chem. Phys. 13 (2013) 5587-5600

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Relating hygroscopicity and composition of organic aerosol particulate matter / Duplissy, J (PSI, Villigen) ; Dommen, J (PSI, Villigen) ; Prevot, A S H (PSI, Villigen) ; Barmpadimos, I (PSI, Villigen) ; Jimenez, J L (Colorado U. ; Colorado U., CIRES) ; Gysel, M (PSI, Villigen) ; Worsnop, D R (Aerodyne Research, Billerica ; Helsinki U.) ; Aiken, A C (Colorado U. ; Colorado U., CIRES) ; Tritscher, T (PSI, Villigen) ; Canagaratna, M R (Aerodyne Research, Billerica) et al.
A hygroscopicity tandem differential mobility analyzer (HTDMA) was used to measure the water uptake (hygroscopicity) of secondary organic aerosol (SOA) formed during the chemical and photochemical oxidation of several organic precursors in a smog chamber. Electron ionization mass spectra of the non-refractory submicron aerosol were simultaneously determined with an aerosol mass spectrometer (AMS), and correlations between the two different signals were investigated. [...]
2011 - Published in : Atmos. Chem. Phys. 11 (2011) 1155-1165

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1	Gysel, Martin

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